2008A&A...484..275V


Query : 2008A&A...484..275V

2008A&A...484..275V - Astronomy and Astrophysics, volume 484, 275-280 (2008/6-2)

The effect of ambipolar resistivity on the formation of dense cores.

VAN LOO S., FALLE S.A.E.G., HARTQUIST T.W. and BARKER A.J.

Abstract (from CDS):

We aim to understand the formation of dense cores by magnetosonic waves in regions where the thermal to magnetic pressure ratio is small. Because of the low-ionisation fraction in molecular clouds, neutral and charged particles are weakly coupled. Ambipolar diffusion then plays an important role in the formation process. A quiescent, uniform plasma is perturbed by a fast-mode wave. Using 2D numerical simulations, we follow the evolution of the fast-mode wave. The simulations are done with a multifluid, adaptive mesh refinement MHD code. Initial perturbations with wavelengths that are 2 orders of magnitude larger than the dissipation length are strongly affected by the ion-neutral drift. Only in situations where there are large variations in the magnetic field corresponding to a highly turbulent gas can fast-mode waves generate dense cores. This means that, in most cores, no substructure can be produced. However, Core D of TMC-1 is an exception to this case. Due to its atypically high ionisation fraction, waves with wavelengths up to 3 orders of magnitude greater than the dissipation length can be present. Such waves are only weakly affected by ambipolar diffusion and can produce dense substructure without large wave-amplitudes. Our results also explain the observed transition from Alfvenic turbulent motion on large scales to subsonic motions at the level of dense cores.

Abstract Copyright:

Journal keyword(s): magnetohydrodynamics (MHD) - shock waves - ISM: clouds - ISM: individual objects: TMC-1 - stars: formation

Simbad objects: 2

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Number of rows : 2
N Identifier Otype ICRS (J2000)
RA
ICRS (J2000)
DEC
Mag U Mag B Mag V Mag R Mag I Sp type #ref
1850 - 2024
#notes
1 TMC-1D PoC 04 41 41.3 +25 41 16           ~ 32 0
2 TMC-1 MoC 04 41 45.9 +25 41 27           ~ 1674 0

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