2005MNRAS.363.1315B -
Mon. Not. R. Astron. Soc., 363, 1315-1328 (2005/November-2)
Spherical isothermal self-similar shock flows.
BIAN F.-Y. and LOU Y.-Q.
Abstract (from CDS):
We explore self-similar dynamical processes in a spherical isothermal self-gravitational fluid with an emphasis on shocks and outline astrophysical applications of such shock solutions. The previous similarity shock solutions of Tsai & Hsu and of Shu et al. may be classified into two types: Class I solutions with downstream being free-fall collapses; and Class II solutions with downstream being Larson-Penston (LP) type solutions. By the analyses of Lou & Shen and Shen & Lou, we further construct similarity shock solutions in the `semicomplete space'. These general shock solutions can accommodate and model dynamical processes of radial outflows (wind), inflows (accretion or contraction), subsonic oscillations and free-fall core collapses all with shocks in various settings such as star-forming molecular clouds, `champagne flows' in HII regions around luminous massive OB stars or surrounding distant quasars, dynamical connections between the asymptotic giant branch phase to the protoplanetary nebula phase with a central hot white dwarf as well as accretion shocks around compact objects such as white dwarfs, neutron stars and supermassive black holes. By a systematic exploration, we are able to construct families of infinitely many discrete Class I and Class II solutions matching asymptotically with a static outer envelope of a singular isothermal sphere; the shock solutions of Tsai & Hsu form special subsets. These similarity shocks travel at either subsonic or supersonic constant speeds. We also construct twin shocks as well as an `isothermal shock' separating two fluid regions of two different yet constant temperatures.
Abstract Copyright:
2005 The Authors. Journal compilation © 2005 RAS
Journal keyword(s):
hydrodynamics - stars: AGB and post AGB - stars: formation - HII regions - planetary nebulae: general - quasars: general
Simbad objects:
3
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