6533b85cfe1ef96bd12bcb3e
RESEARCH PRODUCT
The importance of magnetic-field-oriented thermal conduction in the interaction of SNR shocks with interstellar clouds
Salvatore OrlandoGiovanni PeresGiovanni PeresPaolo PaganoFabrizio BocchinoFabio RealeFabio Realesubject
PhysicsRadiative coolingsupernovaeAstrophysics (astro-ph)Interstellar cloudFOS: Physical sciencesAstronomy and Astrophysicsheat conductionAstrophysicsMagnetohydrodynamicThermal conductionAstrophysicsComputational physicsMagnetic fieldSettore FIS/05 - Astronomia E AstrofisicaSpace and Planetary ScienceThermalRadiative transferMagnetohydrodynamicsSupernova remnantAstrophysics::Galaxy Astrophysicsdescription
We explore the importance of magnetic-field-oriented thermal conduction in the interaction of supernova remnant (SNR) shocks with radiative gas clouds and in determining the mass and energy exchange between the clouds and the hot surrounding medium. We perform 2.5D MHD simulations of a shock impacting on an isolated gas cloud, including anisotropic thermal conduction and radiative cooling; we consider the representative case of a Mach 50 shock impacting on a cloud ten-fold denser than the ambient medium. We consider different configurations of the ambient magnetic field and compare MHD models with or without the thermal conduction. The efficiency of the thermal conduction in the presence of magnetic field is, in general, reduced with respect to the unmagnetized case. The reduction factor strongly depends on the initial magnetic field orientation, and it is minimum when the magnetic field is initially aligned with the direction of shock propagation. The thermal conduction contributes to suppress hydrodynamic instabilities, reducing the mass mixing of the cloud and preserving the cloud from complete fragmentation. Depending on the magnetic field orientation, the heat conduction may determine a significant energy exchange between the cloud and the hot surrounding medium which, while remaining always at levels less than those in the unmagnetized case, leads to a progressive heating and evaporation of the cloud. This additional heating may contrast the radiative cooling of some parts of the cloud, preventing the onset of thermal instabilities.
year | journal | country | edition | language |
---|---|---|---|---|
2008-01-09 |