雷诺数
物理
机械
斯托克斯数
经典力学
打滑(空气动力学)
斯托克斯定律
流量(数学)
粒子(生态学)
斯托克斯流
磁层粒子运动
运动学
粘度
湍流
热力学
磁场
量子力学
海洋学
地质学
作者
Phillip M. Lovalenti,John F. Brady
标识
DOI:10.1017/s0022112093002885
摘要
The hydrodynamic force acting on a rigid spherical particle translating with arbitrary time-dependent motion in a time-dependent flowing fluid is calculated to O ( Re ) for small but finite values of the Reynolds number, Re , based on the particle's slip velocity relative to the uniform flow. The corresponding expression for an arbitrarily shaped rigid particle is evaluated for the case when the timescale of variation of the particle's slip velocity is much greater than the diffusive scale, a 2 / v , where a is the characteristic particle dimension and v is the kinematic viscosity of the fluid. It is found that the expression for the hydrodynamic force is not simply an additive combination of the results from unsteady Stokes flow and steady Oseen flow and that the temporal decay to steady state for small but finite Re is always faster than the t -½ behaviour of unsteady Stokes flow. For example, when the particle accelerates from rest the temporal approach to steady state scales as t -2 .
科研通智能强力驱动
Strongly Powered by AbleSci AI