Defining near-surface groundwater flow regimes in the semi-arid glaciated plains of North America-Reference-Cited by-同舟云学术

Defining near-surface groundwater flow regimes in the semi-arid glaciated plains of North America

Published:2015-11-25 Issue:3 Volume:52 Page:203-213
ISSN:1025-6016
Container-title:Isotopes in Environmental and Health Studies
language:en
Short-container-title:Isotopes in Environmental and Health Studies

Author:

Hendry M. Jim¹,Barbour S. Lee²,Schmeling Erin E.¹

Affiliation:

1. Department of Geological Sciences, University of Saskatchewan, Saskatoon, Canada

2. Department of Civil and Geological Engineering, University of Saskatchewan, Saskatoon, Canada

Funder

Natural Sciences and Engineering Research Council of Canada

Publisher

Informa UK Limited

Subject

Inorganic Chemistry,General Environmental Science,Environmental Chemistry

Link

https://www.tandfonline.com/doi/pdf/10.1080/10256016.2016.1092966

Reference25 articles.

1. Inferring Heterogeneity in Aquitards Using High-Resolution δD and δ18O Profiles

2. High Resolution Pore Water δ2H and δ18O Measurements by H2O(liquid)−H2O(vapor)Equilibration Laser Spectroscopy

3. Christiansen EA. Hydrogeology of surficial and bedrock valley aquifers in Southern Saskatchewan. Groundwater – Proceedings National Research Council of Canada Hydrogeology Symposium No. 3. Ottawa: Canada Department of Northern Affairs and National Resources; 1963. p. 49–66.

4. Paleohydrogeology of the Cretaceous sediments of the Williston Basin using stable isotopes of water

5. Groundwater-wetland ecosystem interaction in the semiarid glaciated plains of North America

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