黄土高填方场地孔隙水压力的变化规律

孔隙水压力是评价黄土高填方场地变形与稳定的重要参数。为探讨沟谷地形中黄土高填方场地孔隙水压力增长和消散规律,对陕北某黄土高填方工程进行了施工期和工后期的孔隙水压力监测和分析。结果表明：在分析超静孔隙水压力的增长和消散规律时,须扣除因土层压缩和地下水位变化而引起的静水压力变化值;孔隙水压力的增长和消散主要受地下水位和填土荷载的影响;土方填筑快,孔隙水压力增长快,反之,孔隙水压力增长慢,甚至消散;施工期的孔隙水压力增量与填土荷载增量呈近似线性关系,多级荷载的孔隙水压力系数小于0.2,土体始终处于稳定状态;工后期孔隙水压力消散缓慢,沉降达到完全稳定需要较长时间。

Variation behavior of pore water pressure in loess deep filled ground

Pore water pressure is an important parameter to evaluate the deformation and stability of loess deep filled ground. In order to explore the law of pore water pressure increase and dissipation in the loess deep filled ground in the valley terrain, the pore water pressure monitoring and analysis were carried out during and after the construction period of a loess deep filled project in Northern Shaanxi. The results show that when analyzing the law of the increase and dissipation of the excess pore water pressure, the change of the hydrostatic pressure caused by compression of the soil layer and the change of the groundwater level must be deducted; the increase and dissipation of pore water pressure are mainly affected by groundwater level and filling load; when the filling speed of earthwork construction is fast, the pore water pressure increases fast. On the contrary, the pore water pressure increases slowly or even dissipates; The increase in pore water pressure during construction period has an approximately linear relationship with the increase in filling load. The pore water pressure coefficient of multistage load is less than 0.2, and the soil is always in a stable state; the dissipation of pore water pressure is slow in the following stage of construction, and it takes a long time for the settlement to reach complete stability.