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首页> 外文期刊>Journal of sedimentary research >THE CRITICAL DENSIMETRIC FROUDE NUMBER OF SUBAQUEOUS GRAVITY CURRENTS CAN BE NON-UNITY OR NON-EXISTENT
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THE CRITICAL DENSIMETRIC FROUDE NUMBER OF SUBAQUEOUS GRAVITY CURRENTS CAN BE NON-UNITY OR NON-EXISTENT

机译:重力流的临界树突率数可以是非统一的或不存在的

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摘要

For decades, the critical densimetric Froude number of subaqueous gravity flows has been regarded to be unity or close to unity, the same as the critical Froude number for open-channel flows. Based on the analysis of specific energy, a concept borrowed from hydraulic engineering, it is shown that two correction terms, the discharge correction and the concentration correction, appear in the formulation of the critical densimetric Froude number for subaqueous gravity flows in a channel. As a result, the critical densimetric Froude number of a subaqueous gravity flow in a channel can be non-unity or nonexistent depending on the degree of entrainment of ambient fluid and the density variation in the currents. Furthermore, it is shown that the lower the critical densimetric Froude number is in a sup ercritical subaqueous gravity flow, the bigger the internal jump is if the flow experiences a change in flow regime.
机译:几十年来,水下引力的临界密度弗洛德数一直被认为是统一的或接近于统一的,与明渠流动的临界弗洛德数相同。通过对比能的分析(从水利工程学借来的一个概念),可以看出,在通道中水下重力流的临界密度弗洛德数的公式中出现了两个校正项,即排放校正和浓度校正。结果,取决于环境流体的夹带程度和电流的密度变化,通道中的水下重力流的临界密度弗洛德数可以是不统一的或不存在的。此外,还表明,在超临界水下水流中,临界密度弗洛德数越低,如果流动经历了流态的变化,内部跳变就越大。

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