黏性土地基流土破坏的临界水力坡降研究
Critical hydraulic gradient of soil flow failure in cohesive soil foundation
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摘要: 针对现行临界水力坡降计算公式不适用于求解黏性土临界水力坡降的情况,假定黏性土地基发生渗透破坏模式为圆柱形或倒圆台形,在太沙基临界水力坡降计算公式的基础上,分别推导了两种破坏模式下考虑土体抗剪强度影响的临界水力坡降解析式。此外,采用自制的渗透破坏仪研究了砂壤土、黄土在不同工况下发生渗透破坏时的临界水力坡降,结果表明:临界水力坡降随土层厚度、破坏半径的增大而减小,且试验结果与其相对应的公式计算结果最大误差不超过16%。Abstract: In view of the fact that the current formula for the critical hydraulic gradient is not suitable to solve the critical hydraulic gradient of cohesive soil, assuming that the seepage failure mode of the cohesive soil foundation is cylindrical or inverted circular, based on the formula for calculating the critical hydraulic slope proposed by Terzaghi, the analytical formula for the critical hydraulic slope under two failure modes considering the influences of the shear strength of the soil is derived respectively.In addition, the critical hydraulic slope of sandy loam and loess under different working conditions is studied by using the self-made permeation failure instrument.The results show that the critical hydraulic slope decreases with the increase of the soil thickness and failure radius, and the maximum error of the test results and the corresponding formula is less than 16%.