Tritium/3He dating of river infiltration: An example from the Danube in the Szigetköz area, Hungary
3H, He, 4He, and Ne data were obtained from a shallow ground-water system being recharged by bank infiltration from the Danube River in northwestern Hungary. After correting for excess air, 4He and Ne concentrations reflect a recharge temperature of about 9° C., close to the mean annual temperature of the Danube (10.4° C). Values of H plus 3Hetrit (“initial tritium”) as a function of the tritium/He age are consistent with time series measurements of tritium in the Danube. Tritium/ He ages increase linearly as a function of distance from the Danube along ground-water flow lines. A horizontal flow velocity of about 530 m yr1 was derived from the age gradient. Most of the deviations between measured Danube tritium data and ground-water tritium/He data can be explained by dispersive mixing.
Citation Information
Publication Year | 1997 |
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Title | Tritium/3He dating of river infiltration: An example from the Danube in the Szigetköz area, Hungary |
DOI | 10.1111/j.1745-6584.1997.tb00160.x |
Authors | M. Stute, J. Deák, K. Révész, J. K. Böhlke, E. Deseö, R. Weppernig, P. Schlosser |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Groundwater |
Index ID | 70185302 |
Record Source | USGS Publications Warehouse |
USGS Organization | Toxic Substances Hydrology Program |