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

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226 EXACT SOLUTIONS AND SCALAR FIELDS IN GRAVITY<br />

of the radial grid <strong>in</strong> such a way as to satisfy the Jeans mass<br />

<strong>and</strong> the three Jeans length conditions<br />

for spherical coord<strong>in</strong>ates, <strong>and</strong> still obta<strong>in</strong>ed fragmentation <strong>in</strong>to a well<strong>de</strong>f<strong>in</strong>ed<br />

b<strong>in</strong>ary. Only when the spatial resolution was <strong>in</strong>creased to<br />

<strong>and</strong> the solution changed behaviour [17]. That is, <strong>in</strong>stead<br />

of fragment<strong>in</strong>g <strong>in</strong>to a b<strong>in</strong>ary, the central collapse produced a bar<br />

which thereafter con<strong>de</strong>nsed <strong>in</strong>to a th<strong>in</strong> filament <strong>in</strong> good agreement with<br />

the AMR results of Ref. [10]. Thus, it appears that for grids based on<br />

spherical coord<strong>in</strong>ates, the four Jeans conditions (1) <strong>and</strong> (2) are necessary<br />

but not sufficient for realistic fragmentation, <strong>and</strong> that these must be<br />

comb<strong>in</strong>ed with sufficiently high spatial resolution to ensure a converged<br />

solution. In Ref. [17] it is argued that one reason for requir<strong>in</strong>g more numerical<br />

resolution <strong>in</strong> spherical coord<strong>in</strong>ate calculations is the occurrence<br />

of high-aspect ratio cells near the center, where <strong>and</strong><br />

may become large compared with a locally uniform Cartesian grid with<br />

unit-aspect ratio.<br />

Here we have recalculated the isothermal Gaussian cloud mo<strong>de</strong>l us<strong>in</strong>g<br />

a modified version of the spherical coord<strong>in</strong>ate co<strong>de</strong> <strong>de</strong>scribed <strong>in</strong><br />

Ref [18] . In or<strong>de</strong>r to ma<strong>in</strong>ta<strong>in</strong> a numerical resolution higher than that<br />

<strong>de</strong>m<strong>and</strong>ed by the Jeans conditions (1) <strong>and</strong> (2), the gravitohydrodynamic<br />

equations are solved <strong>in</strong> the zoom<strong>in</strong>g coord<strong>in</strong>ates, <strong>de</strong>f<strong>in</strong>ed by [19]<br />

where <strong>de</strong>notes the isothermal speed of sound <strong>and</strong> the time difference<br />

is <strong>in</strong> units of the central free-fall time<br />

With these transformations, the gravitohydrodynamic equations can<br />

be written as

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