Topics
Units and Measurements
- Quantitative Science
- System of Units
- Derived Quantities and Units
- Rules and Conventions for Writing SI Units and Their Symbols
- Measurement of Length
- Measurement of Mass
- Measurement of Time
- Dimensions and Dimensional Analysis
- Accuracy, Precision and Uncertainty in Measurement
- Errors in Measurements>Systematic Errors
- Errors in Measurements>Random Errors
- Estimation of Errors
- Combination of Errors
- Significant Figures
- Definitions of SI Units and Constants
Mathematical Methods
- Vector Analysis
- Scalar
- Vector
- Vector Operations>Multiplication of a Vector by a Scalar
- Vector Operations>Addition and Subtraction of Vectors
- Vector Operations>Triangle Law for Vector Addition
- Vector Operations>Law of parallelogram of vectors
- Resolution of Vectors
- Multiplication of Vectors
- Scalar Product(Dot Product)
- Vector Product (Cross Product)
- Concept of Calculus
- Differential Calculus
- Integral Calculus
Motion in a Plane
- Concept of Motion
- Rectilinear Motion
- Displacement
- Path Length
- Average Velocity
- Average Speed
- Instantaneous Velocity
- Instantaneous Speed
- Acceleration in Linear Motion
- Relative Velocity
- Motion in Two Dimensions-Motion in a Plane
- Average and Instantaneous Velocities
- Acceleration in a Plane
- Equations of Motion in a Plane with Constant Acceleration
- Relative Velocity in Two Dimensions
- Projectile Motion
- Uniform Circular Motion (UCM)
- Key Parameters of Circular Motion
- Centripetal Acceleration
- Conical Pendulum
Laws of Motion
- Fundamental Principles of Motion and Mechanics
- Types of Motion
- Aristotle’s Fallacy
- Newton’s Laws of Motion
- Newton's First Law of Motion
- Newton’s Second Law of Motion
- Newton's Third Law of Motion
- Inertial and Non-inertial Frames of Reference
- Types of Forces>Fundamental Forces in Nature
- Types of Forces>Contact and Non-Contact Forces
- Types of Forces>Real and Pseudo Forces
- Types of Forces>Conservative and Non-Conservative Forces
- Types of Forces>Work Done by a Variable Force
- Work Energy Theorem
- Principle of Conservation of Linear Momentum
- Collisions
- Elastic and Inelastic Collisions
- Perfectly Inelastic Collision
- Coefficient of Restitution e
- Expressions for Final Velocities in Elastic Head-On Collision
- Loss of Kinetic Energy in Perfectly Inelastic Head-On Collision
- Collision in Two Dimensions
- Impulse of a Force
- Necessity of Defining Impulse
- Rotational Analogue of a Force: Moment of a Force Or Torque
- Couple and Its Torque
- Proof of Independence of the Axis of Rotation
- Mechanical Equilibrium
- States of Equilibrium
- Centre of Mass>Mathematical Understanding of Centre of Mass
- Centre of Mass>Velocity of Centre of Mass
- Centre of Mass>Acceleration of Centre of Mass
- Centre of Mass>Characteristics of Centre of Mass
- Centre of Gravity
Gravitation
- Concept of Gravitation
- Kepler’s Laws
- Law of Orbit or Kepler's First Law
- Law of Areas or Kepler's Second Law
- Law of Periods or Kepler's Third Law
- Newton's Universal Law of Gravitation
- Measurement of the Gravitational Constant (G)
- Acceleration Due to Gravity (Earth’s Gravitational Acceleration)
- Variation in the Acceleration>Variation in Gravity with Altitude
- Variation in the Acceleration>Variation in Gravity with Depth
- Variation in the Acceleration>Variation in Gravity with Latitude and Rotation of the Earth
- Variation in the Acceleration>Effect of the shape of the Earth
- Gravitational Potential Energy
- Expression for Gravitational Potential Energy
- Connection of Potential Energy Formula with mgh
- Potential and Potential Difference
- Escape Velocity
- Earth Satellites
- Projection of Satellite
- Weightlessness in a Satellite
- Time Period of Satellite
- Binding Energy of an Orbiting Satellite
Mechanical Properties of Solids
- Mechanical Properties of Solids
- Elastic Behavior of Solids
- Stress and Strain
- Types of Stress and Corresponding Strain
- Hooke’s Law
- Elastic Modulus>Young’s Modulus
- Elastic Modulus>Bulk Modulus
- Elastic Modulus>Modulus of Rigidity
- Elastic Modulus>Poisson’s Ratio
- Stress-strain Curve
- Strain Energy
- Hardness of Material
- Friction in Solids
- Origin of Friction
- Types of Friction>Static Friction
- Types of Friction>Kinetic Friction
- Types of Friction>Rolling Friction
Thermal Properties of Matter
- Thermal Properties of Matter
- Temperature and Heat
- Measurement of Temperature
- Absolute Zero and Absolute Temperature
- Ideal Gas Equation
- Thermal Expansion
- Linear Expansion
- Areal Expansion
- Volume Expansion
- Relation Between Coefficient of Expansion
- Specific Heat Capacity
- Specific Heat Capacity of Solids and Liquids
- Specific Heat Capacity of Gas
- Heat Equation
- Thermal Capacity
- Calorimetry
- Change of State
- Analysis of Observation>From Point A to B
- Analysis of Observation>From Point B to D
- Temperature Effects and Considerations
- Evaporation vs Boiling
- Boiling Point and Pressure
- Factors Affecting Cooking
- Sublimation
- Phase Diagram
- Gas and Vapour
- Latent Heat
- Heat Transfer
- Conduction
- Thermal Conductivity
- Coefficient of Thermal Conductivity
- Thermal Resistance
- Applications of Thermal conductivity
- Convection
- Application of Convection
- Free and Forced Convection
- Radiation
- Newton’s Law of Cooling
Sound
- Sound Waves
- Common Properties of All Waves
- Transverse Waves
- Longitudinal Waves
- Mathematical Expression of a Wave
- The Speed of Travelling Waves
- The Speed of Transverse Waves
- The Speed of Longitudinal Waves
- Newton's Formula for Velocity of Sound
- Laplace’s Correction
- Factors Affecting Speed of Sound
- Principle of Superposition of Waves
- Echo
- Reverberation
- Acoustics
- Qualities of Sound
- Doppler Effect
- Source Moving and Listener Stationary
- Listener Approaching a Stationary Source with Velocity
- Both Source and Listener are Moving
- Common Properties between Doppler Effect of Sound and Light
- Major Differences between Doppler Effects of Sound and Light
Optics
- Fundamental Concepts of Light
- Nature of Light
- Ray Optics Or Geometrical Optics
- Cartesian Sign Convention
- Reflection>Reflection from a Plane Surface
- Reflection>Reflection from Curved Mirrors
- Total Internal Reflection
- Refraction of Light
- Applications of Total Internal Reflection
- Refraction at a Spherical Surface and Lenses
- Thin Lenses and Their Combination
- Refraction at a Single Spherical Surface
- Lens Makers' Equation
- Dispersion of Light
- Analysis of Prism
- Thin Prisms
- Some Natural Phenomena Due to Sunlight
- Defects of Lenses
- Optical Instruments
- Simple Microscope or a Reading Glass
- Compound Microscope
- Telescope
Electrostatics
- Concept of Electrostatics
- Electric Charge
- Basic Properties of Electric Charge
- Additive Nature of Charge
- Quantization of Charge
- Conservation of Charge
- Force between Charges
- Coulomb’s Law
- Scalar Form of Coulomb’s Law
- Relative Permittivity or Dielectric Constant
- Definition of Unit Charge from the Coulomb’s Law
- Coulomb's Law in Vector Form
- Principle of Superposition
- Electric Field
- Electric Field Intensity Due to a Point-Charge
- Practical Way of Calculating Electric Field
- Electric Lines of Force
- Electric Flux
- Gauss’s Law
- Electric Dipole
- Couple Acting on an Electric Dipole in a Uniform Electric Field
- Electric Intensity at a Point Due to an Electric Dipole
- Continuous Charge Distribution
Electric Current Through Conductors
- Concept of Electric Currents in Conductors
- Electric Current
- Flow of Current Through a Conductor
- Drift Speed
- Ohm's Law
- Limitations of Ohm’s Law
- Electrical Power
- Resistors
- Rheostat
- A combination of resistors in both series and parallel
- Specific Resistance
- Variation of Resistance with Temperature
- Electromotive Force (emf)
- Cells in Series
- Cells in Parallel
- Types of Cells
Magnetism
- Concept of Magnetism
- Magnetic Lines of Force
- The Bar Magnet
- Magnetic Field due to a Bar Magnet
- Magnetic Field Due to a Bar Magnet at an Arbitrary Point
- Gauss' Law of Magnetism
- The Earth’s Magnetism
Electromagnetic Waves and Communication System
- Foundations of Electromagnetic Theory
- EM Wave
- Sources of EM Waves
- Characteristics of EM Waves
- Electromagnetic Spectrum
- Radio Waves
- Microwaves
- Infrared waves
- Visible Light
- Ultraviolet rays
- X-rays
- Gamma Rays
- Propagation of EM Waves
- Ground (surface) Wave
- Space wave
- Sky wave propagation
- Communication System
- Elements of a Communication System
- Commonly Used Terms in Electronic Communication System
- Modulation
Semiconductors
- Concept of Semiconductors
- Electrical Conduction in Solids
- Band Theory of Solids
- Intrinsic Semiconductor
- Extrinsic Semiconductor
- n-type semiconductor
- p-type semiconductor
- Charge neutrality of extrinsic semiconductors
- p-n Junction
- A p-n Junction Diode
- Basics of Semiconductor Devices
- Applications of Semiconductors and P-n Junction Diode
- Thermistor
- Introduction
- Definition: Acceleration Due to Gravity
- Formula: Acceleration Due to Gravity
- Characteristics
- Derivation and Calculation
- Change along the Surface of the Earth
- Example 1
- Example 2
- Real-Life Examples
Introduction
- The Earth exerts a gravitational force on all objects near its surface.
- According to Newton's Second Law of Motion (F = ma), this force causes a body to accelerate.
- This specific acceleration caused by the Earth's gravity is called acceleration due to gravity.
- It is a vector quantity, denoted by the letter 'g', and is always directed vertically downwards towards the Earth's center.
Definition: Acceleration Due to Gravity
The gravitational force due to the earth on a body results in its acceleration. This is called acceleration due to gravity and is denoted by ‘g’.
Formula: Acceleration due to gravity
The value of the acceleration due to gravity (g) on the surface of the Earth is given by the formula:
Where:
- g = Acceleration due to gravity (in m/s²).
- G = Newton's Universal Gravitational Constant (≈ 6.67 × 10⁻¹¹ N · m² / kg²).
- M = Mass of the Earth (≈ 6 × 1024 kg).
- R = Radius of the Earth (≈ 6.4 × 10⁶ m).
Characteristics
Direction: Always directed towards the center of the Earth (vertically downwards).
Independence: The value of g at a given point does not depend on the properties or mass (m) of the object being attracted.
Variability: The value of g is not constant and varies with:
- Location (latitude) on the Earth's surface.
- Height (altitude) above the surface.
- Depth below the surface.
Highest/Lowest Value: Highest at the poles (≈ 9.832 m /s2) and lowest at the equator (≈ 9.78 m/s²).
Derivation and Calculation
The acceleration due to gravity (g) is derived by equating the general gravitational force and the force from Newton's Second Law.
- Gravitational Force (F): According to Newton's Universal Law of Gravitation, the force between the Earth (Mass M) and an object (Mass m) at a distance r from the Earth's center is:
\[F = \frac{G M m}{r^2} \quad \text{.........(1)}\] - Newton's Second Law Force (F): The force causing the object's acceleration (g) is:
\[F = m g \quad \text{.........(2)}\] - Equating (1) and (2):
\[m g = \frac{G M m}{r^2}\] - Solving for g: The mass of the object (m) cancels out:
\[g = \frac{G M}{r^2} \quad \text{.........(3)}\] - On the Surface: If the object is on the Earth's surface, the distance r equals the Earth's radius R, leading to the final surface value formula:
\[g = \frac{G M}{R^2} \quad \text{.........(4)}\]
Change along the Surface of the Earth
- The Earth is flatter at the poles and bulges at the equator.
- The radius (R) is largest at the equator and smallest at the poles.
- Since g is inversely proportional to R2, a smaller radius at the poles means a higher value of g (highest at the poles), and a larger radius at the equator means a lower value of g (lowest at the equator).
Example 1
Aim: To calculate the mass of the Earth (ME) using the acceleration due to gravity (g).
Given Data:
- Acceleration due to gravity, g = 9.81 m/s²
- Radius of the Earth, RE = 6.37 × 10⁶ m
- Universal Gravitational Constant, G = 6.67 × 10⁻¹¹ N · m² /kg²
Steps:
- Start with the formula for g on the surface:
\[g = \frac{G M_E}{R_E^2}\] - Rearrange the formula to solve for ME:
\[M_E = \frac{g R_E^2}{G}\] - Substitute the given values into the equation:
\[M_E = \frac{9.81 \times (6.37 \times 10^6)^2}{6.67 \times 10^{-11}}\] - Calculate the result:
\[M_E = 5.97 \times 10^{24} \text{ kg}\]
Result: The calculated mass of the Earth is 5.97 × 1024 kg.
Example 2
Aim: To calculate the acceleration due to gravity on the Moon's surface (gm).
Given Data (relative to Earth):
- Mass of the Moon (Mm) = M/80 (where M is Earth's mass).
- Radius of the Moon (Rm) = R/4 (where R is Earth's radius).
- Acceleration due to gravity on Earth, g = 9.8 m/s².
Steps:
- Write the formulas for g on Earth and gm on the Moon:
\[g = \frac{G M}{R^2} \quad \text{...(1)}\]
\[g_m = \frac{G M_m}{R_m^2} \quad \text{...(2)}\] - Find the ratio \[\frac {g_m}{g}\]:
\[\frac{g_m}{g} = \frac{M_m}{M} \times \left(\frac{R}{R_m}\right)^2\] - Substitute the given ratios:
\[\frac{g_m}{g} = \frac{1}{80} \times \left(\frac{4}{1}\right)^2\] - Simplify:
\[\frac{g_m}{g} = \frac{1}{80} \times 16 = \frac{16}{80} = \frac{1}{5}\] - Solve for gm:
\[g_m = \frac{g}{5} = \frac{9.8}{5}\] - Calculate the result:
\[g_m = 1.96 \text{ m/s}^2\]
Result: The acceleration due to gravity on the Moon's surface is 1.96 m/s² (about 1/5th of Earth's value).
Real-Life Examples
- Weight on the Moon: You weigh 1/6 as much on the Moon because gravity there is weaker than on Earth.
- Dropping Objects: A small rock and a heavy ball fall at the same speed (without air) — gravity doesn’t depend on mass.
- Tidal Forces: Tides happen because the Moon pulls harder on the side of Earth closest to it, causing water to bulge.
- Satellite Orbits: Satellites need to be at the right height where gravity keeps them in orbit — not falling or flying away.

