首页> 外文期刊>The Astrophysical journal >A COUPLED DYNAMICAL AND CHEMICAL MODEL OF STARLESS CORES OF MAGNETIZED MOLECULAR CLOUDS. Ⅰ. FORMULATION AND INITIAL RESULTS
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A COUPLED DYNAMICAL AND CHEMICAL MODEL OF STARLESS CORES OF MAGNETIZED MOLECULAR CLOUDS. Ⅰ. FORMULATION AND INITIAL RESULTS

机译:磁化分子星团的耦合动力学和化学模型。 Ⅰ。配方和初始结果

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We develop a detailed chemical model for the starless cores of strongly magnetized molecular clouds, with the ambipolar diffusion-driven dynamic evolution of the clouds coupled to the chemistry through ion abundances. We concentrate on two representative model clouds in this initial study, one with magnetic fields and the other without. The model predictions on the peak values and spatial" distributions of the column densities of CO, CCS, N_2H~+, and HCO~+ are compared with those observationally inferred for the well-studied starless core L1544, which is thought to be on the verge of star formation. We find that the magnetic model, in which the cloud is magnetically supported for several million years before collapsing dynamically, provides a reasonable overall fit to the available data on L1544; the fit is; significantly worse for the nonmagnetic model, in which the cloud collapses promptly. The observed large-peak column density for N_2H~+ and clear central depression for CCS favor the magnetically retarded collapse over the free-fall collapse. A relatively high abundance of CCS is found in the magnetic model, resulting most likely from an interplay of depletion and late-time hydrocarbon chemistry enhanced by CO depletion. These initial results lend some support to the standard picture of dense core formation in strongly magnetized clouds through ambipolar diffusion. They are at variance with those of Aikawa et al., who considered a set of models somewhat different from ours and preferred one in which the cloud collapses more or less freely for L1544.
机译:我们为强磁化分子云的无恒星核开发了详细的化学模型,通过双极扩散驱动的云的动态演化通过离子丰度与化学耦合。在此初始研究中,我们专注于两种代表性的模型云,一种具有磁场,另一种没有磁场。将关于CO,CCS,N_2H〜+和HCO〜+的列密度的峰值和空间“分布”的模型预测与对精心研究的无星核L1544的观测推断相比较。我们发现,磁模型在动态塌陷之前得到了数百万年的磁支撑,该模型对L1544上的可用数据提供了合理的总体拟合;拟合度非常好;对于非磁性模型而言,差得多;观测到的N_2H〜+的大峰柱密度和CCS明显的中央depression陷有利于磁滞塌陷,而不是自由落体塌陷;在磁模型中发现了相对较高的CCS丰度。最初的结果为标准构造的致密岩心形成提供了一定的支持。通过双极扩散使云层完全磁化。它们与Aikawa等人的模型不一致,Aikawa等人考虑了一组与我们的模型有些不同的模型,并且更喜欢其中L1544云或多或少地自由崩溃的模型。

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