1887
24th International Geophysical Conference and Exhibition – Geophysics and Geology Together for Discovery
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

We discuss the theoretical development of the measurement of the T* component from a surface nuclear magnetic resonance (SNMR) experiment using superconducting quantum interference devices (SQUIDS) as a point B-field receiver.

We discuss the differences between point receivers compared to traditional coincident-loop receivers, and demonstrate the first measurements of T* with a SQUID sensor at the hydrogeophysical test site in Schillerslage, Germany.

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/content/journals/10.1071/ASEG2015ab239
2015-12-01
2026-01-17
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References

  1. Chwala, A. et al., 2011, Low temperature SQUID magnetometer systems for geophysical exploration with transient electromagnetics: Superconductor Science and Technology,24(12), 125006.
  2. Davis, A.C. et al., 2012, Aquifer characterisation in the Uley South Basin, South Australia, using NMR: Final Report: CSIRO Water for a Healthy Country National Research Flagship.
  3. Davis, A.C. et al., 2014, First evidence of detecting surface nuclear magnetic resonance signals using a compact B-field sensor: Geophysical Research Letters,41(12), 4222-4229.
  4. Dlugosch, R. et al., 2010, New hydrogeophysical methods examined at the test-site Schillerslage -Derivation of hydraulic parameters in the field scale, in European Geosciences Union General Assembly.
  5. Walsh, D. et al., 2013, A Small-Diameter NMR Logging Tool for Groundwater Investigations: Groundwater,51(6), 914-926.
  6. Walsh, D.O., 2008, Multi-channel surface NMR instrumentation and software for 1D/2D groundwater investigations: Journal of Applied Geophysics,66(3-4), 140-150.
/content/journals/10.1071/ASEG2015ab239
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  • Article Type: Research Article
Keyword(s): B-field; groundwater; NMR; SNMR; SQUID; Surface nuclear magnetic resonance
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