Anna Cwanek , Marco A. Aquino-Lopez , Piotr Kołaczek , Mariusz Lamentowicz , Barbara Fiałkiewicz-Kozieł , Mariusz Gałka , Michał Słowiński , Dominika Łuców , Katarzyna Marcisz , Milena Obremska , Sambor Czerwiński , Edyta Łokas
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引用次数: 0
Abstract
This study concerned high-resolution age reconstructions of modern organic deposits collected from peatlands distributed in Central Europe. The main focus was on 210Pb radioisotope as a fundamental geochronometer along with 14C and 239+240Pu radioisotopes used for dating verification. In addition to simple classical models such as CF/CS or CF, the new approach formulated upon the Plum method was implemented. Examined peat profiles with usually poorly defined equilibrium depth revealed a high complexity manifested by vertical variability of both 210Pb activity concentration and bulk density. The performance of dating models required prior slight corrections, which led to reliable and accurate chronologies for most of the profiles, representing various peatland types (bogs, poor fens and fens). Moreover, the age series of different 210Pb models were highly consistent for a given core. The 210Pb inventory and flux assessment exhibited maxima (SE, 1σ) of 8450 (90) Bq m−2 and 280 (20) Bq m−2 y−1, respectively, reflecting an elevated level of 222Rn exhalation in the Sudetes region. No statistically significant regularities were found in the geographical distribution of 210Pb fluxes or accumulation rates.
期刊介绍:
The Journal of Environmental Radioactivity provides a coherent international forum for publication of original research or review papers on any aspect of the occurrence of radioactivity in natural systems.
Relevant subject areas range from applications of environmental radionuclides as mechanistic or timescale tracers of natural processes to assessments of the radioecological or radiological effects of ambient radioactivity. Papers deal with naturally occurring nuclides or with those created and released by man through nuclear weapons manufacture and testing, energy production, fuel-cycle technology, etc. Reports on radioactivity in the oceans, sediments, rivers, lakes, groundwaters, soils, atmosphere and all divisions of the biosphere are welcomed, but these should not simply be of a monitoring nature unless the data are particularly innovative.