On mixing and transport at a sheared density interface

Author:

Sullivan Greg D.,List E. John

Abstract

Mixing and transport of a stratifying scalar are investigated at a density interface imbedded in a turbulent shear flow. Steady-state interfacial shear flows are generated in a laboratory water channel for layer Richardson numbers, Ri, between about 1 and 10. The flow field is made optically homogeneous, enabling the use of laser-induced fluorescence with photodiode array imaging to measure the concentration field at high resolution. False-colour images of the concentration field provide valuable insight into interfacial dynamics: when the local mean shear Richardson number, Ris, is less than about 0.40–0.45, interfacial mixing appears to be dominated by Kelvin–Helmholtz (K–H) instabilities; when Ris is somewhat larger than this, interfacial mixing appears to be dominated by shear-driven wave breaking. In both cases, vertical transport of mixed fluid from the interfacial region into adjacent turbulent layers is accomplished by large-scale turbulent eddies which impinge on the interface and scour fluid from its outer edges.Motivated by the experimental findings, a model for interfacial mixing and entrainment is developed. A local equilibrium is assumed in which the rate of loss of interfacial fluid by eddy scouring is balanced by the rate of production (local mixing) by interfacial instabilities and molecular diffusion. When a single layer is turbulent and entraining, the model results are as follows: in the molecular-diffusion-dominated regime, δ/hPe−1/2 and ERi−1Pe−1/2; in the wave-breaking-dominated regime, δ/hRi−1/2 and ERi−3/2; and in the K–H-dominated regime, δ/hRi−1 and ERi−2, where δ is the interface thickness, h is the boundary-layer thickness, Pe is the Péclet number, and E is the normalized entrainment velocity. In all three regimes, the maximum concentration anomaly, [gcy ]mRi−1. When both layers are turbulent and entraining, E and δ depend on combinations of parameters from both layers.

Publisher

Cambridge University Press (CUP)

Subject

Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics

Reference30 articles.

1. Price, J. F. 1979 On the scaling of stress-driven entrainment experiments.J. Fluid Mech. 90,509–529.

2. Koochesfahani, M. M. 1984 Experiments on turbulent mixing and chemical reactions in a liquid mixing layer.PhD thesis,California Institute of Technology.

3. Thorpe, S. A. 1973 Experiments on instability and turbulence in a stratified shear flow.J. Fluid Mech. 61,731–751.

4. Narimousa, S. , Long, R. R. & Kitaigorodskii, S. A. 1986 Entrainment due to turbulent shear flow at the interface of a stably stratified fluid.Tellus 38A,76–87.

5. Hannoun, I. A. 1985 Matching the refractive index in density stratified flows. Tech. Mem. 85–1.W. M. Keck Laboratory of Hydraulics and Water Resources, California Institute of Technology.

同舟云学术

1.学者识别学者识别

2.学术分析学术分析

3.人才评估人才评估

"同舟云学术"是以全球学者为主线,采集、加工和组织学术论文而形成的新型学术文献查询和分析系统,可以对全球学者进行文献检索和人才价值评估。用户可以通过关注某些学科领域的顶尖人物而持续追踪该领域的学科进展和研究前沿。经过近期的数据扩容,当前同舟云学术共收录了国内外主流学术期刊6万余种,收集的期刊论文及会议论文总量共计约1.5亿篇,并以每天添加12000余篇中外论文的速度递增。我们也可以为用户提供个性化、定制化的学者数据。欢迎来电咨询!咨询电话:010-8811{复制后删除}0370

www.globalauthorid.com

TOP

Copyright © 2019-2024 北京同舟云网络信息技术有限公司
京公网安备11010802033243号  京ICP备18003416号-3