By the end of this chapter you'll be able to…

  • 1State Kepler's three laws, and explain why the area law follows from angular momentum
  • 2Apply F = Gm1m2/r^2 with superposition, and describe how Cavendish measured G
  • 3Use the two shell results to justify treating a planet as a point mass
  • 4Find how g varies above and below the surface, and say why it is maximum at the surface
  • 5Use U = -GMm/r and V = -GM/r, and explain what the negative sign means
  • 6Derive escape speed, and state what it does and does not depend on
  • 7Derive orbital speed and period, and get T^2 proportional to r^3
  • 8Show that a satellite's total energy is negative, with E = -K
  • 9Explain weightlessness as free fall rather than absence of gravity
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Why this chapter matters
An astronaut floating in the space station is not beyond Earth's gravity — it is close to full strength up there. She floats because she and the station are falling together. That one correction is most of this chapter: gravity is weak enough to need a torsion balance to detect, yet it sets the orbit of every satellite and the period of every planet.

Gravitation

1. What this chapter covers

Textbook sectionTopic
7.1How the modern picture replaced circular orbits
7.2Kepler's three laws
7.3The universal law of gravitation, superposition, and the two shell results
7.4Measuring G — the Cavendish experiment
7.5Acceleration due to gravity of the Earth
7.6Acceleration due to gravity above and below the surface
7.7Gravitational potential energy
7.8Escape speed
7.9Earth satellites
7.10Energy of an orbiting satellite

This maps cleanly onto the CBSE 2026-27 syllabus, with one thing worth knowing before you revise.

Not in the 2026-27 chapter or syllabus

TopicStatus
Geostationary satellitesNot in the chapter, not listed by CBSE
Polar satellitesNot in the chapter, not listed by CBSE
Weightlessness as a taught sectionOnly appears as a Point to Ponder — but see section 12, because Exercise 7.9 needs the idea

Older editions carried sections on all three, and most coaching handouts still do. The words "geostationary" and "polar satellite" do not occur anywhere in the 2026-27 chapter.

One more thing the chapter does not contain: the falling apple. It is a good story, but it is not in this book, and nothing in the syllabus rests on it.


2. How we got here: circles, then ellipses

This is the one chapter in Class 11 Physics where the history is worth a few minutes, because the sequence explains why the laws are numbered the way they are.

The starting picture put the planets on circles around a fixed central Sun. That model was discredited by the church, and its most famous supporter, Galileo, faced prosecution from the state for holding to it.

At about the same time, a Danish nobleman called Tycho Brahe (1546-1601) spent an entire working life recording planetary positions with the naked eye — no telescope. He never explained them. His assistant Johannes Kepler (1571-1640) analysed the compiled data afterwards and pulled three laws out of it.

Notice the order of events. Kepler's laws came from data, and described how planets move. They did not explain why. Newton supplied the why, decades later, and the fact that his single force law reproduces all three of Kepler's is the strongest evidence he had.

So when a question asks you to "derive Kepler's third law", it is asking you to run that history forwards: start from Newton's force, end at Kepler's observation.


3. Kepler's three laws

First law — the law of orbits

All planets move in elliptical orbits with the Sun at one of the two foci.

This was a genuine break from the Copernican model, which allowed only circles.

You should know the parts of the ellipse by name, because questions use the vocabulary without explaining it:

TermWhat it means
FocusOne of two fixed points. The Sun sits at one of them — nothing sits at the other
PerihelionThe point of the orbit closest to the Sun
AphelionThe point farthest from the Sun
Semi-major axis Half the distance from perihelion to aphelion

How to draw one, and why the definition works: pin the two ends of a string at the foci, pull it taut with a pencil tip and move the pencil around. The curve you get is an ellipse, because the string length never changes — so for every point on the curve, the sum of the distances to the two foci is constant.

A circle is a special case, not a different shape. Bring the two foci together and they merge into one point; the semi-major axis becomes the radius. This matters more than it looks: every circular-orbit result you derive later in the chapter is a special case of Kepler's laws, not a separate topic.

Second law — the law of areas

The line joining a planet to the Sun sweeps out equal areas in equal intervals of time.

Where this came from: the observation that planets appear to move slower when they are farther from the Sun and faster when nearer. Equal areas in equal times is exactly that statement made precise — far from the Sun the line is long, so a small angle sweeps a large area; close in, the line is short and the planet must move faster to sweep the same area.

The second law is angular momentum conservation in disguise. In a small time the area swept is

Gravity always points along the line joining planet to Sun, so it exerts no torque about the Sun, so is constant, so is constant.

Carry this consequence: the area law holds for any central force, not only an inverse square one. So the second law tells you gravity points along the line joining the two bodies — but it does not tell you the force goes as .

Third law — the law of periods

where is the semi-major axis. This is the law that pins down the inverse square. Newton's insight was that a force, and essentially only that, reproduces .

Two points the chapter makes explicitly, and both get asked:

  • The constant of proportionality is the same for every planet orbiting the same Sun. That is what makes the law useful — you can compare two planets without knowing either mass.
  • It applies to Earth satellites too. The chapter derives for a satellite, which is the third law again with the Earth in place of the Sun.

4. The universal law of gravitation

Every particle attracts every other particle along the line joining them, with a force

Two properties you must be able to use, not just quote.

The principle of superposition

Gravitational forces add as vectors. If several masses act on one body, the resultant is the vector sum of the individual forces:

Each pair is worked out as if the others were not there, and only then are the results added.

Use symmetry before you use algebra. The chapter's Example 7.1 places equal masses at the corners of an equilateral triangle and asks for the force on a mass at the centre. The full vector sum comes out zero — but you can see it is zero by symmetry in one line, without computing anything. Then when one corner mass is doubled, only the extra mass contributes, and the problem collapses to a single force.

The two shell results — why a planet can be treated as a point

An extended body is not a point, so strictly you would have to add up the pull of every particle in it. Calculus does this, and for a uniform spherical shell the answer takes two remarkably clean forms:

Where the point mass sitsForce from the shell
Outside the shellExactly as if the shell's entire mass were concentrated at its centre
Inside the shellZero, everywhere inside — not just at the centre

These two results carry the rest of the chapter. The first is the reason you are allowed to write for the Earth at all, and the reason Cavendish could treat his lead spheres as points. The second is the reason falls as you descend, and it is what Exercise 7.11 turns on.


5. Measuring G — the Cavendish experiment

G had to be measured, not derived. No theory predicts its value. It was first determined by the English scientist Henry Cavendish in 1798, and the accepted value is

How the apparatus works, since this is a standard 3-mark description:

  1. A bar carries two small lead spheres at its ends, suspended at its centre from a fine wire.
  2. Two large lead spheres are brought close to the small ones, on opposite sides.
  3. Each big sphere attracts its neighbour. The two forces are equal and opposite, so there is no net force on the bar — only a torque, of magnitude where is the bar's length.
  4. The wire twists until its restoring torque balances the gravitational torque. If is the angle of twist and the restoring couple per unit angle:

  1. is found separately, by applying a known torque and measuring the twist. Measure , and follows.

Read step 3 again — it is the design insight. Putting the large spheres on opposite sides deliberately cancels the net force and leaves a pure torque, which a fine wire can register as a visible rotation. A force that small could not be weighed; a twist can be watched.

That an experiment this delicate was needed tells you how weak gravity is between ordinary objects. It only becomes obvious when one of the masses is planet-sized.


6. Why the Earth behaves like a point, and what g really is

Picture the Earth as a large number of concentric spherical shells, the smallest at the centre and the largest at the surface.

A point outside the Earth is outside every one of those shells. By the first shell result, each shell pulls as if its mass sat at the common centre — so the whole Earth pulls as if its entire mass were concentrated at its centre. Hence, for a mass at the surface:

This is where comes from. It is not a fundamental constant — it is , the Earth's mass and the Earth's radius packaged into one number. Change any of the three and changes, which is why the Moon has a different and why the same object weighs slightly different amounts at different places.

The distinction that costs the most marks

What it isUniversal gravitational constantAcceleration due to gravity
ValueAbout at Earth's surface
Units
Depends on the body?No — same everywhere in the universeYes — depends on and

7. Why g falls off in both directions

This is where students lose marks, because the two cases have different formulas and the result is counter-intuitive.

Above the surface, at height , the distance from the centre is simply larger:

Below the surface, at depth , something different happens. Stand at radius from the centre. Every shell of radius greater than has you inside it, and by the second shell result exerts no force at all. Only the sphere of radius beneath you pulls, as if its mass were at the centre.

For a uniform Earth that inner mass goes as , while the force goes as — so the force goes as , linear in the distance from the centre:

Positiong
At the centrezero
Below the surfacedecreases linearly as you go down
At the surfacemaximum
Above the surfacedecreases as inverse square

So g is largest at the surface and falls off whichever way you move from it — but for entirely different reasons. Going up, the distance increases. Going down, the amount of mass pulling you decreases, because everything above you contributes nothing.

The trap: students assume that since gravity is "stronger nearer the centre", must keep rising as you descend. It does the opposite. Getting closer to the centre also means leaving mass behind you, and that effect wins.


8. Potential energy, and why the sign is negative

Take zero potential energy at infinity — the natural choice, since the force vanishes there. Bringing a mass in from infinity then releases energy, so the potential energy is negative:

Gravitational potential is the same thing per unit mass, and CBSE lists it separately, so know both:

Potential energy Potential
Belongs toA pair of massesA point in space
Formula
Unitsjoulejoule per kilogram
Relation

The negative sign is not a bookkeeping quirk. It is what "bound" means. A system with negative total energy cannot reach infinity, because reaching infinity requires getting to at least zero energy. Everything below zero is trapped.

And is only an approximation. It is the small-height limit of the change in this , valid while . Use it for a ball thrown off a roof; do not use it for a rocket.


9. Escape speed

Escape speed is the minimum launch speed for which the total energy reaches zero — the threshold of being unbound:

Three things about escape speed that get asked:

  • It does not depend on the escaping body's mass — cancels. A marble and a spacecraft need the same speed.
  • It does not depend on the direction of projection, because energy is a scalar and depends only on distance.
  • It does depend on where you launch from — height enters through .

Why the Moon has no atmosphere

Put the Moon's own and radius into the same formula and escape speed comes out at about 2.3 km/s, roughly five times smaller than Earth's.

Gas molecules on the Moon's surface routinely reach speeds above that. So any atmosphere it once had simply leaked away into space, molecule by molecule. The Moon is airless because its escape speed is low — a fact about thermal speeds and gravity, not about how the Moon formed.

That is the kind of link worth having ready: one formula, one number, one visible consequence.


10. Satellites, orbital speed and period

A satellite in a circular orbit is in free fall — gravity supplies exactly the centripetal force needed, and nothing else acts:

The period follows from going once round at that speed:

That is Kepler's third law, derived rather than observed. Which is why this derivation is the most-set 5-mark question in the chapter.

Put into the speed formula and you get , which works out to about 7.9 km/s — so

Escape speed is only about 41% more than orbital speed. Worth remembering as a sanity check: if a calculation gives you an escape speed double the orbital speed, you have made an error.

The one thing to take from the period formula: depends only on the orbital radius — not on the satellite's mass, not on how it got there. Two satellites at the same height keep the same period whatever they weigh.


11. The energy of an orbiting satellite

For a circular orbit of radius , substitute the orbital speed into the kinetic energy:

Three relations follow, and they are the ones worth memorising because they turn multi-step problems into one line:

The total energy is negative, which is precisely the statement that the satellite is bound. If ever became positive the satellite would leave and not return.

A consequence that gets asked: to free an orbiting satellite you must supply . That is less than launching the same object from rest on the ground, because the satellite already carries kinetic energy pointed the right way. Exercise 7.6 turns on exactly this point.

And a counter-intuitive one: raising a satellite to a higher orbit increases its total energy but decreases its speed, since falls as grows. Higher orbit, slower satellite, more energy. The extra energy went into potential energy, and more than paid for the kinetic energy lost.


12. Weightlessness — not the absence of gravity

The chapter no longer teaches this as a section, but Exercise 7.9 asks about the effects on an astronaut, so you need it.

At the height of the space station, gravity is close to its full surface strength. An astronaut floats not because gravity is weak, but because she and the station are both in free fall towards Earth, falling together at the same rate. With nothing pushing up on her, there is no sensation of weight.

The chapter's own Point to Ponder puts it plainly: this is free fall, not an absence of gravitational force.

What you actually feel as weight is the normal force — the push of the floor, which is what a bathroom scale reads. Remove the floor's push and the sensation goes, whatever gravity is doing.

The same reasoning covers the lift problems you will meet later: apparent weight drops to zero when floor and passenger accelerate downward together at .


13. Two results the exercises lean on

Gravitational shielding is impossible. Electric fields can be screened by a conductor, because charges rearrange themselves to cancel the field inside. There is no negative mass, so nothing can rearrange to cancel gravity. Putting a body inside a hollow sphere does not shield it from outside matter — the sphere's own pull vanishes inside, but everything beyond it still reaches through. Exercise 7.1 asks this directly.

Tidal effects follow the gradient, not the force. The Sun pulls on the Earth far harder than the Moon does, yet the Moon dominates our tides. Tides depend on how much the pull differs across the Earth's diameter, and that difference falls off as — much faster than the force itself. On that measure the Moon's closeness beats the Sun's mass.


Summary

  • Kepler's laws came from Tycho Brahe's naked-eye data and describe how planets move; Newton's law of gravitation explains why.
  • Orbits are ellipses with the Sun at one focus; a circle is the special case where the two foci merge.
  • The law of areas is angular momentum conservation, and holds for any central force — so it does not by itself imply an inverse square law. The third law does.
  • ; forces from several masses add as vectors.
  • A uniform shell pulls an outside point as if all its mass were at the centre, and pulls an inside point not at all. Everything else in the chapter rests on these two results.
  • was measured by Cavendish in 1798 using a torsion balance, where opposed spheres give a pure torque and no net force.
  • is not fundamental — it is built from , the Earth's mass and its radius.
  • is maximum at the surface: it falls as an inverse square going up, and falls linearly going down, reaching zero at the centre.
  • and , with zero taken at infinity. Negative total energy means bound.
  • km/s — independent of the escaping body's mass and of direction. The Moon's is 2.3 km/s, which is why it has no atmosphere.
  • and : the period depends on orbital radius alone.
  • A bound satellite has , so and .
  • Weightlessness is shared free fall, not absent gravity.

Key formulas & results

Everything you need to memorise, in one card. Screenshot this for revision.

Force between two masses
F = G m1 m2 / r^2
G = 6.67e-11 N m^2/kg^2, measured by Cavendish in 1798. Forces from several masses add as vectors, not as numbers.
The two shell results
outside a shell: acts as if all mass at centre; inside a shell: force = 0
These are why a planet can be treated as a point, and why g falls as you go down. Nearly every result in the chapter rests on one of them.
g at the surface
g = G M_E / R_E^2
g is not a fundamental constant — it is G, the Earth's mass and its radius packaged into one number.
g above the surface
g_h = G M_E/(R_E + h)^2 = g(1 - 2h/R_E) approx
The approximation is only valid for h much smaller than R_E. Falls off as inverse square.
g below the surface
g_d = g(1 - d/R_E)
Linear in depth, not inverse square, because only the sphere beneath you pulls. Zero at the centre.
Gravitational potential energy
U = -G M m / r
Zero taken at infinity. Belongs to a pair of masses, measured in joules. mgh is only its small-height approximation.
Gravitational potential
V = -G M / r, U = mV
Potential energy per unit mass, in J/kg. Belongs to a point in space, not to a pair. CBSE lists this separately from U.
Escape speed
v_e = sqrt(2GM/R) = sqrt(2gR) = 11.2 km/s for Earth
Independent of the escaping body's mass and of the direction of projection. Only 2.3 km/s on the Moon, which is why the Moon has no atmosphere.
Orbital speed of a satellite
v_o = sqrt(G M_E/(R_E + h))
About 7.9 km/s just above the surface, so escape speed is sqrt(2) times orbital speed — only about 41% more.
Period of a satellite
T = 2 pi sqrt(r^3 / G M_E)
Depends only on the orbital radius. Two satellites at the same height share a period whatever their masses.
Kepler's third law
T^2 = (4 pi^2 / G M) a^3
The constant is the same for every body orbiting the same centre. Derived here from the orbital period, not assumed.
Kepler's second law as areal velocity
dA/dt = L / 2m = constant
Follows from gravity exerting no torque about the Sun. True for any central force, so it does not by itself imply an inverse square law.
Energy of an orbiting satellite
K = GMm/2r, U = -GMm/r, E = -GMm/2r
So E = -K and E = U/2. The negative total energy is exactly the statement that the satellite is bound.
⚠️

Common mistakes & fixes

These are the exact errors that cost students marks in board exams. Read them once, save yourself the trouble.

WATCH OUT
Confusing g with G
G is the universal gravitational constant, 6.67e-11 N m^2/kg^2, the same everywhere in the universe. Small g is the local acceleration due to gravity, g = GM/R^2, which changes from planet to planet and with height.
WATCH OUT
Thinking astronauts experience zero gravity
Gravity at the space station is close to its full surface strength. Astronauts float because they and the spacecraft are in free fall together, so nothing pushes up on them — the missing thing is the normal force, not gravity.
WATCH OUT
Assuming g keeps increasing as you go deeper
Going down, g decreases linearly and reaches zero at the centre. Descending brings you closer to the centre but also leaves mass above you, and by the shell result that mass pulls not at all. The second effect wins, so g is maximum at the surface.
WATCH OUT
Using the same formula for height and for depth
Above the surface g falls off as an inverse square, g_h = g(1 - 2h/R). Below it, g falls off linearly, g_d = g(1 - d/R). Two different formulas for two different physical reasons — never substitute a depth into the height formula.
WATCH OUT
Thinking escape speed depends on the direction of projection
Escape speed is derived from energy conservation, and energy is a scalar. It does not depend on direction, and it does not depend on the escaping body's mass either. It does depend on the height you launch from.
WATCH OUT
Mixing up orbital and escape velocity
Orbital speed just above the surface is about 7.9 km/s; escape speed is sqrt(2) times that, about 11.2 km/s — only 41% more, not double. If a calculation gives twice the orbital speed, something is wrong.
WATCH OUT
Confusing gravitational potential with gravitational potential energy
Potential V = -GM/r belongs to a point in space and is measured in joules per kilogram. Potential energy U = -GMm/r belongs to a pair of masses and is measured in joules. They are related by U = mV, and CBSE examines both.
WATCH OUT
Using mgh at large heights
mgh is only the small-height approximation to the change in U = -GMm/r, valid while h is far smaller than the Earth's radius. For satellites, rockets or escape problems, use the full expression.
WATCH OUT
Taking a satellite's total energy as positive
For a bound circular orbit the total energy is E = -GMm/2r, which is negative. Kinetic energy is positive and equals half the magnitude of the potential energy, but the potential energy is larger, so their sum comes out below zero.
WATCH OUT
Thinking a heavier satellite needs a different speed or period
The satellite's mass cancels out of both the orbital speed and the period. At a given orbital radius every satellite moves at the same speed and takes the same time to go round, whatever it weighs.
WATCH OUT
Thinking a hollow sphere shields a body from outside gravity
Gravitational shielding is impossible. Electric fields can be screened because charges rearrange to cancel them, but there is no negative mass to do the same for gravity. The shell's own pull vanishes inside it, yet everything outside still reaches through.
WATCH OUT
Expecting the Sun to dominate the tides because it pulls harder
Tides depend on how much the pull differs across the Earth's diameter, not on the pull itself. That difference falls off as 1/r^3, much faster than the 1/r^2 force, so the Moon's closeness beats the Sun's mass.

NCERT exercises (with solutions)

Every NCERT exercise from this chapter — what it covers and how many questions to expect.

Practice problems

Work through this chapter's problems as a readiness check — reveal each solution, mark yourself honestly, and get your gap report at the end.

Readiness check

Are you exam-ready for Gravitation?

10 problems from this chapter. Try each one, reveal the worked solution, mark yourself honestly — get your gap report at the end.

10 questions~7 min worth ~17 marks in Uttar Pradesh (UPMSP) exams

5-minute revision

The whole chapter, distilled. Read this the night before the exam.

  • Kepler's laws came from Tycho Brahe's naked-eye data; Newton supplied the explanation decades later.
  • Kepler 1: orbits are ellipses with the Sun at one focus. A circle is the special case where the two foci merge.
  • Perihelion is the closest point to the Sun, aphelion the farthest; the semi-major axis is half the distance between them.
  • Kepler 2: equal areas in equal times — this is angular momentum conservation, and holds for any central force.
  • Because the area law works for any central force, it does not by itself prove an inverse square law. The third law does.
  • Kepler 3: T^2 is proportional to a^3, with the same constant for every body orbiting the same centre. It applies to Earth satellites too.
  • F = G m1 m2 / r^2, with G = 6.67e-11 N m^2 / kg^2, first measured by Cavendish in 1798 with a torsion balance.
  • Gravitational forces from several masses add as vectors — use symmetry before algebra.
  • A uniform spherical shell pulls an outside point as if all its mass were at the centre, and pulls an inside point not at all.
  • Those two shell results are why the Earth can be treated as a point mass, and why g falls with depth.
  • At the surface, g = GM/R^2 — built from G, the Earth's mass and its radius, so it is not a fundamental constant.
  • Above the surface g falls off as inverse square; for h much less than R, g_h = g(1 - 2h/R).
  • Below the surface g_d = g(1 - d/R), falling linearly, because only the sphere beneath you pulls.
  • g is maximum at the surface and zero at the centre.
  • Gravitational shielding is impossible — there is no negative mass.
  • U = -GMm/r and V = -GM/r, taking zero at infinity; U = mV.
  • Negative total energy means bound; reaching infinity needs at least zero.
  • mgh is only the small-height approximation to the change in U.
  • Escape speed v_e = sqrt(2GM/R) = sqrt(2gR), about 11.2 km/s for the Earth.
  • Escape speed does not depend on the body's mass or on the direction of projection, but does depend on height.
  • The Moon's escape speed is only 2.3 km/s, which is why it has no atmosphere.
  • Orbital speed V = sqrt(GM/(R+h)); about 7.9 km/s near the surface, so v_e = sqrt(2) times V.
  • A satellite's period depends only on its orbital radius, never on its mass.
  • For a circular orbit: K = GMm/2r, U = -GMm/r, E = -GMm/2r, so E = -K and E = U/2.
  • A higher orbit means more total energy but a slower satellite.
  • Weightlessness is free fall, not the absence of gravity — what disappears is the normal force.
  • Tides follow the 1/r^3 gradient of the pull, not the 1/r^2 force — which is why the Moon beats the Sun.
  • Not in the 2026-27 chapter or syllabus: geostationary satellites, polar satellites.

Uttar Pradesh (UPMSP) marks blueprint

Where the marks come from in this chapter — so you can plan your prep.

Typical chapter weightage: Unit VI sits inside the 17-mark block covering Units III to VI (CBSE Class 11 Physics, 70 marks)

Question typeMarks eachTypical countWhat it tests
Satellites and orbital energy3-51Orbital velocity, time period, satellite energy
Variation of g2-31Height and depth, and why g is maximum at the surface
Potential energy and potential31U = -GMm/r, V = -GM/r, and the meaning of the negative sign
Escape speed2-31Derivation from energy, and what it does not depend on
Kepler's laws2-31Statements, the area law as angular momentum, and the period-radius relation
Universal law and G2-31Inverse square law, superposition, and the Cavendish experiment
Prep strategy
  • Learn the two shell results first — most of the chapter follows from them
  • Keep the height and depth formulas apart; they are different laws, not variants
  • Derive escape and orbital speed from energy rather than memorising them
  • Know gravitational potential separately from potential energy — CBSE lists both
  • Remember that a satellite's total energy is negative, and that E = -K

Where this shows up in the real world

This chapter isn't just an exam topic — it lives in the world around you.

Weighing the Earth

Cavendish's torsion balance gave G. With g and the Earth's radius already known, M = gR^2/G then gives the mass of the planet — which is why his experiment is often described as weighing the Earth.

Choosing a satellite's altitude

Because the period depends only on orbital radius, picking an altitude fixes how often a satellite passes overhead — the single decision behind imaging, weather and communication orbits.

Why the Moon is airless

Its escape speed of 2.3 km/s is below the typical speed of gas molecules at its surface, so any atmosphere leaked away into space.

Ocean tides

The Moon raises larger tides than the far more massive Sun, because tides follow how much the pull changes across the Earth's diameter, which falls off as 1/r^3.

Sending a probe out of Earth orbit

A satellite already in orbit needs only GMm/2r more energy to escape, far less than launching the same mass from rest on the ground — which is why missions park in orbit first.

Exam strategy

Battle-tested tips from teachers and toppers for this chapter.

1
For any satellite question, decide first whether the radius is R or R + h. Substituting the Earth's radius where the orbital radius belongs is the most frequent numerical slip in this chapter.
2
The height and depth formulas are different laws, not variants of one. If a question mentions a mine or a tunnel, reach for g(1 - d/R); if it mentions altitude, reach for the inverse square.
3
When a question says 'show that T^2 is proportional to r^3', the derivation is only complete if you state where the centripetal force comes from before equating anything.
4
Sanity-check any escape speed against sqrt(2) times the orbital speed at the same radius. If your answer is about double, you have squared or halved something by mistake.
5
Write the sign convention down before integrating for potential energy. Most marks lost in that derivation go to signs, not to the calculus.
6
Use GM = 4.0e14 for the Earth as a single number rather than multiplying 6.67e-11 by 6e24 each time — fewer keystrokes, fewer powers of ten to lose.
7
If asked why g varies, name the mechanism, not just the formula: increasing distance above the surface, disappearing mass below it.
8
Answer for potential and potential energy separately if both are asked. They have different units, and one will not be accepted for the other.

Going beyond the textbook

For olympiad aspirants and curious learners — topics that build on this chapter.

STRETCH
Derive the gravitational potential inside a uniform solid sphere and show it varies as (3R^2 - r^2), matching the surface value at r = R.
STRETCH
Show that for an elliptical orbit the total energy is E = -GMm/2a, where a is the semi-major axis — the circular result with r replaced by a.
STRETCH
Find the time period of a body dropped into a tunnel bored through the centre of the Earth, using the fact that g_d is proportional to r, and show the motion is simple harmonic.
STRETCH
Locate the neutral point between two unequal masses, then find the minimum speed a projectile needs to cross it — the method behind the chapter's Example 7.4.
STRETCH
Estimate the tidal acceleration across the Earth's diameter due to the Moon and due to the Sun, and confirm the 1/r^3 dependence numerically.

Where else this chapter is tested

CBSE board isn't the only one — other exams test this chapter too.

CBSE Class 11 Physics examHigh
JEE Main and Advanced (Gravitation)High
NEET PhysicsHigh

Questions students ask

The real ones — pulled from the Q&A community and tutor sessions.

At the height of the International Space Station gravity is only slightly weaker than at the surface (about 8.7 m/s^2). The astronauts feel weightless because they and their spacecraft are in continuous free fall around the Earth, both accelerating toward the Earth at the same rate. With no normal reaction force between them and the craft, there is no sensation of weight -- this is apparent weightlessness, not zero gravity.

Two things change as you descend, and they pull in opposite directions. You do get nearer the centre, which would increase the pull. But you also leave mass above you, and a uniform spherical shell exerts no gravitational force at all on anything inside it, so all the rock above your head contributes nothing. Only the sphere beneath you still pulls, and that shrinking sphere wins the contest. The result is that g falls linearly with depth, g_d = g(1 - d/R), reaching zero at the centre — so g is at its maximum right at the Earth's surface.

Gravitational potential energy U = -GMm/r belongs to a pair of masses and is measured in joules; it tells you the energy of the two-body system at that separation. Gravitational potential V = -GM/r belongs to a point in space, is measured in joules per kilogram, and describes the field created by M regardless of what you place there. The two are related by U = mV. CBSE lists both for this chapter, so a question asking for the potential will not accept the potential energy as an answer.

Because the escaping body's mass cancels. Escape speed is found by setting the total energy to zero: (1/2)mv^2 - GMm/R = 0. Every term carries a factor of m, so dividing through removes it entirely, leaving v_e = sqrt(2GM/R). The mass of the object never appears in the answer. The same cancellation also means escape speed does not depend on the direction you throw the object, since energy is a scalar and the potential energy depends only on distance.

Because its escape speed is too low to hold one. Putting the Moon's own surface gravity and radius into v_e = sqrt(2gR) gives about 2.3 km/s, roughly five times smaller than the Earth's 11.2 km/s. Gas molecules at the Moon's surface temperature routinely move faster than 2.3 km/s, so any gas that was there escaped into space molecule by molecule and never came back. This is a direct consequence of the escape-speed formula, and a good example of how one number in this chapter explains something you can see with your own eyes.

For a circular orbit, the kinetic energy is K = GMm/2r and the potential energy is U = -GMm/r, so the total is E = K + U = -GMm/2r. The potential energy is negative and twice the size of the kinetic energy, so the sum lands below zero. That negative sign is not bookkeeping: it is precisely what it means for the satellite to be bound. To escape, an object must reach at least zero total energy, so anything with negative energy cannot get away. It also tells you how much energy you would need to supply to free it — exactly GMm/2r.

Beyond the syllabus, but worth knowing. Geostationary satellites are not in the 2026-27 NCERT chapter and CBSE does not list them for this chapter, so you will not be examined on them here. The physics is just the orbital-speed result run backwards. A satellite's period depends only on its orbital radius, through T^2 proportional to r^3. Choose the radius that makes T exactly one day, put the satellite in the equatorial plane moving the same way the Earth spins, and it turns at the same rate as the ground below. From the surface it then appears fixed in the sky, which is why dish antennas can be bolted in one position.
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Last reviewed on 6 August 2026. Written and reviewed by subject-matter experts — read about our process.
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