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
- Specific Heat Capacity of Solids and Liquids
- Relation Between Coefficient of Expansion
- 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
- Evaporation vs Boiling
- Boiling Point and Pressure
- 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
- Formula: Average Acceleration
- Formula: Instantaneous Acceleration
- Characteristics
- Graphical Interpretation
- Equations of Motion
- Significance
- Illustrative Example
- Example
- Real-Life Examples
Introduction
Acceleration describes how quickly the velocity of an object changes with time. It is a vector quantity, meaning it has both magnitude and direction. The dimensions of acceleration are [L¹ M⁰ T⁻²]. Understanding acceleration is essential for analyzing motion, especially when objects speed up, slow down, or change direction. This concept is fundamental in physics and helps explain everyday phenomena like falling objects and moving vehicles.
Definition: Acceleration
Acceleration is defined as the rate of change of velocity with time.
Formula: Average Acceleration
Average acceleration is calculated when an object has velocities \[\vec v_1\] and \[\vec v_2\] at times t1 and t2:
\[\vec{a}=\frac{\vec{v_2}-\vec{v_1}}{t_2-t_1}\]
where:
- \[\vec a\] = average acceleration
- \[\vec v_1\] = velocity at time t1
- \[\vec v_2\] = velocity at time t2
Formula: Instantaneous Acceleration
Instantaneous acceleration is the limiting value of average acceleration when the time interval approaches zero:
\[\vec{a}=\lim_{\Delta t\to0}\frac{\Delta\vec{v}}{\Delta t}=\frac{d\vec{v}}{dt}\]
where:
- \[\vec a\] = instantaneous acceleration
- \[d\vec{v}\] = infinitesimal change in velocity
- dt = infinitesimal change in time
The instantaneous acceleration at a given time equals the slope of the tangent to the velocity versus time curve at that time.
Characteristics
- Vector quantity (has both magnitude and direction)
- Dimensions: [L¹ M⁰ T⁻²]
- Can be positive (velocity increasing) or negative (velocity decreasing)
- Can be uniform (constant) or nonuniform (changing)
- Measured as a change in velocity per unit time
- For uniform acceleration, the velocity-time graph is linear
- For nonuniform acceleration, the velocity-time graph is nonlinear
Graphical Interpretation
Case (a): Zero acceleration (Constant Velocity)
- Horizontal line on v-t graph
- Velocity remains constant
- Shaded area under graph = displacement = v0(t2 − t1)

Object moving with constant velocity.
Case (b): Positive Uniform Acceleration
- Straight line sloping upward
- The magnitude of velocity increases uniformly with time
- Area under the curve = displacement

Object moving with velocity (v) along +ve x-axis with uniform acceleration along the same direction.
Case (c): Negative Uniform Acceleration
- Straight line sloping downward
- Acceleration opposite to the velocity direction
- Velocity decreases uniformly with time
- Area under the curve = displacement

Object moving with velocity (v) with negative uniform acceleration.
Case (d): Nonuniform Acceleration
- Curved line on v-t graph
- Acceleration changes with time
- Average acceleration shown by a straight line
- Instantaneous acceleration = slope of tangent at that point

Object moving with nonuniform acceleration.
Displacement from the Velocity-Time Graph
The area under the velocity-time curve represents displacement:
Area = \[\int_{t_1}^{t_2}vdt=\int_{t_1}^{t_2}\frac{dx}{dt}dt=\int_{t_1}^{t_2}dx=x(t_2)-x(t_1)\]
This equals the displacement of the object from t1 to t2.
Equations of Motion
Consider an object at position x = 0 at time t = 0, with initial velocity u and final velocity v at time t.

Derivation of the equation of motion for motion with uniform acceleration.
First Equation:
Acceleration = slope of the velocity-time line
a = \[\frac{v-u}{t-0}=\frac{v-u}{t}\]
v = u + at
Second Equation:
Displacement = area under v-t graph = area of triangle + area of rectangle
s = \[\frac {1}{2}\](v − u)t + ut
Using the first equation:
s = ut + \[\frac {1}{2}\]at2
Third Equation:
Using average velocity:
s = \[v_{av}\cdot t=\frac{v+u}{2}\cdot t=\frac{(v+u)(v-u)}{2a}\]
s = \[\frac{v^2-u^2}{2a}\]
v2 − u2 = 2as
Significance
- Helps analyze the motion of objects that speed up or slow down
- Essential for understanding velocity-time graphs
- Area under the v-t curve gives displacement directly
- The slope of the v-t curve gives the acceleration value
- Enables calculation of motion parameters using three equations
- Applies to real-world situations like free fall
- Foundation for understanding forces and dynamics
- Critical for solving practical motion problems
Illustrative Example
Free Fall
- The most common example of uniform rectilinear motion with uniform acceleration.
- The body falls under Earth's gravity with zero initial velocity.
- Air resistance is negligible for small displacements.
- Acceleration due to gravity acts along the vertical direction.
- Assumed constant over distances small compared to Earth's radius.
- Velocity and acceleration are both along the vertical direction.
Example
Problem
A stone is thrown vertically upward from the ground with a velocity of 15 m/s. Simultaneously, a ball is dropped from rest from a height of 30 m above. Using g = 10 m/s2, find (i) how long until they meet, and (ii) the height above ground where they meet.
Solution step‑by‑step
- Step 1: Set up equations
Both objects move for the same time t0. Using s = ut + \[\frac {1}{2}\] gt2:
For stone (moving upward):
sstone = 15t0 − \[\frac {1}{2}\](10)t02 = 15t0 − 5t02For ball (falling downward):
sball = \[\frac {1}{2}\](10)t02 = 5t02 - Step 2: Apply the condition
When they meet, the total distance = 30 m:
sstone + sball = 3015t0 − 5t02 + 5t02 = 3015t0 = 30t0 = 2 seconds - Step 3: Find meeting height
Distance traveled by the stone in 2 seconds:
sstone = 15(2) − 5(2)2 = 30 − 20 = 10 m
Answer:
- Time of meeting = 2 seconds
- Height from ground = 10 meters
Real-Life Examples
Vehicle Motion
- A car accelerating from rest at a traffic signal shows positive acceleration
- Applying the brakes causes negative acceleration (deceleration)
- Racing cars demonstrate high positive acceleration during starts
Sports Applications
- A cricket ball thrown vertically upward experiences negative acceleration due to gravity
- An athlete sprinting from the starting blocks shows positive acceleration
- A football kicked upward slows down due to gravitational acceleration
Elevator Motion
- Starting upward from the ground floor shows positive acceleration
- Stopping at a floor demonstrates negative acceleration
- Passengers feel changes in acceleration as weight changes
Amusement Park Rides
- Roller coasters experience varying acceleration through loops and drops
- Free-fall rides demonstrate near-constant gravitational acceleration

