Item talk:Q254911
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Tritium/3He dating of river infiltration: An example from the Danube in the Szigetk\u00f6z area, Hungary", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70185302", "url": "https://pubs.usgs.gov/publication/70185302" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70185302 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1111/j.1745-6584.1997.tb00160.x", "url": "https://doi.org/10.1111/j.1745-6584.1997.tb00160.x" } ], "journal": { "@type": "Periodical", "name": "Groundwater", "volumeNumber": "35", "issueNumber": "5" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Groundwater" } ], "datePublished": "1997", "dateModified": "2022-01-25", "abstract": "3H, He,\u00a04He, 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,\u00a04He and Ne concentrations reflect a recharge temperature of about 9\u00b0 C., close to the mean annual temperature of the Danube (10.4\u00b0 C). Values of H plus\u00a03Hetrit (\u201cinitial tritium\u201d) 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\u00a0was derived from the age gradient. 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