Estimation of the hydraulic conductivity of unsaturated soil incorporating the film flow

被引:15
|
作者
Zhai, Qian [1 ]
Ye, Weimin [2 ]
Rahardjo, Harianto [3 ]
Satyanaga, Alfrendo [4 ]
Du, Yanjun [1 ]
Dai, Guoliang [1 ]
Zhao, Xueliang [1 ]
机构
[1] Southeast Univ, Key Lab Concrete & Prestressed Concrete Struct, Minist Educ, Nanjing 210096, Peoples R China
[2] Tongji Univ, Key Lab Geotech & Underground Engn, Minist Educ, Shanghai 200092, Peoples R China
[3] Nanyang Technol Univ, Sch Civil & Environm Engn, Block N1,Nanyang Ave, Singapore 639798, Singapore
[4] Nazarbayev Univ, Sch Engn & Digital Sci, Dept Civil & Environm Engn, Kabanbay Batyr Ave 53, Nur Sultan 010000, Kazakhstan
基金
中国国家自然科学基金;
关键词
hydraulic conductivity; capillary flow; film flow; estimation; PERMEABILITY FUNCTION; POROUS-MEDIA; WATER; SURFACES;
D O I
10.1139/cgj-2021-0361
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
In the conventional method for the estimation of the hydraulic conductivity of unsaturated soil, only the capillary water is considered in the estimation. However, it is known that a water film can be formed around soil particles due to the adsorptive force. The water may migrate in the soil through the water film. As a result, both water flow in the capillary water and water film should be considered in the estimation. In this paper, a new equation was proposed for the estimation of the hydraulic conductivity of unsaturated soil by considering the film flow. The proposed method was verified with the experimental data from the literature. It is recommended that both capillary water flow and film flow should be considered in the estimation of the hydraulic conductivity of unsaturated soil.
引用
收藏
页码:1679 / 1684
页数:6
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