Topics
Units and Measurements
- Quantitative Science
- System of Units
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- Rules and Conventions for Writing SI Units and Their Symbols
- Measurement of Length
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- 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
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- 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
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- 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: Centripetal Force
- Formula: Centripetal Force
- Formula: Centripetal Acceleration
- Characteristics
- Derivation
- Application to Planetary Motion
- Significance
- Experiment
- Example 1
- Example 2
- Real-Life Examples
Introduction
Circular motion is a type of motion where an object moves along a circular path. When you tie a stone to a string and rotate it, the stone moves in a circle. For this motion to happen, a force must act on the object continuously. This force is always directed towards the centre of the circle. Without this force, the object would move in a straight line. This special type of force is called centripetal force, which means "centre-seeking."
Definition: Centripetal Force
A force that acts on any object moving along a circle and is directed towards the centre of the circle. When this force stops acting, the object flies off along a straight line (tangent to the circle) in the direction of its velocity at that instant.
Formula: Centripetal Force
F = \[m\omega^{2}r=\frac{mv^{2}}{r}\] = mωv
where:
- F = Centripetal force (in Newtons)
- m = Mass of the object (in kg)
- ω = Angular speed (in rad/s)
- r = Radius of the circular path (in m)
- v = Linear speed or tangential velocity (in m/s)
Formula: Centripetal Acceleration
a = ω2r = \[\frac {v^2}{r}\] = ωv
where:
-
a = Centripetal acceleration (in m/s²)
Characteristics
- The centripetal force is always directed towards the centre of the circle
- It is perpendicular to the velocity of the object
- The velocity is always tangential to the circular path
- The magnitude of velocity remains constant in uniform circular motion, but its direction continuously changes
- The centripetal force is not a separate external force; it is the resultant of the actual forces acting on the object
- If the centripetal force stops acting, the object moves in a straight line along the tangent to the circle
Derivation
For a particle moving in uniform circular motion with radius r and angular speed ω:
Position Vector:
\[\vec{r}=(r\cos[\omega t])\hat{i}+(r\sin[\omega t])\hat{j}\]
Velocity Vector (first derivative of position):
\[\vec{v}=\frac{d\vec{r}}{dt}=r\omega(-\sin[\omega t]\hat{i}+\cos[\omega t]\hat{j})\]
Acceleration Vector (derivative of velocity):
\[\vec{a}=\frac{d\vec{v}}{dt}=-\omega^2(r\cos[\omega t]\hat{i}+r\sin[\omega t]\hat{j})=-\omega^2\vec{r}\]
The negative sign shows that the acceleration is opposite to the position vector, meaning it points towards the centre of the circle.
Magnitude of Centripetal Acceleration:
a = ω2r = \[\frac {v^2}{r}\] = ωv
Centripetal Force (using Newton's Second Law):
\[\vec{F}=m\vec{a}=-m\omega^2\vec{r}\]
Magnitude of Centripetal Force:
\[F=m\omega^2r=\frac{mv^2}{r}=m\omega v\]
Application to Planetary Motion
The Moon revolves around the Earth in a definite orbit. During this motion:
- The direction of the Moon's motion constantly changes
- The speed of the Moon remains constant, but its velocity direction changes
- The Earth exerts a gravitational force on the Moon that is directed towards the Earth's centre
- This gravitational force acts as the centripetal force for the Moon's circular motion
- Similarly, the Sun attracts all planets, including Earth, towards itself, providing the centripetal force for their orbital motion

Significance
- Centripetal force is essential for any circular motion to occur
- It explains why objects don't fly off when moving in circles
- Understanding centripetal force helps explain planetary motions and satellite orbits
- It is used in designing circular tracks for vehicles (banking of roads)
- Important in understanding the motion of electrons around the nucleus in atoms
- Critical in understanding the dynamics of rotating machinery and equipment
- Helps explain natural phenomena like the motion of celestial bodies
Experiment
Aim:
To demonstrate that a centripetal force directed towards the centre is required to keep an object moving in a circular path.
Requirements:
- A stone or a small weight
- A string
- Your hand (to hold and rotate the string)
- A circular space to perform the rotation
Procedure
- Tie the stone to one end of the string
- Hold the other end of the string in your hand
- Rotate the string so that the stone moves along a circular path
- Observe the direction in which you are pulling the string
- Continue rotating the stone in a steady circular motion
- Suddenly release the string.

A stone tied to a string, moving along a circular path, and its velocity in the tangential direction
Observation
- As you rotate the string, you continuously pull the stone towards the centre of the circle
- The stone moves in a circular path as long as you hold and rotate the string
- When you release the string, the stone immediately flies off
- The stone does not continue moving in a circle; instead, it moves in a straight line
- The direction of the stone's straight-line motion is tangent to the circle at the point of release
Conclusion:
A force is acting on the stone continuously, directed towards the centre of the circle. This force is called the centripetal force. When the centripetal force stops acting (the string is released), the stone moves in a straight line (tangent to the circle) because that is the direction of its velocity at that instant. This proves that centripetal force is necessary to maintain circular motion
Example 1
Problem: An object of mass 50 g moves uniformly along a circular orbit with an angular speed of 5 rad/s. If the linear speed of the particle is 25 m/s, what is the radius of the circle? Calculate the centripetal force acting on the particle.
Solution:
- Mass (m) = 50 g = 0.05 kg
- Angular speed (ω) = 5 rad/s
- Linear speed (v) = 25 m/s
- Radius (r) =?
- Centripetal force (F) = ?
Find the radius using the relationship between linear and angular speed
v = ωr
r = \[\frac {v}{ω}\] = \[\frac {25}{5}\] = 5 m
Calculate centripetal force using the formula
F = \[\frac{mv^{2}}{r}\]
F = \[\frac{0.05\times25\times25}{5}\] = 6.25 N
Answer: The radius of the circle is 5 m, and the centripetal force acting on the particle is 6.25 N.
Example 2
Problem: An object is travelling in a horizontal circle with uniform speed. At t = 0, the velocity is \[\vec u\] = 20\[\hat i\] + 35\[\hat j\] km/s. After one minute the velocity becomes \[\vec v\] = −20\[\hat i\] − 35\[\hat j\] km/s. What is the magnitude of the acceleration?
Solution:
Find the magnitude of initial velocity
u = \[\sqrt{(20)^2+(35)^2}=\sqrt{400+1225}=\sqrt{1625}\] = 40.3 m/s
Observe that the velocity has reversed direction
Since the velocity has changed from \[\vec u\] to −\[\vec u\], the object has completed half a circle.
Determine the time period of revolution
If the object completes half a circle in 1 minute, then the full period T = 2 minutes = 120 seconds.
Find the radius using the relationship
T = \[\frac {2πr}{u}\]
r = \[\frac {uT}{2π}\]
Calculate centripetal acceleration
a = \[\frac{u^2}{r}=\frac{u^2\times2\pi}{uT}=\frac{2\pi u}{T}\]
a = \[\frac{2\times3.14\times40.3}{120}\] = 2.11 m/s²
Answer: The magnitude of the acceleration is 2.11 m/s².
Real-Life Examples
- Vehicles on Circular Tracks: When a car moves on a circular road, friction between the tyres and the road provides the centripetal force to keep the car moving in a circle
- Planetary Motion: All planets, including Earth, revolve around the Sun. The gravitational force from the Sun provides the centripetal force
- Moon's Orbit: The Moon revolves around Earth due to Earth's gravitational force acting as a centripetal force
- Spinning Coin: A coin on a rotating circular disk flies off tangentially when the disk rotates fast enough because the friction force (centripetal force) becomes insufficient
- Merry-Go-Round: When you sit on a rotating merry-go-round, the seat exerts a force towards the centre that keeps you moving in a circle
- Electron Motion: Electrons moving around the nucleus experience centripetal force due to the electric attraction of the nucleus
