1.0 Environmental Physics
The environment is structured within the relationship between:
- Atmosphere: The gaseous envelope surrounding the Earth.
- Hydrosphere: All water bodies including oceans, rivers, and groundwater.
- Lithosphere (Geosphere): The solid Earth, rocks, and soil.
- Biosphere: The zone where life exists, interacting with all other spheres.
1.1 Agriculture Physics
Agriculture physics applies physical principles to soil, plant, and atmospheric systems to optimize food production.
- Phototropism: Growth towards light.
- Photoperiodism: Response to the length of day/night cycles (flowering).
- Wind: Increases transpiration rate by removing the boundary layer of saturated air from leaves. Mechanical stress from wind also strengthens stems (thigmomorphogenesis).
- Air Temperature: Dictates the rate of biochemical reactions (enzyme activity). Every plant has a minimum, optimum, and maximum temperature for growth ($T_{min}, T_{opt}, T_{max}$).
- Rainfall: Provides water for turgidity, nutrient transport, and photosynthesis electrons.
Soil physics deals with the physical properties of soil that influence plant growth:
- Soil Texture & Structure: Determines porosity and aeration.
- Soil Water Potential: Governs how easily plants can extract water.
- Thermal Properties: Soil heat capacity controls how fast soil warms up in spring. Dark soils absorb more heat than light soils (Albedo effect).
1.2 Human Survival Physics
Humans are homeotherms, maintaining a relatively constant body temperature (~37°C) despite environmental changes. Physics governs this thermal regulation.
The Energy Balance Equation
$$ S = M – W \pm R \pm C – E $$
\(M\) = Metabolic rate (Heat production)
\(W\) = Mechanical work done by the body
\(R\) = Radiation heat exchange
\(C\) = Convection heat exchange
\(E\) = Evaporation heat loss (Sweating)
Heat Exchange Mechanisms
- Metabolism ($M$): The biochemical process of converting food into energy. Basal Metabolic Rate (BMR) is the energy required at rest.
- Radiation ($R$): Transfer of heat via electromagnetic waves. Depends on the temperature difference between skin and surroundings ($R \propto T_{skin}^4 – T_{env}^4$).
- Convection ($C$): Heat loss to air or water moving across the skin. Wind chill factor increases convection loss.
- Evaporation ($E$): The most effective cooling mechanism in hot environments. Latent heat of vaporization ($L_v$) removes heat as sweat turns to vapor.
1.3 Energy from the Environment
Renewable energy physics focuses on converting natural energy flows into useful work.
Photovoltaic (PV)
Converts photon energy ($E=hf$) into electrical current using PN-junction semiconductors. Efficiency depends on band-gap energy and temperature.
Wind Power
Power extracted is proportional to the cube of wind speed: $$ P = \frac{1}{2} \rho A v^3 $$ where $\rho$ is air density and $A$ is rotor area.
Geothermal
Utilizes radioactive decay heat from the Earth’s core. Operates via steam turbines driven by hydrothermal reservoirs.
Wave Energy
Captures kinetic and potential energy of ocean waves. Wave power density depends on wave height squared ($H^2$) and period ($T$).
1.4 Built Environment & Remote Sensing
The Built Environment
Physics applied to human-made structures. Key concepts involve heat transfer and comfort.
- Thermal Comfort: Dependent on air temperature, radiant temperature, humidity, and air velocity.
- U-Value: Measure of thermal transmittance through walls. Lower U-values mean better insulation ($Rate = U \cdot A \cdot \Delta T$).
- Natural Ventilation: Using pressure differences caused by wind (Bernoulli’s principle) and stack effect (warm air rising) to cool buildings.
Remote Sensing
The acquisition of information about an object without making physical contact, typically via satellite or aircraft.
- Active Sensors: Emit their own energy (e.g., Radar, LiDAR).
- Passive Sensors: Detect natural energy (Sunlight) reflected (e.g., Photography, Landsat).
1.6 Geophysics (Seismology)
Seismology is the study of earthquakes and the propagation of elastic waves through the Earth.
Elastic Rebound Theory
Explains earthquake generation: Tectonic forces deform rocks. When stress exceeds rock strength, rupture occurs, and rocks “rebound” to an unstrained position, releasing energy as seismic waves.
Seismic Waves Classification
| Type | Name | Nature | Characteristics |
|---|---|---|---|
| Body | P-Waves | Longitudinal | Fastest ($~8 km/s$). Pass through solids, liquids, gases. |
| Body | S-Waves | Transverse | Slower ($~4.5 km/s$). Cannot pass through liquids (Outer Core). |
| Surface | L-Waves | Complex | Slowest. Travel along surface. Cause most structural damage. |
1.7 Environmental Pollution
Transport Mechanisms
How pollutants move in the atmosphere:
- Advection: Horizontal transport of pollutants by wind.
- Diffusion: Spreading of pollutants from high to low concentration due to turbulence.
- Deposition: Removal of pollutants via rain (Wet deposition) or gravity (Dry deposition).
Optical Properties & Visibility
Pollution affects how light travels through the atmosphere, reducing visibility.
- Scattering: Particulates (aerosols) scatter light. Mie Scattering occurs when particles are similar in size to the wavelength of light (causing white smog). Rayleigh Scattering affects smaller molecules (blue sky).
- Absorption: Some pollutants (like soot or $NO_2$) absorb light, causing dark smoke or brownish haze.
Nuclear Waste
Radioactive waste management involves shielding and isolation.
- High-Level Waste (HLW): Spent fuel. Requires cooling and deep geological disposal.
- Half-life ($T_{1/2}$): The time taken for radioactivity to drop to half. Waste must be stored for multiple half-lives.
2.0 Current Electricity
2.1 Drift Velocity Theory
In a conductor, free electrons move randomly. When an electric field $E$ is applied, they acquire a slow average velocity component called Drift Velocity ($v_d$).
Derivation of \(I = nAve\)
- Consider a conductor of length \(L\) and cross-sectional area \(A\).
- Volume of the conductor \(V = A \times L\).
- If \(n\) is the number of free electrons per unit volume, total number of electrons \(N = n \times (AL)\).
- Total Charge \(Q = N \times e = nALe\).
- Time taken for charge to cross length \(L\) with velocity \(v_d\) is \(t = \frac{L}{v_d}\).
- Current \(I = \frac{Q}{t} = \frac{nALe}{L/v_d} = nAev_d\).
Drift Velocity Equation
$$ I = n A v_d e $$
\(n\) = Charge carrier density ($m^{-3}$)
\(A\) = Cross-sectional Area ($m^2$)
\(v_d\) = Drift Velocity ($m/s$)
\(e\) = Electronic charge ($1.6 \times 10^{-19} C$)
2.2 Current Density ($J$)
Current density is a vector quantity defined as the current per unit area.
$$ J = \frac{I}{A} = n v_d e $$
Vector Form (Microscopic Ohm’s Law): $$ J = \sigma E $$
Where $\sigma$ is Conductivity and $E$ is Electric Field intensity.
2.3 Resistance & Resistivity
Resistance ($R$) opposes current flow. It depends on geometry and material properties.
$$ R = \rho \frac{L}{A} $$
- $\rho$ (Rho): Resistivity ($\Omega m$). Intrinsic property of material.
- $L$: Length of conductor.
- $A$: Cross-sectional area.
- Conductivity ($\sigma$): Reciprocal of resistivity ($\sigma = 1/\rho$).
2.4 Temperature Coefficient of Resistance
For metallic conductors, resistance increases with temperature.
Where:
$R_\theta$ = Resistance at temp $\theta$
$R_0$ = Resistance at $0^\circ C$
$\alpha$ = Temperature coefficient of resistance ($K^{-1}$ or $^\circ C^{-1}$)
Lab: Drift Velocity Calculator
Calculate the drift velocity of electrons in a wire using the formula \(v_d = I / (nAe)\).
ACSEE Practice Problems
Question: Calculate the drift velocity in a silver wire of area \(4.5 \times 10^{-6} m^2\) carrying 5 A. ($n = 5.8 \times 10^{28} m^{-3}$).
\(v_d = \frac{I}{nAe} = \frac{5}{(5.8 \times 10^{28})(4.5 \times 10^{-6})(1.6 \times 10^{-19})}\)
\(v_d = \frac{5}{41.76 \times 10^{3}} \approx 1.2 \times 10^{-4} m/s\)
Question: A wire of length 2.0 m and diameter 0.4 mm has a resistance of 2.5 $\Omega$. Calculate its resistivity.
1. Area $A = \pi r^2 = \pi (0.2 \times 10^{-3})^2 = 1.257 \times 10^{-7} m^2$
2. Formula $R = \rho L / A \Rightarrow \rho = RA/L$
3. $\rho = (2.5 \times 1.257 \times 10^{-7}) / 2.0$
4. $\rho = 1.57 \times 10^{-7} \Omega m$
Question: A coil has a resistance of 10 $\Omega$ at $0^\circ C$ and 15 $\Omega$ at $100^\circ C$. Find $\alpha$.
$R_{100} = R_0(1 + \alpha \Delta T)$
$15 = 10(1 + \alpha \cdot 100)$
$1.5 = 1 + 100\alpha \Rightarrow 0.5 = 100\alpha$
$\alpha = 0.005 K^{-1}$
Physics Form 6 - Complete Interactive Notes
These notes reorganize the uploaded Form 6 Physics PDF into clear chapters, large visible formula boxes, a question bank, examples and a complete page-by-page source transcript. Use search to find any concept, formula or page.
Included source: 147 readable pages from the uploaded PDF, with no scanned-page embeds.
Quick Formula Reference
Revision| Concept | Formula | Where used |
|---|---|---|
| Solar constant | S = Energy / (area × time) | Environmental energy |
| Resultant magnetic field | B = √(BH² + BV²) | Earth magnetism |
| Bohr quantization | mvr = nh / 2π | Atomic physics |
| Bohr energy | En = -13.6Z²/n² eV | Hydrogen-like atoms |
| Rydberg formula | 1/λ = RH(1/n₁² - 1/n₂²) | Spectra |
| Photon energy | E = hf | Quantum theory |
| Photoelectric equation | eV₀ = hf - φ | Photoelectric effect |
| Long wire field | B = μ₀I / 2πr | Magnetism |
| Circular coil field | B = μ₀NI / 2r | Magnetism |
| Solenoid field | B = μ₀nI | Magnetism |
| Magnetic force on charge | F = Bqv sinθ | Magnetic fields |
| Force on conductor | F = BIL sinθ | Magnetic fields |
| Magnetic flux | Φ = BA cosθ | Electromagnetism |
| Mutual induction | E = -M dI/dt | Induction |
| AC angular frequency | ω = 2πf | A.C. theory |
| RMS voltage/current | Vrms = V₀/√2, Irms = I₀/√2 | A.C. theory |
| Inductive reactance | XL = 2πfL | A.C. inductance |
| Capacitive reactance | XC = 1 / 2πfC | A.C. capacitance |
| Series RLC impedance | Z = √[R² + (XL - XC)²] | A.C. circuits |
| Resonant frequency | f₀ = 1 / 2π√LC | Resonance |
| Ohm law | V = IR | Circuits |
| Resistivity | R = ρL/A | Electricity |
Clear Formula Learning Centre
EquationsThe most important formulas are shown again in large equation boxes so students can read, copy, revise and apply them easily.
How to read any formula
Write what each symbol means and its SI unit before substituting values.
Convert cm to m, minutes to seconds, and eV to joules where needed.
Put values into the equation line by line to avoid mistakes.
Include the correct unit and a short interpretation of the answer.
Environmental Physics: Meaning and Scope
EnvironmentEnvironmental physics studies physical processes in the atmosphere, biosphere, hydrosphere and geosphere, and how living organisms respond to environmental conditions.
Source coverage: Pages 1-2
The environment is the medium in which an entity exists. For example, the environment of a cloud may be the region of the atmosphere in which it forms.
Main themes covered
- Human environment and survival physics
- Built environment
- Renewable energy
- Remote sensing
- Weather, climate and climate change
- Environmental health
Form 6 coverage in this file
The uploaded notes cover agriculture physics, energy from the environment, geophysics and earthquakes, environmental pollution, atomic physics, photoelectric effect, magnetism, A.C. theory, semiconductor physics and circuit problem-solving.
Agriculture Physics and Plant Environment
AgricultureAgriculture physics relates physical environmental factors to plant growth, including radiation, wind, rainfall, humidity, air temperature, soil water movement and soil heat transfer.
Source coverage: Pages 2-10
Solar radiation and plant growth
- Positive effect: optimum heat favours photosynthesis, allowing plants to manufacture food and grow.
- Negative effect: excessive ultraviolet radiation bleaches chlorophyll, reduces photosynthesis and may kill plants.
- Negative effect: excessive radiation increases transpiration, causing wilting and drying.
Aerial environment
Aerial environment means atmospheric conditions affecting plants: air temperature, wind, humidity and rainfall.
Soil water movement
Water speed in soil depends mainly on the amount of water present and soil porosity. Sandy soil has larger pores and allows fast downward movement; clay soil has very fine pores and holds water strongly; loamy soil allows moderate movement.
| Soil state | Fastest | Moderate | Slowest / highest retention |
|---|---|---|---|
| Unsaturated soil | Sandy | Loamy | Clay |
| Saturated soil | Clay may show high flow under saturation | Loamy | Sand can drain quickly but retain little water |
Soil heat transfer
Heat in soil is transferred mainly by conduction. Since soil is a poor conductor, much heat from the atmosphere remains near the surface. Optimum soil temperature favours growth; high temperature may rot plant roots.
Improving plant environment
- Shading: obstructs excessive solar radiation, reduces transpiration and preserves soil moisture.
- Mulching: covers soil with dry leaves, grasses or paper to conserve water, reduce erosion, reduce compaction, maintain soil temperature, improve nutrition, reduce salt/pesticide contamination, improve establishment and reduce weeds and diseases.
- Windbreaks: rows of trees or strong plants used to slow wind, reduce soil erosion and protect crops.
Solar Constant and Photovoltaic Energy
Renewable EnergySolar energy is a key environmental energy source. The notes emphasize solar constant, photovoltaic cells, solar panels, arrays, and factors affecting efficiency.
Source coverage: Pages 10-12
The solar radiation received at a point on Earth depends on geographical location, season, time of day, altitude, atmosphere, clouds and pollution.
Photovoltaic devices
It is made from semiconductor layers. One layer is P-type and the other is N-type. Light photons absorbed by the semiconductor create electron-hole pairs; electrons flow through an external circuit and produce current.
Uses of solar cells
- Power electronics in satellites and space vehicles.
- Power supply in calculators.
- Generate electricity for homes, offices and industries.
Solar module and array
A solar module is a sealed weatherproof package containing interconnected solar cells. Modules can be connected in series to increase voltage, in parallel to increase current, and in series-parallel combinations to achieve desired power.
Photovoltaic efficiency depends on
- Intensity of light falling on the panel.
- Orientation of the panel; maximum power is produced when sunlight falls perpendicular to the panel.
- Surface area of the panel.
Advantages of photovoltaic systems
- Produce electricity without noise or air pollution.
- Require no fuel purchase.
- Useful for small-scale electricity generation in remote areas.
- Can shave peak loads because peak production often coincides with peak demand.
Geophysics, Earthquakes and Seismic Waves
GeophysicsGeophysics applies physics to Earth structure and processes. The notes focus on earthquakes, seismic waves, wave paths, measurement and prediction.
Source coverage: Pages 13-34
Types of seismic waves
| Wave type | Nature | Main property |
|---|---|---|
| P waves | Primary/body waves | Compressional; travel through solids and liquids; fastest. |
| S waves | Secondary/body waves | Shear waves; travel through solids only; absent in liquid outer core. |
| Love waves | Surface waves | Transverse horizontal motion, restricted to Earth crust, dispersive, destructive. |
| Rayleigh waves | Surface waves | Vertically polarized rolling motion, slowest, dispersive, amplitude decreases with depth. |
Propagation of seismic waves
Seismic waves may undergo reflection, refraction, dispersion, diffraction and attenuation. Reflection occurs at boundaries between rocks of different density. Refraction changes wave velocity and direction when waves enter media of different density.
Seismic wave paths and Earth interior
- P and S waves travel through the Earth in curved paths due to refraction as density and wave speed change with depth.
- Surface waves travel through the crust only.
- The shadow zone between about 105° and 140° has no direct P or S waves.
- S waves do not travel through the liquid outer core, proving the existence of a liquid layer beneath the mantle.
- Change in P-wave velocity at the crust-mantle boundary reveals the Mohorovicic discontinuity.
- Increased P-wave velocity through the inner core suggests the inner core is solid.
Measurement of earthquakes
Size of earthquake
- Mercalli scale: measures intensity according to effects on people and structures; ranges from 1 (no damage) to 12 (total destruction).
- Richter scale: measures magnitude in terms of energy released, determined from seismogram amplitude; logarithmic scale.
- Isoseismal lines: lines joining points of equal earthquake intensity.
Earthquake warning signs
- Change in P-wave velocity.
- Decrease in electrical resistivity of rocks.
- Increase in radon gas emission in soil and water samples.
- Increase in foreshock frequency.
- Local variation in magnetic field.
- Abnormal animal behaviour.
- Rise or fall of well water level.
- Increase in local temperature before an earthquake.
Precautions and hazards
Precautions include constructing buildings with anti-earthquake design, using shock absorbers in foundations, reducing crust stress by pumping water out of the crust, and moving away from tall buildings during earthquakes. Hazards include landslides, avalanches, tsunamis, collapsing buildings, fire outbreaks and backward rivers.
Atmosphere, Ionosphere and Earth Magnetic Field
Earth & SpaceExam examples in the document revise atmospheric layers, ionosphere layers, ozone layer, magnetic field components, and long-distance radio communication.
Source coverage: Pages 26-34
Atmosphere and ionosphere
- The lowest layer of the atmosphere is the troposphere.
- The lowest layer of the ionosphere is the D layer.
- The D layer reflects radio waves and helps communication.
- During daytime, all ionosphere layers D, E, F1 and F2 exist.
- At night, ionospheric conditions improve reception of high-frequency signals because absorption in lower layers is reduced.
Ozone layer
It absorbs ultraviolet radiation from the sun, protecting plants and shielding human beings from skin cancer and eye cataracts.
Earth magnetic field
- Vertical component points vertically downward.
- Horizontal component comprises easterly and northerly components.
- Angle of inclination/dip is the angle made by the magnetic field with the horizontal.
- Angle of declination is the angle between magnetic north and geographic north.
Environmental Pollution
PollutionEnvironmental pollution is the addition of unwanted materials or pollutants into the environment, disturbing natural balance and affecting health, visibility and material properties.
Source coverage: Pages 35-36 and related pages
Types of environmental pollution
- Air pollution / atmospheric pollution
- Water pollution / hydrosphere pollution
- Land or soil pollution
- Noise pollution
- Thermal pollution
Air pollution
Air pollution is environmental pollution caused by gaseous materials and dust particles released into the atmosphere. Pollutants include particulate matter, lead, ground-level ozone, heavy metals, sulphur dioxide, benzene, carbon monoxide and nitrogen dioxide.
Human causes of air pollution
- Clearing and burning vegetation releases carbon dioxide and dust.
- Burning fuels releases greenhouse gases and smoke.
- Construction activities add dust.
- Automobile exhaust releases pollutant gases.
- Industrial smoke pollutes air.
- Agricultural pesticides and insecticides pollute air.
Atomic Physics: Rutherford and Bohr Models
Modern PhysicsThis section explains atomic models, Rutherford model limitations, Bohr postulates, stationary orbits, orbital radius, electron velocity, frequency, energy and emitted wavelengths.
Source coverage: Pages 37-51
Rutherford model of atom
Rutherford proposed that the atom has a tiny central nucleus containing positive charge and most of the mass. Electrons revolve around the nucleus, and most of the atom is empty space.
Energy of electron in Rutherford picture
Limitations of Rutherford model
- According to electromagnetic theory, an accelerating electron should radiate energy continuously.
- The electron would lose energy, spiral into the nucleus and make the atom unstable.
- It predicts continuous spectra, while atoms emit line spectra.
Bohr model postulates
- Electrons revolve in certain stable circular orbits without radiating energy.
- Allowed orbits have quantized angular momentum.
- Radiation is emitted or absorbed only when an electron jumps between energy levels.
Bohr orbit radius, speed and frequency
For hydrogen, the first three orbital radii are approximately 0.53 Å, 2.12 Å and 4.77 Å. Electrons move more slowly in higher orbits.
Total energy and spectral lines
Energy is negative because the electron is bound to the nucleus. As n increases, energy becomes less negative; at n = infinity the electron is free.
Photoelectric Effect and Quantum Theory of Light
Modern PhysicsThe photoelectric effect demonstrates that light energy is delivered in packets called photons. The section covers stopping potential, threshold frequency and the failure of wave theory.
Source coverage: Pages 52-58
The stopping potential measures the maximum kinetic energy of the fastest photoelectrons.
Effects of intensity and frequency
- Increasing light intensity increases the saturation current because more photoelectrons are emitted.
- Changing frequency changes the stopping potential and maximum kinetic energy.
- Stopping potential is directly proportional to frequency of incident radiation above threshold.
Threshold frequency
If the frequency is below threshold, no electrons are emitted regardless of intensity.
Laws of photoelectric emission
- For a given metal, a minimum frequency must be reached before emission occurs.
- For frequency above threshold, photoelectric current is proportional to radiation intensity.
- Maximum kinetic energy is independent of intensity but depends on frequency.
- Photoelectric emission is instantaneous, with negligible time delay.
Failure of wave theory
Wave theory predicts that energy depends on intensity and is spread continuously, so stronger light should eventually emit electrons at any frequency. Experiments show emission depends on frequency and occurs instantly above threshold, proving wave theory is insufficient.
Einstein quantum theory
Magnetic Fields and Force on Moving Charges
MagnetismThis section uses magnetic field formulae for long wires, circular coils, solenoids, toroids, current-carrying conductors and moving charges.
Source coverage: Pages 59-84
Magnetic field produced by currents
Force in magnetic field
If velocity/current is perpendicular to the magnetic field, force is maximum. If parallel, force is zero. Direction is found using Fleming left-hand rule.
Examples contained in the source
- Magnetic field at the centre of a hydrogen electron orbit and helium nucleus orbit.
- Force on an electron moving near a long straight wire.
- Magnetic field inside and outside toroids and solenoids.
- Field at the centre and on the axis of a circular coil.
- Force on a vertical current-carrying wire in a horizontal magnetic field.
Magnetic flux
Flux is maximum when the surface is perpendicular to the magnetic field lines and zero when field lines are parallel to the surface.
Magnetic Materials, Moving Coil Meters and Hall Effect
ElectromagnetismThe document covers magnetic susceptibility, classification of magnetic materials, moving coil meters, Biot-Savart law, Hall effect, mutual inductance and induction.
Source coverage: Pages 72-94
Magnetic materials
Magnetic susceptibility describes how easily a material becomes magnetized. Materials are classified as diamagnetic, paramagnetic and ferromagnetic according to their magnetic response.
Moving coil meters
Moving coil meters use the turning effect of a current-carrying coil in a magnetic field. The coil experiences a torque proportional to current, and a spring provides controlling torque.
Biot-Savart law
The notes use Biot-Savart relationships to obtain magnetic flux density due to current-carrying conductors, especially circular coils and long straight wires.
Hall effect
Hall effect is used to identify charge carriers and measure magnetic flux density.
Mutual inductance and mutual induction
The quantity of electricity induced and e.m.f. depend on the rate of change of magnetic flux linkage.
A.C. Theory and A.C. Circuits
ElectricityA large part of the PDF covers alternating voltage/current, RMS values, AC resistance, inductance, capacitance, R-L-C circuits, resonance, power and AC advantages/disadvantages.
Source coverage: Pages 95-139
Alternating voltage and current
Alternating current changes magnitude and direction periodically. Its instantaneous values are commonly represented by sine functions.
RMS values
Pure resistance
In a purely resistive AC circuit, voltage and current are in phase and power is consumed as heat.
Pure inductance
In an inductive AC circuit, current lags voltage by 90°. The opposition offered by an inductor is inductive reactance.
Pure capacitance
In a capacitive AC circuit, current leads voltage by 90°. The opposition offered by a capacitor is capacitive reactance.
R-L-C series circuit
Resonance
At resonance, inductive and capacitive reactances are equal.
Parallel resonance effects
- Power factor becomes unity.
- Impedance becomes maximum.
- Circuit current becomes minimum.
- Resonance curve relates circuit current and supply frequency.
Advantages of AC over DC
- AC voltage can be stepped up or down efficiently by transformers.
- AC motors are cheaper and simpler.
- AC can be converted to DC using rectifiers.
- AC can be controlled by choke coils with little power loss.
- AC switchgear is cheaper.
Disadvantages of AC
- For the same voltage, AC is more dangerous.
- AC shock may be attractive while DC shock is repulsive.
- AC cannot be stored directly like DC.
Semiconductors, P-N Junctions and Circuit Analysis
ElectronicsThe final pages revise semiconductor types, diode biasing, rectification and circuit calculations using Kirchhoff laws, metre bridge and potential divider ideas.
Source coverage: Pages 140-147
P-type semiconductor
P-N junction diode
The narrow region at the junction containing fixed charges is the depletion layer. A barrier potential difference opposes further diffusion of charges across the junction.
Forward and reverse bias
- Forward bias: P side connected to positive terminal and N side to negative terminal. Electrons and holes cross the junction and current flows easily.
- Reverse bias: P side connected to negative terminal and N side to positive terminal. Only a very small current flows.
Rectification
A P-N junction can act as a rectifier by allowing current mainly in one direction. This is important for converting AC to pulsating DC.
Circuit analysis tools in examples
- Kirchhoff voltage law for loops.
- Kirchhoff current law at junctions.
- Metre bridge balance condition.
- Resistivity calculation using resistance and wire geometry.
- Potential divider output voltage calculations.
Extra Worked Examples for Revision
PracticeThese examples were added to make the notes more useful for learning and examination preparation.
Solar constant calculation example
If 2700 J of solar energy falls on 2 m² in 1 s at the edge of the atmosphere, solar constant S = Energy/(area × time) = 2700/(2×1) = 1350 W m⁻² = 1.35 kW m⁻².
Soil water movement example
Sandy soil drains faster because large pores reduce capillary retention; clay holds more water because very fine pores increase capillary attraction.
Seismic wave evidence example
S-waves do not pass through liquid, so the absence of S-waves beyond the outer core supports the conclusion that the outer core is liquid.
Earth magnetic field example
If horizontal component BH = 40 μT and vertical component BV = 30 μT, resultant B = √(40²+30²) = 50 μT, and tan θ = 30/40, so θ ≈ 36.9°.
Bohr energy level example
For hydrogen at n = 2, E₂ = -13.6/2² = -3.4 eV.
Photon energy example
For light of frequency 5 × 10¹⁴ Hz, E = hf = (6.63 × 10⁻³⁴)(5 × 10¹⁴) = 3.315 × 10⁻¹⁹ J.
Stopping potential example
If K.Emax = 3.2 × 10⁻¹⁹ J, then V₀ = K.Emax/e = 3.2 × 10⁻¹⁹ / 1.6 × 10⁻¹⁹ = 2.0 V.
Force on a conductor example
A 0.5 m wire carrying 4 A perpendicular to a 0.2 T field experiences F = BIL = 0.2×4×0.5 = 0.4 N.
Solenoid field example
For a solenoid with n = 1000 turns m⁻¹ and I = 2 A, B = μ₀nI = 4π×10⁻⁷×1000×2 ≈ 2.51×10⁻³ T.
AC impedance example
For R = 30 Ω, XL = 50 Ω and XC = 10 Ω, Z = √(30² + (50−10)²) = 50 Ω.
Resonance example
If L = 0.1 H and C = 10 μF, f₀ = 1/(2π√LC) ≈ 159 Hz.
Potential divider example
If Vin = 12 V, R1 = 2 kΩ and Rload = 4 kΩ, Vout = 12×4/(2+4) = 8 V.
Clear Question & Example Bank
Exam practiceThis bank makes questions and examples easier to find. The items below were extracted from the uploaded source transcript and displayed separately from the long page transcript.
Page 26 Question / Example 1
Example 11: Necta 1994 P; (a) (i) Name the lowest layer of the atmosphere and the lowest layer of the ionosphere. (ii) State the importance of each of these layers. (b) What is the ozone layer? Answers (a)(i) The lowest layer of the atmosphere is troposphere and the lowest layer of the ionosphere is called the D — layer. (ii) The t troposphere supports life The D layer is important for communication purposes as it reflects radio waves (b) The ozone layer is within the stratosphere. In the ozone layer molecular oxygen (O2) is
Page 26 Question / Example 2
Example 12: Necta 1994 P, (a) Illustrate the component of the earth’s magnetic field at a given point P in the earth’s atmosphere by a suitable diagram. (b) Using a tangent galvanometer, explain how you could determine the earth's magnetic field. Answers
Page 27 Question / Example 3
Example 13: Necta 1995 P; (a) (i) which region of the solid earth includes the e earth’s centre? (ii) On which region of the solid earth do the continent rests directly? {iii Which region of the ionosphere has the highest electron density? (b) Briefly explain how earthquake can be detected Answers (a) (i) inner core (ii) crust (iii) F—region (b) Detection of earthquake is done by recording or measuring the seismic waves generated by the earthquakes. These waves are recorded by instrument called seismograph.
Page 27 Question / Example 4
Example 14: Necta 1995 P, (a) Draw a well labeled diagram which shows the interior structure of the earth. Indicate also which part of the interior are in solid form and which are in liquid form. (b) Name and distinguish the type of waves that are produced by an earthquake. (c) Briefly describe the three ways in which signal form ground based transmitter can reach the receiver. Answers (a) There are four types of seismic waves: Body waves — divided into P and S- waves Surface waves — divided into love and Rayleigh
Page 27 Question / Example 5
Example 15: Necta 1998 P; (a) State any three magnetic components of the earth’s magnetic field
Page 28 Question / Example 6
Example 16: Necta 1998 P; B (a) What is the origin of the earth’s magnetic field? (b) The following diagram shows the main layers forming the interior of the earth name the layers indicated by letters A to G.
Page 29 Question / Example 7
Example 17: Necta 1998 ?2B (a) Explain the following terms; Earthquake, Earthquake focus, Epicenter and body waves. (b) List down three (3) sources of earthquakes, (c) (i) Define ionosphere (ii) Mention the ionosphere layers that exist during the day time
Page 30 Question / Example 8
Example 18: nectar 2000 P; (a) With reference to an earthquake on a certain point of the carth explain the terms ‘focus’ and ‘Epicenter’ (b) What is importance of the following layer of the atmosphere? (i) The lowest layer (ii) The ionosphere (c) (i) Describe two ways by which seismic waves may be produced. {ii) Describe briefly the meaning and application of “seismic prospecting”. Answers (a) Refer notes
Page 31 Question / Example 9
Example 19: Necta 2001 P; (a) (i) Define the terms “angle of declination” as used in the specification of the earth’s magnetic field at a point (ii) The horizontal component of the earth’s magnetic field at a location was found to be 26.0 ME while the angle of inclination was 59°- Find the magnitude of the field and the vertical component of the field at the location (b) (i) Define an earthquake (ii) Distinguish between P and S waves. What factors influence their velocities? Answers (a) (i) Refer notes
Page 31 Question / Example 10
Example 20: Necta 2002 P1 (a) (i) What is the importance of ionosphere to mankind? (ii) Explain why transmission of radio waves is better at night than at day time. (b) (i) What is an earthquake?
Page 32 Question / Example 11
Example 21: Necta 2003 P, (a) Explain the following: {i) Earthquake (ii) Earthquake focus (iii) The epicenter. (b) List down three sources of earthquake (c) (i) Define the ionosphere (ii) State the ionosphere layer that exists during day time. (iii) Give the reason for better waves reception for light frequencies signal at night than during the day time
Page 32 Question / Example 12
Example 22: Necta 2004 P; (a) (i) Explain the terms epicenter and focus as applied to earthquake. (ii) State any four (4) indications that may predict the occurrence of an earthquake. (iii) State and explain two variations of the earth magnetic field. (iv) State one necessary precaution to be taken to people living in a region with a high risk of occurrence of earthquakes. (b) Explain the following (i) Solar wind (ii) Magnetopause (iii) lonosphere.
Page 32 Question / Example 13
Example 23: Necta 2005 P; {a) Define the following terms (i) Epicentral distance (ii) Body wave (iii) Seismograph (b) (i) explain the meaning of reflection seismology state its application (ii) Show how the magnetic field within the atmosphere is generated?
Page 33 Question / Example 14
Example 31: Necta 2012 P, (a) (i) What do you understand by the word environmental physics?
Page 34 Question / Example 15
Example 32: Necta 2013 P; (a) (i) The main interior of the earth core is believed to be in molten form. What seismic evidence supports this belief? (ii) Explain why the small ozone layer on the top of the stratosphere is crucial for human survival (b) Electrical properties of the atmosphere are significantly exhibited in the ionosphere. (i) What is the layer composed of and what you think is the origin of such constituents (ii) Mentioned two uses of the ionosphere (c) Briefly explain why long distance radio broadcasts make use of short wave Answers
Page 35 Question / Example 16
Example 33: Necta 2013 P, (a) Briefly explain on the following types of environmental pollution: (i) Thermal pollution (ii) Water pollution (b) Describe the soil temperature with regard to agriculture, physics which causes lower crop growth at a particular area Answers (b) High soil temperature causes the crop roots to rot, this leads to insufficient water supply to plant leaves and hence lower the growth of crop. Lower soil temperature inactivates soil organisms. Decomposition of organic matter is
Page 35 Question / Example 17
TRY YOURSELF (a) (i) What are auroras? (ii) Define the homosphere (b) (i) What are the factors which contribute toward volcanic eruptions? (ii) What are the effects of volcanic eruptions? (iii) What are lahars? Lahars are rapidly flowing mixtures of rock debris and water that originate on the slopes of a volcano. They are also referred to as volcanic mudflows or debris flow. Volcanic eruptions may directly trigger one of more lahars by quickly melting snow and on a volcano or eject water from a crater lake. The form in a variety of at always including through intense rainfall
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Example 1
Page 145 Question / Example 19
Qn. Determine the magnitude of 4s @7d J
Page 146 Question / Example 20
Qn A wire of length 1.1 meter and Radius 7*10~°m is connected across the right gap of the metre bridge when a resistance of 45 Q is introduced in the left gap from a resistance box connected across it- The balance point is obtained 0,6m from left side. Calculate the specific resistance (resistivity) of the material of the wire Solution The value of resistance Formula of resistivity Soe = BA 06 04 Pry 45x04 _ «— 30x 3.14 x(7.0 x 10~*) x6 = 300 od 7
Page 146 Question / Example 21
Qn. A 2K2 and 3kQ resistor are connected in series combination is connected across a 100v supply of negligible internal resistance as shown in the figure below:
Complete Source Transcript
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ENVIROMENTAL PHYSICS (i) Agriculture physics - Influence of solar radiation on plant growth. - Influence of wind, humidity, rainfall and air temperature on plant growth. - Soil environmental component which influence plant growth. (ii) Energy from the environment Photovoltaic energy Wind energy Geothermal energy Wave energy (iii) Geophysics (Earth quakes) Elastic rebound theory Types of seismic waves Propagation of seismic waves Seismology (iv) — Environmental pollution Types of pollutant in the atmosphere Transport mechanisms of atmospheric pollutant Nuclear waste and their disposal Effects of pollution on visibility and optical properties of materials. INTRODUCTION
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Environmental physics is an interdisciplinary subject that integrates the physics processes in the following disciplines: the atmosphere, the biosphere, the hydrosphere, and the geosphere. Environmental physics can be defined as the response of living organisms to their environment within the framework of the physics of environmental processes and issues. It is structures within the relationship between the atmosphere, the oceans (hydrosphere), land (lithosphere), soils and vegetation (biosphere). It embraces the following themes: (i) Human environment and survival physics, (ii) Built environment (ili) Renewable energy (iv) Remote sensing (v) Weather, climate and climate change, and (vi) Environmental health. The environment may be defined as the medium in which any entity finds itself, For example, for a cloud its environment may be the region of the atmosphere in which it is formed. AGRICULTURE PHYSICS Agriculture physics is concerned with physics environment in relation to plant growth. (a) Influence of Radiation Environment on Plant Growth Radiation environments. Refer to radiations present in the atmosphere, commonly coming from the sun. Components of solar radiation The main components of solar radiation are:
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(i) Visible light (ii) Infrared radiation, and (iii) Ultraviolet radiation. HEATING EFFECT OF SOLAR RADIATION ON PLANTS Positive effect An optimum amount of heat on plant favours the process of photosynthesis. This enables a plant to make its own food and hence provide its growth. Negative effects (i) Excessive solar radiation (ultraviolet light) on plants leads to bleaching of green pigment (chlorophyll), This lowers the amount of food produced by photosynthesis to plant and hence a plant may dic. (ii) Excessive solar radiation on plants leads to excessive water loss in the form of water vapour commonly on plant leaves (transpiration). Hence wilting (drying) of plants may occur. (b) Influence of Aerial Environment on Plant Growth Aerial environments refer to the atmospheric condition resulting from a series of processes occurring in the atmosphere. These include air temperature, wind, humidity and rainfall. WIND EFFECT ON PLANT GROWTH Positive effects (a) Wind acts as pollinating agent for some plants and hence favours plant productivity. (b) Wind also favours evaporation of water from plant leaves and thus maintains water balance for proper plant growth. Negative effects
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(a) Excessive wind on environments leads to plant breaking or cutting of tree branches. This may lead to the death of plant. (b) As the wind speed increases further, cell and Cuticular damage occurs, followed by death of plant tissue, and a gnarled appearance becomes more apparent. (c) At low wind speeds, the effect seems to be an increase in transpiration, which results in water stress. This stress causes the plant to adapt by decreasing leaf area and internodes length, while increasing root growth and stem diameter. (d) Strong wind may also cause shade off flowers; this lowers plant productivity. Effect of Rainfall on Plant Growth Positive effect An optimum amount of rainfall on plants favours its growth. Water is a raw material for the process of photosynthesis from which plants obtain their food and hence their growth. Negative effect Excessive rainfall leads to water logging in soil which in turn leads to root spoil and hence the death of plant. Effect of Humidity on Plant Growth Positive effect Favourable humidity on plants help plants to conserve water for various activities and in seeds helps the development of new leaves. Negative effect Low humidity results into a greater rate of transpiration and hence may result into plant drying. Effect of Air Temperature of Plant Growth Positive effect
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le action.
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Capillary action refers to the attraction of water into soil pores — an attraction which makes water move in soil. Capillary action involves two types of attraction — adhesion and cohesion. Adhesion is the attraction of water to solid surfaces. Cohesion is the attraction of water to itself. Speed of water in a particular soil type depends on: (i) How much water is in the soil, and (ii) Porosity of the soil. The movement of water in the solid is mainly due to gravity. The porosity gives a measure of how much water the soil can hold and the rate at which water flows through the soil. Large pore spaces give a faster rate and vice versa. An experiment to study water movement in soil An experiment to demonstrate the rate of flow of water in the soil is done using a glass tube and sand type filled in it. Water is poured into the tube and the time taken for water to reach the bottom of the tube in notes. Unsaturated soil Saturated soil Soil type Water speed Soil type Water speed Le ce Koc
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ail GB Tm r |
S 60 Vv i
- |
48 he
24 br
130 an. Fil {{(N AE
45 30 15 O 15 30 45 75 60 45 30 15 O I5 30 45 60 75
Distance (cm from center of furrow)
Sandy loam Clay loam
(a) )
i. Sand soil have large pore spaces thus allows water to travel downwards through it at a
fastest rate.
ii. Clay soil can hold water as has very fine pore spaces.
iii. Loamy soil allows water movement at a medium rate.
Heat transfer in the soil
Within the soil heat is transferred by a conduction process. Since soil is poor conductor of
heat most of the heat from the atmosphere appears at the surface of the earth.
An optimum soil temperature favours plants growth but a high temperature can lead to the
rotting of plant roots.
(d) Techniques for the Improvement of the Plant Environment
Plant environment can be improved by using wind breaks, shading and mulching.
ShadingPage 8: full text transcript
Shading is the process of obstructing plants from excessive solar radiation. Positive Impacts of Shading 1. Prevents excessive loss of water by plants through transpiration. This enhances plant productivity. 2. Preserve moisture in the soil and hence water supply to plant. Mulching Mulching is the process of covering the soil by dry leaves, grasses and or papers. Benefits (Advantages) of Mulching 1. Improve soil moisture. Bare soil is exposed to heat, wind and compaction loses water through evaporation and is less able to absorb irrigation or rainfall. Using mulches, the soil has greater water retention, reduced evaporation, and reduced weeds. Mulch can also protect trees and shrubs from drought stress and cold injury 2. Reduce soil erosion and compaction, Mulches protect soils from wind water, traffic induced erosion and compaction that directly contribute to root stress and poor plant health. 3. Maintenance of optimal soil temperatures. Mulches have shown to lower soil temperatures in summer months. Extreme temperatures can kill fine plant roots which can cause stress and root rot. Mulches protect soils from extreme temperatures, cither cold or hot. 4. Increase soil nutrition. Mulches with relatively high nitrogen content often result in higher yields, but low nitrogen mulches, such as straw, sawdust and bark, can also increase soil fertility and plant nutrition. 5. Reduction of salt and pesticide contamination. In arid landscapes, evaporating water leaves behind salt crusts. Because mulches reduce evaporation, water is left in the soil and salts are diluted. Organic mulches can actively accelerate soil desalinization and help degrade pesticides and other contaminants. 6. Improve plant establishment and growth. Mulches are used to enhance the establishment of many woody and herbaceous species. Mulches improve seed germination and seed survival, enhance root establishment, transplant survival, and increase plant performance.
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7. Reduction of disease. Mulches will reduce the splashing of rain or irrigation water, which can carry spores of disease organisms to stems and leaves of plants. Populations of beneficial microbes that reduce soil pathogens can be increased with mulches. Mulches can combat disease organisms directly as well. 8. Reduction of Weeds. Using mulches for weed control is highly effective. Mulches can reduce seed germination of many weed species and reduce light, which stresses existing weeds. 9. Reduce pesticide use. Mulches reduce weeds, plant stress, and susceptibility to pests and pathogens which translates to reduced use of herbicides, insecticides, and fungicides. Mulch Problems (disadvantages of mulching) 1. i, Acidification. Some types of mulches can increase soil acidity. 2. ii, Disease. Many mulches made from diseased plant materials can be composted or treated at temperatures that kill pathogens that can be transmitted to healthy plants, 3. iii.Pests. Many organic mulches, especially wood — based mulches, have the reputation as being “pest magnets”. 4. iv, Weed contamination. Improperly treated crop residues and composts as well as bark mulches are often carriers of weed seed. Mulch must be deep enough to suppress weeds and promote healthy soils and plants. Weed control and enhanced plant performance are directly linked to mulch depth. v. Wind Breaks Wind breaks are long rooted strong plants (trees) that are used to obstruct the path of wind or to slow down the wind. Windbreaks provide many benefits to soil, water, plants, animals and man. They are an important part of the modern day agricultural landscape. Windbreaks come in many different sizes and shapes to serve many different conservation purposes. In agriculture, wind breaks protect small growing plants from strong blowing wind Advantages of Windbreaks to Plant Environment 1. i. Control soil erosion. Windbreaks prevent wind erosion from causing loss of soil productivity. This eliminates plant roots stresses and thus favours plant growth condition.
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Solar constant Solar constant is defined as the solar energy falling per second on a square meter placed normal to the sun’s rays at the edge of the Earth’s atmosphere, when the Earth is at mean distance from the sun. Its value is about 1.35 kWm? The amount of solar radiation received at any point on the earth’s surface depends on: (i) The geographical location, (ii) The season, (summer or winter) (iii) The time of the day, the lower the sun is in the sky the greater is the atmospheric absorption. (iv) The altitude; the greater the height above sea level the less is the absorption by the atmosphere, clouds and pollution PHOTOVOLTAIC DEVICES (SOLAR CELLS) A solar cell (PV, cells) is a PN junction device which converts solar energy directly into electrical energy. How it Works PV cells are made of at least two layers of semiconductor material. One layer has a positive charge (p — type material), the other negative (n-type material). When light enters the cell, some of the photons from the light are absorbed by the semiconductor atoms, freeing electrons from the cell’s negative layer to flow through an external circuit and back into the positive layer. This flow of electrons produces electric current.
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Vv, Negative rr | a <i teen e . . é 5 LE Poutve on! — Le Uses of the solar cell 1. (i)Are used to power electronics in satellite and space vehicles. 2. (ii)Are used as power supply to some calculators. 3. iii)Are used to generate electricity for home, office and industrial uses. Series arrangement of solar cells Solar panel (module) is a sealed, weatherproof package containing a number of interconnected solar cells so as to increase utility of a solar cell. When two modules are wired together in series, their voltage is doubled while the current stays constant. When two modules are wired in parallel, their current is doubled while the voltage stays constant. To achieve the desired voltage and current, modules are wired in series and parallel into what is called a PV array. The flexibility of the modular PV system allows designers to create solar power systems that can meet a wide variety of electrical needs, no matter how large or small.
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Cell Module Efficiency of a photovoltaic system The output power of a solar cell depends on: (i) The amount of light energy from the sun falling on a solar panel (the intensity of light). (ii) The orientation of the solar panel. More electricity is produced if light falls perpendicular to panels. (iii) The surface area of the panel. Large area collects more solar energy and hence greater electricity. The best designed solar cell can generate 240 Wm” in bright sun light at an efficiency of about 24%. Advantages of photovoltaic systems 1. Solar cells can produce electricity without noise or air pollution. 2. A photovoltaic system requires no fuels to purchase. 3. Panels of photovoltaic cells are used for small — scale electricity generation in remote areas where there is sufficient sun. 4. Net metering: This has the potential to help shave peak loads, which generally coincide
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In liquid = V, =0,siece q=0 Note: Since the density and states of the earth layers varies, the speed of the seismic waves also vary from layer to layer, the solid part showing greater speed and the liquid ones lower speed. Primary wave and secondary wave (8 fe emoromstons A WAdode DMD debe AM de DAL ddd 7 HA et (LLL PH Ee wave direction S wave “ OZ Ta Fae em te TT eT (4 I agi deemiatT ddam tT mm a Lewavetengtn Variation of speed of body waves with depth
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zr 7 3 3 - 3f ip 3 i i 8 i H s +H i z $ i soe eeol a 6 8 |3 eee Eo ne 2 wt tt v i . s 5 3 8 — #8 — Ss [ays a3 38 55 gs S 8 FF ee ee es EE SURFACE WAVES/LONG WAVES Surfaces waves are produced when earthquake energy reaches the Earth’s surface. These are the slowest moving waves, but are the most destructive for structures on earth There are two types of L- Waves: (i) Love long waves (ii) Rayleigh long waves i. Love Waves Love waves are Transverse horizontal motion, perpendicular to the direction of propagation and generally parallel to the Earth’s surface. They are formed by the interaction of S waves with Earth’s surface and shallow structure and are dispersive waves. The speed at which a dispersive wave travels depends on the wave’s period. Characteristics of Love Waves
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1. i. Love waves are transverse and restricted to horizontal movement (horizontally polarized). 2. ii. The amplitude of ground vibration caused by a Love wave decrease with depth. The rate of amplitude decrease with depth also depends on the period/frequency. 3. iii. Loves wave are dispersive, i.e. wave velocity is dependent on frequency; low frequency — higher velocity. 4. iv. Speed of love waves is between 2.0 and 4.4 km/s 5. v. Love waves travels within the earth’s crust only. - x Direc Perspective view Ssess see) g CSR eee Sieitsccesecsesccensers, ssesssessessceseigs | eStuceeuaseag” suageeuaesensseaceteceeag oo oiiit!| sense /Suesmessesseeseececseesesssee)i iii! POSE meeststiss Rectangle to view oy deformation as wave propagates through material LOVE WAVE Rayleigh Waves Rayleigh waves are vertically polarized long waves. The slowest of all the seismic wave types and in some ways the most complicated. Characteristics of Rayleigh Waves 1. Rayleigh waves are transverse and restricted to vertical movements (vertically polarized).
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2. The amplitude of Rayleigh wave decreases with depth. The rate of amplitude decrease with depth depends on the period/frequency 3. Rayleigh wave are dispersive, i.e. wave velocity dependent on frequency; low frequency —high velocity 4. Speed of love waves is between 1.0 and 4.2 km/s slowest of all waves. 5. Travels within the earth’s crust only. 6. Depth of penetration of the Rayleigh waves depend frequency, with lower frequencies, penetrating greater depth. PROPAGATION OF SEISMIC WAVES Like all other types of waves, seismic waves may undergo, (i) Reflection, (ii) Refraction, (iii) Dispersion, (iv) Diffraction, (v) Attenuation. Seismic reflection: Seismic waves bounce (reflect) rock boundaries of different rock type (density).
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Seismic refraction: Waves change velocity and direct (refract) when they enter a medium of different density it the one they just passed through. Seismic Dispersion: surface waves are dispersive which means that different periods travel at different velocities. The effects of dispersion become more noticeable with increasing distance because the long travel distance spreads the energy out (it disperses to energy). SEISMIC WAVE PATHS By comparing the data recorded by many stations all over the world the nature, speed and the paths of the seismic waves can be determined. This information can be used to tell us about the earth’s interior such as density sand state in each layer. L— Waves travel within the Earth’s crust only P and S waves travel through the carth in a curve path. The waves are refracted because their speeds a constantly changing with depth due to continue increase in density. Waves are also strongly refracted the Mantle — Core boundary. Surface waves travels through the Farth crust only Shadow zone is the region on the Earth’s surface where no S or P waves are present. This lies between 105° and 140°. Only surface waves may be detected in this region. Shadow zone occurs because: (i) P~ Waves are strongly refracted at the liquid outer core. (ii) S— Waves can’t travel through the liquid outer core. Seismic waves can also be used to locate the discontinuities in the earth’s crust. A change in density or crack would affect the propagation of the waves. This alteration in the wave’s path or speed would indicate the discontinuity.
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a P wave ‘ ts re i ™, Earthquake’ \ \ \ t The fact that S waves do not travel through the core provides evidence for the existence of a liquid layer beneath the rocky mantle The change in the velocity of P waves at crust - Mantle boundary reveals the presence of Mohorovicic discontinuity P waves passing through the inner core show increased velocity suggesting that the inner core is solid. Both P and S — Waves slow down when they reach the asthenosphere. Because of this scientists know that the asthenosphere is partially liquid MEASUREMENTS OF EARTHQUAKES
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i. Seismology is the scientific study of earthquakes (seismic waves) and artificially produced vibrations in the earth.Seismograph is a sensitive instrument that is used to record earthquakes and seismic waves (i.e. ground movements). ji, Seismogram is the record of ground movement drawn by a seismograph. The arrival of seismic waves at a station surface waves minute mark P s _ Seismograph consists of a heavy weight suspended from a frame fixed into the ground. When the earth vibrates the frame moves but the heavy weight remains stationary due to great inertia. A pen attached to weight plots the earth’s movements on a chart recorder to produce a seismogram. To obtain a complete record of the earthquake measurements must be taken in all three planes (x, y and 2).
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SIZE OF AN EARTHQUAKE The size of an earthquake can be measured in terms of its intensity (Mercalli/Wood Neumann scale) or its magnitude (Richter scale). Mercalli Intensity Scale The Mercalli scale measures the intensity of how people and structures are affected by the seismic event. In essence, it measures damage. It is much more subjective and uses numbers ranging from 1 (no damage) to 12 (total destruction). Degree Explana | Detecte 1 seismog Felt by frighten heavy moved, fallen general small Total large waves moving the objects thrown ISOSEISMAL LINES Intensity distribution maps can be drawn up showing the intensities of an earthquake over
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a region. The earthquake is most intense at the epicenter and decreases with distance.
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Isoseismal lines are line joining points of equal intensity. Richter magnitude scale The magnitude of an earthquake is measured in terms of energy released by an earthquake. This is determined from the amplitude of the seismic wave recorded on a seismogram 100 km from the epicenter. The magnitude is equal to the logarithm of the amplitude. Therefore each successive number represents a tenfold (x10) increase in the ground motion. The Richter scale starts at 0 but has no upper limit. -However 8 represent an earthquake that causes total destruction within the region. Magnitude Amount of explosives (TNT) needed to release the equivalent energy, in tons a Intensity of an earthquake is a measure of its strength based on the changes it causes to the landscape. EARTHQUAKE PREDICTIONS (WARNINGS) Forecasting (predicting) earthquakes is very difficult, although there are a number of warning signs which occur before an earthquake happens. (i) Change in the velocity of p — waves (ii) Electrical resistivity of the rocks decreases. (iii) An increase in radon, emission (radon is an inert gas, radon is found to increase in soil and water samples). (iv) Increase in fore shock (small tumors that occur just before an earthquake). (v) Local variations in the magnetic field (vi) Animals begin to behave strange
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(vii) Water levels rise or fall in wells few days before earthquake.
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(viii) Increase in temperature of the area few months before the occurrence of an earthquake PRECAUTIONS Some of the world’s populations are living in regions where there is a high risk of an earthquake. Most of these regions lie along fault lines. However a few precautions can be taken to reduce the damage caused. (a) Build structures that can withstand the forces of an earthquake. One method is to include shock absorbers into the buildings foundations. (b) Scientific rescarch has shown that pumping water out of the carth reduces the stress in the crust hence preventing an earthquake. However this technique is very expensive. () Stay away from tall buildings or structures during an carthquake if you are outside on occurrence, (d) Ifyou are inside a house, stay in a safe place where things will not fall on you EARTHQUAKE HAZARDS Earthquake give rises to a number of hazards which pose a great risk to human life, animals, property and the environment at large. The following are some hazards: 1. Landslides and avalanches: The shaking caused by an earthquake can cause unstable hillsides, mountain slops’ and cliffs to move downwards creating landslides. Earthquakes can also trigger avalanches on snow slopes 2. Tsunamis: If an earthquake occurs under the sea or ocean, the shock waves disturb the water. The ocean floor can rise or fall causing the water to rise and fall too. This movement creates huge water waves called tsunamis that travel across the ocean. 3. Collapsing building: Buildings or structures may collapse during a_ strong earthquake, The collapse of the building may kill people. 4. Fire outbreak: Earthquakes can cause gas or oil pipes to break and or the collapse of electricity lines. This may set up fire.
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5. Backward rivers: Tilting ground due to earthquakes can make rivers change their course.
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3, = [By By = (GA0°Y —Qu07P B, =458X10°T (ii) Angle of inclination is given by 458:40° o-mei)-— fSemaes)-* Example 11: Necta 1994 P; (a) (i) Name the lowest layer of the atmosphere and the lowest layer of the ionosphere. (ii) State the importance of each of these layers. (b) What is the ozone layer? Answers (a)(i) The lowest layer of the atmosphere is troposphere and the lowest layer of the ionosphere is called the D — layer. (ii) The t troposphere supports life The D layer is important for communication purposes as it reflects radio waves (b) The ozone layer is within the stratosphere. In the ozone layer molecular oxygen (O2) is dissociated into atomic oxygen (O) which is then reformed into ozone (Os) The ozone so formed absorbs ultra violet radiation thus protecting plants and shielding people from skin cancer and eye cataracts. Example 12: Necta 1994 P, (a) Illustrate the component of the earth’s magnetic field at a given point P in the earth’s atmosphere by a suitable diagram. (b) Using a tangent galvanometer, explain how you could determine the earth's magnetic field. Answers
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Example 13: Necta 1995 P;
(a) (i) which region of the solid earth includes the e earth’s centre?
(ii) On which region of the solid earth do the continent rests directly?
{iii Which region of the ionosphere has the highest electron density?
(b) Briefly explain how earthquake can be detected
Answers
(a) (i) inner core (ii) crust (iii) F—region
(b) Detection of earthquake is done by recording or measuring the seismic waves generated
by the earthquakes. These waves are recorded by instrument called seismograph.
Example 14: Necta 1995 P,
(a) Draw a well labeled diagram which shows the interior structure of the earth. Indicate also
which part of the interior are in solid form and which are in liquid form.
(b) Name and distinguish the type of waves that are produced by an earthquake.
(c) Briefly describe the three ways in which signal form ground based transmitter can reach
the receiver.
Answers
(a) There are four types of seismic waves:
Body waves — divided into P and S- waves
Surface waves — divided into love and Rayleigh
(b) A telecommunication problem.
Ground wave, sky wave and space waves
Example 15: Necta 1998 P;
(a) State any three magnetic components of the earth’s magnetic fieldPage 28: full text transcript
(b) The horizontal and vertical components of the earth’s magnetic field at a certain location are; 2.73 x 10% and 2.1 x 10°T respectively. Determine the earth’s magnetic field at the location and its angle of inclination @ Solution (a) Components of the earth magnetic field are: Vertical component (which point vertically downward) Horizontal component which comprise If: Eastly component (towards geographic north pole) Northly component (towards magnetic north pole) (b) Be =3-44x10" TandO =37.66° Example 16: Necta 1998 P; B (a) What is the origin of the earth’s magnetic field? (b) The following diagram shows the main layers forming the interior of the earth name the layers indicated by letters A to G.
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| = a c Answers (a) Refer notes (b) A = Farth’s surface, B = Crust, C = Moho discontinuity, D = Gutenberg discontinuity, F = outer core, F = Mantle and G = inner core. Example 17: Necta 1998 ?2B (a) Explain the following terms; Earthquake, Earthquake focus, Epicenter and body waves. (b) List down three (3) sources of earthquakes, (c) (i) Define ionosphere (ii) Mention the ionosphere layers that exist during the day time
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(iii) Give the reason for better reception of radio waves for high frequency signal of
night than during day time.
(a) Explain briefly three different types of radio waves traveling from a transmitting station to
a receiving antenna.
Answers
(a) Refer notes
(b) Refer notes
(c) (i) During the day time all the layers D,E,F,, and F2 — layers exists.
(ii) Refer Necta 1992 (b)
(d) Ground (surface wave)
Space wave
Sky waves) (refer telecommunication notes)
Example 18: nectar 2000 P;
(a) With reference to an earthquake on a certain point of the carth explain the terms ‘focus’
and ‘Epicenter’
(b) What is importance of the following layer of the atmosphere?
(i) The lowest layer
(ii) The ionosphere
(c) (i) Describe two ways by which seismic waves may be produced.
{ii) Describe briefly the meaning and application of “seismic prospecting”.
Answers
(a) Refer notes
{b) (i) Importance of troposphere is supports life on earthPage 31: full text transcript
(ii) lonosphere enhances communication over long distances. (c) (i) Describe any two causes of earth quake (ii) Seismic prospecting is an artificial production of seismic waves purposely for searching underground fuels and oils or gases Example 19: Necta 2001 P; (a) (i) Define the terms “angle of declination” as used in the specification of the earth’s magnetic field at a point (ii) The horizontal component of the earth’s magnetic field at a location was found to be 26.0 ME while the angle of inclination was 59°- Find the magnitude of the field and the vertical component of the field at the location (b) (i) Define an earthquake (ii) Distinguish between P and S waves. What factors influence their velocities? Answers (a) (i) Refer notes (ii) Be =50-48 pTBy = 4527 pT (b) The velocities of P and S waves are influenced by; Density, ? of the media Shear modulus, 7 of the media, and Bulk modulus, B of the media. Example 20: Necta 2002 P1 (a) (i) What is the importance of ionosphere to mankind? (ii) Explain why transmission of radio waves is better at night than at day time. (b) (i) What is an earthquake?
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(ii) Explain briefly any four (4) causes of earthquake
Example 21: Necta 2003 P,
(a) Explain the following:
{i) Earthquake (ii) Earthquake focus (iii) The epicenter.
(b) List down three sources of earthquake
(c) (i) Define the ionosphere
(ii) State the ionosphere layer that exists during day time.
(iii) Give the reason for better waves reception for light frequencies signal at night than
during the day time
Example 22: Necta 2004 P;
(a) (i) Explain the terms epicenter and focus as applied to earthquake.
(ii) State any four (4) indications that may predict the occurrence of an earthquake.
(iii) State and explain two variations of the earth magnetic field.
(iv) State one necessary precaution to be taken to people living in a region with a high risk
of occurrence of earthquakes.
(b) Explain the following
(i) Solar wind (ii) Magnetopause (iii) lonosphere.
Example 23: Necta 2005 P;
{a) Define the following terms
(i) Epicentral distance (ii) Body wave (iii) Seismograph
(b) (i) explain the meaning of reflection seismology state its application
(ii) Show how the magnetic field within the atmosphere is generated?Page 33: full text transcript
Seismic station Focus (close to the earth surface) Distance travelled by the waves (distance between focus and seismic station) is d= RY2 =64x10° x./2 =9.05x10°m Time taken by P —- waves to arrive at the station is a 9.05 x 10° 8 = So = gage = 1131.25sec = 189min Time taken by the waves to arrive at the station is <= 10° _ 1508.33 = 25.11 = =a = jsec = 25.1min The time interval between the arrival of the two waves is t = t)—t; = 25.1 = 18.9 = 6.2 minutes. Example 31: Necta 2012 P, (a) (i) What do you understand by the word environmental physics?
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(ii) Briefly explain three effects of seismic waves.
(b) (i) Mention three types of environmental pollution
(ii) Explain on the following climatic factors which influence plant growth: Temperature,
Relative humidity and wind.
Example 32: Necta 2013 P;
(a) (i) The main interior of the earth core is believed to be in molten form. What seismic
evidence supports this belief?
(ii) Explain why the small ozone layer on the top of the stratosphere is crucial for human
survival
(b) Electrical properties of the atmosphere are significantly exhibited in the ionosphere.
(i) What is the layer composed of and what you think is the origin of such constituents
(ii) Mentioned two uses of the ionosphere
(c) Briefly explain why long distance radio broadcasts make use of short wave
Answers
(a) (i) When P and S seismic waves are sent from one side of earth to the other, only P waves
can be detected on the other side. The fact that S waves do not travel through the core
provides evidence for the existence of a liquid core.
(ii) Ozone absorbs harmful radiation from the sun. The Ozone projects plant and shield
people from skin cancer and eye cataracts.
(b) (i) The layer is composed of free electrons and positive ions. The ionosphere is created by
atoms absorbing UV radiation, gamma and x-rays.
{ii) Uses of the ionosphere
lonosphere supports radio communication over long distances
Particles in the ionosphere absorbs U.V radiation gamma and X-rays, thus protecting
people from harmful effects of these radiations
(c) Refer telecommunication notes.Page 35: full text transcript
Example 33: Necta 2013 P, (a) Briefly explain on the following types of environmental pollution: (i) Thermal pollution (ii) Water pollution (b) Describe the soil temperature with regard to agriculture, physics which causes lower crop growth at a particular area Answers (b) High soil temperature causes the crop roots to rot, this leads to insufficient water supply to plant leaves and hence lower the growth of crop. Lower soil temperature inactivates soil organisms. Decomposition of organic matter is lowered and hence the supply of nutrients to crop which in turn lead to lower crop growth. TRY YOURSELF (a) (i) What are auroras? (ii) Define the homosphere (b) (i) What are the factors which contribute toward volcanic eruptions? (ii) What are the effects of volcanic eruptions? (iii) What are lahars? Lahars are rapidly flowing mixtures of rock debris and water that originate on the slopes of a volcano. They are also referred to as volcanic mudflows or debris flow. Volcanic eruptions may directly trigger one of more lahars by quickly melting snow and on a volcano or eject water from a crater lake. The form in a variety of at always including through intense rainfall ‘on loose volcano rock deposits and as a consequence of debris of debris avalanches ENVIRONMENTAL POLLUTION Pollution is the addition of unwanted materials or pollutants into the environment.
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Pollutant is any substance that does not belong in the natural system and disrupts the natural balance. Type of Environmental pollution (a) Air pollution (atmospheric pollution) (b) Water pollution (hydrosphere pollution) (c) Land (soil) pollution (a) Noise pollution (¢) Thermal pollution ATMOSPHERIC (AIR) POLLUTION ag ________poauurigat This is a form of environmental pollution caused by the release of gaseous materials and dust particles in the atmosphere. The main pollutants found in the air we breathe include, particulate matter, lead, ground-level ozone, heavy metals, sulphur dioxide, benzene, carbon monoxide and nitrogen dioxide Causes of Air Pollution Man made causes: (i) Clearing (deforestation) and burning of vegetation. This releases carbon dioxide in the atmosphere and dust particles which may be carried by wind on bare land (ii) Burning of fuels: This releases green house gases in the atmosphere. Fuels are burnt in cars, power stations and industries. (iii) Construction activities, like road, building, ete construction, can add dust particles in the atmosphere. (iv) Automobile exhausts. Car, trains, etc burns fuels as they move his releases pollutant gases in the atmosphere. (v) Smokes from industries also pollute the atmosphere. (vi) Agriculture activities. The use of pesticide/insecticides pollutes the air.
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Spherical cloud +o of positive charge -° ae © a) + O+ (—) —) o + + © Electron ‘The number of electrons is such that their negative charge is equal to the positive charge of the atom, This atom is electrically neutral This model was called Thomson's plum pudding model because the negatively charge electrons (the plums) were embedded in a sphere of uniform positive charge (the pudding). Drawbacks of this Model 1 It could not provide stability to the atom it is because the positive and negative charges are stationary and will be drawn towards each other, thus destroying the individual negative and positive charges. 2. Itcould not explain the presence of discrete spectral lines emitted by hydrogen and other atoms, RUTHER FORD’S MODEL OF ATOM ‘The salient features of this model are (i)Every atom consist of a tiny central core, called the nucleus which contains all the atom’s positive charge and most of its mass (99.9%). (ii) The radius of the nucleus is of the orde of 10-15m and that of the atom is of the order 10-1°m. Therefore nucleus occupies only an extremely small portion of the size of atom (iii) The electrons occupy the space outside the nucleus. Since an atom is electrically neutral the positive charge on the nucleus is equal to the negative charge on electrons surrounding thenucleus. (iv) Electrons are not stationary but revolve around the nucleus in various circular orbits as do the planets around the sun. In this way Rutherford provided stability to the atom. It is because the centripetal force required by the electrons for revolution is provided by the electrostatic force of attraction between electrons and the nucleus.
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m Ze ge 4megr? e= charge on electron z=total number of protons in the nucleus m=mass of the electron =distance of electron from the nucleus v= linear velocity of the electron Force of attraction between electron and the nucleus is Zeje 4negr F. Ze? elle Frege where Ze is a nuclear charge The centripetal force required to keep the electron moving in circular path is mv? pom r Since the atom is stable Fe = Fe
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mv? __Ze? r+ 4mepr? Ze? es Kinetic energy of electron KE = 5mv? From equation (1) Ze? my? = —_ 4neqr Ze? 2K.E =—— 4negr Ze? tae m= Greer Ze? ORE = Great? Ze? ME = Seer? Potential energy of electron (Ze)(-e) PE cor —Ze? PE= Fe ‘Total energy of electron
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E=KE+PE a Ze? + —Ze? ~ Bxeor \4neor, —Ze? al Bneor The total energy of electron in the orbit is negative hence the electron is bound to the positive nucleus For hydrogen Atom For hydrogen atom z= 1. Therefore K. E and P.E OF electron in hydrogen atom are e KE = Sregr -e PE=—— Gregor The total energy of electrons hydrogen atom is E=K.E+P.E e e pe. Bregr 4megr a B= 8negr Limitations of Rutherford’s model of atom 1. According to Maxwell’s theory of electromagnetism a charge that is accelerating radiates energy as electromagnetic waves ‘The electron moving around the nucleus is under constant accelerating radiates energy as. electromagnetic waves.
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- Due to this continuous loss of energy the electrons in Rutherford’s model were bound to spiral towards the nucleus and fall into it when all of their rotational energy were radiated - Hence Rutherford’s atomic model cannot be stable while in actual practice, an atom is stable This shows that Rutherford’s model is not correct 1. During inward spiraling the electron’s angular frequency continuously increases - _ Asresult electrons will radiate electromagnetic waves of all frequency i.e. the spectrum of these waves will be continuous in nature because these are continuous loss of energy. - But this is contrary to observation experiments shows that an atom emits line spectra and each line corresponds to a particular frequency or wavelength. Rutherford’s model failed to account for the stability of the atom. It was also unable to explain the emission of line spectra. BOHR’S MODEL OF ATOM According to Bohr's atomic model, the revolving electrons in the atom do not emit radiations under all conditions. They do so under certain conditions as expalined by him in his model. BASIC POSTULATES OF BOHR’S MODEL OF ATOM 1. The electrons revolve around the nucleus of the atom in circular orbits. The centripetal force required by electrons for revolution is provided by the electrostatic force of attraction between the electrons and the nucleus. 2. Anelectron can revolve only in those circular orbits in which its angular momentum is an integral multiple of 2/2 mvr= nh “On h= Plank’s constant. Radius of orbit r From, _ ah mT On
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nh me 2umv Since n is a whole number only certain value of r is allowed. ‘Thus according to Bohr, an electron can revolve only in certain orbits of definite radii not in all these are called stable orbits (stationary orbit) According to this postulate the angular momentum of the electron does not have continuous range i.e. the angular momentum of the revolving electron is quantized. While revolving in stable or stationary orbits the electrons do not radiate energy inspite of their acceleration towards the centre of the orbit. - For this reason these permitted orbits are called stable or stationary orbits. e= charge on electron m= mass of electron r= radius of the n™ orbit vn= velocity of electron in the n™ orbit Z= number of positive charge (protons) Positive charge on nucleus Ze RADIUS OF BOHR’S STATIONARY ORBITS As the centripetal force is provided by the electrostatic force of attraction between the nucleus and electron. mv,?__1 (Zee Ta | 4%" Ta? 1 Ze? Grey ty 10) According to Bohr
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h Man = 5 @ Consider equation mu? = 2-282 in tee” Tm =——.Ze? mata = Ge 2e Take equation (ii) square it h Mata = N5— Gi) nth? mn he? = Take equation (iii) “equation (i) MVaTE nth? 4néotn MV; = 4m? Ze? qh? \n? T= — _ nme?) Z Itis clear that ’" © n2, radii of the stationary orbits are in ratio 12: 22:32“ clearly the stationary orbits are not equally spaced. For hydrogen atom For hydrogen atom z= 1, so that equation become Eqh? t= (5) in? ame’ zon? Now =me* = 0.53 x10%m
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m=m, e=electroniccharge T= (0.5310 metres Forn=1 ¥ = (053 x 10-9) x (12) 1m = 053 x 107m 4 =053A Forn=2 1» = (0.53 x 107°) x (22) rm = 212 x 107? ry =2.12A Forn=3 75 = (0.53 x 10-9) x (3?) 3 =4.77x 107m Thus the radii of the first, second and third stationary orbits of hydrogen atom are 0.53 A, 2.12 A and 4.77A respectively. 2. VELOCITY OF ELECTRON IN BOHR’S STATIONARY ORBIT From equation below, we have mvgt,= 2 te On — » = Damn, Putting the value of "® into that equation
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__nh_ nmZe? Y= Damn, “2eonth: _ Ze? n= Deonh wt Um = itis clearthat "7 in other words, electrons move at a lower speed in higher orbits and vice versa. For hydrogen atom 2-1 Then n= Jeon 3. FREQUENCY OF ELECTRON IN STATIONARY ORBIT The number of revolution completed per second by the electron in a stationary orbit around the nucleus Velocity of electron in the 8" orbit Tn =TaWn Uy = Umrah =< In = 2a, Ze? 1 In= 2eonh 2nr_ __ Ze? n= 4negnhr, For hydrogen atom
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z-1 Then, Ze? In = Sregnr, eqn, Frequency of electron in the first orbit of hydrogen atom is n=1, 1:=0.53x10™ ,, e@ h= ake egnhr,, get —# "Amey 1XhXH (1.6 x 10-19)? =9x 10° x 6 x10? fi = 9% 10" x TE 62x 10° x O53 x10 fy = 657 x 10 r.p.s Electron in first orbit of hydrogen atom will have a frequency of 6.57x 10"Srevolutions per second. 4. TOTAL ENERGY OF ELECTRON IN STATIONARY ORBIT The total energy E. of the electron in the n® orbit is the sum of kinetic and potential energy in the n® orbit. - ‘The K.E of electron in the n" orbit is K.E,= 1, mv,? xe.<Z# vn Brom The potential energy of electron in the n™ orbit is
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pe, = 2 OC) Breo tm -ze? PEn= Faon Total energy of electron in the n" orbit is E,=PE,+KE, Ze? Ze? By = —- + 4%, BME OTm g.- met (2 2 Beg2h? \n? But me* ae -10 Begepa = 217 10 n Eq = 21.7 x 1079 w 21.7 10719 Z? En =—T6x10-% “ni 13.6 E,=-—> eV n Thus as n increases i.e. electron moves to higher orbit, the total energy of the electron increases i.e. total energy becomes less negative. For hydrogen atom 2=1 -13.6 E,=—a ev
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Thus the total energy of electron in a stationary orbit is negative which means that the electron is bound to the nucleus and it is not free to leave the atom. We can find the total energy of electron in the various orbits of hydrogen atoms as under. 13.6 Ey=— = -13.6ev First orbitn=1 ‘aoe 13.6 Ey =—“Fy = —13.6eV Second orbit n=2 13.6 Ey =~ = —13.6eV third orbit n-3 The total energy of electron increases i.e. becomes less negative as the electron goes to higher orbits When nee E, =0 and the electron becomes free Ground state/ normal state This is the state of atom when the entire electrons in it occupies their lowest energy levels as required by their n and / values. The energy of an atom is least i.e. largest negative value when n=1 i.e. when electron revolves in the first orbit. The energy of hydrogen atom in the ground state is 13.6eV. Excited state This is the state of an atom when electrons in an atom occupy energy levels higher than those permitted by the values of n and / values. At room temperature most of the hydrogen atoms are in the ground state If hydrogen atom absorbs energy i.e. due to rise in temperature it may be promoted to one of the higher orbits (i.e. n=2, 3, 4.....) The atom is said to be in the excited state.
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WAVE LENGTH OF EMITTED RADIATION. When an electron jumps from a higher orbit (n2) to the lower orbit (m1) the energy difference between the two orbits is released because the energy of electron in the higher orbit is more than in the lower orbit. Consider two orbits having principle quantum numbers n2 and ni where n2>ni Then energy of electron in the two orbits is given by mZze* Ens =~ Bente Beq?n* 2h mZe* Ens = ~ Bett ht Beg nh As the electron jumps from orbit nz to n, energy is released in the form of electromagnetic radiation. Ena — Ena = hf where f= frequency of the emitted radiation —mZ7e* —mZ7e* Ind he| ~ \e,2n2 he | ~ OF Beq2n?,h?| [Beq?n? he —mZ7e* — —mZ*e* af Bey?nyh? Bey?n, 7h f mZ7e* [2 1 | Beh In?, n?, The wavelength of the emitted radiation is given by cof
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af Ase 1_ mZe* [ 1 1 | X” Bep?hFcln?, 22. This equation gives the wavelength of emitted radiation. Now, i 3 -¥ wave number v= mZe* [ 1 1 | ~ Begth8cln2, 22. Wave number These are the number of waves in a unit length, For hydrogen atom For hydrogen atom z=1 1_ mZe* [ 1 1 | X~ Begthecln®, n?, This gives the mathematical formula for the wavelength of radiation emitted by hydrogen atom when electron jumps from outer orbit to inner orbit. 1 11 tended pried Ca os where Ruis Rydberg constant. The value of Ri can be calculated as the value of e, m, h and c are known
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mzZe* Ry = Beq?ch _ (9.1 x 10754) x (1.6 x 10-19)* 8x (6.854 x 107)? x (3 x 10") x (6.62 x 10-*)> Ry = 1.097m* HOW TO CALCULATE THE RYDBERG CONSTANT USING CALCULATOR From Ry =e Begtch? m= 9.1.x 10734 kg m=16x10-%¢ £9 = 8.854 x 10-2F m= ¢=3x 10®ms"? h = 662x 104s y= (9.1.x 10-5) x (1.6 x 10-*9)* 4 Bx (8.854 x 10-22)? x (3 x 10°) x (6.62 x 10-74)? pe 9.1 x (1.6)* 10-31 x (10-79)* #8 x (8.854) x 3 x (6.627)* (10-22)? x 108 x (10-4)> Ry = 1.093 x 10-* x = _ 10-™* x 108 x 10-77 10-31 x 10-76 Ry = 1.093 x 10-* x a 10m, Ry = 1.093 x 10-4 x zal Ry = 1.093 x 10-* x 10% Ry = 1.093 x 10’m=*
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Now saturation current is of higher value as shown in figure below / L L y —Ve _——____* a Retarding potential Anode PotentialV This is expected because the greater the intensity of incident radiation the greater is the photo electric current Stopping potential ‘Stopping potential is the minimum retarding potential at which photoelectric current becomes zero Or is the potential difference when no electrons are able to reach the anode. Itis also known as stopping voltage or cut-off potential. It is denoted by Vp or V, Stopping potential is a measure of the maximum kinetic energy of the photo electrons. Since potential difference V y — Working done(W) Charge(Q) For stopping Voltage Vo
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W = QVo For an electron W =QV, =Q =e w=ev, ne ee zmv? = eV, ‘At Vo, even the photo electrons having maximum kinetic energy KE mu (ie. fastest photo electrons) cannot reach the anode A. Therefore, the stopping potential Vo is a measure of the maximum kinetic energy K.E may of the photo electrons. ‘eVp is the work done by the retarding force to stop the photo electron with maximum kinetic energy and is therefore equal to K.Enax At Vo, it is found that the photoelectric current cannot be obtained even if we increase the intensity of radiation. It is same for different intensities |,, lp and | of incident radiation. 3. Effect of frequency of incident radiation on stopping potential. ‘We now study the relation between the frequency f of the incident radiation and the stopping potential Vo. For this purpose, we take the radiations of different frequencies but of the same intensity. For one frequency say f,, of the incident radiation, we plot the graph between photoelectric current and potential of anode A with respect to cathode C at a constant intensity of incident radiation Keeping the intensity of incident radiation the same, we repeat the experiment for frequency f, of the incident radiation.
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The following is the resulting graph Yo ° 5 t , / / Observations from the graphs 1. The value of stopping potential is different from radiation of different frequencies 2. The value of stopping potential is move in low higher frequency. This implies that the value of maximum kinetic energy depend on the frequency of incident radiation. The greater the frequency of incident radiation, the greater is the kinetic energy of emitted photo electrons. 3. ‘The value of saturation current depends on the intensity of incident radiation but is independent of the frequency of incident radiation if we draw a graph between the frequency of incident radiation (f) and the stopping potential (Vo) at constant intensity of radiation, it will be a straight line AB as shown in figure below
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Ym B A ° 7 fo f / / / From the graph At fo, stopping potential Vo= 0. It means that at fo, the photo electric current is just zero (i.e. photo electrons and emitted with zero velocity) and there is no retarding potential. Vo=0 ‘This limiting frequency fo is called threshold frequency for the cathode material. It is a minimum frequency of the incident radiation which is just sufficient to eject photo electrons (i.e. with zero velocity) from the surface of a metal. Stopping potential is directly proportional to the frequency of incident radiation. Voaf The greater the frequency of incident radiation, the higher is the stopping potential and vice versa. Experiments show that photo electric emission is an instantaneous process.
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As soon as light of suitable frequency (equal to or greater than f.) is incident on the surface of the metal, photo electrons are emitted from the metal surface. The time delay is less than 10° second LAWS OF PHOTOELECTRIC EMISSION ‘The above experimental study of photoelectric effect leads to the following laws of photoelectric emission. i Fora given metal, there exists a certain minimum frequency of incident radiation below which no emission of photo-electrons takes place. This cut off frequency is called threshold frequency fo. ii For a given metal and frequency of incident radiation (>fo) the photo electric current is directly proportional to the intensity of incident radiation. iii, Above the fo, the maximum kinetic energy of the emitted photo-electron is independent of the intensity of the incident radiation but depends only upon the frequency of the incident radiation. iv. The photoelectric emission is an instantaneous process. The above laws of photoelectric emission cannot be explained on the basis of light or radiation. This gave death blow to the wave theory of light or radiation. FAILURE OF WAVE THEORY/CLASSICAL PHYSICS TO EXPLAIN PHOTOELECTRIC EFFECT The wave theory of radiation failed to explain photoelectric effect. This will become clear from the following discussion. 1. According to wave theory of radiation the greater the intensity of the wave the greater the energy of the wave. ‘So wave theory does explain why the number of emitted photoelectrons increase as the intensity of radiation is increased. But it fails to explain the experimentally observed fact that the velocity or kinetic energy of the emitted photoelectron is independent of the intensity of incident radiation. ‘According to the wave theory, an increasing in the intensity of radiation should increase the kinetic energy of the emitted photoelectrons but it is contrary to the experimentally observed fact. Il. According to wave theory, intensity of radiation is independent of it is frequency it depends upon the amplitude of electric field vector.
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Therefore, an increase in the frequency of radiation should not affect the velocity or kinetic energy of the emitted electrons. But it is observed experimentally that if the frequency of the incident radiation is increased, the kinetic energy of the emitted electrons also increases. Ill. According to the wave theory, electrons should always be emitted from a metal by radiation of any frequency if the incident been is strong enough However experiments show that no matter how great is the intensity of the incident radiation; no electrons are emitted from the metallic surface if the frequency of radiation is less than a particular value i.e. threshold frequency. IV. According to the wave theory the energy of radiation is spread continuously over the wave fronts of the radiation. Therefore, a single electron in the metal will intercept only a small fraction of the wave’s energy. Consequently considerable time should be needed for an electron to absorb enough energy from the wave to escape the metal surface. But experiment show that electron are emitted as soon as radiation of suitable frequency falls on the metallic surface. In other words photoelectric emission is instantaneous there is no delay. The above discussion is a convincing proof of the inability of the wave theory to explain the photoelectric effect. EINSTEIN QUANTUM THEORY OF LIGHT Einstein explained photoelectric effect on the basis of Planck’s quantum theory. According to Einstein light radiation consist of tiny packets of energy called quanta. Photon Photon is the single quantum of light radiation which travels with the speed of light. The energy of a photon is given by E. E=hf
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where
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7. In Bohr’s model of hydrogen atom the electron circulates around nucleus ona path of radius 0.51A at a frequency of 6.8x19°~ is rev/second calculate the magnetic field induction at the centre of the orbit. Solution ‘The circulating electron is equivalent to circular current loop carrying current I given by dQ_e fu 2 =~ | l=ef “19 15 1216 * 107 x 6.8 x 10 “3 l= 11% 10 A Magnetic field at the centre due to this current is Hol B, =fe contre => _ Gm x 1077) - (4.1 x 1079) 2 x (0.51 x 10-*°) Beentre = 44T 8. A long straight wire carries a current of SOA. An electron moving at 10"ms is Sem from the wire
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Ve TI Sem —_ Find the Magnetic field acting on the electron velocity is directed (i) Towards the wire (ii) Parallel to the wire (iii) Perpendicular to the directions defined by land ii Solution ‘The magnetic field produced by current carrying long wire at a distance r = Hol 8 2nr pa ttX10 50 "Qn 5x10? B=2x10“T The field is directed downward perpendicular to the plane of the paper (1) The velocity V1 is towards the wire. The angle between Vi and B is 90° force on electron F=Bovein®
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F = 2x 10% x 1.6x10°x10"x Sin 90° F=3.2x101°N (ii) When the electron is moving is moving parallel to the wire ,angle between V2 and B is again 90ES Therefore, force is again 3.2x10"N (iii) When the electron is moving perpendicular to the directions defined by (i) and (ii) the angle between V and B is O F=-O 9. A solenoid has a length of 1.23 mand inner diameter 4cm it has five layers of windings of 850 turns each and carries a current of 5.57A. what is the magnitude of the magnetic field at the centre of the solenoid Solution The magnitude of the magnetic field at the centre of a solenoid is given by B=yponl But N _ 5xe50 n=7 =a = 34553 B = 41x 10” x 3455.3 x 5.557 B=24.2x10°T 10. A to void has a core ( non - ferromagnetic) of inner radius 20cm and over radius 25em around which 1500 tums ofa wire are wound. If current in the wire is 2A Calculate the magnetic field (i) Inside the to void
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(ii) Outside the to void Solution 20+25 Mean radius = ——— r = 22.Sem = 22.5 x 107m L=2ar mean length |= 2nr = 2m x 22.5x 107 =1413m (i) The magnitude of the magnetic field inside the toroid is given by B=jonl B= 41x 1077 x Sx Perciery B=0.003T (ii) The magnetic field outside the toroid is Zero. It is all inside the toroid. 11. A solenoid 1.5m long and dem in diameter possess 10 turns/cm. A current of 5A is flowing through it. Calculate the magnetic induction ()) Inside and (ii) At one end on the axis of the solenoid Solution N p= 1 = 10turns/cm _ 10° turns/cm (i) Inside the solenoid , the magnetic induction is given by
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pateal pa4tX 1077 x 10° x 5 patX10°T (ii) Atthe end of the solenoid the magnetic induction is given by patent _ 2m x 107% 2 2 B=1X10°T 12. (a) How will the magnetic field intensity at the centre of a circular loop carrying current change, if the current through the coil is doubled and the radius of the coil is halved? (b) A long wire first bent in to a circular coil of one tum and then into a circular coil of smaller radius having n turns, if the same current passes in both the cases, find the ratio of magnetic fields produced at the centers in the two cases. (c) A and B are two concentric coils of centre O and carry currents Ia and In_as shown in figure I C-) ,
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If the ratio of their radii is 1:2 and ratio of flux densities at O due to A and B is 1:3, find the tp value of 4 Solution (a) Magnetic field at the centre of circular coil Honl p = Hort 2r I Ba- ; KI pa Kt + Br ak’ I Byr, _ Bat A L B,_h mh Ro An k=l ner I=21 : net = 2 By By B By = 4B, (b)Suppose r is the radius of one turn coil and the r’is the radius of n-turn coil. Then Nn* 2nr* = 2nr rss N
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First ease Second case
so! we be
B= B,="T
B,_ wNI_ 2r
By 2("/y) Hol
By
Br _ ye
B,
Solution
C. Magnetic field at the centre of circular coil
Hol
a
Ban
=
Bry
=
Bara _ Bate
Llp
ta _ Bata
Ty” Bate
boil
Iz 32
Ip 6
13. A helium nucleus makes a full rotation in a circle of radius 0.8m in two seconds. Find the
value of magnetic field at the centre of the circle.
Solution
The charge on helium nucleusPage 66: full text transcript
a: + a=*?* 1.6 x10% Current produced | = 1=2x16x10" 1=1.6 x10%A Magnetic field at the centre of the circle orbit of the helium is, = bel B or ‘2m x10" x16x 10-19 pe a08 B= 1.256 x10" 14, A soft Iron ring has a mean diameter of 0.20m and an area of cross section 5x10“m? it is uniformly wound with 2000turns carrying a current of 2A and the magnetic flux in the iron is 8x 10°Wb. What is the relative permeability of iron? Solution Length of ring 122" 1=27"x0.10m Number of turns per unit length n N 2000 nel 22mx0.1 If Mis the absolute permeability of iron, then magnetic flux density of iron ring is p=Monl
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p- X pose * 2 B= 2x2 x 10*Wb/ cd m? Magnetic flux ® = BA H ‘ + Ex2x10*x5 x10 ™ 10, = 20H 10, 8x10 =—* Magnetic flux ® = BA w= 82x 10-*H/M Relative permeability of Iron yt. _# _8xx107* Mr ig 4X 1077 bi, = 2000 15. Two flat circular coils are made of two identical wires each of length 20cm one coil has number of turns 4 and the other 2. Ifthe some current flows though the wire in which will magnetic field at the centre will be greater? Solution For the first coil Hor p, = tom 1 ry
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For second coil HoNI a, = Holl! 2 2 By mh By mh Length of the wire | = ny; 2nr, = n,27y mh =m my = nm mn By om my By mz Mm By c y B, \n, z-(5) B, \2 Ply B, = Therefore, magnetic field will be greater in coil with 4 turns 16. A plat circular coil of 120 turns has a radius of 18cm and carries currents of 3A. What is the magnitude of magnetic field at a point on the axis of the coil at a distance from the centre equal to the radius of the coil? Solution Number of turns n = 120 Radius of the coil r= 0.18 m Axial distance x = 0.18m_ Current in coil 1= 3A.
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Nir? B= —— 2(r? + x2)" B= (44x 10-7 x 120 x3 x0.18? 2(0.18? * 0.182) 3? Be 44x 047 17. A current of 5A is flowing upward in a long vertical wire. This wire is placed in a uniform northward magnetic field of 0.021. How much force and in which direction will this field exert on 0.06 length of the wire? Solution F=BiLsing 8=0.02T 1=5A L=0.06 e =90° Fe 002x3 x0esing00 P0000 By Fleming's Left hand rules the force is directed towards West 18. A straight wire of mass 200g and length 1.5m carries a current of 2A. It is suspend in mind air by a uniform horizontal magnetic field B. What is the magnitude of the magnetic field? solution M=200 X 10° kg 1=2A 1= 1.5m B=? F=BIL
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Since magnetic field strength B is the magnetic field lines passing per unit area of the material, it is a measure of magnetic permeability of the material. Suppose magnetic flux density in air or vacuum ise, If vacuum/air is replaced by a material, suppose the magnetic flux density in the material becomes B Then ratio B/e called the relative permeability“. of the material (i) Relative permeability “> . Isthe ratio of magnetic flux density Bin that material to the magnetic flux density 3 that would be if the material were replaced by vacuum/ air. Bo Ho= B= 1 Clearly isa pure number and its value per vacuum/air is 1 Bo ==1 By By Relative permeability of a material may also be defined as the ratio of absolute permeability “ of the material to absolute permeability “2 of vacuum/air. # wo=h=1 on Ho (ii) Magnetizing force/ Magnetic intensity H Is the number of ampere - turns flowing per unit length of the toroid. ‘The SI Unit of magnetizing force His Ampere —turns per meter (AT/m) Consider a toroid with n turns per unit length carrying a current I. if the absolute permeability of toroid material is M, then magnetic flux density B in the material is
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B=ynl B= Hou,nl The quantity ™ is called magnetizing force or magnetic intensity Zz Therefore, the ratio” ina material lis from B= pH. B= Holly § Holy H Bo = oll Thus if the some magnetizing force is applied to two identical air cored and iron cored toroid, then magnetic flux density produced inside the toroid is Bo = Mob H (iii) Intensity of magnetization (1) is the magnetic moment developed per unit volume of the material. When a magnetic material is subjected toa magnetizing force , the material is magnetized Intensity of magnetization is the measure of the extent to which the material is a magnetized and depends upon the nature of the material > M i=— v where: M = magnetic moment developed in the material V= volume of the material
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If mis the pole strength developed, @ is the area of X — section of the material and 21 is the magnetic length. Then mx 21 1=——— ax 21 m 1=7 a Hence Intensity of magnetization of a material may be defined as the pole strength developed per unit area of cross-section of the material. ‘Thus the Slunit of lis Am! which is the same as the SI unit of H Magnetic susceptibility ** is the ratio of intensity of magnetic on I developed in the material to the applied magnetizing force H , 1 Itis represented by Xm =F The magnetic susceptibility of a material indicates how easily the material can be magnetized. ‘The unit of | is the same as that of H1 so that ~™ is a number Since I is magnetic moment per volume *™ is also called volume susceptibility of the material . Consider a current carrying toroid having core material of relative permeability “ The total magnetic flux density B inthe material is given by
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B= Bot Bm Where 5. — magnetic flux density due to current in the coils. Fm = magnetic flux density due to the material (Magnetization of the material) Bo = Modi) Bm = Hol . sali) Here | is the intensity of magnetization induced in the toroid material B=30 45x B= ul + ul B=y(H+1) Now, x= I "OH I=X,,H B=yo(H+ X,,H) = uoH(1+ X,,) B=pH = pou * HoH = woH(1+ X,,) Or Equation (iii) give the relation between relative permeability (4, ) and magnetic susceptibility (Xm). CLASSIFICATION OF MAGNETIC MATERIALS: All materials or substances are affected by the external magnetic field. Some attain weak magnetic properties and acquire strong magnetic properties.
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Path described by particle, Q x ox x x x xi x x oe KOK x _ x x x Keo x x a a a a a a ae a RMR KK OK KR KOK KK KK KX X = Magnetic fields into the page The velocity V can be resolved into two rectangular components i) vi= V°°S9 Acting in the direction of the field ii) V2= Vsin® acting perpendicular to the direction The perpendicular component V2 moves the charged particle in a circular party while the horizontal component “imoves it in the direction ofthe magnetic field In other words, the charged particle corers circular path as well as linear path. Consequently the charged particle will follow a helical path, ‘The charged particle rotates in a circle at speed V2 while moving in the direction of the field with a speed Vi PARAMETERS OF MOTION The perpendicular component of velocity V2 determines the parameters of the circular motions while the horizontal component of velocity Vi decides the pitch of helix i) Radius of path
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From Fy = Ma Mv,? BQV, = —— . sq = MB =o MY, roth BQ = MVsin@ r= Muang (i) ~~ T,fandw Since time period (1), frequency (f) and Angular frequency(«) of a charged particle moving in a uniform magnetic field are independent of speed V and radius (r) of the path, these values remain the same 2nM T= BQ f= 2nM w= ™M (iii) Pitch of helix (d) Itis the linear distance covered by charged particle when it completes one
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circular revolution Or It is the linear distance covered by charged particle during time T a=4r a= vos Oy cos@ x 2 d=V BQ 2am d= 0 (Vcos6] The following points may be noted about the behavior of charged particle in a Uniform magnetic field i If acharged particle is at rest V=0 in a magnetic field, it experiences no force From Fra pgysind Frau yQX 0X sind Fra) (i) If a moving charged particle enters a uniform magnetic field at right angles to the field it describes a circular path (iii) Ifa moving charged particle enters a uniform magnetic field. Making an angle to the direction of the field it describes a helical path
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(iv) A moving charged particle in a magnetic field experience maximum force when angle between V and Bis 90° (v) Since magnetic force does not change the speed of a charged particle it means that K.E of the charged particle remains constant in the magnetic field. (vi) Since magnetic force (Fm) is perpendicular to V, it does not work. Therefore work done by the magnetic force on the charged particle is zero WORKED EXAMPLE 1. Anelectron and a proton moving in a circular path at 3x10° Ms" in a uniform magnetic field of magnitude 2 x 10“T. Find the radius of the path Solution v2 Bey == r abe "= 'Be 9 x 1073 x (3 x 10°) (2x 10-4) x (1.6 x 10749) r =85x 107m 2. Anelectron anda proton moving with the same speed enter the same magnetic field region at right angles to the direct of the field. For which of the two particles will the radius of circular path be smaller? Solution From _MV "Be
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rom Since the mass of electron is less than that of the proton the radius of the circular path of electron will be smaller. 3. (a) What will be the path of a charged particle moving along the direction of a uniform magnetic field? (b) A moving charged particle enters a magnetic Solution (a) When a charged particle moves along the direction of a uniform magnetic field ,it experiences no force © 0° therefore the charged particle will more along its original straight path (b) Helical path since the velocity of the charged particle can be resolved into two rectangular components one along the field, and the other perpendicular to the field, The velocity component perpendicular to the field causes the charged particle to more in acircular path while the velocity component along the field cause it to more itin the direction of the field, The combination of these two motions course the charged particle to. move ina helical path. 4. Abecome of a-particles and of proton of the same velocity V, entries a uniform magnetic field at right angles to the field lines. The particle describes circular paths. What is the ratio of radii of the two paths? Solution Radius of a-particle path "
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EAd en) Of proton path "2 av 4 rr od Take equation (i) *. equation (ii) nm _ MW BQ, 7 BQ, MV TG My % QQ M2 1x4 ™% 2 - haa n Therefore, radius of x - particle path is twice that of proton’s path Note a-particle Charge = 2e Mass = mass of helium nucleus 5. A proton with charge ~ mass ratio of 10° CKg “is moving in a circular orbit in a uniform magnetic field of 0.ST. calculate the frequency of revolution
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d=4.37x10°M 7. (a) A particle of charge 0leef moves in acircular path of radius r in a uniform is P = BQr (b) An electron emitted by a heated cathode and accelerated through a potential difference of 2.0KV enters a region of magnetic field of 0.15 determine the trajectory of the electron if the field (i) _ is traverse to its initial velocity (ii) makes an angle of 30 with the initial velocity ¢) Aproton a deuteron and an a ~ particle whose kinetic energies are same enter perpendicularly to a uniform magnetic field. Compare the radii of their circular paths (a) Solution ‘The magnetic force Fm provides the necessary centripetal force Fe Fm = Fe Bq=% momentum BQ= Momentum P = BQr (b) Solution When an electron (e) is accelerated through a p.d of V, it acquires energy eV. IF Vis the velocity gained by electron, then
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IM(v?) y = Me) ° 2 w -\e*#) Vv = J(@x(46 x 10* — 19) x (2x10"3)) ‘v=9x107" @ Force on the electron due to transverse field is Fm = BQr ores =90° Since magnitude of Fm is constant and Fm is perpendicular to both V and B the electron will move in a circle of radius r. The necessary centripetal force is provided by Fm Mv? Paei . Mv? we BQv __ @x10™)x ” * G0-)x 6x10) re 10°M (ii) When electrons enters the magnetic field making an angle 0"ce/ = 30° with the field M (rSin 8°)? BQBVSin® = aoe MVSin@ pel) BQ
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__9x107%4x Sin 30° r * 0.A5x16x 10-9 r =05x10°M (©) Solution Let 1, 2 and 3 be the suffix force proton, deuteron and a - particle respectively K E,=KE=KE; 1 MiVi = | M2V2= | MaVs 2 2 2 IfMI then My =2M and Ms = 4M MV" = 2MV2 = 4MV?s viz VY¥2=2y, V2= VI v2 Also % Yaz Radius of the path r r= Mv 8a I=, Then @2=Q anda3=20 n=MM = MW 8Q, Ba
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p= M.V2= 2M. V; sa, sa Y? nae BQ3 2BQ “2 hi = My: uy, : MY, BQ BQ BQ ninine 12 4 NUMERICAL PROBLEMS 1. What is the radius of the path of an electron (mass 9 x 107!)Kg and charge( 1.6 x 10°C) moving at a speed of 3 x10'm/s in a magnitude field of 6 x 10“T perpendicular to it? What its frequency? Calculate its energy in KeV(1Ev=1.6x10"'J) = 0.28m & 1.7x107 Hz E=2.53KeV 2. Anelectron after being accelerated through a p.d of 100V enters a uniform magnetic field of 0.0041 perpendicular to its direction of motion. Find the radius of the path described by the electron 1=8.410°m 3. Ana-particle is describing a circle of radius of 0.45m in a field of magnetic Induction 1,2Wb/m”, Find its speed, frequency of rotation and kinetic energy. What potential difference will be required which will accelerate the particle so as to this much energy to it? The mass of a-
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N=50 I=1A e=0 t= 1.5 X (7.85 X10) X50X1 t=0.589NM (b) Since torque on the loop is independent of its shape provide area (A) Temains the same the magnitude of the torque will remain unaltered. 4 A circular coil of 20tums and radius 10 cm is placed in a uniform magnetic field of 0.21 normal to the coil. If current in the coil is 5A find. (i) Total torque on the coil (ii) Total force on the coil (“Average force on each electron in the coil due to the magnetic field. ‘The coil is made of copper wire of cross-sectional area 10m? and force of electron density inthe wire is 10°%m?> Solution @ The toque on the coil is given by t= BANIcos@ Since @=0 (ii) The net force ona planar current loop ina uniform magnetic field is always zero (iii) Magnetic force on each electron F=BeVa
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F=Be, =04 BI pa2t nA 0.25%5 F= 102°x10-5 F=10™N MOVING COIL METERS A galvanometer deflects or measures small amount of current passing through it and it gives the direction to which that current is flowing. In these instruments a rectangular of fine insulated copper wire is suspended in an strong magnetic field as shown in the figure below. The field is set up between soft iron poler pierces Ns attacked to a powerful permanent magnet. a b Cis s ° re RH ”, » a ® by sprin ena e 1a Coil gO [pJewelled Bearing (i) Millimeter
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The magnet field is radial to the core and pole pieces over the region which the coil can swing. In this case the deflected coil always comes to rest with the plane parallel to the field in which it then situated. The moving coil galvanometer ha s has hair spring and jewel bearings. The coil is around in the rigid but light aluminium frame which also comes to carries a pivot. The current is led in and out of the springs. Aluminum pointer P shows the deflection of coil, it is balanced by counter weight Q. ‘THEORY OF MOVING COIL GALVANOMETERS The rectangular coil is situated in the radia field B when the current is passed into it the coil rotate to an angle Q which depend on the length of the spring. No matter where the coil comes to rest, the field B in which it is situated always along the plane of the coil because the field is radial. It is shown that the torque T of the coil is given by T= B AN L ie. In equilibrium the deflecting torque T is equal to the opposing torque due to the elastic forces in the springs. The opposing torque ‘Torque = CQ Where C is the constant of the spring Example 1
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Total resistance for the new scale is =15002000 = 30 10° 4,,| Extra resistance required is (30-3) 10° =27 10° a, MAGNITUDES FOR CURRENT CARRYING CONDUCTORS, Laws of Biot and Savant. It state that the flux density dB= at point P due to a small element dl ofa conductor carrying Where r is the distance from the point P to the element is the angle formed it to P. Pp dB ao 1 | / B: FLUX DENSITY = INDUCTION OR MAGNETIC INDUCTION
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MAGNETIC FIELD Equation (1) can be written as dB=KIdlsinx Where K is the constant of proportionality and it depends on the medium in which the conductor is situated. Also K = = aHoldlsine ai — @ The formula is Note that fp = 47 X 10-7 Henry m? B =a r B AT THE CENTRE OF A NARROW CIRCULAR COIL
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Suppose the coil is in air has a radius of r carries a steady current I and it is considered to consist of current clement of length dl. Each element is at the distance r from the centre 0 and it is at the right angles the line joining it to i.e. * 90° dl al at r [~\ ad r al e al o%® 2 1 Ifthe coil have N tums then the length of the wire = 2711N — _ Holdisinx From the equation Gi) dB = "#\°5* Then the magnetic field at the centre is given by = Bo pPN ap = Bot py ZN _ iat at = (Ho = told =SN ; B a B cy Example A coil of wire with 15 turns of radius 6.0cm, has a current of 3.5A flowing through it. What is the magnetic flux density at the center of the coil? Solution B=38 = a = 175k x 10° Tesla 2 = 5.495 x 104 Tesla
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Example What is the magnitude of the flux density produced the center of a coil of radius Scm carrying current of 4A in air. Solution Formula, Given = = BNL amtoxexd I=4A B on 2x5x107? 1.6m r=5x 10%m. N=I B=5.024 x 105 Tesla Example A circular coil of radius 6cm consisting of 5 turns carries a current supplied from 2v accumulator of negligible internal resistance. If the coil has a total resistance of 24,,|. Calculate the magnetic field induced at the centre Solution Formula. y =Ya2-1- wt _ dato as re 2 Axfeso? N=S B= 2x 105 =3.335 x 10% Tesla r= 6x 107m = 3.335 x 10 Tesla uw. = 4x 107 B DUE TO A LONG STRAIGHT WIRE AT A DISTANCE d SIDE THE WIRE Consider a very long wire YN carrying a current I. Take P to be a point outside the wire but also this point is considered to be very near to this wire.
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' N a 8 4B da x di ypa #7 A THE HALL EFFECT Is the phenomenon where by e.m. for voltage is set up transversely or across a current carrying conductor when a perpendicular magnetic field is applied Consider a piece of conducting material in a magnetic field of flux density B Suppose that the field is directed (perpendicularly) into the paper and that there is a current flowing from right to left.If the material is a metal the current is carried by electrons moving from left to right Consider the situation of one of these electrons and suppose that it has a velocity V The electron feels a force F which by Fleming’s left hand rule, is directed downwards . Thus in addition to the electron flow from left to right electrons are urged away from face Y and towards face X. Anegative charged builds up on X, leaving a positive charged on Y so that a potential difference is established between X and Y. The buildup of charge continues until the potential difference becomes so large that it prevents any further increase . This maximum, potential difference is called the Hall voltage Hall voltage
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Is the potential difference created across a current carrying metal strip when the strip is placed in a magnetic field perpendicular to the current flow in the strip. Actually, the magnetic field does not have to be totally perpendicular to the strip the magnetic field only needs to have a component that is perpendicular The flow ceases when the ¢ .m freaches a particular Vi called Hall voltage MAGNITUDE HALL VOLTAGE Suppose Vu is the magnitude of the Hall voltage and d is the width of the slab (the separation of x and y). Then the Electric field strength E set up across the slab is numerical equal to the potential gradient. Ya E=4 let Fy be the force exerted on an electron by the P.d between X and Y. ‘Therefore when the buildup of charged on X and Y has ceased F=Fy BeV=ek BV=E “a By= ¢ Vi BV oooccccccseneeee (i) Where E = The strength of the uniform electric field between X and Y due to the Hall voltage Vu = Hall voltage d= The separation of X and Y
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w=). =e MUTUAL INDUCTANCE (M) the °™S may be induced by in one circuit by changing current in another. This phenomenonis often called mutual induction and the pairs of circuits which shows it are said to have mutual inductance The mutual inductance m between the two circuits is defined by the following equation emf, , , nai Induced in B by changing = M (rate of change of current in A) ie. =i E, = M74 The unit of mutual inductance is Henry the same as that of self-inductance hk M a Ec x 8 MUTUAL INDUCTION since 2 =the rate of change in flux in 8 then =i mat Ea= at at M= dop _ Fluxchange inB dl, current change ind QUANTITY OF ELECTRICITY INDUCED
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Consider a close circuit of total resistance R Ohms which has a total flux linkag@ with magnetic field B. if the flux linkage starts to change cc E=% Induced °F,” ~ 4 but current 122218 R Rat — : | Rg ——————qxqg8F Flux linkage will not change at a steady rate and a current will not be constant. But throughout it changes. Its charge is being carried round the circuit. If a time t seconds is taken to reach a new constant value the charge carried round the circuit in that time is Q = filde. from equation i) we have aise? gp = 15% Om ELE at = 5h, do Where , is the number of linkage at t=o and %., the number of linkage time t (_-Op) _ (®p-04) Thus * al Q _ Change of flux linkage R
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AC THEORY When a battery is connected to a circuit the current flows steadily in one direction, this is called a Direct current (d.c). The use of Direct currents is limited to a few applications e.g charging of batteries, electroplating etc. Most of electrical energy is generated and used in the form of alternating current due to many reasons including, i) Alternating voltages can be changed in value very easily by means of transformers. ii) A.c motors are simpler in construction and cheaper than d.c motors. ALTERNATING VOLTAGE AND CURRENT i) Alternating voltage ‘An alternating voltage is one whose magnitude changes with time and direction reverses periodically. The instantaneous value (i.e value at any time t) of an alternating voltage is given by, E = Ep sinwt where, E = Value of the Alternating voltage at time t £ = Maximum value of the Alternating voltage w= Angular frequency of supply From ® = 27f where fis the frequency of the alternating voltage, If T is the time period of alternating voltage then w= 2nf 2n o=— T
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f Maximum > + f \e» A criy o & a 4 180° 360° > Minimum ' Maximum The voltage varies from zero to a positive peak (*Eo) then back via zero to negative peak (-Eo) and so on. In time period T, the wave completely cycle. E =—— sinwt ii) (ii) Alternating current This is one whose magnitude changes with time and direction reverses periodically. The Instantaneous value (!-© value at any time t) of sinusoidally varying alternating current is given by 1=Iysinwt where 1 = value of alternating current at time t lo = maximum value (Amplitude) of alternating current. w = Angular frequency of supply. w= 2nf 2a o—— T Figure below shows the waveform of alternating current.
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Consider the current variation over one complete cycle. a eS [On 2270 ho bs 2 Average value of J? pottst9 IP? =S67A R.MS value of current VP? =V5.67 =24A «R.M.S value of current = 2.44 A.C CIRCUIT ‘An A.C circuit is the closed path followed by alternating current. When a sinusoidal alternating voltage is applied in a circuit, the resulting alternating current is also sinusoidal and has the same frequency as that of applied voltage. However there is generally a phase difference between the applied voltage and the resulting ‘As we shall see, this phase difference is introduced due to the presence of inductance (L) and capacitance (C) in circuit. While discussing A.C circuits our main points of interest are; (i) Phase difference between the applied voltage and circuit current (ii) Phasor diagram. It is the diagram representation of the phase difference between the applied voltage and the result circuit current. (iii) Wave diagram (iv) Power consumed. A.C CIRCUIT CONTAINING RESISTANCE ONLY
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When an alternating voltage is applied across a pure resistance, then from electrons ‘© current flow in one direction for the first half cycle of the supply and then flow in the opposite direction during the next half cycle, thus constitute alternate current in the circuit. Consider a pure resistor of resistance R connected across an alternating source of &:7”- f E | ER | ‘Suppose the instantaneous value of the alternating &”"-F is given by Pm Rysinetspu aun wet If is the circuit current at that instant, then by ohm’s law 1-£ R 1 — Zasinat R Ey = sino w The value of | will be maximum |, when sinwt =1 Therefore equation (i) becomes 1=2sinat From R
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Since sin t= 1 then I= I. Eo b= oR 1) Phase Angle It is clear from equation (i) and (ii) the applied ©” and circuit current are in phase with each other £-€ they pass through their zero values at the same instant and attain their peak value both positive and negative peaks at the same instant. This is indicated in the wave diagram shown in figure below. The Ph@SOr diagram shown in figure below also reveals that current is in phase with the applied voltage. e / f Ps ) Wave diagram oe ly Fy (0) Phasor diagram Hence in an a.c circuit, current through R is in phase with voltage across R. This means that current in R varies in step with voltage across R. If voltage across R is maximum current in Ris also maximum, if voltage across R is zero, current in R is also zero and so on.
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2) Power Absorbed In a.c circuit, voltage and current vary from instant to instant. Therefore power at any instant is equal to the product of voltage and current at that instant. Instantaneous power P P=El P = (Ey sin wt). (Iysin wt) P = Eplol[sin? wt] P=Eole - — cos —| P= fale - Fel cos a | ‘Since power varies from instant to instant the average power over a complete cycle is to be considered. This is found by integrating equation. .........(iv) with respect to time for 1 cycle and dividing by the time of 1 cycle. The time per one cycle is T. Average power P
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r r 1f Flo , 1 [Fol P==| — d-= | — 7! 2 z/ 2 cos 2wt dt a a Now Then fj cos 2wt dt =0 1 (TE, pP=—| dt el. 2 Bet,'f* p= dt ar i E,l, p= 22 1e7 acd p = Fole P= Ee x fo v2 v2 P = Evmslrms Therefore, average power absorbed by a resistor in an a.c circuit is equal to the product of virtual voltage ( Ens) across it and virtual current ( lms) through it. Obviously, this power is supplied by the source of alternating &™-f. Since E, ne | R — Eims ealind Or P= [2asR
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‘WORKED EXAMPLES 1, An a.c circuit consists of a pure resistance of 100 and is connected across an a.c supply of 230V, 50 Hz. Calculate i) Circuit current ii) Power dissipated and iii) Equations for voltage and current Solution Erms=230v R=100 f=SOHZ i) Circuit current ba oe aia R 10 Ips = 234 ii) Power dissipated P P= Enmslrms = 230x 23 + P=5290W iii)Equations for voltage and current Eo = V2 Enns =V2x230
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Eo =325.27V Ip = V2XI pms =2x23 a rf '0=32.52A w=2"f 227 x 50 w=3145 « The equations of voltage and current E = 325.27 sin 314t and | = 3.52 sin 314t 2. Ina pure resistive circuit, the instantaneous voltage and current are given E=250sin 314t 1=10 sin 314t Determine i) Peak power ii) Average power Solution Ina pure resistive circuit i) Peak power = Zo/o =250x 10 + Peak power = 2500W
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ii) Average power P- Foxy Pz 2 p= 2 = P=1250W 3. Calculate the resistance and peak current in a 1000 W hair dryer connected to 120V, 60Hz ‘supply. What happens if it is connected to 240V line? Solution Enms= 120V, P=1000W Ins =? P=Enms lms P a aa ae Ipms= 833A Peak current lo 1b=V2 Inms =2x 8.33 “ Ig = 118A Resistance of hair dryer R E, R= Trms R 120 ~ 8.33 ~ R=144Q2
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When connected to 240V line, the average power delivered would be — Ffms — R P 240? ~ 144 + P=4000W This would undoubtedly melt the heating element or the coils of the motor. 4. Avoltage E = 60sin 314t is applied across a 20 © resistor. What will; i) An a.c ammeter ii) Ordinary moving coil ammeter in series with resistor read? Solution i) E=60sin 314 An a.c ammeter will read the r.m.s value. He Ey. iva ~ *24V ty = = 4 = 2124 v"R 20 ~*~ Therefore a.c a meter will read 2.12A ii) An ordinary moving coil ammeter will read average value of alternating current. Since the average value of a.c over one cycle is zero, this meter will record zero reading. 5. What is the peak value of an alternating current which produces three times the heat per second as a direct current of 2A in a resistor R? Solution Heat per second by 2A
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Ao ealR H=27R # ' 4k Three times heat per second HL T= 3X4R # 32 =12R If lis the r.m.s value of the a.c heat per second in R ca = LR aar=!"vR 17212 VP, = Vi2 Peak value is given by, fo = V2 1, Ip = V2 x Vi2 «Peak value = 24 = 4.9A 6. An a.c voltage of 4V peak (maximum) is connected to a 1000 resistor R a) What is the phase of the current and voltage? b) Calculate the current in R in mA. c) What is the power in R in mW Solution
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a) The current and voltage are in phase
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b) Current is R Ey = V2 X Ey E,p=4V 5, 23 =e fai = 2 v2 Ey=2.83V From, = © ly = 2.83 ta v™ 100 = 0.0283A Or ly = 28mA c) Power inR pale P = 0.028" x 100 P=0.078W P=78mW A.C CIRCUIT CONTAINING INDUCTANCE,
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When alternating voltage is applied across a pure inductive coil a back © -F (E) is induced in the coil due to its self inductance. a e--ta The negative sign indicates that induced e. mf opposes the change in current. In order to maintain the flow of current the applied voltage must be equal and opposite to induced voltage at every instant. Consider a pure inductor of inductance L connected across an alternating source of @:™-f L Ey n E E=E,sinwt Suppose the instantaneous value of the alternating e. m. fis given by Be Ea sin Wt enn (8) dl If Lis the current in the circuit and a is the rate of change of current at that instant, then e. m. f induced in Lis given by E L a © dt As applied voltage is equal and opposite to induce e.m_f at every instant dt E=-(12)
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a o Bliss vena From, Equation (i) and Equation (ii) inwt = L& FE, Sinwt = b= dt = © Sinwtde Integrating both sides we get 1 Ey i) dl= [ —sin wtdt 0 ob Fo? 1= 2] sin wede L 0 , Ey [ cos oy L @ Io E 1= 2 [-cos wt] oL Be, m I= sr lsia (wt = =| The value of | will be maximum I, when, Sin(Wt — 77/2) = 1 Then, L=2 0 ek poe? Substituting the value of a2 =/o in equation (iii) & 1=tsin (wt- 77/2) ee al a OE)
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1) Phase Angle It is clear from equation (i) and (iv) that circuit current lags behind the applied voltage by (772) radians or 90°. This fact is also indicated in the wave diagram. The phase diagram in figure below also reveals the fact that /v lags behind 2v by 902 By a / | = on Wy (a) Phasordiagram (b) wave diagram Hence in an a.c circuit current through L lags behind the voltage across L by 902 This means that when voltage across L is zero, current through L is maximum and vice versa. From =: E=Ler a a Now, @¢ is maximum when circuit current is zero and @¢ is zero when circuit current is maximum INDUCTIVE REACTANCE Inductive reactance is the opposition in which an inductor offers to current flow. It is denoted by X, Inductance not only causes the current to lag behind the voltage but it also limits the magnitude of current in the circuit.
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We have seen above that, 5a Ip = wok & wl=% Clearly the opposition of inductance to current flow is wl. This quantity wl is called inductive reactance XL of the inductor. Inductive reactance X, X= eo Or X, = 2nfL Or Ey ee Le Tp a) From y Kah But £o = V2Ey andi,=V24v Then, X= %: y Zw =x Ket hy b) For d.c f=0 so that, xe 2mfl
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X22TXOXL X, =0 Therefore a pure inductance offers zero opposition to d.c Xi of ) X= 27 FL Therefore,the greater f.the greater is X, and vice versa. 4) We can show that the units of X: are that of ohm 2 By vote Xi=wl=2eK Henry = #° ~ amp/see and volt ——=ohm X,= ampere Ill) Average Power consumed £=Fosinwt 1=£osin(ut2) = locosut Instantaneous power P P=El P= (Fosin wt) (cos wt) P= -Fo lo sin wt cos wt — he P= 2 Sin2ut Average power P is equal to average of power over one cycle.
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Lf g he P=T/0 2 Sin 2wtdt P=0 Hence average power absorbed by pure inductor is zero During one quarter cycle of alternating source of e.m_f. energy is stored in the magnetic field of the inductor this energy is supplied by the source. During the next quarter cycle the stored energy is returned to the source. For this reason average power absorbed by a pure inductor over a complete cycle is zero. NUMERICAL EXAMPLES 1. A pure inductive coil allows a current of 10A to flow from a voltage of 230V and frequency 60Hz supply. Find i) Inductive reactance ii) Inductance of the coil iii) Power consumed Write down equations for voltage and current: Solution Ey =230V. Iv=10A f=S0Hz i) Inductive reactance X, ke = B= 230 ii) Inductance of the coil L
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From Xe =20fL L=2t=2x50 inf On L=0.073H iii) Power absorbed = 0 Also Fox 230xV2 Tox 10x V2 Eo=325.27V To= 14.148 w=2t X50 w=314 Since in pure inductive circuit current lags behind the applied voltage by 7 radians. The equation for voltage and current are, E£=325 .27sin314t, | = 14.14 sin (314t) 2. Calculate the frequency at which the inductive reactance of 0.7H inductor is 2200 Solution XL = 2200 L=0.7H f=? X, = 2nfL « f=50Hz
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3. A coil has self inductance of 1.4H. The current through the coil varies sinusoidally with amplitude of 2A and frequency 50 Hz Calculate i) Potential difference across the coil li) r.m.s value of P.d across the coil. Solution T= Ipsinwt (i) P.d across the coil a E=Lae Uy sinwt) E=L ae aU, sin 2ft) E=_ ae =o cost, E=L02"F cosa ft p=2X 14 2X 2 x 50 X Cos 20x 50t E = 880 cos 100 7 ii) r.m.s value of potential different across the coil 4S Ey a2 = Eyat Ey = 622.2V
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4, How much inductance should be connected to 200V, 50 Hz a.c supply so that a maximum current of 0.94 flows through it? Solution E,=200v 1,=0.9A f=S0HZ Peak value of voltage Fo Eoz V2E, Ez V2 200 Inductive reactance L a X= b X= VEx200 ro X= 314.270 Inductance L, aL L=2nf 318.27 L= 2x50 L=1H 5. An Inductor of 2H and negligible resistance is connected to 12V, SOHz supply. Find the circuit current, what current flows when the inductance is changed to 6H? Solution * For the First case Xi
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x= anf X= 20 X50X2 X= 6280 Circuit current x ye = & Ty = 0.0198 * For the second case Xi’ x= 20fL X¢=27 X50 X 6 X= 1884.0 Circuit current w= y= x, Iyz tees 1v= 0.00638 A.C CIRCUIT CONTAINING CAPACITANCE ONLY When an alternating voltage is applied to a capacitor, the capacitor is charged first in one direction and then in the opposite direction. The result is that electrons move to and fro round the circuit connecting the plates, thus constituting alternating current.
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Consider a capacitor of capacitance C connected across an alternating source of e.m. f . c _ Ve _ ! Suppose the instantaneous value of the alternating e.m.f E is given by = Fbsin wt (i) If lis the current in the circuit and Q is the charge on the capacitor at this instant, then the Potential difference across the capacitor Vc Q #12 ey At every instant the applied e.m.f E must be equal to the potential difference across the capacitor. este | E,Sin wt == a=CFosinwt From, l=ee a(CESin wt)
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1= cwFocos wt 1= Cw Zosin (wt 7/2) Eo 1= ~sinwt + 2/2 Y we The value of lp will be maximum lo when sin (wt+7"/2) = 1 h= a ° Toc Substituting the value of le in equation (i) T=Ipsin(w + 1/2) 1) Phase Angle It is clear from equation (1) and (ii) that circuit current leads the applied voltage by n/2 radians or 90S. This fact is also indicated in the wave diagram. W ey (2) Phasor Diagram (b) Wave Diagram It also reveals that ly leads E, by 90°, hence in a.c circuit current in capacity leads the voltage. This means that when voltage across capacitor is zero, current in capacitor is maximum and vice versa. When P.d across capacitor is maximum £0, the capacitor is fully charged, i.e circuit current is zero. Since the rate at which a sinusoidally varying p.d falls is greater as it reaches zero, the current has its maximum value when P.d across capacitor is zero. Hence, current and voltage are out of phase by 90°.
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CAPACITIVE RESISTANCE Capacitive resistance is the opposition which a capacitor offers to current flow. Itis denoted by Xc. Capacitance not only causes the voltage to lag behind the current but it also limits the magnitude of current in the circuit. We have seen above that ss oz Moe fo z= oC Then Bifa. Bs Tp we Clearly, the opposition offered by capacitance to current flow is 1/wC The quantity 1/wC is called capacity reactance Xc of the capacitor Ec xc=— Ip Or xC = — wc Xewill be in 9 if fis in Hz and Cin Farad 2) From fo hz Then
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2. Acoil has an inductance of 1H a) At what frequency will it have a reactance of 31420? b) What should be the capacitance of a condenser which has the same reactance at that frequency? Solution a)L=1H X= 31420 f=? x= 2mfL fs Int =2exa: Jf 500H2 b) Xc= 3142, f=500 Hz c=? a Xc= 2876 = c= Bfke = C=iefke -6 c=0.11% 10 c=o011eF 3. aSOHF capacitor is connected to a 230V, SOHz supply. Determine i) The maximum charge on the capacitor
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ii) The maximum energy stored in the capacitor Solution The charge and energy in capacitor will be maximum when p.d across the capacitor is maximum. i) Maximum charge on the capacitor a=cFo a=cEyv2 = (50x20) x (230xv2) -3 Q=16.26x10%¢ ii) Maximum energy stored in the capacitor U u=2cE? os U=1/2x (50x20) x(230x V2» U=2.65) 4. The Instantaneous current in a pure inductance of SH is given be 1= 10sin (314t-™/2)amperes A capacitor is connected in parallel with the inductor. What should be the capacitance of the capacitor to receive the same amount of energy as inductance at the same terminal voltage? Solution The current flowing through pure inductor is 1=10 Sin (314t— 7/2) To= 108 w= 314s?
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Maximum energy stored in the inductor glgre W= SLI Mex 5S 107 U= 250) (i) Now Foz wtlo =314x5x10 Fo=15700v Max energy stored in the capacitor of capacitance C a Uc 22CE,? =x 5 x 157007 Equate the equation (1) and (ii) i 2 23% CX 157007). 250x2 C= is700* -6 C=2.03x 10"f c=2.034F ‘A.C CIRCUIT CONTAINING R AND LIN SERIES
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Consider a resistor of resistance R ohms connected in series with pure inductor of L Henry. R L a VR ————>+—_- VL lv Ev Let Ev= r.ms value of applied alternating e.m.f Jozr,m.s value of the circuit current Vn = 4vR when Vris in phase with /v vi=/y X1 where “i leads /v by 902 Taking current as the reference phasor, the phasor diagram of the circuit can be drawn as shown in figure. Ev | Vi a) ° z lv The voltage drop Vsis in phases with current and is represented in magnitude and direction by the phase OA. The voltage drop V. leads the current by 902 and is represented in magnitude and direction by the phase AB.
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The applied voltage ©v is the phasor sums of these two voltage drops Ey72Vq 4 Vi? Ey (IyR)? + (lyX,)* By fir (A? +4) Eye lyVR? + X,? E y= —__ VR? + XE 1) Phase Angle It is clear from the phasor diagram that circuit current /v lags behind the applied voltage Fv by @2. Therefore we arrive at a very important conclusion that in an inductive circuit current lags behind the voltage. NUMERICAL EXAMPLE 1, Three impedance are connected in series across a 200V, 50Hz supply. The first impedance is a 104,,| resistor and the second is a coil or 15 4,,| inductive reactance and 5 4,,| resistance while the third consists of a 15 4,,| resistor in series with a 254,,| capacitor Calculate i) Circuit current il) Circuit phase angle iii) Circuit power factor iv) Power consumed
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Solution i) Total circuit Resistance R=10+5+15 R=304,) Total Circuit reactance KEK - Xe X=15-25 X=-104,| (capacitive) Circuit impedance Z z= 307+ (—10)? 2=31.64,! Circuit current lv W=Ev Zz v= 200 31.6 W=6.33A
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ji) Circuit phase Angle XX tang = ——— R pan 2-055 tan®= -—= -0: mt 30 © = tan7*(—0.33) = -18.26° = 18.26° lead iii) Circuit power factor Power factor = COS 8 = COS 18.262 Power factor = 0. 949, iv) Power consumed P P=EvlvCos @ P = (200 x 6.33) x0. 949 P=1201.4W alt P=i’R 2. A230V, SOH2 supply is applied to a coil of 0.06 H inductance and 2.5 resistance connected in series with 6.8 uF capacitor
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Calculate i. Circuit impedance ii. Circuit current iii, Phase angle between Ey and Iv iv. Power factor v. Power consumed Solution i) Inductive reactance X, X= 20fL X= 21k 50 x 0.60 X= 18.850 Capacitive reactance Xe = 1 C" 2nft x, 1 ¢ 2n X50 X68 x 10-6 Xc = 4680 Circuit Impedance Z= JR? + (X, — Xe)? Z= (25)? + 4885 — 468)?
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2=449.209 ii) Circuit current lv = I, z = 230 W=0.152A ili) Phase angle between Ey and ly X,- X, Tano = —— R tan o = 18:85 468 se tan © = —179.66 0 = tan™?(—179.66) 0=-89.7 lead iv) Power factor ° R Cos® = : 2.5 cos aang =a at © = 92 Cos @ = 0.0056
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v) Power consumed P P=EvisCos® P = 230.x 0.512 x 0.0056 P=0.66W 3. Aresistance R, and inductance L = 0.01H and a capacitance C are connected in series. When an alternating voltage E = 400Sin (3000t- 20°) is applied to the series combination, the current flowing is 10v2 Sin (3000t - 650). Find the value of R and C Solution The circuit current lags behind the applied voltage by @ @=65°-20 6=45° This implies that the circuit is inductive i.e. Xi > Xe The net circuit reactance X X=X Xe Now X=wl X: = 3000 x 0.01 X%=300
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Also rromane== = 45" Tan 45= z 1-2 R Circuit Impedance Z za Fe = 400 T, 10V2 Z=28.309 Now P=R+xX? Z=R?+R? P=2R’ Z=Rv2 R=200 Now X =X Xe 20 = 30=Xe
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Xc= 100 From x, 1 © 2nfc c=— 2nfX, c=———_ 3000 x 10 C=33.3x10°F 4. Aseries RLC circuit is connected to an a.c (220V, 50 H) as shown in the figure below | | 100Q 220 V, 50 Hz WY c @) om If the reading of the three volt meter V; V 2 and V; are 65V, 415V and 204V respectively. Calculate
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i, The currentin the circuit ji, The value of inductor L ili. The value of capacitor C Solution Here voltmeters are considered ideal i.e. having infinite resistance. Therefore, it is a series RLC circuit i) Circuit current Iv W=0.65A ii) Inductive reactance X. Vv; 204 X,= L ry X= 318.850 Inductance L L= XL - 313.85 2nf 20x50 L=1H ili) Capacitive reactance X<
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Xc= 638. 460 Capacitance C c-_3 2nfXe ¢=—______ 2m X 50 X 638.46 C=5x10°F 5. Acoil of resistance 80 and inductance 0.03H is connected to an a.c supply of 240V, 50 Hz. Calculate i) The current the power and power factor. ii) The value of a capacitance which when connected in series with the above coil causes no change in the value of current and power taken from the supply Solution i) Reactance of the coil X: X, = 2nfl X, = 2m x 50 x 0.03 X=9.420 Impedance of the coil Z Z = R+X, = /8? +9.42?
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2= 12.460 Circuit Current ly =” ly = 1-24 v "12.46 W=19.42A Power consumed P= HR P= (19.42)? x8 P= 3017 W Power factor Cos © cosp== os@= = Z - 8 o3@=—— Oo” 12.46 Cos © = 0.65 lag ii) To maintain the same current and power, the impedance of the circuit should remain unchanged. Thus the value of capacitance in the series circuit should be such so as to cause the current to lead by the same angles as it previously lagged. This can be achieved if the series capacitor has a capacitive reactance equal to twice the inductive reactance. Xe= 2K, Xc=2x9.42
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L b OO OINS Iv The circuit will be in resonance when the circuit power factor is unity. This means that wattles component of the circuit current should be zero. hI ‘The resonance in a parallel a .c circuit can be achieved by changing the supply frequency because X: and Xcare frequency dependent . Ata certain frequency called resonant frequency fa, lc become equal to , and resonance occur. At resonance le=h From YW=Ve I, = Ip ae XOX X, = Xe
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2nf,L = ——— fol =>, fC f. 1 ° 2nvlc fo will be in Hz if Lis in Henry and Cis in farad EFFECTS OF PARALLEL RESONANCE 1) The circuit power factor becomes unity. This implies that the circuit act as a resistor 2) The impedance (resistive) of the circuit becomes maximum. 3) The circuit current is minimum the small current |v flowing in the circuit is only the amount needed to supply the resistance losses. RESONANCE CURVE This is the curve between the circuit current and the supply frequency. Figure below shows the resonance curve of a parallel a.c circuit. I Ey a re w= 7 ' ' ' i fo # The circuit current ly is minimum at parallel resonance. ‘As the frequency changes from resonance, the circuit current increases rapidly.
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This action can be explained as follows. For frequencies other than the resonance, the reactive currents
(i.and Ic) in the two branches of the circuit are not equal.
The resultant reactive current must be supplied by the a.c source
As the difference of the reactive currents in the two branches increase with the amount of deviation
from the resonant frequency, the circuits current will also increase.
“ADVANTAGE OF A.C OVER D.C
(i Alternating voltages can be stepped up or stepped down efficiently by a transformer.
This permits the transmission of electric power at high voltages to achieve economy and
distribute the power at utilization voltages.
(ii) A.C motors are cheaper and simpler in construction than the d.c motors.
(iil) A. Ccan be easily converted into d.c by rectifiers.
(iv) Alternating current can be controlled with a choke coil without any appreciable loss of electrical
energy.
(v) The switch gear (e.g. switches, circuit breakers) for a.c system is cheaper than the d.c system.
DISADVANTAGE OF A.C OVER D.C
{i) For the same voltage (same value of voltage), a.c is more dangerous than d.c.
(ii) The shock of a.c is attractive whereas that of d.cis repulsive.
(iii) A.C cannot be used for some processes e.g. electroplating, charging of batteries etc.
(iv) A.Cis transmitted more over the surface of the conductor than from inside. This is called skin
effect.
To avoid skin effect, a.c is transmitted over several fine insulated wires instead of a single thick wire.
WORKED EXAMPLES.
1. A coil of resistance 1009 and inductance 100j1H is connected in series with a 100 pF capacitor. The
circuit is connected to a 10V variable frequency source.
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Gm GE EO Fan ( ( © Silicon atom g . Free electron y. 0 9. P-SEMICONDUCTORS A-P- Semiconductor is made by adding a trivalent atom (an acceptor) such as B or on to pure semi conductor such as germanium. Since there is a production of large number of holes (positive charges) the impure semiconductor is called P- Semiconductor. Cae a 0 a pe ( () ie) Germanium atom 4 f.) fe} Holes ) 0) = (7 Ca (<a> LD Z P-N=JUNCTION/DIODE:
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This is formed when P and N semiconductors are melted to form a junction between them ys N 0 0 0 LM/ es fo} [o} ° or ‘d ba ° ° 1o} ‘A P-N junction The marrow region at the P-n junction which contains the negative and positive charge is called depletion layer. A barrier dip is a p.d which oppose more diffusion of charges across the junction. This is produced when the flow of +ve and -ve Charges ceases P—N JUNCTION AS A RECTIFIER: FORWARD BIAS. Is said to be forward biased when its P- semiconductor is connected to the +ve terminals of the battery and its N- Semi conductors is connected to the -ve terminal at the battery. In this case electrons and holes flow across the P-n junction. This happen because the +ve pole of the battery repel the +ve charge and —Ve pole rel the -ve charges.
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P N b oe li or H \Ey Pe) Co - +e or yt ~~ Or OF ||! +e <0 + H - REVERSE BIAS. A-P-N junction is said to be reverse biased when its P. Semiconductor is connected to the negative pole junction of a battery and N. Semiconductor is connected to the +ve [p:e pf the battery in this case only a very small a current flows. P N +0 +0! 1o> O +0 <0} |O> Or +0 +0! |Or Or = | + P-N JUNCTION AS RECTIFIERS
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Direction of traverse Direction of traverse | _K-— 4 . pd=+E p.d=-E The choice of the direction of the traverse depend on yourself Qa - : In fig given below E=2.0 volts E, = 4.0 volts M=10Q2 1=2.0Q2 713=5Q. What is the current I flowing in the circuit n n Cc 8 ‘aD Ley Solution E, and E are opposing each other but since £2 > E, then Ez must be controlling the direction of current. Applying Kirchhofi"s laws in the clockwise direction we have In, + Ey — Ep + 1% +17, =0 In, + Itz + Ig = Ez — Ey
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10, +m +73) = E,- Ey pe 22 Bs ~ (+n +7) Qa Find the current in each resistor in the circuit shown below: A Lov 7 1s. C al m2 42 32 a ee I F hep a) Take the loop A B E F in the clockwise direction —15+1,+91, — 21, + 10 + (-3h,) =0 10Ly — Sly = § = Dy = Ty = Devens vn owe (A) Take the loop BCDE in clockwise direction. 25-41-91, + 15-1, =0 But! = 1, +1, 41 =4(I, +h) + 25 — 4h, — 41, - 91, +15—1, =0 —141, — 41, = —40 divide by -2 both side Ty + Dy = 20 oe eer ve (2) To solve the equations simultaneously. 71, + 2I, = 20 2h —Ib=1 _ ith =
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: 7 (#) +21, = 20 7+7Iz + 21, = 40 111, = 33 a-yA73 1+3 == a 2 2 1,=2A and I, = 3A Qn. Determine the magnitude of 4s @7d J
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Therefore IP = [pRy ou. .-.(1) similarly 1Q = [pS os uo ue (2) Dividing (1) by (2) gives 1Q=15 1P=hRp at Qs Now since R a C then we have Pa ADandQaDCso P= a Q. be Qn A wire of length 1.1 meter and Radius 7*10~°m is connected across the right gap of the metre bridge when a resistance of 45 Q is introduced in the left gap from a resistance box connected across it- The balance point is obtained 0,6m from left side. Calculate the specific resistance (resistivity) of the material of the wire Solution The value of resistance Formula of resistivity Soe = BA 06 04 Pry 45x04 _ «— 30x 3.14 x(7.0 x 10~*) x6 = 300 od 7 p = 4.2x 10-70m Qn. A 2K2 and 3kQ resistor are connected in series combination is connected across a 100v supply of negligible internal resistance as shown in the figure below:
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3k = 100V Yo R; R (i) What is the output voltage Vout of the load resistance Rx =30k2 (ii) What current resistance through the load resistor R2_ in (i) above. 121.15 Solution The resistance = 2kn + <2 = 52 Vv _ 10x13 Current = 2 == 21.15 Voltage V = = x 21.5] = 57.6V
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