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
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.