However, the dissipation model of excess pore water pressure after liquefaction is only affected by the confining pressure.
相对密度仅对液化后的本构模型有较大的影响，而对孔压消散模型基本没有影响。
The fluctuating characteristics of excess pore water pressure (EPWP) are the basics to establish the transient EPWP model.
饱和砂土中振动孔压波动特性的研究是建立瞬态孔隙水压力模型的基础。
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