178FieldsStretch

Gravitational Potential

Near Earth’s surface, mgΔhmg\Delta h is good enough for potential energy. But launch a spacecraft thousands of kilometres up and gg is no longer constant. Gravitational potential\textbf{Gravitational potential} handles changing fields properly, and it explains why the energy needed to escape a planet entirely is finite.

35 min Topic 12 · Gravitational Fields

What you'll be able to do

  • Define gravitational potential and explain why it is negative
  • Use Vgrav=−GM/rV_{\text{grav}} = -GM/r and ΔEp=mΔV\Delta E_{p} = m\Delta V
  • Relate field strength to potential gradient, g=−ΔV/Δrg = -\Delta V/\Delta r
  • Derive and use escape velocity, v=2GM/rv = \sqrt{2GM/r}
1

Potential in a radial field

The gravitational potential\textbf{gravitational potential} at a point is the work done per unit mass in bringing a small mass from infinity to that point. It is measured in J kg−1\mathrm{J\,kg^{-1}}.

At infinity the potential is zero. Because gravity attracts, the field does work on a mass as it moves inwards, so the work done by an external agent\textit{by an external agent} is negative, and potential at every finite distance is negative.

For a spherical mass MM, the potential at distance rr from the centre is V=−GM/rV = -GM/r. It rises towards zero as rr increases.

Vgrav=−GMrV_{\text{grav}} = -\dfrac{GM}{r}
Potential in a radial field.
Example 1Find the gravitational potential at Earth’s surface. M=5.97×1024M = 5.97\times10^{24} kg, R=6.37×106R = 6.37\times10^{6} m.
1V=−6.67×10−11×5.97×10246.37×106V = -\dfrac{6.67\times10^{-11} \times 5.97\times10^{24}}{6.37\times10^{6}}.
Answer−6.25×107 J kg−1-6.25\times10^{7}\ \mathrm{J\,kg^{-1}}
2

Potential energy and work

A mass mm at a point of potential VV has gravitational potential energy Ep=mV=−GMm/rE_{p} = mV = -GMm/r.

The work done moving a mass between two points is ΔEp=mΔV\Delta E_{p} = m\Delta V. Moving outwards, VV becomes less negative, so ΔV\Delta V is positive and work must be done.

For small height changes near the surface, mΔVm\Delta V reduces to the familiar mgΔhmg\Delta h. For large changes, mgΔhmg\Delta h overestimates the energy because gg decreases with height.

ΔEp=mΔV\Delta E_{p} = m\Delta V
Work done moving a mass.
Example 1How much energy is needed to lift a 500 kg satellite from Earth’s surface to an orbit radius of 1.20×1071.20\times10^{7} m (ignoring its kinetic energy)?
1Vorbit=−3.982×10141.20×107=−3.318×107 J kg−1V_{\text{orbit}} = -\dfrac{3.982\times10^{14}}{1.20\times10^{7}} = -3.318\times10^{7}\ \mathrm{J\,kg^{-1}}.
2ΔV=−3.318×107−(−6.251×107)=2.933×107\Delta V = -3.318\times10^{7} - (-6.251\times10^{7}) = 2.933\times10^{7}.
3ΔEp=500×2.933×107\Delta E_{p} = 500 \times 2.933\times10^{7}.
Answer1.47×1010 J1.47\times10^{10}\ \mathrm{J}

Tip — Using mgΔhmg\Delta h with g=9.81g = 9.81 here would give 2.8×10102.8\times10^{10} J — nearly double. Large height changes always need mΔVm\Delta V.

3

Field as potential gradient and equipotentials

Field strength is the negative of the potential gradient: g=−ΔV/Δrg = -\Delta V/\Delta r. On a graph of VV against rr, the gradient at any point gives the field strength there.

Equipotential surfaces\textbf{Equipotential surfaces} join points of equal potential. Around a planet they are concentric spheres, spaced further apart with increasing distance. No work is done moving along one.

Equipotentials are perpendicular to field lines, exactly as in electric fields.

g=−ΔVΔrg = -\dfrac{\Delta V}{\Delta r}
Field from potential gradient.

Tip — For equal steps in potential, equipotentials get further apart moving outwards because the field weakens.

4

Escape velocity

To escape a planet’s gravity completely, a projectile must reach infinity, where Ep=0E_{p} = 0. It must therefore start with kinetic energy at least equal to the depth of the potential well.

Setting 12mv2=GMm/r\tfrac12 mv^{2} = GMm/r gives the escape velocity\textbf{escape velocity}. It does not depend on the projectile’s mass, and it ignores air resistance.

For Earth it is about 11.2 km s−111.2\ \mathrm{km\,s^{-1}}. A black hole is an object whose escape velocity at its surface exceeds the speed of light.

vesc=2GMrv_{\text{esc}} = \sqrt{\dfrac{2GM}{r}}
Escape velocity.
Example 1Find the escape velocity from the Moon. M=7.35×1022M = 7.35\times10^{22} kg, R=1.74×106R = 1.74\times10^{6} m.
1v=2×6.67×10−11×7.35×10221.74×106v = \sqrt{\dfrac{2 \times 6.67\times10^{-11} \times 7.35\times10^{22}}{1.74\times10^{6}}}.
Answer2.37×103 m s−12.37\times10^{3}\ \mathrm{m\,s^{-1}}

Equation recap

V=−GM/rV = -GM/r
Radial field potential.
ΔEp=mΔV\Delta E_{p} = m\Delta V
Work done.
g=−ΔV/Δrg = -\Delta V/\Delta r
Field from potential.
vesc=2GM/rv_{\text{esc}} = \sqrt{2GM/r}
Escape velocity.

Common mistakes to avoid

Giving gravitational potential as positive.
It is negative everywhere at finite distance.
Using mgΔhmg\Delta h for a satellite launch.
gg changes with height; use mΔVm\Delta V.
Writing V=−GM/r2V = -GM/r^{2}.
Potential goes as 1/r1/r; field strength as 1/r21/r^{2}.
Thinking escape velocity depends on mass launched.
mm cancels in the derivation.

Key takeaways

  • Gravitational potential is work per unit mass from infinity; it is always negative.
  • Radial field: V=−GM/rV = -GM/r; potential energy Ep=−GMm/rE_{p} = -GMm/r.
  • Work done =mΔV= m\Delta V; field strength g=−ΔV/Δrg = -\Delta V/\Delta r.
  • Equipotentials are perpendicular to field lines.
  • Escape velocity v=2GM/rv = \sqrt{2GM/r} is independent of projectile mass.

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