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Mathematical Methods for Physicists: A concise introduction - Site Map

Mathematical Methods for Physicists: A concise introduction - Site Map

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THE CALCULUS OF VARIATIONS<br />

p<br />

Letting 1=c ˆ a and solving <strong>for</strong> y<br />

0<br />

gives<br />

y 0 ˆ dy<br />

dx ˆ<br />

and solving <strong>for</strong> dx and integrating we obtain<br />

Z<br />

Z<br />

dx ˆ<br />

r<br />

a y<br />

;<br />

y<br />

r<br />

y<br />

dy:<br />

a y<br />

We then let<br />

y ˆ a sin 2 ˆ a …1 cos 2†<br />

2<br />

which leads to<br />

Z<br />

x ˆ 2a<br />

Z<br />

sin 2 d ˆ a<br />

…1 cos 2†d ˆ a …2 sin 2†‡k:<br />

2<br />

Thus the parametric equation of the path is given by<br />

x ˆ b…1 cos †;<br />

y ˆ b… sin †‡k;<br />

where b ˆ a=2;ˆ 2. The path passes through the origin so we have k ˆ 0 and<br />

x ˆ b…1 cos †;<br />

y ˆ b… sin †:<br />

The constant b is determined from the condition that the particle passes through<br />

P 2 …x 2 ; y 2 †:<br />

The required path is a cycloid and is the path of a ®xed point P 0 on a circle of<br />

radius b as it rolls along the x-axis (Fig. 8.3).<br />

A line that represents the shortest path between any two points on some surface<br />

is called a geodesic. On a ¯at surface, the geodesic is a straight line. It is easy to<br />

show that, on a sphere, the geodesic is a great circle; we leave this as an exercise<br />

<strong>for</strong> the reader (Problem 8.3).<br />

Figure 8.3.<br />

352

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