Two Decades of Environmental Isotope Records in Croatia: Reconstruction of the Past and Prediction of Future Levels
A two-decade-long record of environmental isotopes (2H, 3H, 14C, 18O) in Croatia is presented and the data are statistically analyzed. The atmospheric 14C activity for the period before the actual measurements started is reconstructed by measuring tree rings from the clean-air sites, and the past tr...
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Veröffentlicht in: | Radiocarbon 1998-01, Vol.40 (1), p.399-416 |
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description | A two-decade-long record of environmental isotopes (2H, 3H, 14C, 18O) in Croatia is presented and the data are statistically analyzed. The atmospheric 14C activity for the period before the actual measurements started is reconstructed by measuring tree rings from the clean-air sites, and the past tritium activity in precipitation is estimated by the correlation of our data with the Vienna station record. The long-term 3H record helped to determine a locally contaminated sampling site, and new clean sites are put into operation. The 14C data were fitted by an analytical function and the prediction of future levels is given assuming that the rate of the 14C releases remains constant. From the long-term stable isotope data record, the local meteoric water line and the temperature gradient of δ18O in precipitation are determined. |
doi_str_mv | 10.1017/S0033822200018282 |
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The atmospheric 14C activity for the period before the actual measurements started is reconstructed by measuring tree rings from the clean-air sites, and the past tritium activity in precipitation is estimated by the correlation of our data with the Vienna station record. The long-term 3H record helped to determine a locally contaminated sampling site, and new clean sites are put into operation. The 14C data were fitted by an analytical function and the prediction of future levels is given assuming that the rate of the 14C releases remains constant. From the long-term stable isotope data record, the local meteoric water line and the temperature gradient of δ18O in precipitation are determined.</description><subject>B. Anthropogenic 14C Variations</subject><subject>Dating</subject><subject>Excavation and methods</subject><subject>III. 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Anthropogenic 14C Variations</topic><topic>Dating</topic><topic>Excavation and methods</topic><topic>III. 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source | EZB-FREE-00999 freely available EZB journals; Free Full-Text Journals in Chemistry; Cambridge University Press Journals Complete |
subjects | B. Anthropogenic 14C Variations Dating Excavation and methods III. Geophysics and Geochemistry of 14C Laboratory methods Methodology and general studies Part 1: Methods Prehistory and protohistory |
title | Two Decades of Environmental Isotope Records in Croatia: Reconstruction of the Past and Prediction of Future Levels |
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