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Astronomy Principles and Practice Fourth Edition.pdf

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The two-body problem 181<br />

Figure 13.8. Example 13.1—the orbit of an artificial satellite.<br />

The size of the major axis AA ′ of the ellipse is given by<br />

AA ′ = 4023 + 2 × 6372 + 660 = 17 427 km<br />

so that the semi-major axis a 1 is of length 8713·5 km. The period of revolution is T 1 = 134 minutes.<br />

For the Earth orbit,<br />

a = 149·5 × 10 6 km<br />

T = 365·25 × 24 × 60 = 5·2596 × 10 5 minutes.<br />

Letting M <strong>and</strong> m be the masses of Sun <strong>and</strong> Earth respectively, we have, using equation (13.35),<br />

(<br />

) ( )<br />

M<br />

m = 134 2 3<br />

149·5 × 10<br />

6<br />

5·2596 × 10 5 8713·5<br />

giving, after a little calculation,<br />

M<br />

= 327 800.<br />

m<br />

Hence, the Earth’s mass is only about three-millionths that of the Sun.<br />

13.6.8 Co-periodic orbits<br />

Rewriting equation (13.31), we have<br />

( )1<br />

a<br />

3 2<br />

T = 2π . (13.31)<br />

µ<br />

Re-arranging equation (13.29), we obtain<br />

/ ( 2<br />

a = 1<br />

r − V )<br />

2<br />

. (13.36)<br />

µ<br />

If we eliminate a between equations (13.31) <strong>and</strong> (13.36), there results<br />

( 2µ<br />

T = 2πµ<br />

r<br />

− V 2 ) −3/2<br />

. (13.37)<br />

Equations (13.31), (13.36) <strong>and</strong> (13.37) highlight some interesting properties of elliptical motion.<br />

It is seen that the semi-major axis is a function of the radius vector <strong>and</strong> the square of the velocity.<br />

If, therefore, a body of mass m 1 is projected at a given distance r from another body of mass m 2 with

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