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On magnetohydrodynamic turbulence and angular momentum transport in accretion disk boundary layers

机译:磁性动力学湍流与磁盘边界层中的角动量输送

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The physical modeling of the accretion disk boundary layer, the region where the disk meets the surface of the accreting star, usually relies on the assumption that angular momentum transport is opposite to the radial angular frequency gradient of the disk. The standard model for turbulent shear viscosity, widely adopted in astrophysics, satisfies this assumption by construction. However, this behavior is not supported by numerical simulations of turbulent magnetohydrodynamic (MHD) accretion disks, which show that angular momentum transport driven by the magnetorotational instability is inefficient in this inner disk region. I will discuss the results of a recent study on the generation of hydromagnetic stresses and energy density in the boundary layer around a weakly magnetized star. Our findings suggest that although magnetic energy density can be significantly amplified in this region, angular momentum transport is rather inefficient. This seems consistent with the results obtained in numerical simulations and suggests that the detailed structure of turbulent MHD boundary layers could differ appreciably from those derived within the standard framework of turbulent shear viscosity.
机译:吸积盘边界层的物理建模,磁盘遇到的区域的区域,通常依赖于角动量传输与盘的径向角频率梯度相反的假设。在天体物理学中广泛采用的湍流剪切粘度的标准模型满足了施工的这种假设。然而,湍流磁力学动力学(MHD)吸收磁盘的数值模拟不支持这种行为,其示出了在该内盘区域中的磁化机构不稳定性驱动的角动量输送。我将讨论最近关于在弱磁化星周围的边界层中产生氢细应力和能量密度的研究的结果。我们的研究结果表明,尽管在该区域中可以显着放大磁能密度,但是角动量运输相当效率。这似乎与数值模拟中获得的结果一致,并表明湍流MHD边界层的详细结构可能从湍流剪切粘度的标准框架内衍生的那些。

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