论文标题
狼射线风的第一个3D辐射流动力模拟
First 3D Radiation-Hydrodynamic Simulations of Wolf-Rayet Winds
论文作者
论文摘要
经典的狼雷特(WR)恒星是经历剧烈损失的直接超新星祖细胞。因此,了解此类WR恒星的致密和快速流出对于理解恒星进化的高级阶段,环境上巨大恒星的动态反馈以及表征黑洞质量的分布至关重要。在本文中,我们开发了第一次依赖的,多维的,辐射流动力学模型的延长光学厚度大气和无氢经典WR星的风流。有限体积网格使用通量限制辐射流体动力学方法,以模拟WR流出。使用列表的Rosseland平均不熟悉度和超音速流中预期的增强线的不相处的组合来描述不良度。对于高光度模型,辐射驱动的,密集的,超音速的风是从与罗斯兰峰的深度子表面区域发射的,平均不透明度。另一方面,对于较低的发光度模型,Rosseland表示不透明度不足以维持地下区域中的净radial流出。相反,在这种情况下,发展的是一种“标准”线驱动的风,它是从延伸且高度动荡的氛围上方的光学薄区域发射的。因此,我们在这里发现了从光学厚的经典WR恒星流出到热,紧凑的亚矮人的风向薄的风。在我们的模拟中,这种过渡大约以埃德丁顿光度的40%的光度出现。由于风力发射机制的特征变化,这种过渡还伴随着平均质量损失率的大滴(在低亮度端)。
Classical Wolf Rayet (WR) stars are direct supernova progenitors undergoing vigorous mass-loss. Understanding the dense and fast outflows of such WR stars is thus crucial for understanding advanced stages of stellar evolution, the dynamical feedback of massive stars on their environments, and characterizing the distribution of black hole masses. In this paper, we develop first time-dependent, multi-dimensional, radiation-hydrodynamical models of the extended optically thick atmospheres and wind outflows of hydrogen-free classical WR stars. A flux limiting radiation hydrodynamics approach is used on a finite volume mesh to model WR outflows. The opacities are described using a combination of tabulated Rosseland mean opacities and the enhanced line opacities expected within a supersonic flow. For high-luminosity models, a radiation-driven, dense, supersonic wind is launched from deep sub-surface regions associated with peaks in the Rosseland mean opacity. For a model with lower luminosity, on the other hand, the Rosseland mean opacity is not sufficient to sustain a net-radial outflow in the sub-surface regions. Rather, what develops in this case is a "standard" line-driven wind launched from the optically thin regions above an extended and highly turbulent atmosphere. We thus find here a natural transition from optically thick outflows of classical WR stars to optically thin winds of hot, compact sub-dwarfs; in our simulations this transition occurs approximately at a luminosity that is about 40% of the Eddington luminosity. Because of the changing character of the wind-launching mechanism, this transition is also accompanied by a large drop (on the low-luminosity end) in average mass-loss rate.