AMBIPOLAR DIFFUSION, INTERSTELLAR DUST, AND THE FORMATION OF CLOUD CORES AND PROTOSTARS .3. TYPICAL AXISYMMETRICAL SOLUTIONS

Citation
Ge. Ciolek et Tc. Mouschovias, AMBIPOLAR DIFFUSION, INTERSTELLAR DUST, AND THE FORMATION OF CLOUD CORES AND PROTOSTARS .3. TYPICAL AXISYMMETRICAL SOLUTIONS, The Astrophysical journal, 425(1), 1994, pp. 142-160
Citations number
82
Categorie Soggetti
Astronomy & Astrophysics
Journal title
ISSN journal
0004637X
Volume
425
Issue
1
Year of publication
1994
Part
1
Pages
142 - 160
Database
ISI
SICI code
0004-637X(1994)425:1<142:ADIDAT>2.0.ZU;2-Z
Abstract
In a previous paper we formulated the problem of the formation of prot ostellar cores by ambipolar diffusion in axisymmetric, isothermal, sel f-gravitating, thermally supercritical but magnetically subcritical mo del molecular clouds, accounting for a cosmic abundance of interstella r grains (both charged and neutral). Using an implicit code with an ad aptive mesh, we follow the evolution to a central density enhancement of 10(6) (e.g., from 2.6 x 10(3) cm-3 to 2.6 x 10(9) cm-3). First, amb ipolar diffusion slowly increases the mass-to-flux ratio of a cloud's central flux tubes, leading to the formation and contraction of therma lly supercritical but magnetically subcritical cores. The timescale fo r this process is essentially the initial central flux-loss timescale, which exceeds the dynamical timescale (congruent-to free-fall timesca le) typically by a factor 10-20. Eventually, the mass-to-flux ratio ex ceeds the critical value for collapse. The subsequent contraction of t he thermally and magnetically supercritical cores becomes progressivel y more dynamic, while the envelopes remain relatively well supported b y magnetic forces, in agreement with early theoretical predictions by Mouschovias. A typical supercritical core consists of a uniform-densit y central region and a ''tail'' of infalling matter with a power-law d ensity profile n(n) is-proportional-to r(s), -1.5 approximately-greate r-than s approximately-greater-than -1.85. The mass infall (or accreti on) rate from the subcritical envelopes is controlled by ambipolar dif fusion, and differs both qualitatively and quantitatively from estimat es based on non-magnetic models and their extrapolations to magnetic c louds. Model clouds that include the macroscopic (collisional) effects of grains have their evolution retarded (typically by 50%) with respe ct to models accounting only for neutral-ion drag. Neutral-grain drag typically dominates the neutral-ion drag at core densities n(n, c) app roximately-greater-than 10(8) cm-3. Electrostatic attraction by electr on-shielded ions (''quasiparticles'') keeps charged grains partially a ttached to the magnetic field for densities n(n, c) approximately-grea ter-than 3 x 10(5) cm-3, at which detachment would otherwise occur bec ause of collisions with neutrals. Neutral grains also couple to the ma gnetic field by inelastic charge-capture processes. The grains lengthe n the timescale for the formation of a core, accentuate the core-envel ope separation, and, by any given central density enhancement, increas e a core's size, mass, and magnetic flux.