Impact of Artificial Recharge on Dissolved Noble Gases in Groundwater in California

2008 ◽  
Vol 42 (4) ◽  
pp. 1017-1023 ◽  
Author(s):  
Bradley D. Cey ◽  
G. Bryant Hudson ◽  
Jean E. Moran ◽  
Bridget R. Scanlon
Keyword(s):  
Noble Gases ◽  
Artificial Recharge ◽  
Dissolved Noble Gases

New evidences on groundwater dynamics from the Souss-Massa system (Morocco): Insights gained from dissolved noble gases

2019 ◽  
Vol 109 ◽  
pp. 104395 ◽  
Author(s):  
Mohammed Hssaisoune ◽  
Lhoussaine Bouchaou ◽  
Takuya Matsumoto ◽  
Luis Araguas ◽  
Michael Kraml ◽  
...  
Keyword(s):  
Noble Gases ◽  
Groundwater Dynamics ◽  
Dissolved Noble Gases

Reconstructing the evolution of Lake Bonney, Antarctica using dissolved noble gases

2015 ◽  
Vol 58 ◽  
pp. 46-61 ◽  
Author(s):  
Rohit B. Warrier ◽  
M. Clara Castro ◽  
Chris M. Hall ◽  
Fabien Kenig ◽  
Peter T. Doran
Keyword(s):  
Noble Gases ◽  
Dissolved Noble Gases

scholarly journals A paleotemperature record derived from dissolved noble gases in groundwater of the Aquia Aquifer (Maryland, USA)

2002 ◽  
Vol 66 (5) ◽  
pp. 797-817 ◽  
Author(s):  
Werner Aeschbach-Hertig ◽  
Martin Stute ◽  
Jordan F Clark ◽  
Robert F Reuter ◽  
Peter Schlosser
Keyword(s):  
Noble Gases ◽  
Dissolved Noble Gases

DISSOLVED NOBLE GASES AS FORENSIC TRACERS TO INVESTIGATE MOUNTAIN FRONT SPRINGS IN OWENS VALLEY, CA

2018 ◽  
Author(s):  
Zachary P. Meyers ◽  
◽  
Marty D. Frisbee ◽  
Laura Rademacher ◽  
Carolyn Box ◽  
...  
Keyword(s):  
Noble Gases ◽  
Owens Valley ◽  
Mountain Front ◽  
Dissolved Noble Gases

scholarly journals Dissolved noble gases in the porewater of lacustrine sediments as palaeolimnological proxies

2005 ◽  
Vol 69 (7) ◽  
pp. 1665-1674 ◽  
Author(s):  
Kuno M. Strassmann ◽  
Matthias S. Brennwald ◽  
Frank Peeters ◽  
Rolf Kipfer
Keyword(s):  
Noble Gases ◽  
Lacustrine Sediments ◽  
Dissolved Noble Gases

Properties of the closed-system equilibration model for dissolved noble gases in groundwater

2013 ◽  
Vol 339 ◽  
pp. 291-300 ◽  
Author(s):  
Michael Jung ◽  
Martin Wieser ◽  
Amany von Oehsen ◽  
Werner Aeschbach-Hertig
Keyword(s):  
Closed System ◽  
Noble Gases ◽  
Equilibration Model ◽  
Dissolved Noble Gases

scholarly journals Detection of a previously unknown deep-water source for Mt. Fuji’s freshwater springs via dissolved noble gases, microbial DNA and vanadium

2021 ◽  
Author(s):  
Oliver Schilling ◽  
Matthias Brennwald ◽  
Rolf Kipfer ◽  
Kazuyo Nagaosa ◽  
Philip Brunner ◽  
...  
Keyword(s):  
Deep Water ◽  
Noble Gases ◽  
Water Source ◽  
Microbial Dna ◽  
Dissolved Noble Gases ◽  
Freshwater Springs

Development of the Hydrogeological Survey Method Using the Natural Dissolved Noble Gases for the Site-Characterization for Radwastes Disposal

1994 ◽  
Vol 353 ◽  
Author(s):  
Yasunori Mahara
Keyword(s):  
Noble Gases ◽  
Early Stage ◽  
Groundwater Age ◽  
Isotopic Ratio ◽  
Active Faults ◽  
Alpha Decay ◽  
Site Characterization ◽  
Survey Method ◽  
Mixing Rate ◽  
Dissolved Noble Gases

AbstractThis study focused on developing the tracer method using the dissolved natural noble gases. The method measures precisely helium and neon dissolved in groundwater for dating. Since the dissolved helium consists of three different components (Atmospheric He, Radiogenic He and Mantle He), if it is possible to separate total dissolved helium into each component, the mixing rate between young groundwater and ancient will be predicted in in-situ groundwater. Then, dating of young groundwater is determined by measuring tritium and tritiogenic 3He in a groundwater sample. On the other hand, the dating method for old groundwater is not still verified. In this study, the old groundwater age is predicted by the accumulating rate of radiogenic helium through the alpha decay of uranium and thorium contained in rock.This tracing method was applied to a confined aquifer in the Kumamoto plain (10km × 20km ), where the groundwater flow and the geohydrological formation of aquifer was investigated in detail in the past. The groundwater in the area consists of mixture of young groundwater (less than 20 yrs old) and ancient isolated groundwater (more than 1000 yrs old). Furthermore, the drastic change in the helium isotopic ratio revealed unexpectedly the existence of active faults covered in groundwater basins. Consequently, the method using the dissolved noble gases is practicably available for investigating the geohydrologic formation of aquifer at the early stage of the site characterization.

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