Gravitational Fields

Newton's law of gravitation; g = GM/r²; gravitational potential; orbits

# Gravitational Fields — A-Level Physics

Gravitational fields describe how masses interact at a distance. At A-Level, we move from the simplified F=mgF = mg to Newton's Law of Gravitation and the concept of gravitational potential.


1. Newton's Law of Gravitation

F=GMmr2\boxed{F = \frac{GMm}{r^2}}

Where:

  • G=6.67×1011G = 6.67 \times 10^{-11} N m² kg⁻² (gravitational constant)
  • MM, mm = masses (kg)
  • rr = distance between centres (m)

The force is always attractive and acts along the line joining the centres.

2. Gravitational Field Strength

g=Fm=GMr2\boxed{g = \frac{F}{m} = \frac{GM}{r^2}}

Units: N/kg or m/s²

  • At Earth's surface: g=9.81g = 9.81 N/kg
  • gg decreases with r2r^2 (inverse square law)
  • Inside a uniform sphere: gg increases linearly from centre to surface

Field Lines

  • Point towards the mass (direction of force on test mass)
  • Closer lines = stronger field
  • Radial field for point/spherical masses
  • Uniform field near Earth's surface (parallel lines, constant gg)

3. Gravitational Potential

V=GMr\boxed{V = -\frac{GM}{r}}

  • Units: J/kg
  • Always negative (zero at infinity)
  • The work done per unit mass to bring a test mass from infinity to that point

Gravitational Potential Energy

Ep=mV=GMmrE_p = mV = -\frac{GMm}{r}

4. Relationship Between $g$ and $V$

g=dVdrg = -\frac{dV}{dr}

gg = negative gradient of the VV vs rr graph.

5. Orbits

For a circular orbit, gravitational force provides centripetal force:

GMmr2=mv2r\frac{GMm}{r^2} = \frac{mv^2}{r}

v=GMrv = \sqrt{\frac{GM}{r}}

Period of Orbit

T=2πr/v=2πr3GMT = 2\pi r/v = 2\pi\sqrt{\frac{r^3}{GM}}

This gives Kepler's Third Law: T2r3T^2 \propto r^3

Geostationary Orbit

  • Period = 24 hours (synchronous with Earth)
  • Orbits above the equator
  • Used for communications satellites
  • r42,200r \approx 42{,}200 km from Earth's centre

6. Escape Velocity

The minimum speed to escape a gravitational field (reach infinity with zero KE):

12mv2=GMmr\frac{1}{2}mv^2 = \frac{GMm}{r} vesc=2GMr\boxed{v_{\text{esc}} = \sqrt{\frac{2GM}{r}}}

Worked Example: Example 1

Problem

Calculate gg at a height of 400 km above Earth (RE=6.37×106R_E = 6.37 \times 10^6 m, ME=5.97×1024M_E = 5.97 \times 10^{24} kg).

r=6.37×106+4×105=6.77×106r = 6.37 \times 10^6 + 4 \times 10^5 = 6.77 \times 10^6 m g=GM/r2=6.67×1011×5.97×1024/(6.77×106)2=3.98×1014/4.58×1013=8.69g = GM/r^2 = 6.67 \times 10^{-11} \times 5.97 \times 10^{24}/(6.77 \times 10^6)^2 = 3.98 \times 10^{14}/4.58 \times 10^{13} = 8.69 N/kg

Solution

Worked Example: Orbital Speed

Problem

Find the speed of the ISS at 400 km altitude.

v=GM/r=3.98×1014/6.77×106=5.88×107=7670v = \sqrt{GM/r} = \sqrt{3.98 \times 10^{14}/6.77 \times 10^6} = \sqrt{5.88 \times 10^7} = 7670 m/s

Solution

Worked Example: Gravitational Potential

Problem

Find the gravitational potential at the Moon's orbit (r=3.84×108r = 3.84 \times 10^8 m).

V=GM/r=6.67×1011×5.97×1024/3.84×108=1.04×106V = -GM/r = -6.67 \times 10^{-11} \times 5.97 \times 10^{24}/3.84 \times 10^8 = -1.04 \times 10^6 J/kg

Solution

8. Practice Questions

    1. Calculate the gravitational force between Earth and the Moon (ME=5.97×1024M_E = 5.97 \times 10^{24} kg, MM=7.35×1022M_M = 7.35 \times 10^{22} kg, r=3.84×108r = 3.84 \times 10^8 m). (2 marks)
    1. A satellite orbits at 2RE2R_E from Earth's centre. If gg at the surface is 9.81 N/kg, find gg at the satellite. (2 marks)
    1. Calculate the escape velocity from Earth's surface. (2 marks)
    1. Show that T2r3T^2 \propto r^3 for circular orbits. (3 marks)

    Answers

    1. F=GMm/r2=6.67×1011×5.97×1024×7.35×1022/(3.84×108)2=1.98×1020F = GMm/r^2 = 6.67 \times 10^{-11} \times 5.97 \times 10^{24} \times 7.35 \times 10^{22}/(3.84 \times 10^8)^2 = 1.98 \times 10^{20} N.

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Summary

  • F=GMm/r2F = GMm/r^2; g=GM/r2g = GM/r^2; V=GM/rV = -GM/r
  • g=dV/drg = -dV/dr
  • Orbital speed: v=GM/rv = \sqrt{GM/r}; Kepler: T2r3T^2 \propto r^3
  • Escape velocity: v=2GM/rv = \sqrt{2GM/r}
  • All potentials are negative; zero at infinity

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