Tritium 3he Dating Of Shallow Groundwater
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Tritium/3He dating of shallow groundwater - ScienceDirect
Tritium/3He dating of shallow groundwater - ScienceDirect
Tritium/ 3 He dating of shallow groundwater - NASA/ADS
Age dating of shallow groundwater with chlorofluorocarbons . . .
(PDF) Tritium Peak Method and 3H/3HE Dating Technique use . . .
(PDF) Age Dating of Shallow Groundwater with . . .
Basics of 3H/3He dating
Age Dating of Shallow Groundwater with Chlorofluorocarbons . . .
PDF Dating of shallow groundwater: comparison of the transient . . .
PDF Tritium Peak Method and 3h/3he Dating Technique Use for . . .
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For the bomb tritium peak the deviation of the tritium / 3 He age from the age determined by identifying the groundwater layer recharged between 1962 and 1965 is about 3 years (15%) . The deviation can be explained by diffusive 3 He loss across the groundwater table and by flow dispersion . Previous article . in issue .
Abstract . Combined tritium / 3 He data from three multi-level sampling wells (DFG 1, DFG 4, DFG 7) located at Liedern/ Bocholt, West Germany, are presented and principles of the tritium / 3 He method in shallow groundwater studies are discussed . The 3 He excess produced by radioactive decay of bomb tritium (released mainly between 1952 and 1963) is . . .
Combined tritium / 3 He data from three multi-level sampling wells (DFG 1, DFG 4, DFG 7) located at Liedern/ Bocholt, West Germany, are presented and principles of the tritium / 3 He method in shallow groundwater studies are discussed . The 3 He excess produced by radioactive decay of bomb tritium (released mainly between 1952 and 1963) is clearly reflected in the data .
Groundwater age dating through the combination of transient tracer methods (chlorofluorocarbons (CFCs) and tritium /helium 3 (3 H/ 3 He)) and groundwater flow path analysis is useful for investigating groundwater travel times, flow patterns, and recharge rates, as demonstrated by this study of the homogeneous shallow , unconfined Kirkwood-Cohansey aquifer system in the southern New Jersey coastal plain . Water samples for age dating were collected from three sets of nested observation wells (10 . . .
For the bomb tritium peak the deviation of the tritium/3He age from the age determined by identifying the groundwater layer recharged between 1962 and 1965 is about 3 years (15%) .
Age Dating of Shallow Groundwater with Chlorofluorocarbons, Tritium /Helium: 3, and Flow Path Analysis, Southern New Jersey Coastal Plain Water Resources Research, 1996 Stefan Drenkard
Because 3 He is a gas, the application of the tritium / 3 He method to dating of groundwater depends strongly on the degree of confinement of 3 He trit in the groundwater . The confinement of 3 He trit is mainly determined by the ratio of advection to dispersion in water parcels moving away from the water table .
Groundwater age dating through the combination of transient tracer methods (chlorofluorocarbons (CFCs) and tritium /helium 3 ( 3 H/ 3 He)) and groundwater flow path analysis is useful for investigating groundwater travel times, flow patterns, and recharge rates, as demonstrated by this study of the homogeneous shallow , unconfined Kirkwood-Cohansey aquifer system in the southern New Jersey coastal plain .
The comparison of 3H/ 3He , CFC-11, CFC-12, and 85Kr age dating techniques in shallow groundwater shows close agreement between results obtained by the individual methods . This agreement can be attributed to aerobic conditions, permeable sand, nearly complete gas confinement, and low dispersion found on the Delmarva Peninsula .
in the groundwater are diffusing out to the gas phase until new solubility equilibrium has been reached . The main problem with degassing effects is that 3H/ 3He dating cannot provide definite apparent water ages since it is not known how tritiogenic 3He has been affected . If the degassing occurs at time zero (t=0), and
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Tritium 3he Dating Of Shallow Groundwater
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