冲击荷载下饱和砂土孔压发展模式的影响因素分析OA
Analysis of Influencing Factors of Pore Pressure Development Pattern of Saturated Sand under Impact Loading
饱和砂土在动荷载下的孔压发展模式是研究土体液化特性的基础.除了地震动等循环荷载外,实际工程中还常出现爆炸、打桩、建筑物坍塌触地等冲击型荷载,这类瞬态荷载引起的孔压变化也值得关注.为研究冲击荷载下不同因素对砂土液化过程中孔压发展的影响,设计了饱和砂土冲击液化试验.结果表明:渗透系数、相对密度和荷载幅值等因素相互耦合,显著影响孔压的发展特征.(1)渗透系数是影响动孔压发展的最重要参数之一.其主要影响孔压发展的基本模式及孔压消散时长;(2)当土层渗透系数较大(粗砂)时:相对密度对孔压峰值的影响显著,成为主控因素,此时荷载幅值的变化则主要影响孔压的峰值;(3)当土层渗透系数较小(中细砂)时:相对密度对孔压发展的阶段性特征影响更大,成为主导因素;而荷载幅值的变化主要影响并控制孔压消散时长;(4)当渗透系数较小时,超孔压消散总体呈两阶段指数函数分布特征,不同阶段与上述渗透系数、相对密度等因素相关.
Understanding the pore pressure development pattern in saturated sand under dynamic load-ing is fundamental to the study of soil liquefaction behavior.In addition to cyclic loads such as seismic motion,impact loads including blasting,pile driving,and ground contact of building collapse are also common in practical engineering,and the pore pressure changes caused by such transient loads also de-serve attention.To investigate the effects of different factors on pore pressure development during sand liquefaction under impact loading,a series of impact liquefaction tests of saturated sand were de-signed and conducted.The results showed that factors such as permeability coefficient,relative densi-ty,and load amplitude were mutually coupled and significantly influenced the development characteris-tics of pore pressure.(1)The permeability coefficient was one of the most important parameters affect-ing dynamic pore pressure development,primarily governing the basic pattern of pore pressure devel-opment and the duration of pore pressure dissipation.(2)When the permeability coefficient of the soil layer was large(coarse sand),relative density had a significant influence on the peak pore pressure and became the main controlling factor,while the changes in load amplitude mainly affected the peak value of pore pressure at this time.(3)When the permeability coefficient of the soil layer was small(medium and fine sand),relative density had a greater influence on the stage characteristics of pore pressure de-velopment and became the dominant factor,whereas the changes in load amplitude primarily affected and controlled the duration of pore pressure dissipation.(4)When the permeability coefficient was small,the dissipation of excess pore water pressure generally exhibited the distribution characteristics of a two-stage exponential function,and each stage was related to factors such as permeability coeffi-cient and relative density.
金丹丹;高瑄;张杰;王炳辉;张雷
江苏大学土木工程与力学学院,江苏 镇江 212013||中国地震局工程力学研究所中国地震局地震工程与工程振动重点实验室,黑龙江 哈尔滨 150000江苏大学土木工程与力学学院,江苏 镇江 212013江苏大学土木工程与力学学院,江苏 镇江 212013江苏科技大学土木工程与建筑学院,江苏 镇江 212100江苏科技大学土木工程与建筑学院,江苏 镇江 212100
建筑与水利
超孔隙水压力冲击荷载渗透系数相对密度荷载幅值
excess pore water pressureimpact loadingpermeability coefficientrelative densityload amplitude
《防灾减灾工程学报》 2026 (3)
632-641,10
中国地震局地震工程与工程振动重点实验室开放研究专项(2021D19)、国家自然科学基金面上项目(51978317)资助
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