论文标题
基于三方程式非本地理论的恒星演化模型I.物理基础和耗散率的计算
Stellar evolution models with overshooting based on 3-equation non-local theories I. Physical basis and the computation of the dissipation rate
论文作者
论文摘要
语境。长期以来,人们长期以对流过度进行混合,对恒星对流核心可用于核燃烧的氢量发挥重要作用。建模这种效果的最佳方法仍是辩论。目标。我们建议一个改进的模型,用于计算湍流动能的耗散速率,该模型可用于非本地对流模型,并可以轻松地实现并自愿用于一维恒星进化计算。方法。我们回顾了各种模型的物理学,以计算局部局部,尤其是在恒星天体物理学中的非本地对流模型中的湍流动能的耗散率。分析了对耗散率及其对局部分层和非本地运输的依赖的不同贡献,并提出了一种至少某些物理机制的新方法。结果。我们展示了新方法如何影响中间质量主要序列恒星恒星模型的预测,以及这些变化与非本地对流模型的其他修改有何不同,该模型的其他修改侧重于水平与垂直(湍流)动能的比率。结论。该新模型显示出可以对对流过度旋转和混合在巨大的恒星中进行物理上更完整的描述。发现通过浮力耗散是一种关键成分,必须在非本地湍流对流模型中解释。
Context. Mixing by convective overshooting has long been suggested to play an important role for the amount of hydrogen available to nuclear burning in convective cores of stars. The best way to model this effect is still debated. Aims. We suggest an improved model for the computation of the dissipation rate of turbulent kinetic energy which can be used in non-local models of stellar convection and can readily be implemented and self-consistently used in 1D stellar evolution calculations. Methods. We review the physics underlying various models to compute the dissipation rate of turbulent kinetic energy, ε, in local and particularly in non-local models of convection in stellar astrophysics. The different contributions to the dissipation rate and their dependence on local stratification and on non-local transport are analysed and a new method to account for at least some of these physical mechanisms is suggested. Results. We show how the new approach influences predictions of stellar models of intermediate-mass main-sequence stars and how these changes differ from other modifications of the non-local convection model that focus on the ratio of horizontal to vertical (turbulent) kinetic energy. Conclusions. The new model is shown to allow for a physically more complete description of convective overshooting and mixing in massive stars. Dissipation by buoyancy waves is found to be a key ingredient which has to be accounted for in non-local models of turbulent convection.