The expression of k-n is crucial in the analysis and calculation of fluid-solid coupling problems in geotechnical engineering. The relationship of k-n obtained from conventional laboratory seepage test deviates from reality as the fluid-solid coupling effect is not considered. To get a more accurate relationship between porosity and permeability coefficient, triaxial fluid-solid coupling test under varying consolidation pressure was conducted on a self-developed SRS-1 seepage and creep coupling test apparatus. The variation of porosity against time was obtained, and the fitted expressions of k-n with and without fluid-solid coupling effect are acquired. The expressions together with Kozeny-Caman's empirical formula were analyzed and then were used in the numerical simulation of one-dimensional saturated foundation consolidation in consideration of fluid-solid coupling. Then the calculation results were compared with the result of classical seepage mechanics method. Results show that 1) fluid-solid coupling effect should be taken into consideration as porosity changes dynamically in the process of seepage; 2) fluid-solid coupling problem should not be solved with classical seepage mechanics method, otherwise the error is too big; 3) since Kozeny-Caman's empirical formula, which is widely used in numerical simulation of fluid-solid coupling problem, could not accurately reflect the relationship between permeability coefficient and porosity of clay, we do not recommend it for numerical modeling; 4) the expression of k-n in consideration of fluid-solid coupling effect is recommended to improve the accuracy of numerical simulation results.
Key words
fluid-solid coupling /
seepage test /
k-n relationship /
numerical modeling /
consolidation of foundation
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References
[1] 张克恭,刘松玉.土力学[M]. 北京:中国建筑工业出版社, 2001.
[2] 冉启全, 李士伦. 流固耦合油藏数值模拟中物性参数动态模型研究[J]. 石油勘探与开发, 1997, 24(3): 61-65.
[3] 李 平, 骆亚生. 饱和土的三轴渗透试验研究[J]. 路基工程, 2006 ,(6): 32-33.
[4] 柯 瀚, 王文芳, 魏长春, 等. 填埋体饱和渗透系数影响因素室内研究[J]. 浙江大学学报 (工学版), 2013, 47(7): 1164-1170.
[5] 唐延贵. 降雨条件下非饱和土流—固耦合试验与数值研究[D].成都:成都理工大学, 2013.
[6] KLEINBERG R L, FLAUM C, GRIFFIN D D, et al . Deep Sea NMR: Methane Hydrate Growth Habit in Porous Media and Its Relationship to Hydraulic Permeability, Deposit Accumulation, and Submarine Slope Stability[J]. Journal of Geophysical Research: Solid Earth, 2003, 108(B10):429-432.
[7] 王春波, 丁文其, 刘书斌, 等. 各向异性渗透系数随应变场动态变化分析[J]. 岩石力学与工程学报,2014,33(增1):3015-3021.
[8] SINGH P N, WALLENDER W W. Effects of Adsorbed Water Layer in Predicting Saturated Hydraulic Conductivity for Clays with Kozeny-Carman Equation[J]. Journal of Geotechnical and Geoenvironmental Engineering, 2008, 134(6): 829-836.
Funding
国家自然科学基金面上项目(41372359)