MARKOVIAN STOCHASTIC BASIS FOR TRANSPORT OF WATER THROUGH UNSATURATED SOIL

被引：9

作者：

BHATTACHARYA, RN

GUPTA, VK

SPOSITO, G

机构：

[1] UNIV ARIZONA,DEPT HYDROL & WATER RESOURCES,TUCSON,AZ 85721

[2] UNIV ARIZONA,DEPT MATH,TUCSON,AZ 85721

[3] UNIV CALIF RIVERSIDE,DEPT SOIL SCI 9 AGR ENGN,RIVERSIDE,CA 92502

来源：

关键词：

D O I：

10.2136/sssaj1976.03615995004000030043x

中图分类号：

S15 [土壤学];

学科分类号：

0903 ; 090301 ;

摘要：

引用

页码：465 / 467

页数：3

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[4]

Egelstaff P. A., 1967, INTRO LIQUID STATE, V2nd

[5]

Gihman II, 1972, STOCHASTIC DIFFERENT

[6]

KIRKHAM D, 1972, ADV SOIL PHYSICS

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RAATS, PAC .

SOIL SCIENCE SOCIETY OF AMERICA PROCEEDINGS, 1970, 34 (05) :709-+

[8] Capillary conduction of liquids through porous mediums [J].

Richards, L. A. .

PHYSICS-A JOURNAL OF GENERAL AND APPLIED PHYSICS, 1931, 1 (01) :318-333

[9]

Springer T., 1972, SPRINGER TRACTS MODE, V64, P1, DOI [10.1007/BFb0042411, DOI 10.1007/BFB0042411]

[10]

SWARTZENDRUBER D, 1969, FLOW POROUS MEDIA, P215