FLUX AND WATER-CONTENT RELATION AT THE SOIL SURFACE

被引：14

作者：

PARLANGE, JY ^{[1
]}

HOGARTH, WL ^{[1
]}

BOULIER, JF ^{[1
]}

TOUMA, J ^{[1
]}

HAVERKAMP, R ^{[1
]}

VACHAUD, G ^{[1
]}

机构：

[1] INST MECAN GRENOBLE,F-38041 GRENOBLE,FRANCE

来源：

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL | 1985年 / 49卷 / 02期

关键词：

D O I：

10.2136/sssaj1985.03615995004900020001x

中图分类号：

S15 [土壤学];

学科分类号：

0903 ; 090301 ;

摘要：

引用

页码：285 / 288

页数：4

共 19 条

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[2]

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[5] A COMPARATIVE-STUDY OF 3 FORMS OF THE RICHARD EQUATION USED FOR PREDICTING ONE-DIMENSIONAL INFILTRATION IN UNSATURATED SOIL [J].

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SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1981, 45 (01) :13-20

[6] COMPARISON OF NUMERICAL-SIMULATION MODELS FOR ONE-DIMENSIONAL INFILTRATION [J].

HAVERKAMP, R ;

VAUCLIN, M ;

TOUMA, J ;

WIERENGA, PJ ;

VACHAUD, G .

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1977, 41 (02) :285-294

[7] NOTE ON ESTIMATING FINITE-DIFFERENCE INTERBLOCK HYDRAULIC CONDUCTIVITY VALUES FOR TRANSIENT UNSATURATED FLOW PROBLEMS [J].

HAVERKAMP, R ;

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[8] THE 3-PARAMETER INFILTRATION EQUATION [J].

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[9] WATER TRANSPORT IN SOILS [J].

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[10]

PARLANGE JY, 1972, SOIL SCI, V111, P134

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