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Compressibility of pore fluid of unsaturated soils and pore pressure parameter

机译:非饱和土孔隙流体的可压缩性和孔隙压力参数

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In engineering, the pore pressure parameter is a useful factor. However, the expression of the compressibility coefficient of pore fluid, which is needed in calculating the parameter, is still not acceptable. Based on the pore water pressure, the definition of compressibility coefficient is proposed. The difference between pore air pressure and pore water pressure is considered according to the effect of surface tension. In order to simply the expression, introduced are two parameters: parameter TR which deals with the influence of surface tension; parameter Φ which is used to reflect the status of pore air. The expression of compressibility coefficient derived can be extended to the application on unsaturated soils with lower degree of saturation. Then, the pore pressure parameters for K0 loading and isotropic loading are presented. Finally, the formula is validated with the experimental results from field and laboratory tests reported in the literatures, and the agreement is good. The pore pressure parameter is not constant during loading, as should be indicated.
机译:在工程中,孔隙压力参数是一个有用的因素。但是,计算该参数所需的孔隙流体的压缩系数的表达仍然不可接受。基于孔隙水压力,提出了压缩系数的定义。根据表面张力的影响来考虑孔隙空气压力和孔隙水压力之间的差异。为了简化表达式,引入了两个参数:处理表面张力影响的参数T R 。用于反映孔隙空气状态的参数Φ。所推导的可压缩系数的表达式可以扩展到在饱和度较低的非饱和土壤中的应用。然后给出了K 0 载荷和各向同性载荷的孔隙压力参数。最后,通过文献报道的田间试验和实验室试验得到的实验结果验证了该公式的正确性。应当指出,在加载过程中,孔隙压力参数不是恒定的。

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