In circumstellar disks, the size of dust particles varies from submicron to several centimeters, while planetesimals have sizes of hundreds of kilometers. Therefore, various regimes for the aerodynamic drag between solid bodies and gas can be realized in these disks, depending on the grain sizes and velocities: Epstein, Stokes, and Newton, as well as transitional regimes between them. For small bodies moving in the Epstein regime, the time required to establish the constant relative velocity between the gas and bodies can be much less than the dynamical time scale for the problem - the time for the rotation of the disk about the central body. In addition, the dust may be concentrated in individual regions of the disk, making it necessary to take into account the transfer of momentum between the dust and gas. It is shown that, for a system of equations for gas and monodisperse dust, a semi-implicit first-order approximation scheme in time in which the interphase interaction is calculated implicitly, while other forces, such as the pressure gradient and gravity are calculated explicitly, is suitable for stiff problems with intense interphase interactions and for computations of the drag in non-linear regimes. The piece-wise drag coefficient widely used in astrophysical simulations has a discontinuity at some values of the Mach and Knudsen numbers that are realized in a circumstellar disk. A continuous drag coefficient is presented, which corresponds to experimental dependences obtained for various drag regimes.
翻译:在环球磁盘中,灰尘粒子的大小从亚微微小到几厘米不等,而行星动物则有数百公里的大小。因此,根据颗粒大小和速度的不同,可以在这些磁盘中实现固体身体和气体之间空气动力阻力的各种制度:Epstein, Stokes, Newton, 以及它们之间的过渡制度。对于在Epstein制度中移动的小体体体来说,在气体和机体之间确定恒定相对速度所需的时间可能大大低于问题动态时间尺度—— 磁盘在中央体上旋转的时数。此外,灰尘可能集中在磁盘的各个区域,从而有必要考虑到灰尘和气体之间动力的转移。 事实证明,对于气体和单盘尘的等方程系统来说,一个半不精确的第一顺序的近似方法,在时间里可以以隐含的方式计算出气和机体之间的相互作用,而其他力量,如压力梯度和重力梯度等,可以明确计算出在中央体的磁盘上对硬质的硬度问题进行旋转的旋转,在磁盘中,在磁体间相互作用中可以广泛计算。