论文标题
降低表面张力对风波生长和空气水标量转移的影响
Effects of surface tension reduction on wind-wave growth and air-water scalar transfer
论文作者
论文摘要
通过直接数值模拟(DNS)的空气水 - 两相湍流研究,研究表面张力降低对风波生长的影响。空气和水侧的不可压缩的Navier-Stokes方程使用任意的Lagrangian-eulerian方法,带有边界拟合的移动网格。有限振幅和非破裂的重力波的波长 - 毛细血管波长小于0.07 m,在两个不同的表面紧张局部的情况下,在低 - 风速条件下,每秒几米。结果表明,较小的表面张力情况的显着波高比较大的表面张力案例的增加速度快。重力和毛细管波尺度的能量通量表明,当表面张力降低时,从明显的重力波到毛细管波的能量转移减少,而明显的波会积累更多由风提供的能量。这会导致较小的表面张力案例更快的波长。还研究了对跨空气水接口的标量转移的影响。结果表明,由于表面张力的降低,水侧的标量转移系数降低。减少是由于抑制水侧的湍流引起的。为了支持猜想,将表面张力效应与小型风波储罐中的实验室实验进行了比较。
Effect of surface tension reduction on wind-wave growth is investigated using direct numerical simulation (DNS) of air-water two-phase turbulent flow. The incompressible Navier-Stokes equations for air and water sides are solved using an arbitrary Lagrangian-Eulerian method with boundary-fitted moving grids. The wave growth of finite-amplitude and non-breaking gravity--capillary waves, whose wavelength is less than 0.07 m, is simulated for two cases of different surface tensions under a low--wind speed condition of several meters per second. The results show that significant wave height for the smaller surface tension case increases faster than that for the larger surface tension case. Energy fluxes for gravity and capillary wave scales reveal that, when the surface tension is reduced, the energy transfer from the significant gravity waves to capillary waves decreases and the significant waves accumulate more energy supplied by wind. This results in faster wave growth for the smaller surface tension case. Effect on the scalar transfer across the air-water interface is also investigated. The results show that the scalar transfer coefficient on the water side decreases due to the surface tension reduction. The decrease is caused by suppression of turbulence in the water side. In order to support the conjecture, the surface tension effect is compared with laboratory experiments in a small wind-wave tank.