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https://doi.org/10.4133/1.2923...
Article . 2006 . Peer-reviewed
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https://doi.org/10.3997/2214-4...
Article . 2006 . Peer-reviewed
Data sources: Crossref
https://dx.doi.org/10.4122/1.1...
Other literature type . 2006
Data sources: Datacite
https://dx.doi.org/10.4122/1.1...
Other literature type . 2006
Data sources: Datacite
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Structural Mapping of Large Aquifer Structures

Authors: Auken, Esben; Christiansen, Anders Vest; Sørensen, Kurt; Auken, Esben;

Structural Mapping of Large Aquifer Structures

Abstract

In this presentation we show results from a large hydrogeophysical survey carried out in Vendsyssel in the northernmost part of Jutland, Denmark. In the search for groundwater resources the survey clearly demonstrates the effectiveness of using cost-efficient transient electromagnetic (TEM) methods in combination with geological evaluations of existing borehole data and other geological information. Transient EM (TEM) is commonly used in hydrogeophysical investigations as a fast and relatively cheap screening method of the subsurface. The method yields a high resolution of layers with low resistivity making it suitable for delineation of high resistivity aquifers bounded by low resistivity clays, or for mapping fresh water - salt water interfaces. Recently a new helicopter-borne TEM system, SkyTEM, have been developed utilizing a fast and accurate mapping of large survey areas. The methodology used in the survey comprises five phases: Phase 1: Phase 1 involves an extensive evaluation of existing geological information. This information originates mainly from existing boreholes in the form of geological samples and geophysical logs. Phase 2: Areas of interest are chosen for extensive mapping with electromagnetic geophysical methods. Phase 3: Cross sections and geophysical thematic maps are produced based on the results from Phase 2. The information is entered into a geological/hydro- geological model for the area. Phase 4: The geological/hydrogeological model forms the basis for pointing out sites for supplementary investigation drillings or geophysical measurements. Phase 5: A final model is produced enabling hydrological modelling of the groundwater flow and assessment of the extent and vulnerability of the groundwater resources. The described methodology is cost-efficient as the number of the generally expensive drillings is cut down to a minimum. Also, the methodology is general in all aspects and directly applicable to sedimentary areas worldwide.

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selected citations
These citations are derived from selected sources.
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Citations provided by BIP!
popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
1
Average
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Average