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Astron. Astrophys. 356, 73-82 (2000)

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3. The physical problem

We study the evolution of a cylindrical fluid jet impinging upon a cold heavy steady inhomogeneity, namely the cloud, in pressure equilibrium with the external medium. The relevant equations governing the jet evolution, for mass, momentum conservation, and radiative losses, are

[EQUATION]

[EQUATION]

[EQUATION]

[EQUATION]

where the fluid variables p, [FORMULA], [FORMULA] and E are, as customary, pressure, density, velocity, and thermal energy ([FORMULA]) respectively; [FORMULA] is the ratio of the specific heats; [FORMULA] represents the radiative energy loss term (energy per unit volume per unit time, Raymond & Smith 1977).

The jet occupies initially a cylinder of length L. The initial flow structure has the following form:

[EQUATION]

where m is a `steepness' parameter for the shear layer separating the jet from the external medium (see Fig. 1). The choice of separating the jet's interior from the ambient medium with a smooth transition, instead of a sharp discontinuity, avoids numerical instabilities that can develop at the interface between the jet and the exteriors, especially at high Mach numbers.

[FIGURE] Fig. 1a and b. In panel a the computational domain is sketched. The grid is finer on the region of jet/cloud interaction, while it is coarser far from the region of our interest. In panel b the physical domain is shown.

Regarding the cloud, we fix its initial density [FORMULA] and impose pressure equilibrium with respect to external medium; for simplicity we consider a steady cloud, with a thickness equal to the jet diameter.

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© European Southern Observatory (ESO) 2000

Online publication: March 28, 2000
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