Variability in Timing and Transport of Pleistocene Meltwater Recharge to Regional Aquifers-Reference-Cited by-同舟云学术

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Variability in Timing and Transport of Pleistocene Meltwater Recharge to Regional Aquifers

Published:2021-10-21 Issue:20 Volume:48 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys Res Lett

Author:

Mowat Aidan C.¹^ORCID,Francis Daniel J.¹^ORCID,McIntosh Jennifer C.²³^ORCID,Lindsay Matthew B. J.¹^ORCID,Ferguson Grant A. G.²³^ORCID

Affiliation:

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

2. Department of Hydrology and Atmospheric Sciences University of Arizona Tucson AZ USA

3. Department of Civil, Geological and Environmental Engineering University of Saskatchewan Saskatoon SK Canada

Funder

Global Water Futures

Natural Sciences and Engineering Research Council of Canada

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL094285

Reference47 articles.

1. Regional‐scale flow of formation waters in the Williston Basin;Bachu S.;AAPG Bulletin,1996

2. Transient hydrodynamics within intercratonic sedimentary basins during glacial cycles;Bense V. F.;Journal of Geophysical Research,2008

3. The diffusive tortuosity of fine-grained unlithified sediments

4. Predicted tortuosity of muds

5. Groundwater flow beneath ice sheets: Part I — Large scale patterns

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1. Geological controls on lithium production from basinal brines across North America;Journal of Geochemical Exploration;2024-02

2. Geochemistry of groundwater: Major and trace elements;Reference Module in Earth Systems and Environmental Sciences;2024

3. Groundwater deeper than 500 m contributes less than 0.1% of global river discharge;Communications Earth & Environment;2023-02-23

4. The Impact of Ice Sheet Geometry on Meltwater Ingress and Reactive Solute Transport in Sedimentary Basins;Water Resources Research;2022-10

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