1887
1st Australasian Exploration Geoscience Conference – Exploration Innovation Integration
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Buried valley aquifers, consisting of permeable sand and gravel deposits in eroded bedrock valleys, are important sources of groundwater supply in many regions of the United States and Canada.

Investigations of the Spiritwood aquifer in southern Manitoba by the Geological Survey of Canada and other workers, have demonstrated the value of helicopter time domain electromagnetic (HTEM) surveys in aquifer mapping and characterization using the contrasts between Quaternary glacio-lacustrine sand-gravels (high resistivity) that are relatively permeable and clay-tills (low resistivity) that are relatively impermeable, as well as the deeper, much less resistive Cretaceous Pierre Formation Shale basement rocks. This success provided the impetus for the North Dakota State Water Commission to fly a VTEM helicopter EM survey in the Jamestown, ND region in October, 2016.

The VTEM data collected over the Spiritwood-JT block allowed for geological mapping from near surface to depth, in spite of relatively weak resistivity contrasts (<10X). These data were inverted with a layered-earth algorithm to produce resistivity-depth models. These models were able to resolve the location and depths to the top and bottom of the Spiritwood aquifer throughout the central portion of the block providing more detailed pictures of the aquifer’s geometry. In addition to resolving the main aquifer as well as its deeper channels, the VTEM data and models highlighted several smaller, previously undiscovered aquifers that cross-cut/branch-off from the main Spiritwood channel. These are interpreted as probable transverse low-K barriers that were apparent from the existing test drilling and aquifer testing.

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2018-12-01
2026-01-13
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References

  1. Legault, J.M., Eadie, T., Plastow, G., and Prikhodko, A., 2017, Spiritwood valley aquifer characterization using a helicopter TDEM system: National Groundwater Association Conference on hydrogeology and deep groundwater, NGWA, abstract, 1 p.
  2. Legault, J.M., Prikhodko, A., Dodds, D.J., Macnae, J.C., and Oldenborger, G.A., 2012, Results of recent VTEM helicopter system development testing over the Spiritwood Valley aquifer, Manitoba: 25th SAGEEP Symposium on the Application of Geophysics to Engineering and Environmental Problems, EEGS, Expanded Abstract, 17 p.
  3. Ley-Cooper, A.Y., 2016, Dealing with uncertainty in AEM models (and learning to live with it): 25TH International Geophysical Conference and Exhibition, ASEG, Extended Abstracts, 713-718.
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  5. Patch, J.C., and Honeyman, R. , 2005, Water Supply Investigation for the City of Devils Lake Spiritwood Aquifer near Warwick and the Sheyenne River Ramsey, Benson, Eddy and Nelson Counties, North Dakota: North Dakota Ground-Water Studies, No. 113, prepared by North Dakota State Water Commission, 339 p.
  6. Prikhodko, A., Morrison, E., Bagrianski, A., Kuzmin, P., Tishin, P., and Legault, J.M., 2010, Evolution of VTEM solutions for effective exploration:. 21ST Geophysical Conference and Exhibition, ASEG, Extended Abstracts , 1-5. technical
  7. Reid, J.E., Pfaffling, A. and Vrbancich, J., 2006, Airborne electromagnetic footprints in 1D earths: Geophysics, 71 (2), G63-G72.
  8. Witherly, K., R. Irvine, and E.B. Morrison, 2004, The Geotech VTEM time domain electromagnetic system: Society of Exploration Geophysicists, SEG, Expanded Abstracts, 1217-1221.
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  • Article Type: Research Article
Keyword(s): airborne; electromagnetic; groundwater; inversion; resistivity
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