and non-Darcy flow characteristics under low hydraulic gradient of natural soft clay have been gradually understood.Theory research considering both structural characteristics of natural soft clay and non-Darcy flow was rarely reported.By taking the influence of non-Darcy flow and the structural characteristics of natural soft clay into account
an one-dimensional large strain consolidation model under various loads was established in the Lagrange coordinate system
and the corresponding finite difference numerical solution was obtained.Meanwhile
the results were compared with the large-strain consolidation solution without considering the influence of structural characteristics.The reliability of the solution in this paper was analyzed and verified.Besides
the influences of structural characteristics of natural soft clay
non-Darcy flow characteristic
and external loads on the consolidation behavior were emphatically analyzed.Results show that the consolidation rate considering non-Darcy flow is slower than that without considering Darcy flow.This consolidation delay phenomenon becomes more obvious with the growth of non-Darcy flow parameters.However
the final settlement value is nearly the same.When under the same non-Darcy flow parameters
large-strain consolidation rate is greater than small-strain consolidation rate
while there is no effect on consolidation rate difference between large strain and small strain.In addition
the soil strain is small when the external load is less than the yield stress of natural soft clay
and the corresponding consolidation rate difference between large strain and small strain can be negligible.With the increase of the external load or the decrease of the yield stress
the soil strain increases gradually
and the difference between consolidation rate of large strain and small strain becomes obvious.
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Keywords
references
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