Molecular evolution and star formation: From prestellar cores to protostellar cores

被引:198
作者
Aikawa, Yuri [1 ]
Wakelam, Valentine [2 ]
Garrod, Robin T. [3 ]
Herbst, Eric [4 ,5 ,6 ]
机构
[1] Kobe Univ, Dept Earth & Planetary Sci, Kobe, Hyogo 6578501, Japan
[2] Univ Bordeaux 1, LAB, UMR5804, F-33270 Floirac, France
[3] Max Planck Inst Radioastron, D-53121 Bonn, Germany
[4] Ohio State Univ, Dept Phys, Columbus, OH 43210 USA
[5] Ohio State Univ, Dept Chem, Columbus, OH 43210 USA
[6] Ohio State Univ, Dept Astron, Columbus, OH 43210 USA
关键词
ISM : clouds; ISM; individual; IRAS; 16293-2422; L1527); ISM : molecules; stars : formation;
D O I
10.1086/524096
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We investigate molecular evolution in a star-forming core that is initially a hydrostatic starless core and collapses to form a low-mass protostar. The results of a one-dimensional radiation-hydrodynamics calculation are adopted as a physical model of the core. We first derive radii at which CO and large organic species sublimate. CO sublimation in the central region starts shortly before the formation of the first hydrostatic core. When the protostar is born, the CO sublimation radius extends to 100 AU, and the region inside less than or similar to 10 AU is hotter than 100 K, at which temperature some large organic species evaporate. We calculate the temporal variation of physical parameters in infalling shells, in which the molecular evolution is solved using an updated gas-grain chemical model to derive the spatial distribution of molecules in a protostellar core. The shells pass through the warm region of 10-100 K in several x 10(4) yr, and fall into the central star similar to 100 yr after they enter the region where T greater than or similar to 100 K. We find that large organic species are formed mainly via grain-surface reactions at temperatures of 20-40 K and then desorbed into the gas phase at their sublimation temperatures. Carbon-chain species can be formed by a combination of gas-phase reactions and grain-surface reactions following the sublimation of CH4. Our model also predicts that CO2 is more abundant in isolated cores, while gas-phase large organic species are more abundant in cores embedded in ambient clouds.
引用
收藏
页码:984 / 996
页数:13
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