Cross-hole electrical imaging of a controlled saline tracer injection

被引:306
作者
Slater, L
Binley, AM
Daily, W
Johnson, R
机构
[1] Univ Missouri, Dept Geosci, Kansas City, MO 64110 USA
[2] Univ Lancaster, Inst Environm & Nat Sci, Lancaster LA1 4YQ, England
[3] Lawrence Livermore Natl Lab, Livermore, CA 94550 USA
[4] Oregon Grad Inst Sci & Technol, Ctr Groundwater Res, Portland, OR 97291 USA
基金
英国自然环境研究理事会;
关键词
resistivity; tomography; solute transport; pixel-breakthroughs;
D O I
10.1016/S0926-9851(00)00002-1
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Electrical imaging of tracer tests can provide valuable information on the spatial variability of solute transport processes. This concept was investigated by cross-borehole electrical imaging of a controlled release in an experimental tank. A saline tracer (conductivity 8 X 10(3) ms/m volume 270 1) was injected into a tank facility (dimensions 10 X 10 X 3 m) consisting of alternating sand and clay layers. Injection was from 0.3 m below the surface, at a point where maximum interaction between tank structure and tracer transport was expected. Repeated imaging over a two-week period detected non-uniform tracer transport, partly caused by the sand/clay sequence. Tracer accumulation on two clay layers was observed and density-driven spill of tracer over a clay shelf was imaged. An additional unexpected flow pathway, probably caused by complications during array installation, was identified close to an electrode array. Pore water samples obtained following termination of electrical imaging generally supported the observed electrical response, although discrepancies arose when analysing the response of individual pixels. The pixels that make up the electrical images were interpreted as a large number of breakthrough curves. The shape of the pixel breakthrough-recession curve allowed some quantitative interpretation of solute travel time, as well as a qualitative assessment of spatial variability in advective-dispersive transport characteristics across the image plane. Although surface conduction effects associated with the clay layers complicated interpretation, the plotting of pixel breakthroughs was considered a useful step in the hydrological interpretation of the tracer test. The spatial coverage provided by the high density of pixels is the factor that most encourages the approach. (C) 2000 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:85 / 102
页数:18
相关论文
共 24 条
[1]  
[Anonymous], 1996, J ENVIRON ENG GEOPH, DOI DOI 10.4133/JEEG1.3.189
[2]  
[Anonymous], 1998, J ENVIRON ENG GEOPH
[3]   The electrical resistivity log as an aid in determining some reservoir characteristics [J].
Archie, GE .
TRANSACTIONS OF THE AMERICAN INSTITUTE OF MINING AND METALLURGICAL ENGINEERS, 1942, 146 :54-61
[4]   Examination of solute transport in an undisturbed soil column using electrical resistance tomography [J].
Binley, A ;
HenryPoulter, S ;
Shaw, B .
WATER RESOURCES RESEARCH, 1996, 32 (04) :763-769
[5]   OBSERVED MIGRATION OF A CONTROLLED DNAPL RELEASE BY GEOPHYSICAL METHODS [J].
BREWSTER, ML ;
ANNAN, AP ;
GREENHOUSE, JP ;
KUEPER, BH ;
OLHOEFT, GR ;
REDMAN, JD ;
SANDER, KA .
GROUND WATER, 1995, 33 (06) :977-987
[6]  
BUSELLI G, 1990, INVESTIGATIONS GEOPH, V5, P27
[7]   CROSS-BOREHOLE RESISTIVITY TOMOGRAPHY [J].
DAILY, W ;
OWEN, E .
GEOPHYSICS, 1991, 56 (08) :1228-1235
[8]   ELECTRICAL-RESISTIVITY TOMOGRAPHY OF VADOSE WATER-MOVEMENT [J].
DAILY, W ;
RAMIREZ, A ;
LABRECQUE, D ;
NITAO, J .
WATER RESOURCES RESEARCH, 1992, 28 (05) :1429-1442
[9]   ELECTRICAL-RESISTANCE TOMOGRAPHY EXPERIMENTS AT THE OREGON-GRADUATE-INSTITUTE [J].
DAILY, W ;
RAMIREZ, A ;
LABRECQUE, D ;
BARBER, W .
JOURNAL OF APPLIED GEOPHYSICS, 1995, 33 (04) :227-237
[10]   SALINE WATER INTRUSION IN SOUTHEAST TANZANIA [J].
GONDWE, E .
GEOEXPLORATION, 1991, 27 (1-2) :25-34