3.7.2.4 - Orbits of Planets and Satellites

3.7.2.4 - Orbits of Planets and Satellites

Use gravity as the centripetal force to derive circular-orbit speed and period. Track kinetic, potential and total energy to explain orbital changes and escape, then select an orbit suitable for a satellite’s purpose.

Circular-orbit speed, period and graph tests

A circular orbit needs an inward acceleration even when speed is constant, because velocity changes direction. In the model below gravity alone supplies that acceleration: a satellite of mass mm orbits a much larger spherical mass MM, with negligible drag, thrust and influence from other bodies. Measure orbital radius rr from the source centre.

Equate gravitational force to the required centripetal force, rather than adding “centripetal force” as a second physical interaction:

GMmr2=mv2r⇒v=GMr.\frac{GMm}{r^2}=\frac{mv^2}{r}\quad\Rightarrow\quad v=\sqrt{\frac{GM}{r}}.

The satellite mass cancels. For the same source, a higher circular orbit has lower speed. Doubling radius reduces speed by 1/21/\sqrt2. The force is radial and velocity tangential, so gravity changes velocity’s direction without doing work in this circular orbit.

For one circuit, v=2πr/Tv=2\pi r/T. Substituting into the force relation gives

GMmr2=4π2mrT2⇒T2=4π2GMr3.\frac{GMm}{r^2}=\frac{4\pi^2mr}{T^2}\quad\Rightarrow\quad T^2=\frac{4\pi^2}{GM}r^3.

Thus T2∝r3T^2\propto r^3 for circular orbits around the same central mass. If the radius doubles, the period becomes 23/2=222^{3/2}=2\sqrt2 times as long. An elliptical orbit has changing speed and radius; the constant-radius derivation must not be applied to its instantaneous radius.

Inferring a central mass and testing a power law

A plot of T2T^2 against r3r^3 is a straight line through the origin, with gradient 4π2/(GM)4\pi^2/(GM) in s2 m−3\mathrm{s^2\,m^{-3}}. Rearrange the gradient to infer MM. For example, a gradient 9.86×10−14 s2 m−39.86\times10^{-14}\,\mathrm{s^2\,m^{-3}} gives M=6.00×1024 kgM=6.00\times10^{24}\,\mathrm{kg} using G=6.67×10−11 N m2 kg−2G=6.67\times10^{-11}\,\mathrm{N\,m^2\,kg^{-2}}.

Choose a reference radius r0r_0 and let T0T_0 be its circular-orbit period around the same mass. Taking logarithms gives

log⁡(T/T0)=32log⁡(r/r0).\log(T/T_0)=\tfrac32\log(r/r_0).

The reference values make the ratios dimensionless. A plot of log⁡(T/T0)\log(T/T_0) against log⁡(r/r0)\log(r/r_0) has gradient 1.51.5, not 33. A plot of log⁡(T2/T02)\log(T^2/T_0^2) against log⁡(r/r0)\log(r/r_0) instead has gradient 33. Read both axes before interpreting a logarithmic gradient.

[DIAGRAM: asset_name: 7.2.4 - Orbits of Planets and Satellites - Diagram 1; asset_slug: 7.2.4 - Orbits of Planets and Satellites - Diagram 1; recommended_method: retained_png; caption: Circular-orbit graph tests. T₀ is the period at radius r₀. The logarithmic gradient is 1.5.; description: Exact circular-orbit plots for one central mass: T² against r³ is linear, while log(T/T₀) against log(r/r₀) has gradient 1.5. The points are model satellite data, not evenly spaced real planets.]
Circular-orbit graph tests. T₀ is the period at radius r₀. The logarithmic gradient is 1.5.

For an order-of-magnitude check on Earth’s orbital kinetic energy, estimate MS∼2×1030 kgM_S\sim2\times10^{30}\,\mathrm{kg}, mE∼6×1024 kgm_E\sim6\times10^{24}\,\mathrm{kg} and r∼1.5×1011 mr\sim1.5\times10^{11}\,\mathrm m. Then v∼3×104 m s−1v\sim3\times10^4\,\mathrm{m\,s^{-1}} and K∼12(6×1024)(3×104)2∼3×1033 JK\sim\tfrac12(6\times10^{24})(3\times10^4)^2\sim3\times10^{33}\,\mathrm J.

Kinetic, potential and total orbital energy

A circularly orbiting satellite has positive kinetic energy and negative gravitational potential energy when the zero is at infinity. Substituting v2=GM/rv^2=GM/r gives

K=12mv2=GMm2r,U=−GMmr.K=\tfrac12mv^2=\frac{GMm}{2r},\qquad U=-\frac{GMm}{r}. E=K+U=−GMm2r.E=K+U=-\frac{GMm}{2r}.

Thus U=−2KU=-2K and E=−K=U/2E=-K=U/2 for a circular orbit. The negative total energy means the satellite is gravitationally bound in this isolated two-body model. Potential energy being negative alone is insufficient: a sufficiently fast object can have nonnegative total energy and escape.

[DIAGRAM: asset_name: 7.2.4 - Orbits of Planets and Satellites - Diagram 2; asset_slug: 7.2.4 - Orbits of Planets and Satellites - Diagram 2; recommended_method: retained_png; caption: Energies of alternative circular orbits: U = −2K and E = −K. R and E₀ are fixed reference scales.; description: Exact circular-orbit energies. The fixed reference E₀ = GMm/(2R) makes the vertical coordinate dimensionless; at each radius U = −2K and E = −K. These are alternative circular orbits, not successive positions in one ellipse.]
Energies of alternative circular orbits: U = −2K and E = −K. R and E₀ are fixed reference scales.

Compare two circular orbits. At larger rr, KK decreases, UU increases towards zero, and EE increases towards zero. Energy must therefore be supplied to reach the higher circular orbit even though the final speed is lower. The potential-energy increase is twice the magnitude of the kinetic-energy decrease.

For a 400 kg400\,\mathrm{kg} satellite raised from r1=7.0×106r_1=7.0\times10^6 to r2=8.0×106 mr_2=8.0\times10^6\,\mathrm m around M=6.0×1024 kgM=6.0\times10^{24}\,\mathrm{kg},

ΔE=GMm2(1r1−1r2)=+1.43×109 J.\Delta E=\frac{GMm}{2}\left(\frac1{r_1}-\frac1{r_2}\right)=+1.43\times10^9\,\mathrm J.

The final kinetic energy is lower by 1.43×109 J1.43\times10^9\,\mathrm J, while potential energy rises by 2.86×109 J2.86\times10^9\,\mathrm J. A real transfer involves thrust and a non-circular path between these two states; the circular formulas describe its endpoints. Conversely, slow orbital decay through weak drag can reduce total energy while the speed of the eventual lower orbit is higher.

Escape speed from energy conservation

Escape speed is the minimum initial speed at a specified radius that lets an unpowered object reach indefinitely large distance with no remaining kinetic energy. The often-used name “escape velocity” refers to this speed threshold, not a single required direction.

Assume an isolated, non-rotating spherical source, no atmosphere or other dissipative force, no further thrust and a trajectory that does not hit the source. Energy conservation for marginal escape gives

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