R-5 REVISITED .1. SPATIAL VARIABILITY OF INFILTRATION ON A SMALL RANGELAND CATCHMENT

被引:138
作者
LOAGUE, K [1 ]
GANDER, GA [1 ]
机构
[1] USDA ARS,WATER QUAL & WATERSHED RES LAB,DURANT,OK 74702
关键词
D O I
10.1029/WR026i005p00957
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In this paper, results from a large set of steady state infiltration experiments made for a small rangeland catchment are presented. We report a geostatistical characterization of infiltration variability for the new data. The scale of spatial correlation between infiltration measurements is determined to be less than 20 m. Steady state infiltration rates are linked to vegetation type and found to be variant with time. The infiltration data described in this paper are used in a companion paper (Loague, this issue) to reexcite and reevaluate the quasi‐physically based rainfall‐runoff model employed by Loague and Freeze (1985). Copyright 1990 by the American Geophysical Union.
引用
收藏
页码:957 / 971
页数:15
相关论文
共 23 条
[1]   SPATIAL AND SEASONAL VARIABILITY OF FIELD MEASURED INFILTRATION RATES ON A RANGELAND SITE IN UTAH [J].
ACHOURI, M ;
GIFFORD, GF .
JOURNAL OF RANGE MANAGEMENT, 1984, 37 (05) :451-455
[2]  
[Anonymous], 1978, MINING GEOSTATISTICS
[3]   FACTORS INFLUENCING INFILTRATION AND SEDIMENT PRODUCTION OF SEMIARID RANGELANDS IN NEVADA [J].
BLACKBURN, WH .
WATER RESOURCES RESEARCH, 1975, 11 (06) :929-937
[4]  
BOUWER H, 1986, PHYSICAL MINERALOGIC, P825
[5]  
Delfiner P., 1976, ADV GEOSTATISTICS MI, V24, P49
[6]  
DEMARSILY G, 1984, FUNDAMENTALS TRANSPO, P719
[7]  
DEMARSILY G, 1986, QUANTITATIVE HYDROGE, P284
[8]  
DUNNE T, 1980, Z GEOMORPHOL S, V33, P40
[9]   MECHANISM OF NATURAL GROUND-WATER RECHARGE AND DISCHARGE .2. LABORATORY COLUMN EXPERIMENTS AND FIELD MEASUREMENTS [J].
FREEZE, RA ;
BANNER, J .
WATER RESOURCES RESEARCH, 1970, 6 (01) :138-&
[10]  
GRAY DM, 1969, ANN M AM SOC RANGE M