Please use this identifier to cite or link to this item:
Title: Environmental isotopes as indicators of aquitard effectiveness, Murray Basin, Australia
Other Titles: 13th International Conference on Water-Rock Interaction, WRI-13, Guanajuato, Mexico, 16-20 August 2010
Authors: Cartwright, I
Weaver, TR
Cendón, DI
Swane, IC
Keywords: Environment
South Australia
Ground water
Inland waterways
Issue Date: 2010
Publisher: CRC Press
Citation: Cartwright, I., Weaver, T., Cendon, D., & Swane, I. (2010). Environmental isotopes as indicators of aquitard effectiveness, Murray Basin Australia. In P. Birkle & I. S. Torres-Alvarado (Eds.). Water-rock interaction : proceedings of the 13th international conference on water-rock interaction, WRI-13, Guanajuato, Mexico, 16-20 August 2010. Boca Raton : CRC Press, (pp. 67-70).
Abstract: The distribution of δ¹³C values,⁸⁷Sr/⁸⁶Sr ratios, and¹⁴C activities (a¹⁴C) show that considerable inter-aquifer flow occurs in the Wimmera Region of the Murray Basin, southern Australia. Many of the potential aquitards, (e.g., Bookpurnong Beds and Ettrick Marl) are ineffective barriers to groundwater flow; only the Geera Clay forms an effective aquitard and restricts inter-aquifer leakage between the Loxton-Parilla Sands and/or the Murray Group and the underlying Renmark Formation. This study illustrates the utility of environmental isotopes in determining inter-aquifer flow and aquitard effectiveness in regions where direct studies of aquitards is lacking.
ISBN: 9780415604260
Appears in Collections:Conference Publications

Files in This Item:
There are no files associated with this item.

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.