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

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

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Self–gravitat<strong>in</strong>g stationary axisymmetric perfect fluids 5<br />

Note that equations (5)-(7) are equivalent to their follow<strong>in</strong>g first <strong>in</strong>tegral:<br />

where <strong>and</strong> are constants.<br />

The rigidly rotat<strong>in</strong>g case is characterized by vanish<strong>in</strong>g shear <strong>and</strong> expansion.<br />

Such conditions reduce here to which <strong>in</strong> the<br />

present case is equivalent to where a prime <strong>de</strong>notes differenti-<br />

ation with respect to In other words, we have for<br />

rigid rotation. Another <strong>in</strong>terest<strong>in</strong>g case is that of an irrotational rotation<br />

hence, where<br />

is a constant. In the irrotational case, which blows up<br />

at the axis of rotation; however, one should bear <strong>in</strong> m<strong>in</strong>d that regular<br />

toroidal-like irrotational configurations may be possible, as the rotation<br />

axis is outsi<strong>de</strong> the fluid <strong>in</strong> that case.<br />

For positivity reasons, not all velocity profiles are allowed for a particular<br />

equation of state; for <strong>in</strong>stance, <strong>in</strong> the case of dust (pressureless<br />

fluid), we have from (9): By substitut<strong>in</strong>g this<br />

value of <strong>in</strong> (8), we obta<strong>in</strong> which exclu<strong>de</strong>s<br />

differential rotations with if the natural requirement<br />

is ma<strong>de</strong>. In particular, an irrotational dust is not allowed.<br />

F<strong>in</strong>ally, let us say a word about the match<strong>in</strong>g conditions. Outsi<strong>de</strong> the<br />

fluid, assum<strong>in</strong>g a surround<strong>in</strong>g vacuum<br />

to be solved reduce to<br />

the equations<br />

for the gravitational potential U. The match<strong>in</strong>g conditions are <strong>de</strong>rived<br />

from the physical requirement that the body forces (<strong>in</strong> the present case,<br />

the gravitational force) be cont<strong>in</strong>uous across the boundary:<br />

The surface forces (let us call them t) should also be cont<strong>in</strong>uous across<br />

the boundary. If where n is the normal to the boundary <strong>and</strong><br />

the stress tensor, the follow<strong>in</strong>g has to hold:<br />

As for vacuum, <strong>and</strong> for a perfect fluid, the three<br />

conditions (13) reduce <strong>in</strong> the perfect fluid case to the s<strong>in</strong>gle condition

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