NEET Ug . NEET Physics . Physics . Gravitation
Chapter 8: Gravitation
Ch 8
NEET Physics
NEET Ug
Introduction
Historical Background
Nicolaus Copernicus (1473–1543): Proposed heliocentric model with planets moving in circular orbits around the Sun.
Galileo Galilei: Supported Copernicus; faced prosecution for his beliefs.
Tycho Brahe (1546–1601): Made precise naked-eye planetary observations.
Johannes Kepler (1571–1640): Derived three laws of planetary motion from Brahe's data.
Isaac Newton: Used Kepler's laws to formulate universal law of gravitation.
Solved Examples
Ex 1
Identify the scientist who proposed elliptical orbits: Kepler.
State the law that relates period and orbit size: Kepler's Third Law.
Practice Set
Q1: Who proposed that planets move in elliptical orbits?
A. Newton
B. Copernicus
C. Kepler
D. GalileoQ2: Which scientist compiled precise planetary data with naked eye?
A. Kepler
B. Brahe
C. Newton
D. CopernicusQ3: Newton used data from which scientist to propose universal gravitation?
A. Galileo
B. Brahe
C. Kepler
D. Copernicus
Answer Key
Q1: C - Kepler formulated elliptical orbits.
Q2: B - Tycho Brahe made detailed observations.
Q3: C - Newton used Kepler's laws for gravitation.
Memory Aids
Copernicus: Circle model
Kepler: Elliptical orbits + 3 laws
Brahe: Data collector
Newton: Gravity from Kepler's laws
Kepler's Laws
Law of Orbits
Planets move in elliptical orbits.
Sun is at one focus of ellipse.
Law of Areas
Line joining planet and Sun sweeps equal areas in equal times.
Area swept in small time \( \Delta t \): \( \Delta A = \frac{1}{2} r v \Delta t \)
Vector form: \( \Delta \vec{A} = \frac{1}{2} (\vec{r} \times \vec{v} \Delta t) \)
Rate of area swept: \( \frac{\Delta \vec{A}}{\Delta t} = \frac{1}{2} (\vec{r} \times \vec{v}) \)
Using momentum \( \vec{p} = m \vec{v} \): \( \frac{\Delta \vec{A}}{\Delta t} = \frac{\vec{L}}{2m} \) where \( \vec{L} = \vec{r} \times \vec{p} \) is angular momentum.
Angular momentum \( \vec{L} \) is constant for central force → area rate constant.

Law of Periods
Square of orbital period \( T \) is proportional to cube of semi-major axis \( R \):
\( T^2 \propto R^3 \)
Solved Examples
Ex 1
Calculate area swept in 10 s if \( r = 1.5 \times 10^{11} \) m, \( v = 3 \times 10^4 \) m/s.
\( \Delta A = \frac{1}{2} r v \Delta t = 0.5 \times 1.5 \times 10^{11} \times 3 \times 10^4 \times 10 = 2.25 \times 10^{16} \, m^2 \)
Ex 2
If Earth's orbital radius is \( 1.5 \times 10^{11} \) m and period is 1 year, find period for a planet at \( 2.25 \times 10^{11} \) m.
Using \( T^2 \propto R^3 \):
\( \frac{T_2^2}{T_1^2} = \left( \frac{R_2}{R_1} \right)^3 = \left( \frac{2.25}{1.5} \right)^3 = (1.5)^3 = 3.375 \)
\( T_2 = T_1 \sqrt{3.375} = 1 \times 1.837 = 1.837 \) years
Practice Set
Q1: According to Kepler's second law, the area swept by the radius vector in equal time intervals is:
A. Increasing
B. Decreasing
C. Constant
D. ZeroQ2: The angular momentum of a planet about the Sun is:
A. Increasing
B. Decreasing
C. Constant
D. ZeroQ3: If the semi-major axis of a planet's orbit is doubled, its orbital period becomes:
A. Double
B. Four times
C. \( 2\sqrt{2} \) times
D. \( 2\sqrt{8} \) times
Answer Key
Q1: C - Equal areas in equal times means constant area sweep rate.
Q2: C - Angular momentum is conserved under central force.
Q3: D - \( T^2 \propto R^3 \) so \( T = R^{3/2} \). Doubling R: \( T_2 = 2^{3/2} T_1 = 2\sqrt{2} T_1 \).
Memory Aids
Law 1: Ellipse with Sun at focus
Law 2: Equal areas in equal times → constant angular momentum
Law 3: Period squared ∝ radius cubed
Formula: \( \Delta A = \frac{1}{2} r v \Delta t \)
Universal Law of Gravitation
Newton's Law
Every particle attracts every other particle.
Force \( F \) is proportional to product of masses \( m_1, m_2 \).
Force inversely proportional to square of distance \( r \) between them.
Mathematically, \( F = \dfrac{G m_1 m_2}{r^2} \), where \( G \) is universal gravitational constant.
Characteristics of Gravitational Force
Always attractive, acts along line joining particles.
Equal and opposite forces on both masses (action-reaction pair): \( \vec{F}_1 = -\vec{F}_2 \).
Independent of medium between particles.
Valid for all distances: interatomic to interplanetary.
Conservative force: work done depends only on initial and final positions.
No work done in closed path motion.
Vector form: \( \vec{F} = -G \dfrac{m_1 m_2}{r^2} \hat{r} = -G \dfrac{m_1 m_2}{|\vec{r}|^3} \vec{r} \).

Solved Examples
Ex 1
Find force between two masses \( m_1 = 5\,kg \) and \( m_2 = 10\,kg \) separated by \( r = 2\,m \).
Use \( G = 6.67 \times 10^{-11} \; N m^2/kg^2 \).
\( F = \dfrac{6.67 \times 10^{-11} \times 5 \times 10}{2^2} = 8.34 \times 10^{-10} \; N \).
Practice Set
Q1
What is the direction of gravitational force between two masses?
A) Repulsive along line joining masses
B) Attractive along line joining masses
C) Perpendicular to line joining masses
D) Zero
Q2
Two masses \( m_1 = 3\,kg \) and \( m_2 = 6\,kg \) are 4 m apart. Calculate gravitational force. (Use \( G = 6.67 \times 10^{-11} \))
A) \(7.5 \times 10^{-11} N\)
B) \(3.0 \times 10^{-10} N\)
C) \(7.5 \times 10^{-10} N\)
D) \(1.0 \times 10^{-9} N\)
Q3
If distance between two masses is halved, gravitational force becomes?
A) Halved
B) Doubled
C) Quadrupled
D) Quartered
Answer Key
Q1: B - Gravitational force is always attractive along the line joining the masses.
Q2: C - \( F = \dfrac{6.67 \times 10^{-11} \times 3 \times 6}{4^2} = 7.5 \times 10^{-11} \times 3 = 7.5 \times 10^{-10} N \).
Q3: C - Force varies inversely as square of distance, halving distance increases force by 4 times.
Memory Aids
Force \( \propto m_1 m_2 / r^2 \).
Always attractive, acts along line joining masses.
Action = Reaction (equal & opposite forces).
Halving distance quadruples force.
Gravitational Force Vector Sum
Force on Multiple Masses
Force on a mass due to several masses is vector sum of individual forces.
For mass \( m_1 \), total force \( \vec{F}_1 = \sum \dfrac{G m_i m_1}{r_{i1}^2} \hat{r}_{i1} \).
Unit vector \( \hat{r}_{i1} \) points from \( m_1 \) to \( m_i \).
Direction of force is attractive towards other masses.

Solved Examples
Ex 1
Calculate net gravitational force on \( m_1 \) due to \( m_2, m_3, m_4 \) given their masses and distances.
Calculate each force using \( F = \dfrac{G m_i m_1}{r_{i1}^2} \) and add vectorially.
Practice Set
Q1
Force on \( m_1 \) due to \( m_2 \) is \( F_{12} \). What is force on \( m_2 \) due to \( m_1 \)?
A) \( F_{12} \)
B) \( -F_{12} \)
C) Zero
D) Depends on distance
Q2
Net force on \( m_1 \) due to \( m_2 \) and \( m_3 \) is vector sum of individual forces. This is an example of?
A) Scalar addition
B) Vector addition
C) No addition
D) None
Q3
If \( m_2 = m_3 = m \), distances \( r_{21} = r_{31} = r \), and forces \( \vec{F}_{12} \) and \( \vec{F}_{13} \) are perpendicular, magnitude of net force on \( m_1 \) is?
A) \( 2 \dfrac{G m m_1}{r^2} \)
B) \( \sqrt{2} \dfrac{G m m_1}{r^2} \)
C) \( \dfrac{G m m_1}{r^2} \)
D) Zero
Answer Key
Q1: B - Forces are equal in magnitude and opposite in direction (Newton's third law).
Q2: B - Gravitational forces add vectorially.
Q3: B - Net force is vector sum: \( \sqrt{F^2 + F^2} = \sqrt{2} F \).
Memory Aids
Net force = vector sum of individual gravitational forces.
Action-reaction forces are equal and opposite.
Use Pythagoras for perpendicular force vectors.
Gravitational Constant
Definition and Discovery
Gravitational constant \( G \) quantifies the strength of gravity between two masses.
First measured by Henry Cavendish in 1798 using a torsion balance experiment.
Cavendish Experiment Setup
Two small masses \( m \) fixed at ends A and B of a light rod, rotating about a vertical axis at the center.
Two large spheres \( S_1 \) and \( S_2 \) placed near the small masses exert gravitational force.
When large spheres are moved to opposite sides (positions \( S'_1 \) and \( S'_2 \)), the rod rotates due to torque change.
Angle of rotation \( \theta \) is measured to calculate \( G \).

Equilibrium Condition and Formula
At equilibrium, gravitational torque equals restoring torque from the wire.
Torque due to gravity: \( \tau_g = G \frac{Mm}{r^2} L \)
Restoring torque: \( \tau_r = k \theta \), where \( k \) is torsion constant, \( \theta \) is angle of twist.
Equating: \( G \frac{Mm}{r^2} L = k \theta \)
Rearranged formula for \( G \): \( G = \frac{k \theta r^2}{M m L} \)
\( r \): distance between centers of large and small spheres; \( L \): length of the rod.
Accepted Value
Current accepted value: \( G = 6.67 \times 10^{-11} \text{ N m}^2/\text{kg}^2 \)
Solved Examples
Ex 1
Given: \( k = 2 \times 10^{-6} \text{ Nm/rad} \), \( \theta = 0.01 \text{ rad} \), \( r = 0.05 \text{ m} \), \( M = 1.0 \text{ kg} \), \( m = 0.01 \text{ kg} \), \( L = 0.4 \text{ m} \).
Calculate \( G \): \( G = \frac{2 \times 10^{-6} \times 0.01 \times (0.05)^2}{1.0 \times 0.01 \times 0.4} = 1.25 \times 10^{-11} \text{ N m}^2/\text{kg}^2 \).
Practice Set
Q1
In Cavendish's experiment, the torque due to gravitational force is balanced by:
A) Magnetic torque
B) Restoring torque of the wire
C) Frictional torque
D) Centrifugal torque
Q2
Which of the following is the correct formula for \( G \) in Cavendish's experiment?
A) \( G = \frac{k \theta r^2}{M m L} \)
B) \( G = \frac{M m L}{k \theta r^2} \)
C) \( G = \frac{k \theta M m}{r^2 L} \)
D) \( G = \frac{k r^2}{\theta M m L} \)
Q3
In an experiment, \( k = 3 \times 10^{-6} \text{ Nm/rad} \), \( \theta = 0.02 \text{ rad} \), \( r = 0.04 \text{ m} \), \( M = 2 \text{ kg} \), \( m = 0.02 \text{ kg} \), \( L = 0.5 \text{ m} \). Calculate \( G \).
A) \( 4.8 \times 10^{-11} \text{ N m}^2/\text{kg}^2 \)
B) \( 1.92 \times 10^{-10} \text{ N m}^2/\text{kg}^2 \)
C) \( 9.6 \times 10^{-11} \text{ N m}^2/\text{kg}^2 \)
D) \( 3.84 \times 10^{-11} \text{ N m}^2/\text{kg}^2 \)
Answer Key
Q1: B) Restoring torque of the wire — It balances gravitational torque at equilibrium.
Q2: A) \( G = \frac{k \theta r^2}{M m L} \) — Correct rearranged formula from torque balance.
Q3: D) \( 3.84 \times 10^{-11} \text{ N m}^2/\text{kg}^2 \) — Calculated using given values in formula.
Memory Aids
Remember: \( G \) relates torque balance: gravitational torque = restoring torque.
Formula cue: \( G = \frac{k \theta r^2}{M m L} \) — torsion constant × angle × distance squared over masses and rod length.
Value of \( G \) is very small (~10⁻¹¹), indicating weak gravitational force.
Acceleration due to Gravity
Concepts
Acceleration due to gravity (\( g \)) is the acceleration produced in a body falling freely under Earth's gravity.
At Earth's surface, \( g = 9.8\, \mathrm{m/s^2} \).
Gravitational force between Earth (mass \( M_E \)) and a body (mass \( m \)) at distance \( R_E \) (Earth's radius) is \( F = \frac{G M_E m}{R_E^2} \).
Weight of the body: \( W = mg \).
Equating weight and gravitational force: \( mg = \frac{G M_E m}{R_E^2} \Rightarrow g = \frac{G M_E}{R_E^2} \).
Numerical value: \( g = \frac{6.67 \times 10^{-11} \times 6 \times 10^{24}}{(6400 \times 10^3)^2} = 9.8\, \mathrm{m/s^2} \).

Solved Examples
Ex 1: Calculate \( g \) using \( G = 6.67 \times 10^{-11} \mathrm{Nm^2/kg^2} \), \( M_E = 6 \times 10^{24} \mathrm{kg} \), \( R_E = 6400 \times 10^3 \mathrm{m} \).
Use formula: \( g = \frac{G M_E}{R_E^2} \).
Substitute values and compute \( g = 9.8\, \mathrm{m/s^2} \).
Practice Set
Q1: What is the acceleration due to gravity on Earth's surface?
A) 9.8 m/s²
B) 10 m/s²
C) 9.2 m/s²
D) 8.9 m/s²
Q2: If Earth's mass doubles and radius remains the same, what happens to \( g \)?
A) Doubles
B) Halves
C) Remains same
D) Quadruples
Q3: Calculate \( g \) on a planet with mass \( 3 \times 10^{24} \mathrm{kg} \) and radius \( 4 \times 10^6 \mathrm{m} \).
A) 12.5 m/s²
B) 10.5 m/s²
C) 8.3 m/s²
D) 15.0 m/s²
Answer Key
Q1: A) 9.8 m/s² — Standard acceleration due to gravity on Earth.
Q2: A) Doubles — \( g \) is directly proportional to mass \( M_E \).
Q3: C) 8.3 m/s² — Using \( g = \frac{GM}{R^2} \), substitute values to calculate.
Memory Aids
Formula: \( g = \frac{GM_E}{R_E^2} \).
Remember: \( g \) depends on Earth's mass and radius.
Standard \( g = 9.8\, \mathrm{m/s^2} \) at surface.
Relationship between g and G
Concepts
Earth's mass: \( M_E = \frac{4}{3} \pi R_E^3 \rho \), where \( \rho \) is Earth's density.
Substitute in \( g = \frac{G M_E}{R_E^2} \):
\( g = G \frac{4}{3} \pi R_E^3 \rho / R_E^2 = \frac{4}{3} \pi G R_E \rho \).
Shows \( g \) depends on gravitational constant \( G \), Earth's radius \( R_E \), and density \( \rho \).
Solved Examples
Ex 1: Calculate \( g \) if \( R_E = 6.4 \times 10^6 \mathrm{m} \), \( \rho = 5500 \mathrm{kg/m^3} \), \( G = 6.67 \times 10^{-11} \mathrm{Nm^2/kg^2} \).
Use formula: \( g = \frac{4}{3} \pi G R_E \rho \).
Calculate \( g \approx 9.8\, \mathrm{m/s^2} \).
Practice Set
Q1: Which factor does NOT affect \( g \)?
A) Earth's radius
B) Earth's density
C) Gravitational constant \( G \)
D) Mass of the falling object
Q2: If Earth's density doubles, what happens to \( g \)?
A) Doubles
B) Halves
C) Remains same
D) Quadruples
Q3: Express \( g \) in terms of \( G, R_E, \) and \( \rho \).
A) \( g = G R_E \rho \)
B) \( g = \frac{4}{3} \pi G R_E \rho \)
C) \( g = \frac{G \rho}{R_E} \)
D) \( g = \frac{4}{3} \pi G \rho / R_E \)
Answer Key
Q1: D) Mass of the falling object — \( g \) is independent of falling object's mass.
Q2: A) Doubles — \( g \) is directly proportional to density \( \rho \).
Q3: B) \( g = \frac{4}{3} \pi G R_E \rho \) — Derived formula.
Memory Aids
Formula: \( g = \frac{4}{3} \pi G R_E \rho \).
Think: \( g \) depends on Earth's size and density.
Density increase → \( g \) increase.
Gravitational Field
Concepts
Gravitational field: Space around a mass where its gravitational pull is felt.
Field intensity (\( E \)) at a point: Force per unit mass placed at that point.
Formula: \( E = - \frac{GM}{r^2} \), where \( M \) is mass, \( r \) is distance from center.
Negative sign indicates attractive nature of gravity.
Solved Examples
Ex 1: Calculate gravitational field intensity \( E \) at \( 10^7 \mathrm{m} \) from mass \( 5 \times 10^{24} \mathrm{kg} \).
Use \( E = - \frac{GM}{r^2} \).
Calculate magnitude \( E = \frac{6.67 \times 10^{-11} \times 5 \times 10^{24}}{(10^7)^2} = 33.35\, \mathrm{N/kg} \).
Practice Set
Q1: Gravitational field intensity is defined as?
A) Force on unit mass
B) Force on unit charge
C) Energy per unit mass
D) Mass per unit volume
Q2: Gravitational field intensity at distance \( r \) from mass \( M \) is?
A) \( \frac{GM}{r} \)
B) \( \frac{GM}{r^2} \)
C) \( -\frac{GM}{r^2} \)
D) \( -\frac{GM}{r} \)
Q3: What does the negative sign in \( E = -\frac{GM}{r^2} \) indicate?
A) Repulsive force
B) Attractive force
C) Zero force
D) Variable force
Answer Key
Q1: A) Force on unit mass — Definition of gravitational field intensity.
Q2: C) \( -\frac{GM}{r^2} \) — Correct formula with negative sign.
Q3: B) Attractive force — Negative sign shows attraction.
Memory Aids
Formula: \( E = -\frac{GM}{r^2} \).
Negative sign = gravity pulls inward.
Field intensity = force per unit mass.
Acceleration due to Gravity Below and Above Earth Surface
Effect of Altitude
Force on mass \( m \) at height \( h \): \( F(h) = \frac{GM_Em}{(R_E + h)^2} \)
Acceleration due to gravity at height \( h \): \( g(h) = \frac{F(h)}{m} = \frac{GM_E}{(R_E + h)^2} = g \left(1 + \frac{h}{R_E}\right)^{-2} \)
For small \( h \) (\( h \ll R_E \)), using binomial approximation: \( g(h) \approx g \left(1 - \frac{2h}{R_E}\right) \)
Gravity decreases with altitude by factor \( (1 - 2h/R_E) \)

Effect of Depth
Mass inside radius \( R_E - d \): \( M_s = M_E \left(\frac{R_E - d}{R_E}\right)^3 \)
Force on mass \( m \) at depth \( d \): \( F(d) = \frac{GM_sm}{(R_E - d)^2} = \frac{GM_Em(R_E - d)}{R_E^3} \)
Acceleration due to gravity at depth \( d \): \( g(d) = \frac{F(d)}{m} = g \left(1 - \frac{d}{R_E}\right) \)
Gravity decreases linearly with depth by factor \( (1 - d/R_E) \)

Solved Examples
Ex 1: Calculate gravity at 10 km above Earth surface. Given \( R_E = 6400 \text{ km} \), \( g = 9.8 \text{ m/s}^2 \).
Use \( g(h) \approx g (1 - 2h/R_E) \)
\( g(10) = 9.8 \times (1 - 2 \times 10 / 6400) = 9.8 \times 0.996875 = 9.76 \text{ m/s}^2 \)
Ex 2: Find gravity at 5 km depth.
Use \( g(d) = g (1 - d/R_E) \)
\( g(5) = 9.8 \times (1 - 5/6400) = 9.8 \times 0.99922 = 9.79 \text{ m/s}^2 \)
Practice Set
Q1: Gravity at 20 km above Earth surface is approximately:
A) 9.5 m/s²
B) 9.7 m/s²
C) 9.8 m/s²
D) 10 m/s²
Q2: At 3 km depth, gravity is:
A) Increased by factor \( 1 + 3/R_E \)
B) Decreased by factor \( 1 - 3/R_E \)
C) Same as surface gravity
D) Zero
Q3: If gravity at surface is 9.8 m/s², gravity at 100 km altitude is approximately:
A) 9.5 m/s²
B) 9.1 m/s²
C) 8.8 m/s²
D) 9.0 m/s²
Answer Key
Q1: B - Gravity decreases slightly with altitude by \( 1 - 2h/R_E \), so 20 km gives about 9.7 m/s².
Q2: B - Gravity decreases linearly with depth by \( 1 - d/R_E \).
Q3: A - Using \( g(h) \approx g (1 - 2h/R_E) \), 100 km altitude gives about 9.5 m/s².
Memory Aids
Gravity decreases with altitude as \( (1 - 2h/R_E) \)
Gravity decreases with depth as \( (1 - d/R_E) \)
Use binomial approximation for small heights
Variation in Acceleration due to Gravity
Factors Affecting Gravity
Gravity decreases with height above Earth surface
Gravity decreases with depth below surface, zero at center
Earth's rotation reduces gravity at equator due to centrifugal force
Gravity varies with latitude \( \lambda \): \( g_\lambda = g - R_E \omega^2 \cos^2 \lambda \)
Minimum gravity at equator (\( \lambda=0^\circ \)), maximum at poles (\( \lambda=90^\circ \))
Earth's shape (equatorial bulge) also reduces gravity at equator

Solved Examples
Ex 1: Calculate difference in gravity between pole and equator.
\( g_p - g_e = R_E \omega^2 \)
Given \( R_E = 6.4 \times 10^6 \text{ m} \), \( \omega = 7.27 \times 10^{-5} \text{ rad/s} \)
\( g_p - g_e = 6.4 \times 10^6 \times (7.27 \times 10^{-5})^2 = 0.034 \text{ m/s}^2 \)
Practice Set
Q1: Gravity at equator is:
A) Maximum
B) Minimum
C) Same as poles
D) Zero
Q2: Gravity at latitude 45° is:
A) \( g - R_E \omega^2 \cos^2 45^\circ \)
B) \( g + R_E \omega^2 \cos^2 45^\circ \)
C) \( g \)
D) Zero
Q3: Earth's equatorial radius is larger than polar radius by about:
A) 21 km
B) 100 km
C) 5 km
D) 50 km
Answer Key
Q1: B - Gravity is minimum at equator due to rotation and bulge.
Q2: A - Gravity reduces by \( R_E \omega^2 \cos^2 \lambda \) at latitude \( \lambda \).
Q3: A - Earth's equatorial radius is about 21 km larger than polar radius.
Memory Aids
Gravity minimum at equator, maximum at poles
Gravity variation: \( g_\lambda = g - R_E \omega^2 \cos^2 \lambda \)
Earth's bulge reduces gravity at equator
Gravitational Field and Potential of Continuous Mass Distributions
Key Relations
Gravitational potential \( V \): work done per unit mass from infinity to point
Relation: \( E = -\frac{dV}{dr} \)
\( dV = - \mathbf{E} \cdot d\mathbf{r} \)
Uniform Ring (Mass \( M \), Radius \( R \))
Field on axis at distance \( x \): \( E = - \frac{GMx}{(R^2 + x^2)^{3/2}} \)
Potential on axis: \( V = - \frac{GM}{\sqrt{R^2 + x^2}} \)
Uniform Disc (Mass \( M \), Radius \( R \))
Field on axis: \( E = - \frac{2GM}{R^2} \left[1 - \frac{x}{\sqrt{R^2 + x^2}}\right] \)
Potential on axis: \( V = - \frac{2GM}{R^2} \left[x - \sqrt{R^2 + x^2}\right] \)
Thin Spherical Shell (Mass \( M \), Radius \( R \))
Inside shell (\( r < R \)): \( E = 0 \), \( V = -\frac{GM}{R} \)
On surface (\( r = R \)): \( E = -\frac{GM}{R^2} \), \( V = -\frac{GM}{R} \)
Outside shell (\( r > R \)): \( E = -\frac{GM}{r^2} \), \( V = -\frac{GM}{r} \)


Solid Sphere (Mass \( M \), Radius \( R \), Uniform Density)
Inside (\( r < R \)): \( E = -\frac{GMr}{R^3} \), \( V = -\frac{GM}{2R^3}(3R^2 - r^2) \)
On surface (\( r = R \)): \( E = -\frac{GM}{R^2} \), \( V = -\frac{GM}{R} \)
Outside (\( r > R \)): \( E = -\frac{GM}{r^2} \), \( V = -\frac{GM}{r} \)
At center (\( r=0 \)): \( V = -\frac{3GM}{2R} \)


Solved Examples
Ex 1: Find gravitational field at \( r = R/2 \) inside solid sphere.
\( E = -\frac{GM (R/2)}{R^3} = -\frac{GM}{2R^2} \)
Ex 2: Potential at center of solid sphere.
\( V = -\frac{3GM}{2R} \)
Practice Set
Q1: Gravitational field inside a thin spherical shell is:
A) \( -\frac{GM}{r^2} \)
B) Zero
C) \( -\frac{GM}{R^2} \)
D) \( -\frac{GM}{R^3} r \)
Q2: Gravitational potential outside a solid sphere at distance \( r > R \) is:
A) \( -\frac{GM}{r} \)
B) \( -\frac{GM}{R} \)
C) Zero
D) \( -\frac{GM}{2R^3}(3R^2 - r^2) \)
Q3: Gravitational field at surface of solid sphere is:
A) \( -\frac{GM}{R^2} \)
B) Zero
C) \( -\frac{GM}{R^3} r \)
D) \( -\frac{GM}{r^2} \)
Answer Key
Q1: B - Field inside thin shell is zero.
Q2: A - Potential outside sphere is \( -GM/r \).
Q3: A - Field at surface is \( -GM/R^2 \).
Memory Aids
Inside shell: zero field, constant potential
Outside mass: field \( \propto 1/r^2 \), potential \( \propto 1/r \)
Inside solid sphere: field \( \propto r \), potential quadratic in \( r \)
Gravitational Potential Energy
Definition and Formula
Work done to bring a body from infinity to a point in a gravitational field.
Between two masses M and m separated by distance r: U = -\(\frac{GMm}{r}\)
Potential energy zero at infinite separation (r → ∞).
Scalar quantity; Dimensional formula: [ML2T-2]; SI unit: Joule (J).
Near Earth Surface
At height h above Earth surface: Uh = -\(\frac{GM_{e}m}{R_{e} + h}\)
At Earth surface: Us = -\(\frac{GM_{e}m}{R_{e}}\)
Change in potential energy moving up height h:
\(\Delta U = U_{h} - U_{s} = GM_{e}m \left( \frac{1}{R_{e}} - \frac{1}{R_{e} + h} \right) = \frac{GM_{e}mh}{R_{e}^2 (1 + \frac{h}{R_{e}})} = \frac{mgh}{1 + \frac{h}{R_{e}}}\)Since \(\frac{GM_{e}}{R_{e}^2} = g\), for h << Re, \(\Delta U \approx mgh\)
Solved Examples
Ex 1: Calculate gravitational potential energy of 2 kg mass at 10 m above Earth surface.
Given: g = 9.8 m/s², h = 10 m
Solution: \(\Delta U = mgh = 2 \times 9.8 \times 10 = 196\) JEx 2: Find change in potential energy when 5 kg mass is moved from surface to 1000 m height.
Given: g = 9.8 m/s², h = 1000 m, Re = 6.4 × 106 m
Solution: \(\Delta U = \frac{mgh}{1 + \frac{h}{R_{e}}} = \frac{5 \times 9.8 \times 1000}{1 + \frac{1000}{6.4 \times 10^{6}}} \approx 49000\) J
Practice Set
Q1: Gravitational potential energy between two masses M and m separated by distance r is:
A) \(\frac{GMm}{r}\) B) \(-\frac{GMm}{r}\) C) \(GMmr\) D) ZeroQ2: The change in gravitational potential energy when a 3 kg mass is raised 20 m near Earth surface (g = 9.8 m/s²) is:
A) 588 J B) -588 J C) 60 J D) 0 JQ3: For a height h = 1000 m, Earth radius Re = 6.4 × 106 m, the exact change in potential energy for mass m is:
A) \(mgh\) B) \(\frac{mgh}{1 + \frac{h}{R_{e}}}\) C) \(mgh (1 + \frac{h}{R_{e}})\) D) Zero
Answer Key
Q1: B; Gravitational potential energy is negative and given by \(-\frac{GMm}{r}\).
Q2: A; \(\Delta U = mgh = 3 \times 9.8 \times 20 = 588\) J (positive when raised).
Q3: B; Exact formula includes correction factor \(1 + \frac{h}{R_{e}}\) in denominator.
Memory Aids
Gravitational potential energy is always negative; zero at infinity.
Near Earth, \(\Delta U \approx mgh\) for small heights.
Use correction factor \(1 + \frac{h}{R_{e}}\) for large heights.
Escape Speed
Concept and Formula
Minimum speed to escape a planet's gravity without returning.
Escape speed from surface: \( v_e = \sqrt{\frac{2GM}{R}} \)
Where, \( M \) = mass of planet, \( R \) = radius of planet, \( G \) = gravitational constant.
Using density \( \rho \) and volume: \( v_e = \sqrt{\frac{8\pi G \rho R^2}{3}} \)
For Earth, \( v_e = 11.2\ \text{km/s} \)
If projection speed \( v < v_e \), body returns or orbits.
If \( v > v_e \), body escapes with speed \( v' = \sqrt{v^2 - v_e^2} \)
Solved Examples
Ex 1: Calculate escape speed from a planet of mass \( 5 \times 10^{24} \) kg and radius \( 6 \times 10^6 \) m.
Use \( v_e = \sqrt{\frac{2GM}{R}} \)
\( G = 6.67 \times 10^{-11} \) N·m²/kg²
\( v_e = \sqrt{\frac{2 \times 6.67 \times 10^{-11} \times 5 \times 10^{24}}{6 \times 10^6}} \approx 11.8 \times 10^3 \) m/s
\( v_e = 11.8 \) km/s
Practice Set
Q1: Escape speed depends on
A) Mass only
B) Radius only
C) Both mass and radius
D) Neither mass nor radius
Q2: If escape speed from a planet is 10 km/s, what is the speed of a body projected at 15 km/s after escaping?
A) 5 km/s
B) 11.18 km/s
C) 18.3 km/s
D) 25 km/s
Q3: A planet has twice the radius and same density as Earth. Escape speed from this planet is (Earth's escape speed = 11.2 km/s):
A) 22.4 km/s
B) 15.8 km/s
C) 11.2 km/s
D) 7.9 km/s
Answer Key
Q1: C) Both mass and radius — Escape speed formula depends on \( M \) and \( R \).
Q2: B) 11.18 km/s — \( v' = \sqrt{15^2 - 10^2} = \sqrt{225 - 100} = \sqrt{125} = 11.18 \) km/s.
Q3: B) 15.8 km/s — \( v_e \propto R \) for constant density, so \( v_e = 11.2 \times \sqrt{2} = 15.8 \) km/s.
Memory Aids
Escape speed \( v_e = \sqrt{2GM/R} \) — remember "2GM over R".
For constant density, \( v_e \propto R \).
Speed after escape: \( v' = \sqrt{v^2 - v_e^2} \).
Earth Satellites
Definition and Examples
A satellite is a lighter body revolving continuously in an orbit around a much larger body.
Example: Earth is a satellite of the Sun; Moon is a satellite of Earth.
Solved Examples
Ex 1: Identify the satellite in the Earth-Sun system.
Answer: Earth is the satellite revolving around the Sun.
Practice Set
Q1: Which of the following is a natural satellite?
A) Earth
B) Moon
C) Sun
D) MarsQ2: The Moon revolves around which body?
A) Sun
B) Earth
C) Mars
D) JupiterQ3: Which of the following is NOT a satellite?
A) Earth
B) Moon
C) Artificial satellite
D) Mars
Answer Key
Q1: B - Moon is Earth's natural satellite.
Q2: B - Moon revolves around Earth.
Q3: D - Mars is a planet, not a satellite.
Memory Aids
Satellite = smaller body orbiting a larger one.
Moon → Earth → Sun (satellite chain).
Motion of a Satellite
Key Points
Satellites move in circular orbits around Earth.
Velocity direction is tangent to the orbit.
Acceleration (centripetal) points towards the center of the orbit.
Solved Examples
Ex 1: Direction of acceleration of a satellite?
Answer: Towards the center of Earth (centripetal acceleration).
Practice Set
Q1: The velocity of a satellite is always:
A) Radial
B) Tangential
C) Zero
D) Opposite to accelerationQ2: The acceleration of a satellite is directed:
A) Tangent to orbit
B) Away from Earth
C) Towards Earth center
D) Perpendicular to velocityQ3: Which force provides centripetal acceleration to a satellite?
A) Gravitational force
B) Frictional force
C) Magnetic force
D) Electrostatic force
Answer Key
Q1: B - Velocity is tangent to the orbit.
Q2: C - Acceleration is centripetal, towards Earth center.
Q3: A - Gravity provides centripetal force.
Memory Aids
Velocity tangent, acceleration radial inward.
Gravity = centripetal force for satellites.
Orbital Speed of a Satellite
Formulas and Facts
Orbital speed at height h: \( v_0 = \sqrt{\frac{GM_E}{R_E + h}} = R_E \sqrt{\frac{g}{R_E + h}} \)
Near Earth's surface (\( h \ll R_E \)): \( v_0 = \sqrt{g R_E} \)
Orbital speed is independent of satellite's mass.
Solved Examples
Ex 1: Calculate orbital speed near Earth's surface.
Given: \( g = 9.8\,m/s^2 \), \( R_E = 6.4 \times 10^6 m \)
\( v_0 = \sqrt{9.8 \times 6.4 \times 10^6} = 7.9 \times 10^3 m/s \)
Practice Set
Q1: Orbital speed depends on:
A) Mass of satellite
B) Height of orbit
C) Both A and B
D) NoneQ2: Orbital speed near Earth's surface is approximately:
A) 3 km/s
B) 8 km/s
C) 15 km/s
D) 30 km/sQ3: Orbital speed at height \( h = R_E \) is:
A) \( \sqrt{\frac{g R_E}{2}} \)
B) \( \sqrt{\frac{g R_E}{3}} \)
C) \( \sqrt{\frac{g R_E}{4}} \)
D) \( \sqrt{\frac{g R_E}{1}} \)
Answer Key
Q1: B - Depends on height, not mass.
Q2: B - Approximately 8 km/s near surface.
Q3: A - At \( h = R_E \), speed is \( \sqrt{\frac{g R_E}{2}} \).
Memory Aids
\( v_0 = \sqrt{\frac{GM_E}{R_E + h}} \)
Near surface: \( v_0 = \sqrt{g R_E} \)
Speed independent of satellite mass.
Time Period of a Satellite
Formulas and Notes
Time period: \( T = 2\pi \sqrt{\frac{(R_E + h)^3}{GM_E}} = \frac{2\pi}{\sqrt{g}} \sqrt{\frac{(R_E + h)^3}{R_E^2}} \)
Near Earth's surface (\( h \ll R_E \)): \( T = 2\pi \sqrt{\frac{R_E}{g}} = 84.6 \text{ minutes} \)
Solved Examples
Ex 1: Calculate time period near Earth's surface.
Given: \( R_E = 6.4 \times 10^6 m \), \( g = 9.8 m/s^2 \)
\( T = 2\pi \sqrt{\frac{6.4 \times 10^6}{9.8}} = 5076 s = 84.6 min \)
Practice Set
Q1: Time period depends on:
A) Mass of satellite
B) Height of orbit
C) Both A and B
D) NoneQ2: Time period near Earth's surface is about:
A) 45 min
B) 60 min
C) 85 min
D) 120 minQ3: If height doubles, time period:
A) Increases by \( \sqrt{8} \)
B) Doubles
C) Triples
D) Remains same
Answer Key
Q1: B - Depends on orbit height, not mass.
Q2: C - Approximately 85 minutes.
Q3: A - Time period \( \propto (R_E + h)^{3/2} \), so doubling height increases \( T \) by \( \sqrt{8} \).
Memory Aids
\( T = 2\pi \sqrt{\frac{(R_E + h)^3}{GM_E}} \)
Near surface: \( T \approx 84.6 \text{ min} \)
Height of Satellite
Formula
Height above Earth surface:
\( h = \left( \frac{T^2 R_E^2 g}{4 \pi^2} \right)^{1/3} - R_E \)
Solved Examples
Ex 1: Find height for \( T = 2 \text{ hours} = 7200 s \).
Use formula to calculate \( h \).
Practice Set
Q1: Height depends on:
A) Time period
B) Mass of satellite
C) Both A and B
D) NoneQ2: For \( T = 84.6 \text{ min} \), height is:
A) 0 km
B) 100 km
C) 500 km
D) 1000 kmQ3: If time period increases, height:
A) Increases
B) Decreases
C) Remains same
D) Zero
Answer Key
Q1: A - Height depends on time period.
Q2: A - At 84.6 min, satellite is near surface, so height ~ 0 km.
Q3: A - Height increases with time period.
Memory Aids
Height from \( T \): \( h = \left( \frac{T^2 R_E^2 g}{4 \pi^2} \right)^{1/3} - R_E \)
Longer period → higher orbit.
Energy of an Orbiting Satellite
Potential Energy
Potential energy (U) of satellite at height h: U = -\(\frac{GM_Em}{R_E + h}\)
G = universal gravitational constant (6.67 × 10-11 N·m²/kg²)
ME = mass of Earth, m = mass of satellite
RE = radius of Earth, h = height above Earth surface (m)
Kinetic Energy
Kinetic energy (K) of satellite: K = \(\frac{1}{2}mv_0^2 = \frac{1}{2} \frac{GM_Em}{R_E + h} = \frac{|U|}{2}\)
v0 = orbital speed of satellite
Total Mechanical Energy
Total energy (E) = K + U = −\(\frac{GM_Em}{2(R_E + h)}\) = \(\frac{U}{2}\)
Energy is negative, indicating a bound system
Near Earth Surface Orbit
For h << RE, total energy: E = −\(\frac{GM_Em}{2R_E}\)
Energy Relations
Kinetic energy equals negative total energy: K = −E
Potential energy equals twice total energy: U = 2E
Binding Energy
Energy required to remove satellite to infinity: E_B = −E = \(\frac{GM_Em}{2(R_E + h)}\)
Elliptic Orbit
Kinetic and potential energies vary along orbit
Total energy remains constant and negative
Solved Examples
Ex 1: Calculate total energy of satellite of mass 1000 kg orbiting at 300 km above Earth surface (RE = 6.4 × 106 m, ME = 6 × 1024 kg, G = 6.67 × 10-11 N·m²/kg²).
Use formula: E = −GMm/2(RE + h)
Calculate denominator: 6.4 × 106 + 3 × 105 = 6.7 × 106 m
E = −(6.67×10-11)(6×1024)(1000) / (2 × 6.7×106)
E ≈ −2.99 × 1010 J
Ex 2: Find kinetic energy of satellite in above example.
K = −E = 2.99 × 1010 J
Practice Set
Q1: Potential energy of satellite at height h is given by:
A) \(\frac{GM_Em}{R_E + h}\)
B) −\(\frac{GM_Em}{R_E + h}\)
C) \(\frac{1}{2} \frac{GM_Em}{R_E + h}\)
D) −\(\frac{1}{2} \frac{GM_Em}{R_E + h}\)
Q2: Total mechanical energy of satellite is:
A) Equal to kinetic energy
B) Equal to potential energy
C) Half of potential energy
D) Twice kinetic energy
Q3: A satellite of mass 500 kg orbits Earth at 200 km height. Calculate binding energy. (Use RE = 6.4 × 106 m, ME = 6 × 1024 kg, G = 6.67 × 10-11 N·m²/kg²)
A) 1.5 × 1010 J
B) 3.0 × 1010 J
C) 7.5 × 109 J
D) 6.0 × 1010 J
Answer Key
Q1: B
Potential energy is negative due to gravitational attraction: U = −GMm/(R + h)
Q2: C
Total energy E = U/2, i.e., half of potential energy
Q3: A
Binding energy E_B = GMm/2(R + h) = (6.67×10-11)(6×1024)(500) / (2 × 6.6×106) ≈ 1.5 × 1010 J
Memory Aids
Potential energy is negative: U = −GMm/(R + h)
Kinetic energy is half magnitude of |U|: K = |U|/2
Total energy is half of potential: E = U/2
Binding energy equals negative total energy
NEET Physics — ALL CHAPTERS
1
Basic Mathematics
2
Units and Measurement
3
Motion in a Straight Line
4
Motion in a Plane
5
Laws of Motion
6
Work, Energy and Power
7
System of Particles and Rotational Motion
8
Gravitation
9
Mechanical Properties of Solids
10
Mechanical Properties of Fluids
11
Thermal Properties of Matter
12
Thermodynamics
13
Kinetic Theory
14
Oscillations
15
Waves
16
Electric Charges and Fields
17
Electrostatic Potential and Capacitance
18
Current Electricity
19
Moving Charges and Magnetism
20
Magnetism and Matter
21
Electromagnetic Induction
22
Alternating Current
23
Electromagnetic Waves
24
Ray Optics and Optical Instruments
25
Wave Optics
26
Dual Nature of Radiation and Matter
27
Atoms
28
Nuclei
29
Semiconductor Electronics: Materials, Devices and Simple Circuits