Choosing appropriate techniques for quantifying groundwater recharge

被引:1298
作者
Scanlon, BR [1 ]
Healy, RW
Cook, PG
机构
[1] Univ Texas, Bur Econ Geol, Austin, TX 78713 USA
[2] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA
[3] CSIRO, Glen Osmond, SA 5064, Australia
关键词
groundwater recharge/water budget; numerical modeling; arid regions; unsaturated zone; groundwater age;
D O I
10.1007/s10040-001-0176-2
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Various techniques are available to quantify recharge; however, choosing appropriate techniques is often difficult. Important considerations in choosing a technique include space/time scales, range, and reliability of recharge estimates based on different techniques; other factors may limit the application of particular techniques. The goal of the recharge study is important because it may dictate the required space/time scales of the recharge estimates. Typical study goals include water-resource evaluation, which requires information on recharge over large spatial scales and on decadal time scales; and evaluation of aquifer vulnerability to contamination, which requires detailed information on spatial variability and preferential flow. The range of recharge rates that can be estimated using different approaches should be matched to expected recharge rates at a site. The reliability of recharge estimates using different techniques is variable. Techniques based on surface-water and unsaturated-zone data provide estimates of potential recharge, whereas those based on groundwater data generally provide estimates of actual recharge. Uncertainties in each approach to estimating recharge underscore the need for application of multiple techniques to increase reliability of recharge estimates.
引用
收藏
页码:18 / 39
页数:22
相关论文
共 198 条
[1]   WATER-BALANCE APPROACH UNDER EXTREME ARID CONDITIONS - A CASE-STUDY OF TABALAH BASIN, SAUDI-ARABIA [J].
ABDULRAZZAK, MJ ;
SORMAN, AU ;
ALHAMES, AS .
HYDROLOGICAL PROCESSES, 1989, 3 (02) :107-122
[2]   QUANTITATIVE ASSESSMENT OF THE FLOW PATTERN IN THE SOUTHERN ARAVA VALLEY (ISRAEL) BY ENVIRONMENTAL TRACERS AND A MIXING CELL MODEL [J].
ADAR, EM ;
ROSENTHAL, E ;
ISSAR, AS ;
BATELAAN, O .
JOURNAL OF HYDROLOGY, 1992, 136 (1-4) :333-352
[3]  
AEBY P, 1998, THESIS SWISS FEDERAL
[4]   DETERMINING SOIL HYDROLOGIC CHARACTERISTICS ON A REMOTE FOREST WATERSHED BY CONTINUOUS MONITORING OF SOIL-WATER PRESSURES, RAINFALL AND RUNOFF [J].
AHUJA, LR ;
ELSWAIFY, SA .
JOURNAL OF HYDROLOGY, 1979, 44 (1-2) :135-147
[5]  
ALLEN RG, 1991, P INT S LYS AM SOC C
[6]   RECHARGE IN KARST AND DUNE ELEMENTS OF A SEMI-ARID LANDSCAPE AS INDICATED BY NATURAL ISOTOPES AND CHLORIDE [J].
ALLISON, GB ;
STONE, WJ ;
HUGHES, MW .
JOURNAL OF HYDROLOGY, 1985, 76 (1-2) :1-25
[7]   LAND CLEARANCE AND RIVER SALINIZATION IN THE WESTERN MURRAY BASIN, AUSTRALIA [J].
ALLISON, GB ;
COOK, PG ;
BARNETT, SR ;
WALKER, GR ;
JOLLY, ID ;
HUGHES, MW .
JOURNAL OF HYDROLOGY, 1990, 119 (1-4) :1-20
[8]   USE OF ENVIRONMENTAL CHLORIDE AND TRITIUM TO ESTIMATE TOTAL RECHARGE TO AN UNCONFINED AQUIFER [J].
ALLISON, GB ;
HUGHES, MW .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1978, 16 (02) :181-195
[9]   THE USE OF NATURAL TRACERS AS INDICATORS OF SOIL-WATER MOVEMENT IN A TEMPERATE SEMI-ARID REGION [J].
ALLISON, GB ;
HUGHES, MW .
JOURNAL OF HYDROLOGY, 1983, 60 (1-4) :157-173
[10]   HISTORY OF T FALLOUT IN SOUTHERN AUSTRALIA AS INFERRED FROM RAINFALL AND WINE SAMPLES [J].
ALLISON, GB ;
HUGHES, MW .
EARTH AND PLANETARY SCIENCE LETTERS, 1977, 36 (02) :334-340