A field comparison of multiple techniques to quantify groundwater-surface-water interactions

被引:71
作者
Gonzalez-Pinzon, Ricardo [1 ]
Ward, Adam S. [2 ]
Hatch, Christine E. [3 ]
Wlostowski, Adam N. [4 ]
Singha, Kamini [5 ]
Gooseff, Michael N. [4 ]
Haggerty, Roy [6 ]
Harvey, Judson W. [7 ]
Cirpka, Olaf A. [8 ]
Brock, James T. [9 ]
机构
[1] Univ New Mexico, Dept Civil Engn, Albuquerque, NM 87131 USA
[2] Indiana Univ, Sch Publ & Environm Affairs, Bloomington, IN 47405 USA
[3] Univ Massachusetts, Dept Geosci, Amherst, MA 01003 USA
[4] Colorado State Univ, Ft Collins, CO 80523 USA
[5] Colorado Sch Mines, Dept Geol & Geol Engn, Golden, CO 80401 USA
[6] Oregon State Univ, Coll Earth Ocean & Atmospher Sci, Corvallis, OR 97331 USA
[7] US Geol Survey, Natl Res Program, Reston, VA 20192 USA
[8] Univ Tubingen, Ctr Appl Geosci, Tubingen, Germany
[9] Desert Res Inst, Div Earth & Ecosyst Sci, Reno, NV 89512 USA
基金
美国国家科学基金会;
关键词
stream-groundwater; hyporheic exchange; transient storage; resazurin; tracers; distributed temperature sensing; DTS; heat as a tracer; electrical resistivity; hydraulic head; SOLUTE TRANSPORT; HYPORHEIC ZONE; TIME-SERIES; TRANSIENT STORAGE; HEADWATER STREAMS; TRACER; RIVER; HEAT; DISCHARGE; EXCHANGE;
D O I
10.1086/679738
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Groundwater-surface-water (GW-SW) interactions in streams are difficult to quantify because of heterogeneity in hydraulic and reactive processes across a range of spatial and temporal scales. The challenge of quantifying these interactions has led to the development of several techniques, from centimeter-scale probes to whole-system tracers, including chemical, thermal, and electrical methods. We co-applied conservative and smart reactive solute-tracer tests, measurement of hydraulic heads, distributed temperature sensing, vertical profiles of solute tracer and temperature in the stream bed, and electrical resistivity imaging in a 450-m reach of a 3(rd)-order stream. GW-SW interactions were not spatially expansive, but were high in flux through a shallow hyporheic zone surrounding the reach. NaCl and resazurin tracers suggested different surface-subsurface exchange patterns in the upper 2/3 and lower 1/3 of the reach. Subsurface sampling of tracers and vertical thermal profiles quantified relatively high fluxes through a 10- to 20-cm deep hyporheic zone with chemical reactivity of the resazurin tracer indicated at 3-, 6-, and 9-cm sampling depths. Monitoring of hydraulic gradients along transects with MINIPOINT streambed samplers starting approximate to 40 m from the stream indicated that groundwater discharge prevented development of a larger hyporheic zone, which progressively decreased from the stream thalweg toward the banks. Distributed temperature sensing did not detect extensive inflow of ground water to the stream, and electrical resistivity imaging showed limited large-scale hyporheic exchange. We recommend choosing technique(s) based on: 1) clear definition of the questions to be addressed (physical, biological, or chemical processes), 2) explicit identification of the spatial and temporal scales to be covered and those required to provide an appropriate context for interpretation, and 3) maximizing generation of mechanistic understanding and reducing costs of implementing multiple techniques through collaborative research.
引用
收藏
页码:139 / 160
页数:22
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