STEADY-STATE SEEPAGE IN A HILLSIDE

被引：6

作者：

MORIN, GCA ^{[1
]}

WARRICK, AW ^{[1
]}

机构：

[1] UNIV ARIZONA,DEPT SOILS WATER & ENGN,TUCSON,AZ 85721

来源：

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL | 1973年 / 37卷 / 03期

关键词：

Drainage - FLOW OF WATER - Underground;

D O I：

10.2136/sssaj1973.03615995003700030012x

中图分类号：

S15 [土壤学];

学科分类号：

0903 ; 090301 ;

摘要：

The complex potential function is obtained for two-dimensional seepage of water through a hillside using conformal transformations. Two cases are considered. In the first a straight slope of finite length intersects an infinitely wide horizontal plane; in the second, a horizontal plane of finite width is between two symmetric hillsides. Flow nets and graphical relations characterize the flow patterns.

引用

页码：346 / 351

页数：6

共 11 条

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[2] Churchill R. V., 1960, COMPLEX VARIABLES AP
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[4] KIRKHAM DON, 1947, SOIL SCI SOC AMER PROC, V12, P73
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SCOTT, EJ
WHISLER, FD
[J]. WATER RESOURCES RESEARCH, 1965, 1 (02) : 287 - &
[6] McCracken D.D., 1964, NUMERICAL METHODS FO
[7] POLUBARINOVAKOC.PY, 1962, THEORY GROUND WATER
[8] ORTHONORMAL FUNCTION TABLES AND SEEPAGE OF STEADY RAIN THROUGH SOIL BEDDING
POWERS, WL
KRIKHAM, D
SNOWDEN, G
[J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1967, 72 (24): : 6225 - &
[9] SELIM S, 1972, SOIL SCI SOC AM J, V36, P402
[10] WARRICK A W, 1970, Soil Science Society of America Proceedings, V34, P849

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