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Physics · Ch 8 — Gravitation

Earth Satellites

8.9

Earth Satellites

Earth Satellites

An object that moves around a planet in a closed orbit is called a satellite. The Moon is Earth's natural satellite. But humans have also placed many artificial satellites in orbit around Earth — these are used for communication, weather monitoring, navigation, and scientific research.

The motion of an Earth satellite is governed entirely by the gravitational force of Earth. For a satellite of mass mm moving in a circular orbit of radius rr (measured from Earth's centre), the gravitational force provides the necessary centripetal acceleration.

Orbital Velocity

For a circular orbit, the gravitational force equals the centripetal force:

GMEmr2=mv2r\frac{G M_E m}{r^2} = \frac{m v^2}{r}

Here MEM_E is Earth's mass, GG is the universal gravitational constant, and vv is the orbital speed. Cancelling mm and one factor of rr gives:

v2=GMErv^2 = \frac{G M_E}{r}

vo=GMErv_o = \sqrt{\frac{G M_E}{r}}

This is the orbital velocity — the speed a satellite must have to stay in a circular orbit of radius rr. Notice that vov_o depends only on rr, not on the satellite's mass. A satellite in a higher orbit (larger rr) moves slower than one in a lower orbit.

Watch out

Do not confuse orbital radius rr with altitude hh above Earth's surface. If RER_E is Earth's radius, then r=RE+hr = R_E + h. Always use rr in the formula.

Time Period of a Satellite

The time period TT is the time taken to complete one full revolution. For a circular orbit of circumference 2πr2\pi r: …

Figure 7.11A hemispherical bowl-shaped shell of uniform density, with force-direction arrows a, b, c radiating from the centre C, and arrows d, e, f, g radiating from an arbitrary point P inside the shell, used to test intuition about gravitational-intensity direction at different points of a hemispherical mass distribution.
Fig. 7.11 — A hemispherical bowl-shaped shell of uniform density, with force-direction arrows a, b, c radiating from the centre C, and arrows d, e, f, g radiating from an arbitrary point P inside the shell, used to test intuition about gravitational-intensity direction at different points of a hemispherical mass distribution.

Drawn by us to help you understand the concept clearly, and verified to make sure it's accurate. For exams, practice from your textbook's own diagram.

The figure shows a hemispherical shell of uniform mass density, drawn in cross-section as a bowl shape. Its centre (the centre of the full sphere the hemisphere is half of) is marked C, sitting on the flat rim of the bowl. Three arrows radiate from C in different directions, labelled a (pointing right), b (pointing up), and c (pointing down) -- these are the candidate directions for the gravitational intensity a test mass would feel if placed exactly at C.

A second point, P, is marked at an arbitrary location inside the shell (not at the centre). Four more arrows radiate from P, labelled d, e, f, g, in different directions -- these are the candidate directions for the gravitational intensity at this off-centre point. …