THE DYNAMICS OF LOW-MASS MOLECULAR CLOUDS IN EXTERNAL RADIATION-FIELDS

Citation
Rp. Nelson et Wd. Langer, THE DYNAMICS OF LOW-MASS MOLECULAR CLOUDS IN EXTERNAL RADIATION-FIELDS, The Astrophysical journal, 482(2), 1997, pp. 796-826
Citations number
57
Categorie Soggetti
Astronomy & Astrophysics
Journal title
ISSN journal
0004637X
Volume
482
Issue
2
Year of publication
1997
Part
1
Pages
796 - 826
Database
ISI
SICI code
0004-637X(1997)482:2<796:TDOLMC>2.0.ZU;2-I
Abstract
We present the results of three-dimensional hydrodynamic calculations of the evolution of low-mass molecular clouds, performed using the num erical method of smoothed particle hydrodynamics. The clouds that we c onsider are subject to heating by the interstellar radiation held and by cosmic rays. They are able to cool through molecular line emission (primarily CO and its isotopes) and by emission from the fine structur e lines of C+ and O I. We also include gas-dust thermal coupling in ou r models. A simplified chemical network is incorporated that models th e conversion between C+ and CO, where the chemical balance is determin ed by the local flux of dissociating radiation. Calculations are perfo rmed for initially uniform density clouds, with masses in the range M= 100-400 M., sizes in the range R=1.7-3.4 pc, with the initial number d ensity in all cases being n=100 cm(-3). We performed calculations for clouds with different geometrical shapes: spherical, prolate, and obla te. Additionally, we considered the effects of an anisotropic radiatio n held on the cloud evolution. These are the main results: 1. Clouds t hat are initially Jeans stable are able to collapse because of the cou pling between the dynamical and thermal evolution. This collapse resul ts in core-halo structure where we have a cold, dense, CO core surroun ded by a warmer, tenuous, C+ envelope. 2. A pressure gradient is set u p in the clouds by the attenuation of the UV radiation field. When a c loud is anisotropically heated, this pressure gradient leads to the fo rmation of a highly flattened cloud core when it collapses. 3. The com bined thermal and dynamical evolution of the prolate and oblate clouds leads to the formation of highly elongated or flattened structures. T hese structures are able to fragment, typically with four to eight sub condensations forming, which have masses in the range 3-7.5 M..