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Exact Solutions and Scalar Fields in Gravity - Instituto Avanzado de ...

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Rotat<strong>in</strong>g equilibrium configurations <strong>in</strong> E<strong>in</strong>ste<strong>in</strong>’s theory of gravitation 71<br />

2. ROTATING DUST CONFIGURATIONS –<br />

THE MACLAURIN DISK<br />

In Newton’s theory of gravitation, it can easily be shown that a rotat<strong>in</strong>g,<br />

axially symmetric <strong>and</strong> stationary dust (Here “dust” means a perfect<br />

fluid with vanish<strong>in</strong>g pressure.) configuration of f<strong>in</strong>ite mass must be an<br />

<strong>in</strong>f<strong>in</strong>itesimally th<strong>in</strong> disk.<br />

Therefore, the basic equations to be solved are the Poisson equation<br />

<strong>and</strong> the equation express<strong>in</strong>g the equilibrium between centrifugal <strong>and</strong><br />

gravitational forces <strong>in</strong> the disk<br />

Here U is the gravitational potential, <strong>and</strong> are cyl<strong>in</strong>drical coord<strong>in</strong>ates.<br />

It should be noted that for a prescribed rotation law the<br />

surface mass–<strong>de</strong>nsity cannot be chosen arbitrarily but has to be<br />

calculated from the solution of the result<strong>in</strong>g boundary–value problem<br />

for the Laplace equation accord<strong>in</strong>g to<br />

We assume<br />

lead<strong>in</strong>g to the boundary condition<br />

In addition to (11) we require at <strong>in</strong>f<strong>in</strong>ity <strong>and</strong> a boun<strong>de</strong>d surface<br />

mass–<strong>de</strong>nsity at the rim of the disk The latter requirement leads<br />

to a relation between the parameters <strong>and</strong> see Eq. (15). This<br />

boundary–value problem has the unique solution<br />

with oblate elliptic coord<strong>in</strong>ates related to by

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