1887
ASEG2009 - 20th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Introduction

The Chowilla floodplain in South Australia (Figure 1) is part of the Bookmark Biosphere Reserve with wetlands supporting a wide range of plants and animals, and has provided recreational opportunities to the general public (MDBC, 2006). However, the threats from saline groundwater and salt accumulation at the surface, combined with the overall low rainfall and the lack of natural flooding events in the recent past, have had a negative consequence for vegetation health, especially the river red gums. Information on the spatial patterns of groundwater salinity and the near surface (top 15 m) salt stores in the floodplain is integral to our understanding of floodplain hydrological processes that may be active in the Lower Murray Basin of Australia. This information can be used to help develop appropriate remedial activities for the management of ecologically important wetlands and in particular assist in the maintenance of a healthy vegetation community.

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/content/journals/10.1071/ASEG2009ab135
2009-12-01
2026-01-22
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References

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  2. Finnan, J.B. 1966. Stratigraphy of the Chowilla area in the Murray Basin. Quarterly Geological Notes. Geological Survey of South Australia. 20, 3-7.
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  6. Murray-Darling Basin Commission 2006. The Chowilla Floodplain and Lindsay-Wallpolla Islands Icon Site Environmental Management Plan 2006-2007. MDBC Publication No. 33/06.
  7. Tan, K.P., Berens,V., Hatch, M, and Lawrie, K., 2006, Determining the suitability of In Stream NanoTEM for delineating zones of salt accession to the River Murray: A review of survey results from Loxton, South Australia, CRCLEME Open File Report 192, 24pp.
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  • Article Type: Research Article
Keyword(s): Airborne Electromagnetic; Chowilla; floodplain; Salinity; Salt store
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