Using terrigenic 4 He to identify and quantify regional groundwater discharge to streams-Reference-Cited by-同舟云学术

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Using terrigenic 4 He to identify and quantify regional groundwater discharge to streams

Published:2011-06 Issue:6 Volume:47 Page:
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Gardner W. Payton¹,Harrington Glenn A.¹²,Solomon D. Kip³,Cook Peter G.¹²

Affiliation:

1. CSIRO Water for a Healthy Country Flagship; CSIRO Land and Water; Glen Osmond South Australia Australia

2. National Centre for Groundwater Research and Training; Flinders University; Adelaide South Australia Australia

3. Department of Geology and Geophysics; University of Utah; Salt Lake City Utah USA

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2010WR010276/fullpdf

Reference33 articles.

1. Paleotemperature reconstruction from noble gases in ground water taking into account equilibration with entrapped air;Aeschbach-Hertig;Nature,2000

2. State of disequilibrium between 238U, 234U, 226Ra and 222Rn in groundwater from bedrock;Asikainen;Geochim. Cosmochim. Acta,1981

3. Identification of geographic runoff sources in a data sparse region: Hydrological processes and the limitations of tracer-based approaches;Barthold;Hydrol. Processes,2010

4. Essai sur la theories des eaux courantes;Boussinesq;Mem. Presentes Divers Savant Acad. Sci. Inst. Natl. Fr.,1877

5. Regionalized drought flow hydrographs from a mature glaciated plateau;Brutsaert;Water Resour. Res.,1977

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