Modelling groundwater residence time in a sub-irrigated buffer zone

Ecohydrology ◽  
2013 ◽  
Vol 7 (3) ◽  
pp. 1054-1063 ◽  
Author(s):  
M. Mastrocicco ◽  
B. Boz ◽  
N. Colombani ◽  
G. M. Carrer ◽  
M. Bonato ◽  
...  
Keyword(s):  
Residence Time ◽  
Buffer Zone ◽  
Groundwater Residence Time

Groundwater residence time downgradient of Trench No. 22 at the Chernobyl Pilot Site: Constraints on hydrogeological aquifer functioning

2012 ◽  
Vol 27 (7) ◽  
pp. 1304-1319 ◽  
Author(s):  
C. Le Gal La Salle ◽  
L. Aquilina ◽  
E. Fourre ◽  
P. Jean-Baptiste ◽  
J.-L. Michelot ◽  
...  
Keyword(s):  
Residence Time ◽  
Pilot Site ◽  
Groundwater Residence Time

Radiocarbon and Other Environmental Isotopes in the Groundwater of the Sites for a Planned New Nuclear Power Plant in Lithuania

Radiocarbon ◽  
2013 ◽  
Vol 55 (2) ◽  
pp. 951-962 ◽  
Author(s):  
Jonas Mažeika ◽  
Tõnu Martma ◽  
Rimantas Petrošius ◽  
Vaidotė Jakimavičiūtė-Maselienė ◽  
Žana Skuratovič
Keyword(s):  
Power Plant ◽  
Nuclear Power Plant ◽  
Residence Time ◽  
Nuclear Power ◽  
Safety Assessment ◽  
Depth Interval ◽  
Near Surface ◽  
Helium Content ◽  
Aquifer System ◽  
Groundwater Residence Time

The assessment of construction sites for the new Visaginas Nuclear Power Plant (Visaginas NPP), including groundwater characterization, took place over the last few years. For a better understanding of the groundwater system, studies on radiocarbon; tritium; stable isotopes of hydrogen, oxygen, and carbon; and helium content were carried out at the location of the new NPP, at the Western and Eastern sites, as well as in the near-surface repository (NSR) site. Two critical depth zones in the Quaternary aquifer system were characterized by different groundwater residence times and having slightly different stable isotope features and helium content. The first shallow interval of the Quaternary multi-aquifer system consists of an unconfined aquifer and semiconfined aquifer. The second depth interval of the system is related to the lower Quaternary confined aquifer. Groundwater residence time in the first flow system was mainly based on tritium data and ranges from 6 to 60 yr. These aquifers are the most important in terms of safety assessment and are considered as a potential radionuclide transfer pathway in safety assessment. Groundwater residence time in the lower Quaternary aquifers based on 14C data varies from modern to several thousand years and in some intervals up to 10,500 yr.

Sediment dating and groundwater residence time in the lower basin of the Var river by radiochemistry and γ-ray spectrometry methods

2009 ◽  
Vol 12 (8) ◽  
pp. 861-864 ◽  
Author(s):  
Vittorio Barci ◽  
Geneviève Barci-Funel ◽  
Hervé Michel ◽  
Gilbert Féraud ◽  
Michel Dubar ◽  
...  
Keyword(s):  
Residence Time ◽  
Sediment Dating ◽  
Γ Ray ◽  
Groundwater Residence Time

Estimating groundwater residence time and recharge patterns in a saline coastal aquifer

2016 ◽  
Vol 30 (22) ◽  
pp. 4202-4213 ◽  
Author(s):  
M. Caschetto ◽  
N. Colombani ◽  
M. Mastrocicco ◽  
M. Petitta ◽  
R. Aravena
Keyword(s):  
Residence Time ◽  
Coastal Aquifer ◽  
Groundwater Residence Time

scholarly journals Groundwater residence time in a dissected and weathered sandstone plateau: Kulnura–Mangrove Mountain aquifer, NSW, Australia

2014 ◽  
Vol 61 (3) ◽  
pp. 475-499 ◽  
Author(s):  
D. I. Cendón ◽  
S. I. Hankin ◽  
J. P. Williams ◽  
M. Van der Ley ◽  
M. Peterson ◽  
...  
Keyword(s):  
Residence Time ◽  
Groundwater Residence Time
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