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Isotropic case: <v2> = 3<vr2>� (why?)
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If
velocity dispersion independent of masses:
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T = 3/2 M <vr2>,
where M is total mass
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More
complex if the above is not true.
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Assuming
spherical symmetry and an
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observed
surface distribution, get a weighted
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mean
separation Rcl:
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