Controls on δ34S and δ18O of dissolved sulfate in aquifers of the Murray Basin, Australia and their use as indicators of flow processes
- 31 March 2001
- journal article
- Published by Elsevier BV in Applied Geochemistry
- Vol. 16 (4), 475-488
- https://doi.org/10.1016/s0883-2927(00)00052-4
Abstract
No abstract availableKeywords
This publication has 21 references indexed in Scilit:
- Stable isotope geochemistry of sulfate in relation to hydrogeology in southern Saskatchewan, CanadaApplied Geochemistry, 1993
- Geochemistry and isotope systematics of sulphur in the mixing zone of Bahamian blue holesApplied Geochemistry, 1991
- Isotopic constraints on the origin of salts in Australian playas. 1. SulphurPalaeogeography, Palaeoclimatology, Palaeoecology, 1991
- Use of isotope fractionation of sulfate-sulfur and sulfate-oxygen to assess bacterial desulfurication in a sandy aquiferJournal of Hydrology, 1990
- Sulfur and oxygen isotopes of sulfate in precipitation and lakewater, Quebec, CanadaApplied Geochemistry, 1986
- Isotope composition of sulphate in acid mine drainage as measure of bacterial oxidationNature, 1984
- Variations of δ34S(SO4), δ18O(H2O) and Cl/SO4 ratio in rainwater over northern Israel, from the Mediterranean Coast to Jordan Rift Valley and Golan HeightsEarth and Planetary Science Letters, 1982
- Oxygen-18 study of the aqueous-phase oxidation of sulfur dioxideAtmospheric Environment (1967), 1981
- Direct reduction of sulfates to sulfate dioxide for isotopic analysisAnalytical Chemistry, 1978
- THERMODYNAMIC PROPERTIES OF ISOTOPIC COMPOUNDS OF SULPHURCanadian Journal of Research, 1950