1887
ASEG2003 - 16th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

The Riverland area, located on the southern bank of the River Murray in South Australia, is a priority area for intervention under the National Action Plan. As part of the South Australian Salinity Mapping and Management Support Project, airborne geophysics was recognised as having potential to provide valuable biophysical data relevent to the management of irrigation development and groundwater recharge reduction in the area. We examine this potential, giving particular regard to the process involved in understanding the target, defining an appropriate geophysical tool and testing whether the desired output could be delivered economically and at an appropriate resolution.

The target in the Riverland area is the near surface Blanchetown Clay unit. Forward modelling suggested that a frequency domain helicopter electromagnetic (HEM) system could map spatial variability associated with this unit. A test survey was conducted using the RESOLVE HEM system further demonstrated that potential. CDI's of these data were compared with shallow drilling, EM31, EM34 and broadband ground TEM data. Results confirmed that near surface conductivity variations mapped by the airborne EM system were associated with the clay and that a product which could be incorporated with hyrogeological models to help predict rechage and influence management decisions in the area could be generated for the whole area.

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/content/journals/10.1071/ASEG2003ab114
2003-08-01
2026-01-21
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References

  1. Brown, CM. & Stephenson, A.E., 1991. Geology of the Murray Basin, Southeastern Australia. Bureau of Mineral Resources, Australia, Bulletin 235.
  2. Cook, P.G., and Kilty, S., 1992, A helicopter-borne electromagnetic survey to delineate groundwater recharge rates: Water Resources Research, 28, 2953-2961.
  3. Cook, P.O., Walker, G.R., Buselli, G, Potts, I., and Dodds, A.R., 1992, The application of electromagnetic techniques to groundwater recharge investigations: Journal of Hydrology, 130, 201-229.
  4. Fraser, D.C., 1978, Resistivity mapping with airborne multicoil electromagneitic system. Geophysics, V43, 144-172.
  5. Hatch, M., Barrett, B., Bennetts, D., Heinson, G.S., Telfer, A. and Roberts, C, 2002, Improved near surface mapping in groundwater studies: Application of fast-sampling time-domain EM surveying methods, Preview, 96, 27.
  6. Maclnnes, S. and Raymond, M., 2001, STEMINV Documentation - Smooth-Model TEM Inversion, version 3.00: Zonge Engineering and Research Organization, Inc.
  7. Macnae, J.C., King, A., Stolz, N., Osmakoff, A. and Blaha, A., 1998, Fast AEM data processing and inversion. Expl. Geophys., 29, 163-169.
  8. Raiche, A. 2001 AMIRA Project Report P223E.
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  • Article Type: Research Article
Keyword(s): airborne electromagnetics; Blanchetown Clay; groundwater recharge; modelling
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