The hydrogeologic information in cross-borehole complex conductivity data from an unconsolidated conglomeratic sedimentary aquifer

被引:21
作者
Binley, Andrew [1 ]
Keery, John [1 ]
Slater, Lee [2 ]
Barrash, Warren [3 ]
Cardiff, Mike [4 ]
机构
[1] Univ Lancaster, Lancaster, England
[2] Rutgers Univ Newark, Newark, NJ USA
[3] Boise State Univ, Boise, ID 83725 USA
[4] Univ Wisconsin Madison, Madison, WI USA
基金
美国国家科学基金会;
关键词
SPECTRAL INDUCED POLARIZATION; HYDROGEOPHYSICAL RESEARCH SITE; HYDRAULIC CONDUCTIVITY; FIELD-SCALE; RESISTIVITY TOMOGRAPHY; SALINITY DEPENDENCE; TIME; INVERSION; SURFACE; BOISE;
D O I
10.1190/GEO2015-0608.1
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Accurate estimation of the hydrological properties of near-surface aquifers is important because these properties strongly influence groundwater flow and solute transport. Laboratory-based investigations have indicated that induced polarization (IP) properties of porous media may be linked, through either semi-empirical or fully mechanistic models, to hydrological properties including hydraulic conductivity. Therefore, there is a need for field assessments of the value of IP measurements in providing insights into the hydrological properties of aquifers. A cross-bore-hole IP survey was carried out at the Boise Hydrogeophysical Research Site (BHRS), an unconsolidated fluvial aquifer that has previously been well-studied with a variety of geophysical and hydrogeologic techniques. High-quality IP measurements were inverted, with careful consideration of the data error structure, to provide a 3D distribution of complex electrical conductivity values. The inverted distribution was further simplified using k-means cluster analysis to divide the inverted volume into discrete zones with horizontal layering. Identified layers based on complex electrical conductivity inversions are in broad agreement with stratigraphic units identified in previous studies at the site. Although mostly subtle variations in the phase angle are recovered through inversion of field data, greater contrasts in the IP data are evident at some unit boundaries. However, in coarse-grained aquifers, such as the BHRS, the discrimination of mildly contrasting lithologic units and associated changes in hydraulic conductivity of one or two orders of magnitude are unlikely to be achieved through field IP surveys. Despite the difficulty of differentiating subtle differences between all units, overall estimates of hydraulic conductivity purely from our field IP data are typically within an order of magnitude of independently measured values.
引用
收藏
页码:E409 / E421
页数:13
相关论文
共 78 条
[1]  
[Anonymous], 2007, THESIS
[2]   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
[3]   Spectral induced polarization measurements for predicting the hydraulic conductivity in sandy aquifers [J].
Attwa, M. ;
Guenther, T. .
HYDROLOGY AND EARTH SYSTEM SCIENCES, 2013, 17 (10) :4079-4094
[4]  
Barrash W, 1999, PROCEEDINGS OF THE SYMPOSIUM ON THE APPLICATION OF GEOPHYSICS TO ENGINEERING AND ENVIRONMENTAL PROBLEMS, P389
[5]   Significance of porosity for stratigraphy and textural composition in subsurface, coarse fluvial deposits: Boise Hydrogeophysical Research Site [J].
Barrash, W ;
Reboulet, EC .
GEOLOGICAL SOCIETY OF AMERICA BULLETIN, 2004, 116 (9-10) :1059-1073
[6]   Hierarchical geostatistics and multifacies systems: Boise Hydrogeophysical Research Site, Boise, Idaho [J].
Barrash, W ;
Clemo, T .
WATER RESOURCES RESEARCH, 2002, 38 (10)
[7]  
Barrash W., 2013, WATER RESOUR RES, V49, P1, DOI [10.1029/2012WR012444, DOI 10.1029/2012WR012444]
[8]   Field, laboratory, and modeling investigation of the skin effect at wells with slotted casing, Boise Hydrogeophysical Research Site [J].
Barrash, Warren ;
Clemo, Tom ;
Fox, Jessica J. ;
Johnson, Timothy C. .
JOURNAL OF HYDROLOGY, 2006, 326 (1-4) :181-198
[9]   Two- and three-dimensional electrical resistivity imaging at a heterogeneous remediation site [J].
Bentley, LR ;
Gharibi, M .
GEOPHYSICS, 2004, 69 (03) :674-680
[10]  
Borner F., 1991, LOG ANALYST, P612