Study Class 11 Physics Gravitation notes covering Newton's law, Kepler's laws, g variation, escape speed, satellites, orbital motion and weightlessness.
Gravitation is the study of the universal force of attraction between masses. This chapter begins with the historical shift from the geocentric model of Ptolemy to the heliocentric model supported by Aryabhata and later Copernicus, and then to Kepler's three laws of planetary motion based on Tycho Brahe's observations. Newton's universal law of gravitation is introduced, along with the universal gravitational constant G measured by Henry Cavendish. You will learn how gravitational force and potential behave for point masses and spherical shells, how the acceleration due to gravity g varies with height and depth, and how gravitational potential energy and potential are defined. The chapter then explains escape speed, the motion of Earth satellites, orbital speed, time period and the energy of an orbiting satellite, ending with the concept of weightlessness in a freely falling spacecraft.
What you'll learn
1State Newton's universal law of gravitation and use F = Gm₁m₂/r² to solve numerical problems.
2Explain Kepler's three laws of planetary motion and apply T² ∝ a³ to orbital problems.
3Describe how gravitational force and potential behave outside and inside a spherical shell.
4Derive and apply expressions for the variation of g with height and with depth.
5Define gravitational potential energy and gravitational potential, and relate them to work done.
6Calculate escape speed and orbital speed for a satellite using standard formulas.
7Analyse the kinetic, potential and total energy of a satellite in a circular orbit.
8Explain weightlessness in terms of free fall rather than the absence of gravity.
Chapter at a glance
01Newton's Law of Universal Gravitation
02Gravitational Field and Potential
03Orbital Motion and Escape Velocity
04Gravitational Effects on Earth
Detailed chapter notes
01
Historical Background and Kepler's Laws
Early models of the universe placed the Earth at the centre (Ptolemy's geocentric theory), with the Sun, Moon and planets moving around it. Aryabhata in the 5th century and later Copernicus proposed a heliocentric picture with the Sun at the centre. Tycho Brahe collected very accurate planetary observations, which Johannes Kepler used to formulate three laws. The first law states that every planet moves in an elliptical orbit with the Sun at one focus. The second law states that the line joining a planet to the Sun sweeps equal areas in equal intervals of time, so a planet moves faster near the Sun (perihelion) and slower far from it (aphelion). The third law states that the square of the orbital period is proportional to the cube of the semi-major axis: T² ∝ a³.
Perihelionnearest point to the Sun; Aphelion: farthest point from the Sun.
Semi-major axis ahalf of the longest diameter of the elliptical orbit.
For a circular orbit, both foci coincide and a equals the radius.
Kepler's second law follows from conservation of angular momentum.
02
Newton's Universal Law of Gravitation
Newton proposed that every particle in the universe attracts every other particle with a force that is directly proportional to the product of their masses and inversely proportional to the square of the distance between them. In symbols, F = Gm₁m₂/r², where G is the universal gravitational constant. The force is always attractive, acts along the line joining the two particles, is a central force, and is mutual — both particles experience equal and opposite forces. It obeys an inverse square law and has infinite range. When several masses are present, the net gravitational force on any one mass is the vector sum of the individual forces, which is the principle of superposition.
F = Gm₁m₂/r²
G = 6.67 × 10⁻¹¹ N m² kg⁻²
G was first measured by Henry Cavendish in 1798 using a torsion balance.
Knowing G allows us to determine the mass of the Earth and of other planets.
03
Gravitational Field due to a Spherical Shell
For a uniform spherical shell of mass M and radius R, the gravitational force it exerts on a particle of mass m outside the shell is the same as if the entire mass M were concentrated at the centre: F = GMm/r², where r is the distance from the centre. This is true for any point outside the shell. However, for a point inside a hollow spherical shell, the gravitational force is exactly zero. This is an important result: inside a hollow shell, the gravitational field vanishes, but the gravitational potential is not zero. These results are often called the shell theorem and are useful in treating the Earth as a sphere.
Outside a shellF = GMm/r², as if all mass is at the centre.
Inside a hollow shellF = 0.
Inside a hollow shell, gravitational potential is non-zero even though force is zero.
04
Acceleration due to Gravity and its Variation
The acceleration produced in a body due to the Earth's gravitational pull is called the acceleration due to gravity, denoted by g. For a body on the surface of the Earth, g = GM/R², where M is the mass of the Earth and R its radius. Its standard value is about 9.8 m s⁻². Importantly, g does not depend on the mass of the falling body. As we go to a height h above the surface, g decreases: g_h = GM/(R+h)². For h much smaller than R, this can be approximated as g_h ≈ g(1 − 2h/R). As we go to a depth d below the surface, g decreases linearly: g_d = g(1 − d/R). At the centre of the Earth, g becomes zero.
g = GM/R² ≈ 9.8 m s⁻²
g_h = GM/(R+h)²; for h << R, g_h ≈ g(1 − 2h/R)
g_d = g(1 − d/R); g = 0 at the Earth's centre.
g is independent of the mass of the falling body.
05
Gravitational Potential Energy and Potential
The gravitational potential energy of a mass m at a distance r from a point mass M is U = −GMm/r. The negative sign indicates that the force is attractive and that the potential energy is taken as zero at infinity. Gravitational potential V at a point is defined as the potential energy per unit mass: V = −GM/r. Its SI unit is J kg⁻¹. Both U and V are scalar quantities, so when several masses are present, the total potential at a point is the algebraic sum of the potentials due to each mass individually. Gravitational force is conservative, which is why a potential energy function can be defined.
U = −GMm/r
V = −GM/r, unit J kg⁻¹
Potential is zero at infinity and negative elsewhere.
Potential is a scalar; use algebraic addition for multiple masses.
06
Escape Speed
Escape speed is the minimum speed required for an object to escape from the gravitational influence of a planet without any further propulsion. For the Earth, it is given by v_e = √(2GM/R), which can also be written as v_e = √(2gR). Substituting the values for the Earth gives v_e ≈ 11.2 km s⁻¹. The escape speed depends only on the mass and radius of the planet, not on the mass of the projectile or the direction of launch. This concept explains why the Moon, with an escape speed of about 2.3 km s⁻¹, cannot retain a significant atmosphere: gas molecules can easily exceed this speed.
v_e = √(2GM/R) = √(2gR)
For Earth, v_e ≈ 11.2 km s⁻¹
Independent of the mass and direction of projection.
Moon's escape speed ≈ 2.3 km s⁻¹, so it has no significant atmosphere.
07
Earth Satellites: Orbital Speed, Time Period and Energy
A satellite revolves around the Earth because the gravitational force provides the necessary centripetal force. For a satellite of mass m in a circular orbit of radius r around the Earth of mass M, we equate mv²/r = GMm/r², giving the orbital speed v = √(GM/r). Near the Earth's surface, this becomes v = √(gR) ≈ 7.9 km s⁻¹. The time period of the satellite is T = 2π√(r³/GM), which shows that T² ∝ r³, consistent with Kepler's third law. For a satellite near the Earth, the period is about 84–85 minutes. The kinetic energy is K = GMm/(2r), the potential energy is U = −GMm/r, and the total energy is E = −GMm/(2r). Note that U = −2K and E = −K. The total energy of a bound satellite is always negative.
Orbital speedv = √(GM/r); near Earth, v ≈ 7.9 km s⁻¹
Time periodT = 2π√(r³/GM); near Earth, T ≈ 84–85 minutes
Kinetic energy K = GMm/(2r)
Potential energy U = −GMm/r
Total energy E = −GMm/(2r); E is negative for a bound orbit.
08
Weightlessness
Astronauts in an orbiting spacecraft feel weightless not because gravity is absent, but because both the astronaut and the spacecraft are in a state of continuous free fall towards the Earth. Since they fall together with the same acceleration, the astronaut does not press against the floor of the spacecraft, and the normal reaction becomes zero. This condition is called weightlessness. The gravitational force is still acting, and it is this force that provides the centripetal acceleration needed to keep the spacecraft in orbit. Thus, weightlessness is a consequence of free fall, not of zero gravity.
Weightlessness occurs because astronaut and spacecraft are in free fall together.
Gravity is not zero; it provides the centripetal force.
Normal reaction on the astronaut becomes zero.
Want the complete chapter resources?Topic notes, quizzes and flashcards for Gravitation.
Newton's Law of Universal Gravitation states that the gravitational force between two masses is directly proportional to the product of their masses and inversely proportional to the square of the distance between them. Which of the following correctly represents this law?
AF = G(m₁ + m₂)/r²
BF = Gm₁m₂/r²
CF = Gm₁m₂/r
DF = G(m₁m₂)²/r²
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Answer: (B) F = Gm₁m₂/r²
Newton's law of universal gravitation is expressed as F = Gm₁m₂/r², where G is the gravitational constant, m₁ and m₂ are masses, and r is the distance between their centers. This is the only correct mathematical representation among the options.
Question 02
The gravitational field intensity at a point is defined as the gravitational force experienced per unit ___.
Amass
Bvolume
Carea
Ddistance
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Answer: (A) mass
Gravitational field intensity is defined as the force per unit mass (E = F/m), making it a measure of the strength of the gravitational field at any point in space.
Question 03
The escape velocity from Earth's surface is approximately 11.2 km/s. What does this mean?
AAn object must travel at this speed to orbit Earth at ground level
BAn object needs this minimum speed to break free from Earth's gravitational pull completely
CThis is the speed at which objects fall to Earth
DAn object travels at this speed when in geostationary orbit
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Answer: (B) An object needs this minimum speed to break free from Earth's gravitational pull completely
Escape velocity is the minimum speed required for an object to escape a planet's gravitational field entirely. It does not depend on direction but only on the planet's mass and radius.
Question 04
What is the SI unit of gravitational field strength?
AN/kg
BN·m²/kg²
Ckg/N
Dm/s²·kg
Show answer
Answer: (A) N/kg
Gravitational field strength is force per unit mass, measured in N/kg or equivalently m/s². This is the acceleration experienced by a unit mass in a gravitational field.
Question 05
The gravitational constant G has a numerical value of approximately 6.67 × 10⁻¹¹ N·m²/kg². What does this value tell us about the strength of the gravitational force?
AGravitational force is the strongest force in nature
BGravitational force is extremely weak compared to other fundamental forces
CGravitational force depends only on the mass of one object
DGravitational force increases with distance
Show answer
Answer: (B) Gravitational force is extremely weak compared to other fundamental forces
The very small value of G (10⁻¹¹) indicates that gravity is an extremely weak force at the atomic and molecular scales. This is why electromagnetic and nuclear forces dominate at small scales, while gravity only becomes significant for very large masses.
Ready for more practice?Unlock the full quiz for this chapter.
Q1. State Newton's law of universal gravitation. Write the mathematical expression and explain the meaning of each symbol.
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Model answer
Newton's law of universal gravitation states that every body in the universe attracts every other body with a force which is directly proportional to the product of their masses and inversely proportional to the square of the distance between them. The mathematical expression is F = G m1 m2 / r^2, where F is the gravitational force, G is the universal gravitational constant (6.67×10^-11 N m^2/kg^2), m1 and m2 are the masses of the two bodies, and r is the distance between their centres.
Sample question3 marks
Q2. Define gravitational potential energy of a body. Derive an expression for the gravitational potential energy of a body of mass m placed at a distance r from the centre of the earth.
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Model answer
Gravitational potential energy of a body is the work done in bringing it from infinity to that point. For a body of mass m at distance r from earth's centre, the force is F = GM_E m / r^2. Work done from infinity to r is W = -GM_E m / r. This is the potential energy (U = -GM_E m / r).
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Q3. Explain how the acceleration due to gravity (g) varies with height above the Earth's surface. Write the expression for g at a height h (h << R_E) and state the effect on g.
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Model answer
The acceleration due to gravity decreases with height above the Earth's surface. For a height h above the surface, the value of g is given by g(h) = GM_E/(R_E + h)^2. For h << R_E, using binomial expansion, g(h) ≈ g(0)(1 - 2h/R_E), where g(0) is the value at the surface. Thus, g decreases as height increases.
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Q4. What is the universal gravitational constant G? Why is it called 'universal'? Give its SI units and value.
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Model answer
The universal gravitational constant G is the constant of proportionality in Newton's law of gravitation. It is called 'universal' because its value is the same for any pair of bodies anywhere in the universe. Its SI unit is N m^2 kg^-2 and its value is 6.67 × 10^-11 N m^2 kg^-2. G was first measured experimentally by Henry Cavendish using a torsion balance.
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Q5. What is gravitational field intensity? Give its expression at a point outside a uniform spherical shell.
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Model answer
Gravitational field intensity at a point is the force experienced by a unit mass placed at that point. For a point outside a uniform spherical shell, the field intensity is as if the entire mass of the shell is concentrated at its centre. Thus, I = GM / r^2, where M is mass of shell and r is distance from centre.
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Newton's universal law of gravitation states that every particle of matter attracts every other particle with a force directly proportional to the product of their masses and inversely proportional to the square of the distance between them. Mathematically, F = Gm₁m₂/r², where G is the universal gravitational constant.
What is the difference between gravitational potential and gravitational potential energy?
Gravitational potential at a point is the gravitational potential energy per unit mass at that point, V = −GM/r, with unit J kg⁻¹. Gravitational potential energy is the energy of a mass m at that point, U = −GMm/r, with unit joule. Potential is a property of the field, while potential energy depends on the mass placed in the field.
Why is the acceleration due to gravity zero at the centre of the Earth?
At the centre of the Earth, the mass of the Earth is distributed symmetrically all around, so the gravitational pulls from different parts cancel out. Using the formula g_d = g(1 − d/R), at the centre d = R, so g_d = 0. Thus the net gravitational acceleration is zero at the centre.
How do you calculate escape velocity from Earth?
Escape velocity is calculated using v_e = √(2GM/R) or v_e = √(2gR). For Earth, using G = 6.67 × 10⁻¹¹ N m² kg⁻², M = 5.97 × 10²⁴ kg and R = 6.37 × 10⁶ m, we get v_e ≈ 11.2 km s⁻¹. It does not depend on the mass of the object or the direction of launch.
Why do astronauts feel weightless in a spacecraft?
Astronauts feel weightless because both they and the spacecraft are in continuous free fall towards the Earth. Since they fall together with the same acceleration, the astronaut does not press against the spacecraft floor, and the normal reaction becomes zero. Gravity is still acting and provides the centripetal force for the orbit.
What is the relation between the time period of a satellite and its orbital radius?
The time period T of a satellite in a circular orbit of radius r is given by T = 2π√(r³/GM). This shows that T² is proportional to r³, which is Kepler's third law. For a satellite very close to the Earth's surface, the time period is about 84–85 minutes.