01
CONCEPT
Newton’s Law of Gravitation
In one line
Every body attracts every other body with a force proportional to the product of their masses and inversely proportional to the square of the distance between them.
Every body attracts every other body with a force proportional to the product of their masses and inversely proportional to the square of the distance between them.
THE LAW
8.1.1 Newton’s law of gravitation
Equal and opposite forces along the line joining the centres
- The force acts along the line joining the two particles.
- The two forces are an action–reaction pair: the earth pulls the moon as hard as the moon pulls the earth.
THE CONSTANT G
8.1.2 Universal gravitational constant
- G equals the force between two unit masses kept unit distance apart.
- Dimensions: [M−1L3T−2].
- First measured by Cavendish with a torsion balance.
- G does not depend on the nature or size of the bodies, or on the medium.
PROPERTIES
8.1.3 Nature of the gravitational force
- Always attractive.
- Independent of the medium between the bodies.
- Acts over a wide range: planets to atoms.
- Central: along the line joining the centres.
- Weakest force in nature: Fnuclear > Felectromagnetic > Fgravitational.
- Between two electrons, gravity is about 10−43 of the electrostatic force.
- Conservative: work around a closed path is zero.
SUPERPOSITION
8.1.4 Force due to many particles
- The force between two particles is not affected by other particles.
- The net force is the vector sum.
- Equal masses placed symmetrically around a point give zero force there.
- A particle at the centre of a uniform ring feels zero force.
- Square of side a with mass m at each corner: force on one mass is
FINITE BODIES
8.1.5 What distance to use
Irregular bodies have no single r; for spheres take the distance between centres
- The law is stated for point masses.
- A uniform sphere acts as a point mass for any point outside it.
- Two identical spheres in contact are 2R apart, with m = 43πR3ρ:
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Vector form of the law
- r21 is the unit vector from m2 to m1; the minus sign shows the force on m1 points towards m2.
- F12 = −F21 is Newton’s third law.
Sphere with a cavity
- Treat the cavity as a filled sphere plus a sphere of negative mass.
- Force of the rest = force of the full sphere − force of the removed part.
- A part of radius Rn has mass Mn3. Measure its distance from its own centre.
Two bodies released from rest
- Their centre of mass stays at rest, so distance covered ∝ one over the mass.
- They collide when the centres are R1 + R2 apart.
Continuous bodies
- Semicircular wire of length L, mass M, at the centre: F = 2πGMmL2.
- Rod with λ(x): F = Gm ∫ λ dxx2.
02
CONCEPT
Acceleration Due to Gravity
In one line
Near a planet every body falls with the same acceleration g, whatever its mass. It depends only on the planet’s mass and radius.
Near a planet every body falls with the same acceleration g, whatever its mass. It depends only on the planet’s mass and radius.
g FROM THE LAW
8.2.1 Acceleration due to gravity
Pull on a body at the surface
- Pull of the earth on the body = mg.
- Put M = volume × density = 43πR3ρ:
- g does not depend on the mass, shape or density of the falling body.
- g is a vector, directed towards the centre of the planet.
- Dimensions [LT−2]; average value 9.8 m s−2.
- GM = gR2: use it to replace GM in every formula.
COMPARING PLANETS
8.2.2 Which formula to use
| Given | Use |
|---|---|
| M and R | g ∝ MR2 |
| ρ and R | g ∝ ρR |
| same density | g ∝ R, and g ∝ M1/3 |
| same mass | g ∝ 1R2 |
| same g | ρ ∝ 1R |
- Radius falls by x% (mass fixed): g rises by 2x%.
- Mass rises by x% (radius fixed): g rises by x%.
- Density falls by x% (radius fixed): g falls by x%.
- Diameter halved (mass fixed): g becomes 4g.
USES OF g
8.2.3 What changes with g on a planet
- Weight: W = mg, while the mass m stays the same.
- Work in lifting a body: W = mgh.
- A seconds pendulum keeps T = 2 s, so its length l ∝ g.
MASS AND DENSITY
8.2.4 Weighing the earth
- With g = 9.8 m s−2 and R = 6400 km, M ≈ 6 × 1024 kg.
- ρ ≈ 5478 kg m−3 for the earth.
- ρ is directly proportional to g.
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Inertial and gravitational mass
- Inertial mass measures opposition to acceleration; an inertial balance measures it.
- Gravitational mass measures the gravitational pull; a spring balance measures it.
- Both are scalars with the same unit, and their ratio is 1.
- A moving body: m = m0√1 − v2/c2.
Mass and weight
| Mass | Weight |
|---|---|
| quantity of matter | pull of the earth on the body |
| does not change with g | changes with g |
| never zero | zero at the centre of the earth |
| kg, [M], scalar | N, [MLT−2], vector |
03
CONCEPT
Variation of g
In one line
g is largest at the surface of the earth. It falls as you go up or down, and it rises from the equator to the poles.
g is largest at the surface of the earth. It falls as you go up or down, and it rises from the equator to the poles.
HEIGHT
8.3.1 g above the surface
r = R + h
- At infinity g′ = 0.
- At h = R: g′ = g4. At h = 2R: g′ = g9.
- Weight changes in the same way: W′ = mg′.
- When h ≪ R:
- Pendulum at height h: T′T = R + hR.
- Seconds pendulum: lhls = (RR + h)2.
DEPTH
8.3.2 g below the surface
Only the inner sphere pulls the body
- At the centre d = R: g′ = 0, so weight is zero.
- At d = R2: g′ = g2.
- To get g′ = gn: d = R(n − 1n).
- Frequency of a pendulum: n′ = n √(1 − dR).
- Capillary rise h ∝ 1g: h2h1 = RR − d in a mine.
HEIGHT AND DEPTH
8.3.3 Comparing the two
g rises in a straight line up to R, then falls
- Same g at height h and depth d (both small): d = 2h, not d = h.
- Going up, g falls twice as fast as going down.
- Ratio: gdgh = R − dR − 2h.
SHAPE
8.3.4 Equator and poles
The equatorial radius is about 21 km longer
- Requator > Rpole, so gpole > gequator.
- Due to shape alone: gp = ge + 0.018 m s−2.
ROTATION
8.3.5 g at latitude λ
Point P moves in a circle of radius r = R cos λ
- The latitude λ is the angle from the equatorial plane.
| Place | λ | g′ |
|---|---|---|
| pole | 90° | g (no effect) |
| equator | 0° | g − ω2R (largest effect) |
- gp − ge = ω2R = 0.034 m s−2 due to rotation.
- Shape and rotation together: gp = ge + 0.052 m s−2.
- If the earth stops rotating, g at the equator rises by ω2R.
- A body hung by a string at the equator:
WEIGHTLESS AT THE EQUATOR
8.3.6 How fast must the earth spin?
- T = 2π√(Rg) ≈ 84.6 minutes ≈ 1.4 h.
- That is about 17 times faster than now.
- To weigh x times the present weight:
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Tunnel through the earth
- Inside the earth the pull is proportional to the distance from the centre.
- A particle in a tunnel along the diameter therefore moves in SHM.
Spring balance: equator and height
- Spring balance reading at the equator = reading at height h over the pole.
04
CONCEPT
Gravitational Field
In one line
The space around a mass where its pull can be felt is its gravitational field. Its strength at a point is the force on a unit mass placed there.
The space around a mass where its pull can be felt is its gravitational field. Its strength at a point is the force on a unit mass placed there.
INTENSITY
8.4.1 Gravitational field intensity
- A vector, directed towards the source of the field.
- Unit: N/kg or m/s2. Dimensions: [M0LT−2].
Field at distance r from a point mass M
- At the surface of the earth, I = g.
- I = 0 at infinity.
- Field lines of an isolated mass point radially inwards.
Field lines around an isolated mass
- Several masses: add the fields as vectors.
NULL POINT
8.4.2 Where the field is zero
P lies between the masses, nearer the smaller one
- Earth and moon (81 : 1): x = 9d10 from the earth.
- A test mass at P feels no force.
FIELD FROM POTENTIAL
8.4.3 Link with V
- V = −Kx gives I = −Kx2.
SOLID SPHERE
8.4.4 Uniform sphere of mass M
Field grows linearly inside and falls outside
| Outside, r > R | Surface, r = R | Inside, r < R |
|---|---|---|
| GMr2 | GMR2 | GMrR3 |
- Point inside and point outside: IoutIin = R3r12r2.
- Largest at the surface; zero at the centre.
SPHERICAL SHELL
8.4.5 Thin shell of mass M
Zero inside, then a jump at the surface
| Outside, r > R | Surface, r = R | Inside, r < R |
|---|---|---|
| GMr2 | GMR2 | 0 |
- Only the mass inside the point counts.
- Sphere inside a shell: between them only the sphere pulls; outside the shell both pull.
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Uniform circular ring
Point P on the axis of a ring of mass M
- I is largest at r = a√2.
Uniform disc
Point P on the axis of a disc of mass M
Sphere with non-uniform density
- Inside, use the mass enclosed: I = G m(r)r2, with m(r) = ∫ 4πr2ρ dr.
- For maximum field set dIdr = 0.
Flux of the gravitational field
- Any closed surface around mass M has flux of magnitude 4πGM.
- Its size and shape do not matter.
05
CONCEPT
Gravitational Potential & Energy
In one line
Potential is the work per unit mass to bring a body from infinity to a point. It is a scalar and is negative everywhere.
Potential is the work per unit mass to bring a body from infinity to a point. It is a scalar and is negative everywhere.
POTENTIAL
8.5.1 Gravitational potential
- Scalar. Unit: J/kg. Dimensions: [M0L2T−2].
- Reference: V = 0 at infinity.
- Given field I(r), find V by integrating: dV = −I dr.
- Uniform field: V = −(Exx + Eyy).
Moving unit mass from A to B
MANY MASSES
8.5.2 Scalar addition
Potentials simply add at P
- Potential at a null point is not zero.
- Masses m and M, distance d, at the null point:
SHELL
8.5.3 Thin spherical shell
Constant inside
| Outside | Surface | Inside |
|---|---|---|
| −GMr | −GMR | −GMR |
- Inside a shell the field is zero, the potential is constant but not zero.
SOLID SPHERE
8.5.4 Uniform sphere
Deepest at the centre
| Outside | Surface | Inside |
|---|---|---|
| −GMr | −GMR | −GM2R3(3R2 − r2) |
POTENTIAL ENERGY
8.5.5 Energy of position
Work done bringing m from infinity to r
- Negative, because the force is attractive.
- Zero (its maximum) at infinity.
- It rises (becomes less negative) as r increases.
- Conservative: work depends only on the end points, not the path.
- At the surface: U = −GMmR.
WORK AGAINST GRAVITY
8.5.6 Raising a body by height h
| h | ΔU |
|---|---|
| R | 12 mgR |
| 2R | 23 mgR |
| 3R | 34 mgR |
| nR | nn + 1 mgR |
| h ≪ R | mgh |
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Potential of a ring
Energy of a system of masses
- Count each pair once.
- n masses have n(n − 1)2 pairs.
- Work to expand or shrink a system = Ufinal − Uinitial.
Energy to break up the earth
- Supplying this much energy takes all its mass to infinity.
06
CONCEPT
Escape Velocity
In one line
Escape velocity is the least speed a body needs at the surface to leave the planet’s pull for ever. It does not depend on the body’s mass or direction.
Escape velocity is the least speed a body needs at the surface to leave the planet’s pull for ever. It does not depend on the body’s mass or direction.
THE FORMULA
8.6.1 Kinetic energy pays for the escape
- Work to go from the surface to infinity:
- For the earth: 11.2 km s−1.
- Independent of the mass of the body and of the angle of projection.
- Escape energy = GMmR.
- Ant or elephant: the same speed.
COMPARING PLANETS
8.6.2 Which formula to use
| Given | Use |
|---|---|
| M and R | ve ∝ √MR |
| g and R | ve ∝ √gR |
| same density | ve ∝ R |
| ρ and R | ve ∝ R√ρ |
- Radius doubled at the same density: escape velocity doubled.
- Radius doubled at the same mass: it becomes 1 ÷ √2 times.
- vo = orbital speed close to the surface.
v LESS THAN ve
8.6.3 Maximum height reached
- If v = kve:
| v | h |
|---|---|
| 12 ve | R3 |
| 13 ve | R8 |
| KE = half the escape KE | R |
v GREATER THAN ve
8.6.4 Speed far away
- v = 3ve gives v′ = 2√2 ve.
FALLING BODIES
8.6.5 Speed on reaching the surface
- The same energy equation, read backwards.
- From infinity: v = ve = 11.2 km s−1.
- Small h: v = √(2gh).
- KE gained between two points: GMm(1r2 − 1r1).
OTHER STARTING POINTS
8.6.6 Not from the surface
- Use the potential at the starting point:
- From height h = 3R, r = 4R: v = √GM2R.
- Between earth and moon: V has a term from each.
- At a distance r3 from M1, on the line to M2:
- A satellite near the surface needs its speed raised by the factor √2 (41.4% more) to escape.
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Why some planets have no atmosphere
- A planet keeps its atmosphere if vrms of its gas molecules is less than its escape velocity.
- Earth keeps it. The moon has vrms > ve, so it has no atmosphere.
Black hole
- If the escape velocity equals the speed of light c, nothing can escape, not even light.
Two planets starting at rest far apart
- When they are a distance d apart, use momentum and energy conservation together.
- Two planets: v1 = m2√2Gd(m1 + m2).
07
CONCEPT
Kepler’s Laws of Planetary Motion
In one line
Planets move in ellipses with the sun at a focus, sweep equal areas in equal times, and obey T2 ∝ a3.
Planets move in ellipses with the sun at a focus, sweep equal areas in equal times, and obey T2 ∝ a3.
THE THREE LAWS
8.7.1 Kepler’s laws
- Law of orbits: every planet moves in an ellipse with the sun at one focus.
- Law of areas: the line from the sun to a planet sweeps equal areas in equal times.
- Law of periods: T2 ∝ a3, where a is the semi-major axis.
The sun is at one focus
LAW OF AREAS
8.7.2 Areal velocity
The two shaded areas take equal times
- Comes from conservation of angular momentum.
- The planet moves fastest when nearest the sun.
- Time taken ∝ area swept.
LAW OF PERIODS
8.7.3 Comparing planets
- For the earth T = 1 year.
- Period 8 times ⇒ radius 4 times.
- Radius 14 ⇒ period 18.
- Radius 3 times ⇒ period 3√3 times.
- These laws hold for satellites too.
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Perigee and apogee
- Force is central ⇒ no torque ⇒ angular momentum conserved.
- rp = a − c and ra = a + c, where e = c ÷ a.
Speeds in terms of eccentricity
- Kinetic energy is greatest at perigee and least at apogee.
- Total energy stays constant along the orbit.
08
CONCEPT
Satellites: Orbital Velocity & Period
In one line
Gravity supplies the centripetal force of a satellite. So its speed and period depend on the orbit radius and the planet’s mass, not on the satellite’s mass.
Gravity supplies the centripetal force of a satellite. So its speed and period depend on the orbit radius and the planet’s mass, not on the satellite’s mass.
ORBITAL VELOCITY
8.8.1 Speed in a circular orbit
r = R + h
- Independent of the mass of the satellite.
- Depends on the central mass and the orbit radius.
- Planets around the sun obey the same rule.
- r four times ⇒ speed half.
- If gravity vanished, the satellite would fly off along the tangent.
- A ball released from a satellite stays in the same orbit.
NEAR THE SURFACE
8.8.2 h ≪ R
- At radius nR: speed = 7.9√n km s−1.
- At altitude nR: speed = 7.9√(1 + n) km s−1.
WHAT THE SPEED DOES
8.8.3 Horizontal velocity VH at a height
| VH | Path |
|---|---|
| less than Vc | falls back to the earth |
| equal to Vc | circular orbit |
| between Vc and Ve | elliptical orbit |
| Ve or more | escapes |
- Vc is the critical (orbital) velocity at that height.
TIME PERIOD
8.8.4 One revolution
- Independent of the mass of the satellite.
- r four times ⇒ T eight times.
- At h = R: T = 4π√(2Rg).
NEAR THE SURFACE
8.8.5 Shortest period
- T2ρ = 3πG, a constant.
OTHER FORCE LAWS
8.8.6 If F ∝ 1 ÷ rⁿ
- Equate mv2/r to the force, then read off the powers.
- n = 2 gives back T ∝ r3/2.
- n = 52 gives T ∝ r7/4.
MUTUAL ORBITS
8.8.7 Particles moving under their own gravity
- Find the net pull towards the centre; set it equal to mv2/r.
- Two particles sit a diameter apart: the distance in the law is 2r, the radius in the orbit is r.
| System | Result |
|---|---|
| two masses m, circle r | v = √Gm4r |
| three masses, side L | T ∝ L3/2 |
| four masses M, circle R | v = 12√GMR(1 + 2√2) |
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Binary stars
- Both stars move about the common centre of mass with the same ω and T.
- For masses m1, m2 a distance d apart:
Other mass distributions
- Find M enclosed within r, then mv2r = F.
- Density ρ ∝ 1 ÷ r2: T ∝ r.
- Long cylinder: field ∝ 1 ÷ r, so v is constant and T ∝ r.
09
CONCEPT
Geostationary Satellite & Angular Momentum
In one line
A geostationary satellite has the same period as the earth’s spin, so it seems fixed in the sky. A satellite’s angular momentum grows as √r.
A geostationary satellite has the same period as the earth’s spin, so it seems fixed in the sky. A satellite’s angular momentum grows as √r.
HEIGHT OF A SATELLITE
8.9.1 From its period
GEOSTATIONARY SATELLITE
8.9.2 Fixed over one place
A communication satellite in the parking orbit
- Orbit must be concentric and coplanar with the equator.
- Sense of rotation same as the earth: west to east.
- Period equal to the earth’s: T = 24 h.
- The orbit is called the parking orbit.
ITS ORBIT
8.9.3 Radius, height and speed
- r ≈ 42000 km ≈ 7R.
- Height h ≈ 36000 km ≈ 6R.
- Speed v ≈ 3.08 km s−1.
- Rearranged: R2 = r3ω2 ÷ g.
USING T ∝ r3/2
8.9.4 Another satellite of the same planet
- Add R to each height first: use the radius from the centre.
- Radius half of the geostationary radius: T = 24 ÷ 2√2 = 6√2 h.
- Radius one-fourth: T = 3 h.
- Another planet: r3 ∝ MT2.
ANGULAR MOMENTUM
8.9.5 Of a satellite
- Depends on both masses and on the orbit radius.
- Force is central ⇒ torque = 0 ⇒ L is conserved.
- “Increased by eight times” means r′ = 9r, so L′ = 3L.
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Satellite seen from the earth
- A satellite in the equatorial plane moving west to east has relative angular velocity ωS − ωE.
- If ωS = ωE the time is infinite: the satellite looks stationary.
10
CONCEPT
Satellite Energy & Weightlessness
In one line
A satellite’s total energy is negative: it is bound to the planet. Its kinetic energy is half the size of its potential energy.
A satellite’s total energy is negative: it is bound to the planet. Its kinetic energy is half the size of its potential energy.
THE THREE ENERGIES
8.10.1 In a circular orbit
- K = −E; U = 2E; U = −2K.
- K : |U| = 1 : 2.
- With GM = gR2: K = mgR22r.
- Orbit radius r = 4R: K = mgR8.
- E ∝ mr: two satellites compare through m and r.
K is positive; U and E are negative
BINDING ENERGY
8.10.2 To free the satellite
- The energy needed to take the satellite from its orbit to infinity.
LAUNCHING
8.10.3 From the surface into orbit
| Altitude | r | Energy |
|---|---|---|
| R | 2R | 3GMm4R |
| 2R | 3R | 5GMm6R |
| 3R | 4R | 7GMm8R |
- Add R to the altitude before using the formula.
RAISE AND ORBIT
8.10.4 Two different jobs
CHANGE OF ORBIT
8.10.5 Moving to a higher orbit
From r1 to r2
| Quantity | As r rises | Relation |
|---|---|---|
| speed | falls | v ∝ 1√r |
| period | rises | T ∝ r3/2 |
| linear momentum | falls | p ∝ 1√r |
| angular momentum | rises | L ∝ √r |
| kinetic energy | falls | K ∝ 1r |
| potential energy | rises | U ∝ −1r |
| total energy | rises | E ∝ −1r |
| binding energy | falls | BE ∝ 1r |
WEIGHTLESSNESS
8.10.6 Weight is the reaction of the support
- You feel your weight only when something opposes it.
- If the support gives no reaction, the apparent weight is zero.
Gravity alone provides the acceleration
- Seen in free fall, in an orbiting satellite and at null points in space.
- Gravity is not zero in a satellite; it is what keeps the satellite in orbit.
- A pendulum in a satellite does not oscillate: T is infinite.
- A spring balance still works, by measuring a force other than weight.
- On the moon a person is not weightless, because the moon’s own gravity acts.
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Energy in an elliptical orbit
KE is largest at perigee, PE is largest at apogee
- a is the semi-major axis; E depends only on a.
Collisions in orbit
- Find the speed just after the collision by conserving momentum.
- Same speed as orbital speed: circular. Different but less than escape speed: ellipse.
- A satellite whose speed is raised by the factor √2 escapes.
Splitting and launching
- Rockets ejected: use momentum conservation for the parts.
- Energy accounts must include both KE and PE of every part.
EXAM-DAY CARD
Just see this before the exam
F = Gm1m2r2
Newton
g = GMR2
at the surface
I = GMr2
field
ve = √2gR
escape
T2 ∝ a3
Kepler
E = −GMm2r
satellite
FORMULA SHEET
Whole chapter on one page
Law & g
F = Gm1m2r2
g = GMR2 = 43πρGR
M = gR2G, ρ = 3g4πGR
Variation of g
g′ = g(RR + h)2
h ≪ R: g(1 − 2hR)
g′ = g(1 − dR)
g′ = g − ω2R cos2λ
Field
I = GMr2, I = −dVdr
sphere inside: GMrR3
shell inside: 0
x = √m1 d√m1 + √m2
Potential & PE
V = −GMr, U = −GMmr
Vc = 32 Vs (sphere)
ΔU = mgh1 + hR
h = nR: nn + 1 mgR
Escape
ve = √2GMR = √2gR
h = Rk21 − k2
v′ = √v2 − ve2
ve = √2 vo
Satellites
v = √GMr, T = 2π√r3GM
L = m√GMr
K = GMm2r, E = −K, U = 2E
rgeo = (gR2ω2)1/3
TOP MISTAKES
Avoid these = easy marks
MISTAKE ✗
Same g at height h and depth h
Using height h where r is needed
Gravity is zero in a satellite
Launch energy = orbital KE only
CORRECT ✓
d = 2h for the same g
r = R + h, always from the centre
N = 0, but gravity still acts
Energy = GMmR − GMm2r