Modeling Riparian Restoration Impacts on the Hydrologic Cycle at the Babacomari Ranch, SE Arizona, USA

被引:17
作者
Norman, Laura M. [1 ]
Callegary, James B. [2 ]
Lacher, Laurel [3 ]
Wilson, Natalie R. [1 ]
Fandel, Chloe [4 ]
Forbes, Brandon T. [2 ]
Swetnam, Tyson [5 ]
机构
[1] US Geol Survey, Western Geog Sci Ctr, 520 N Pk Ave,Ste 102K, Tucson, AZ 85719 USA
[2] US Geol Survey, Arizona Water Sci Ctr, 520 N Pk Ave, Tucson, AZ 85719 USA
[3] Lacher Hydrol Consulting, Tucson, AZ 85719 USA
[4] Univ Arizona, Hydrol & Atmospher Sci, Tucson, AZ 85719 USA
[5] Univ Arizona, BIO5 Inst, Tucson, AZ 85719 USA
关键词
restoration science; surface-to-groundwater; modeling; hydrologic budget; augmented recharge; WATER ASSESSMENT-TOOL; GROUNDWATER RECHARGE; LAND-COVER; SOIL; CALIBRATION; FLOW; SWAT; UNCERTAINTY; SENSITIVITY; HILLSLOPE;
D O I
10.3390/w11020381
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This paper describes coupling field experiments with surface and groundwater modeling to investigate rangelands of SE Arizona, USA using erosion-control structures to augment shallow and deep aquifer recharge. We collected field data to describe the physical and hydrological properties before and after gabions (caged riprap) were installed in an ephemeral channel. The modular finite-difference flow model is applied to simulate the amount of increase needed to raise groundwater levels. We used the average increase in infiltration measured in the field and projected on site, assuming all infiltration becomes recharge, to estimate how many gabions would be needed to increase recharge in the larger watershed. A watershed model was then applied and calibrated with discharge and 3D terrain measurements, to simulate flow volumes. Findings were coupled to extrapolate simulations and quantify long-term impacts of riparian restoration. Projected scenarios demonstrate how erosion-control structures could impact all components of the annual water budget. Results support the potential of watershed-wide gabion installation to increase total aquifer recharge, with models portraying increased subsurface connectivity and accentuated lateral flow contributions.
引用
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页数:20
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