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Direct and indirect methods for groundwater investigations: a case of MRS and VES in the southern part of Sweden
Luleå University of Technology, Department of Civil, Environmental and Natural Resources Engineering, Geosciences and Environmental Engineering.
2008 (English)In: Journal of Applied Geophysics, ISSN 0926-9851, E-ISSN 1879-1859, Vol. 66, no 3-4, p. 104-117Article in journal (Refereed) Published
Abstract [en]

Magnetic Resonance Sounding (MRS) has been successfully tested for detecting groundwater in two areas in southern Sweden. Measurements of Schlumberger VES have been conducted in the same place as the MRS and the results are generally consistent. Low resistivity layers interpreted as clay are sometimes identified close to the surface. The MRS result in site 2 is a good example of signals penetrating through the clay and deeper aquifer still being detected. The MRS data suggest aquifers that are not only hosted in soft sediment materials (moraine, sand, and mixed materials), but hosted in basement rocks. Based on the MRS and borehole pumping test data, the results agree with yield, average water content and subsurface geological data.

Place, publisher, year, edition, pages
2008. Vol. 66, no 3-4, p. 104-117
National Category
Geophysics
Research subject
Applied Geophysics
Identifiers
URN: urn:nbn:se:ltu:diva-8651DOI: 10.1016/j.jappgeo.2008.04.005ISI: 000261354300005Scopus ID: 2-s2.0-54549093822Local ID: 72b6e1a0-a427-11dc-8fee-000ea68e967bOAI: oai:DiVA.org:ltu-8651DiVA, id: diva2:981589
Note
Validerad; 2008; 20071206 (ysko)Available from: 2016-09-29 Created: 2016-09-29 Last updated: 2018-07-10Bibliographically approved

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Wattanasen, KamhaengElming, Sten-åke

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