The conclusion is suggested for the case of cohesionless soils preferably.
本文的结论似较适用于无粘性土层。
It is shown, for cohesionless soil, change of some parameters results in big sinkage, but others are not.
结果表明，对于无粘性土，一些参数的变化将会导致较大的下沉量，而另一些参数对结果的影响甚微。
And created by the conditions of flow at the dynamic interface between a body of cohesionless sediments particles and a fluid.
由无粘结性沉积物颗粒和流体间的动态界面的流动条件所造成。
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