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FLOW CHARACTERISTICS OVER EQUILIBRIUM AND NON-EQUILIBRIUM DUNES

机译:均衡和非平衡沙丘上的流动特性

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This paper concerns the coupling between flow, sediment transport and morphological changes of dunes. Its objective is to investigate intrinsic differences between the flow over equilibrium and non-equilibrium dunes that might explain their different behavior. The study is based on a dune development experiment previously carried out at Queen's University, in which equilibrium dunes were subjected to a sudden decrease in flow depth. For the present purposes, the equilibrium dunes in the experiment under consideration were recreated and immobilized, to enable the study of the flow field at equilibrium state, and just after the flow depth was suddenly decreased. It was found that the near bed time-averaged flow characteristics, as well as the near bed streamwise Reynolds stresses do not correlate well with the observed dune morphological changes. This study further suggests that the local bed-load rates and the local bed shear stress are not as strongly correlated as in the case of uniform flows.
机译:本文涉及沙丘流量,沉积物运输和形态变化之间的耦合。其目标是调查可能解释其不同行为的平衡和非平衡沙丘的流量之间的内在差异。该研究基于先前在女王大学进行的沙丘开发实验,其中均衡沙丘受到流动深度的突然减少。对于本目的,正在考虑的实验中的平衡沙丘进行重新创建和固定,以使得流场在平衡状态下的研究,并且在流动深度突然下降之后。结果发现,近床时平均流动特性,以及近床流动雷诺应力与观察到的沙丘形态变化没有良好相关。该研究进一步表明,本地床载速率和本地床剪切应力与均匀流的情况下不如强烈相关。

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