| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4699287 | Chemical Geology | 2012 | 12 Pages |
Abstract
⺠Provenance of unconfined groundwater is required for water balance studies. ⺠Under evaporative conditions Na-HCO3-Cl artesian contribution can be identified. ⺠Under evaporative conditions Na-Cl-SO4 artesian contribution more difficult to identify. ⺠Unconfined and artesian groundwater have similar stable isotope signatures. ⺠Forward evaporative modelling effective in water balance studies of Na-HCO3 systems.
Keywords
Related Topics
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Geochemistry and Petrology
Authors
Justin F. Costelloe, Elizabeth C. Irvine, Andrew W. Western, Murray Tyler,