The simplest kind of orbit is the circular one: the satellite keeps a constant distance rr from the centre. Here gravity does just one thing, curving the trajectory, and the physics reduces to a single equation. The gravitational force provides exactly the centripetal acceleration required by circular motion:

GMmr2=mv2r    v=GMr\frac{GMm}{r^2} = m\frac{v^2}{r} \;\Rightarrow\; v = \sqrt{\frac{GM}{r}}

Orbital velocity

vorb=GMr\ev{v_\text{orb} = \sqrt{\frac{GM}{r}}} Compared with the escape velocity at the same distance: vorb=vfuga/2v_\text{orb} = v_\text{fuga}/\sqrt{2}. Escaping requires 2\sqrt{2} times the speed needed to orbit.

A counter-intuitive fact emerges from the formula: the higher the orbit (larger rr), the slower the satellite moves. Low satellites zip along, distant ones proceed calmly. This is why the Space Station, in low orbit, travels at 7,7  km/s7{,}7\;\text{km/s}, while a geostationary satellite, much further away, moves at only 3  km/s3\;\text{km/s}.

Geostationary satellite

A geostationary satellite has period T=24  h=86400  sT = 24\;\text{h} = 86\,400\;\text{s}: it must stay fixed relative to a point in the sky. From Kepler’s third law: r3=GMTT24π2    r4,2107  mr^3 = \frac{GM_T T^2}{4\pi^2} \;\Rightarrow\; r \approx 4{,}2\cdot 10^7\;\text{m} that is, about 35800  km35\,800\;\text{km} above the surface (Earth’s radius 6400  km6\,400\;\text{km}). The corresponding orbital velocity is: vorb=GMTr3,1  km/sv_\text{orb} = \sqrt{\frac{GM_T}{r}} \approx 3{,}1\;\text{km/s}

The geostationary orbit is unique: there is only one radius for which the period is exactly 24 hours. This is why satellite dishes can point fixed at one spot in the sky: the satellite there appears motionless.

Topics: Gravitazione Concepts: Orbite · Velocità di fuga · Leggi di Keplero Objects: Satellite

Related exercises: Vero o falso su energia e orbite · Altitudine dell’orbita geostazionaria · Dimostrazione della velocità di fuga