Orbital Motion of Satellites

A satellite in orbit is essentially an object in continuous free fall — it moves so fast horizontally that as it falls toward Earth, the surface curves away beneath it at the same rate. This elegant balance between gravitational attraction and inertia produces circular (or elliptical) orbital paths and represents one of the most beautiful applications of rotational and gravitational dynamics in classical physics. Orbital motion connects Newton's law of universal gravitation with the kinematics of circular motion. The gravitational force between a planet of mass MM and a satellite of mass mm provides exactly the centripetal force required to keep the satellite moving in a curved path. Because the satellite's own mass cancels out of the governing equations, all satellites at the same orbital radius orbit with the same speed and period, regardless of how heavy they are. Understanding satellite orbits is essential for modern technology: GPS constellations, weather satellites, the International Space Station, and communications networks all rely on precise orbital mechanics. The same physics governs natural satellites like the Moon and the moons of other planets, making orbital motion one of the unifying themes of both engineering and astrophysics.

Key takeaways
  • Setting Gravity Equal to Centripetal Force
  • Finding the Orbital Period
  • Orbital Energy
  • Geostationary Orbit

Setting Gravity Equal to Centripetal Force

For a satellite of mass mm orbiting a planet of mass MM at orbital radius rr (measured from the planet's center), Newton's law of universal gravitation gives the attractive force: F_g = \frac{GMm}{r^2} This force acts as the centripetal force keeping the satellite in its circular orbit: F_c = \frac{mv^2}{r} Setting Fg=FcF_g = F_c and cancelling mm from both sides: \frac{GM}{r^2} = \frac{v^2}{r} Solving for orbital speed: v_{\text{orb}} = \sqrt{\frac{GM}{r}} Notice that mm disappeared — the orbital speed depends only on the central mass MM and the orbital radius rr, not on the satellite's own mass.

Finding the Orbital Period

The orbital period TT is the time to complete one full revolution. Since the circumference of a circular orbit is 2πr2\pi r and the satellite travels at speed vorbv_{\text{orb}}: T = \frac{2\pi r}{v_{\text{orb}}} = \frac{2\pi r}{\sqrt{GM/r}} = 2\pi\sqrt{\frac{r^3}{GM}} Squaring both sides reveals Kepler's Third Law: T^2 = \frac{4\pi^2}{GM}\,r^3 This states that the square of the period is proportional to the cube of the orbital radius — a result Kepler discovered empirically decades before Newton derived it from first principles.

Orbital Energy

The total mechanical energy of a satellite combines kinetic and gravitational potential energy. Using vorb2=GM/rv_{\text{orb}}^2 = GM/r, the kinetic energy is: K = \frac{1}{2}mv^2 = \frac{GMm}{2r} The gravitational potential energy (taking zero at infinity) is: U = -\frac{GMm}{r} The total orbital energy is therefore: E = K + U = \frac{GMm}{2r} - \frac{GMm}{r} = -\frac{GMm}{2r} The negative sign indicates a bound orbit. To move a satellite to a higher orbit (larger rr), energy must be added; EE becomes less negative (increases toward zero). A satellite with E=0E = 0 has exactly escape velocity and follows a parabolic trajectory, while E>0E > 0 corresponds to a hyperbolic (unbound) path.

Geostationary Orbit

A geostationary satellite appears stationary over a fixed point on the equator because its orbital period equals Earth's rotation period: T=24 h=86400 sT = 24\text{ h} = 86400\text{ s}. Using Kepler's Third Law, we can solve for the required radius: r = \left(\frac{GMT^2}{4\pi^2}\right)^{1/3} Substituting G=6.674×10−11 N m2kg−2G = 6.674\times10^{-11}\,\text{N m}^2\text{kg}^{-2}, ME=5.972×1024 kgM_E = 5.972\times10^{24}\,\text{kg}, and T=86400 sT = 86400\,\text{s} gives r≈42,164 kmr \approx 42{,}164\,\text{km} from Earth's center, or about 35,786 km35{,}786\,\text{km} above the surface. All geostationary satellites share this single orbital radius.

The Key Equation

vorb=GMrv_{\text{orb}} = \sqrt{\frac{GM}{r}}
  • v_{\text{orb}} — Orbital speed (m/s): The tangential speed required to maintain a circular orbit at radius r
  • G — Gravitational constant (N m² kg⁻²): Universal constant equal to 6.674 × 10⁻¹¹ N m² kg⁻²
  • M — Mass of central body (kg): Mass of the planet or star being orbited (e.g., Earth: 5.972 × 10²⁴ kg)
  • r — Orbital radius (m): Distance from the center of the central body to the satellite

Worked Example

Problem. The International Space Station (ISS) orbits Earth at an altitude of approximately 408 km above the surface. Earth's radius is RE=6.371×106 mR_E = 6.371\times10^6\,\text{m}, Earth's mass is ME=5.972×1024 kgM_E = 5.972\times10^{24}\,\text{kg}, and G=6.674×10−11 N m2kg−2G = 6.674\times10^{-11}\,\text{N m}^2\text{kg}^{-2}. (a) Find the orbital speed of the ISS. (b) Find its orbital period in minutes.

vorb≈7670 m/s,T≈92.6 minv_{\text{orb}} \approx 7670\,\text{m/s},\quad T \approx 92.6\,\text{min}

Answer. The ISS orbits at approximately 7.67 km/s and completes one orbit every 92.6 minutes.

Figure
Diagram
EarthMv_orbF_grGeostationary orbit:r ≈ 42,164 km (T = 24 h)ISS orbit:r ≈ 6,779 km (T ≈ 92.6 min)Circular orbit(dashed)
Origins · 1 minJohannes Kepler and how this was discovered
JK
Johannes Kepler
1571–1630 · German

Kepler formulated his three laws of planetary motion (published 1609–1619) by meticulously analyzing Tycho Brahe's observational data. His Third Law — T2∝r3T^2 \propto r^3 — provided the quantitative relationship between orbital period and distance that Newton later derived from first principles using universal gravitation. Kepler defended his mother against witchcraft charges while simultaneously writing Harmonices Mundi, the book containing his Third Law — a remarkable feat of scientific focus under personal crisis.

  • Centripetal Force and Acceleration — Orbital motion is maintained by gravitational force acting as centripetal force; understanding Fc=mv2/rF_c = mv^2/r is essential to deriving orbital speed.
  • Newton's Law of Universal Gravitation — The gravitational force F=GMm/r2F = GMm/r^2 is the source of the centripetal acceleration in orbital motion and directly determines orbital speed and period.
  • Gravitational Potential Energy — Total orbital energy combines kinetic energy and gravitational potential energy U=−GMm/rU = -GMm/r; negative total energy defines a bound orbit.
  • Conservation of Angular Momentum — Angular momentum L=mvrL = mvr is conserved in orbital motion (no torque), which explains why satellites speed up at closer orbital radii in elliptical orbits (Kepler's Second Law).