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Weakly nonhydrostatic effects in compositionally-driven gravity flows

机译:由成分驱动的重力流中的弱静水效应

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In the study of compositionally-driven gravity currents it is customary to adopt the hydrostatic assumption for the pressure field which, in turn, leads to a depth-independent horizontal velocity field and significant simpilifications to the governing equations. The hydrostatic assumption is reasonable in, say, the case of a two-layer flow when the depth variations of the lower layer are small when considered as a function of space and time. However, for larger deflections of the interface (such as those caused by bottom topography) the flow will deviate in its behavior from the low aspect ratio, slowly varying purely hydrostatic flow because of the presence of vertical accelerations. In this paper we present an approach to capture the contribution of interface curvature to nonhydrostatic effects in fully time-dependent flows in two-fluid systems. Our approach involves expanding the relevant dependent variables in the form of an asymptotic expansion f = f((0)) + delta(2)f((1)) + o(delta(2)), where 0 < 8 much less than 1 is the aspect ratio of the flow, and obtaining the first-order correction to hydrostatic theory. Numerical results and comparisions with the purely hydrostatic theory are included. [References: 39]
机译:在成分驱动重力流的研究中,习惯上采用静水压力假设作为压力场,进而导致与深度无关的水平速度场和对控制方程的显着简化。流体静力学假设在例如两层流的情况下是合理的,当考虑到空间和时间的函数时,下层的深度变化较小。但是,对于较大的界面挠度(例如由底部形貌引起的挠度),流量将因低纵横比而偏离其行为,由于存在垂直加速度,因此会缓慢地改变纯静液压流。在本文中,我们提出了一种方法来捕获两流体系统中完全依赖时间的流动中界面曲率对非静水效应的贡献。我们的方法涉及以渐近展开形式f = f((0))+ delta(2)f((1))+ o(delta(2))展开相关因变量,其中0 <8小于图1是流动的长宽比,并且获得了对静水力理论的一阶校正。包括数值结果和与纯静水压理论的比较。 [参考:39]

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