The unidirectional emptying box

被引:18
作者
Coffey, C. J. [1 ]
Hunt, G. R. [1 ]
机构
[1] Univ London Imperial Coll Sci Technol & Med, Dept Civil & Environm Engn, London SW7 2AZ, England
基金
英国工程与自然科学研究理事会;
关键词
mixing and dispersion; stratified flows; turbulent mixing; TURBULENT BUOYANT CONVECTION; PLUME DISPERSION; FLUID-MECHANICS; ENTRAINMENT; MODEL;
D O I
10.1017/S0022112010002739
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
A theoretical description of the turbulent mixing within and the draining of a dense fluid layer from a box connected to a uniform density, quiescent environment through openings in the top and the base of the box is presented in this paper. This is an extension of the draining model developed by Linden et al. (Annu. Rev. Fluid Mech. vol. 31, 1990, pp. 201-238) and includes terms that describe localized mixing within the emptying box at the density interface. Mixing is induced by a turbulent flow of replacement fluid into the box and as a consequence we predict, and observe in complementary experiments, the development of a three-layer stratification. Based on the data collated from previous researchers, three distinct formulations for entrainment fluxes across density interfaces are used to account for this localized mixing. The model was then solved numerically for the three mixing formulations. Analytical solutions were developed for one formulation directly and for a second on assuming that localized mixing is relatively weak though still significant in redistributing buoyancy on the timescale of the draining process. Comparisons between our theoretical predictions and the experimental data, which we have collected on the developing layer depths and their densities show good agreement. The differences in predictions between the three mixing formulations suggest that the normalized flux turbulently entrained across a density interface tends to a constant value for large values of a Froude number Fr-T, based on conditions of the inflow through the top of the box, and scales as the cube of Fr-T for small values of Fr-T. The upper limit on the rate of entrainment into the mixed layer results in a minimum time (t(D)) to remove the original dense layer. Using our analytical solutions, we bound this time and show that 0.2t(E) less than or similar to t(D) less than or similar to t(E), i.e. the original dense layer may be depleted up to five times more rapidly than when there is no internal mixing and the box empties in a time t(E).
引用
收藏
页码:456 / 474
页数:19
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