MOVEMENT OF WATER THROUGH SOIL AS INFLUENCED BY OSMOTIC PRESSURE AND TEMPERATURE GRADIENTS

被引：10

作者：

LETEY, J

机构：

来源：

HILGARDIA | 1968年 / 39卷 / 14期

关键词：

D O I：

10.3733/hilg.v39n14p405

中图分类号：

S3 [农学（农艺学）];

学科分类号：

0901 ;

摘要：

引用

页码：405 / &

共 12 条

[1]

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[2]

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[3]

CARY J. W., 1962, SOU SCI SOC AMER PROC, V26, P417

[4]

CARY J. W., 1962, SOIL SCI SOC AMER PROC, V26, P413

[5]

Cary J. W., 1964, INT J HEAT MASS TRAN, V7, P531, DOI DOI 10.1016/0017-9310(64)90050-X

[6] ONSAGERS RELATION AND NON-ISOTHERMAL DIFFUSION OF WATER VAPOR [J].

CARY, JW .

HANKS, RJ ;

GARDNER, HR ;

FAIRBOURN, ML .

SOIL SCIENCE SOCIETY OF AMERICA PROCEEDINGS, 1967, 31 (05) :593-+

[8]

Katchalsky A., 1965, NONEQUILIBRIUM THERM

[9]

KEMPER W. D., 1963, SOIL SCI SOC AMER PROC, V27, P485

[10] OSMOTIC EFFICIENCY COEFFICIENTS ACROSS COMPACTED CLAYS [J].

KEMPER, WD ;

ROLLINS, JB .

SOIL SCIENCE SOCIETY OF AMERICA PROCEEDINGS, 1966, 30 (05) :529-&