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Asymmetric Dipole‐Flow Test in a Fractured Carbonate Aquifer
Author(s) -
Halihan Todd,
Zlotnik Vitaly A.
Publication year - 2002
Publication title -
groundwater
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.84
H-Index - 94
eISSN - 1745-6584
pISSN - 0017-467X
DOI - 10.1111/j.1745-6584.2002.tb02533.x
Subject(s) - aquifer , geology , dipole , flow (mathematics) , carbonate , petrology , geotechnical engineering , mechanics , groundwater , materials science , chemistry , physics , metallurgy , organic chemistry
In this study, a new method‐the asymmetric dipole‐flow test—is proposed and tested for characterization of conductive properties and structure of fractured aquifers. Analytical solutions were developed and then used for interpretation of a modification of the dipole‐flow test with a single packer at the Bissen Quarry test site (Wisconsin, USA). The asymmetric dipole‐flow tests were conducted by packing a well at various elevations, and fluids were pumped from the upper section (chamber) of the well to the lower section (chamber). The head was then monitored at 11 observation points and in both sections of the well, and the conductivities of the well segments were determined. The tests at seven packer elevations in the well were rapid (less than one hour to reach steady state). The asymmetric dipole‐flow test demonstrates the potential to quantify heterogeneities of a fractured aquifer and delineate the applicability of the continuum and discrete approaches for conceptualization of ground water flow.