Determination of groundwater discharge rates and water residence time of groundwater-fed lakes by stable isotopes of water (18 O, 2 H) and radon (222 Rn) mass balances-Reference-Cited by-同舟云学术

Determination of groundwater discharge rates and water residence time of groundwater-fed lakes by stable isotopes of water (18 O, 2 H) and radon (222 Rn) mass balances

Published:2018-03-01 Issue:6 Volume:32 Page:805-816
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Petermann Eric¹^ORCID,Gibson John J.²³,Knöller Kay⁴,Pannier Thomas¹,Weiß Holger¹,Schubert Michael¹

Affiliation:

1. Department of Groundwater Remediation; Helmholtz Centre for Environmental Research - UFZ; Permoserstraße 15 04318 Leipzig Germany

2. InnoTech Alberta; 3-4476 Markham Street Victoria BC Canada

3. Department of Geography; University of Victoria; P.O. Box 3060 STN CSC Victoria BC Canada

4. Department of Catchment Hydrology; Helmholtz Centre for Environmental Research - UFZ; Theodor-Lieser-Straße 4 06120 Halle Germany

Publisher

Wiley

Subject

Water Science and Technology

Reference43 articles.

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2. Interactions between groundwater and seasonally ice-covered lakes: Using water stable isotopes and radon-222 multi-layer mass balance models;Arnoux;Hydrological Processes,2017

3. Estimating the dynamics of groundwater input into the coastal zone via continuous radon-222 measurements;Burnett;Journal of Environmental Radioactivity,2003

4. Radon tracing of groundwater input into Par Pond, Savannah River site;Corbett;Journal of Hydrology,1997

5. Craig , H. Gordon , L. I. 1965 Deuterium and oxygen 18 variations in the ocean and the marine atmosphere

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