Residence times of groundwater along a flow path in the Great Artesian Basin determined by 81Kr, 36Cl and 4He: Implications for palaeo hydrogeology-Reference-Cited by-同舟云学术

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Residence times of groundwater along a flow path in the Great Artesian Basin determined by 81Kr, 36Cl and 4He: Implications for palaeo hydrogeology

Published:2023-02 Issue: Volume:859 Page:159886
ISSN:0048-9697
Container-title:Science of The Total Environment
language:en
Short-container-title:Science of The Total Environment

Author:

Purtschert R.,Love A.J.,Jiang W.,Lu Z.-T.,Yang G.-M.,Fulton S.,Wohling D.,Shand P.,Aeschbach W.,Bröder L.,Müller P.,Tosaki Y.

Funder

US Department of Energy Office of Nuclear Energy

Swiss National Science Foundation

Publisher

Elsevier BV

Subject

Pollution,Waste Management and Disposal,Environmental Chemistry,Environmental Engineering

Reference57 articles.

1. Noble gas thermometry in groundwater hydrology;Aeschbach-Hertig,2013

2. Lower groundwater 14C age by atmospheric CO2 uptake during sampling and analysis;Aggarwal;Groundwater,2014

3. Isotope Methods for Dating Old Groundwater;Aggarwal,2013

4. Continental degassing of 4He by surficial discharge of deep groundwater;Aggarwal;Nat.Geosci.,2015

5. Inert gases in groundwater from the Bunter Sandstone of England as indicators of age and palaeoclimatic trends;Andrews;J. Hydrol.,1979

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