JOURNAL OF YANGTZE RIVER SCIENTIFIC RESEARCH INSTI ›› 2015, Vol. 32 ›› Issue (1): 102-105.DOI: 10.3969/j.issn.1001-5485.2015.01.021

• ROCK-SOIL ENGINEERING • Previous Articles     Next Articles

Hydraulic Conductivity Functions for Unsaturated SoilsBased on Statistical Models

WANG Xiao-feng1,2, SHI Hong-lian1, TANG Zhi-zheng1, NIU Chao-ying1   

  1. 1.Faculty of Engineering, China University of Geosciences, Wuhan 430074, China;
    2.Shandong Zhengyuan Construction Engineering Co., Ltd., Yantai 264670, China
  • Received:2013-08-21 Online:2015-01-01 Published:2015-01-15

Abstract: By comparing and analyzing two methods (Kunze’s method and Fredlund’s method) based on statistical models to predicting the hydraulic conductivity of unsaturated soils, we found that they are exactly the same in essence just with different limits of integration and integration variable forms. Moreover, by analyzing the selection of parameters in their simplified calculation we obtain that it is more reasonable to determine the value of m within 15-50. Theoretically the prediction result will be larger if ln(1000000) (residual water content is assumed to be 0) is taken as the integration upper limit and logarithm of air-entry value as the integration lower limit in Fredlund method.

Key words: unsaturated soil, hydraulic conductivity, statistical model, Kunze’s method, Fredlund’s method, residual water content

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