Scavenging and particle residence times determined from 234Th/238U disequilibria in the coastal waters of Mecklenburg Bay |
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| Institution: | 1. Institute of Geosciences, Christian-Albrechts-Universität Kiel, Ludewig-Meyn-Str. 14, 24118 Kiel, Germany;2. Leibniz Laboratory for Radiometric Dating and Stable Isotope Research, Christian-Albrechts-Universität Kiel, Max-Eyth Str. 11, 24118 Kiel, Germany;1. Dept. of Earth Sciences, University of Southern California, 3651 Trousdale Pkwy, Los Angeles, CA, 90089, United States;2. RSMAS, University of Miami, 4600 Rickenbacker Causeway, Miami, FL 33149, United States;3. Earth, Ocean and Atmospheric Science Dept., Florida State University, Tallahassee, FL 32306, United States;4. Dept. of Biological Sciences, University of Southern California, 3616 Trousdale Pkwy, Los Angeles, CA 90089, United States;1. Department of Biological Sciences, Macquarie University, North Ryde, NSW 2109, Australia;2. National Marine Science Centre, Southern Cross University, Coffs Harbour, NSW 2450, Australia;3. Sydney Institute of Marine Science, Mosman, NSW 2088, Australia;4. School of Mathematics and Statistics, University of New South Wales, Sydney, NSW 2052, Australia |
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| Abstract: | Activities of the naturally occurring radionuclide 234Th were determined in water samples of Mecklenburg Bay (SW Baltic Sea) using a new Th-specific diatomite adsorption technique followed by liquid scintillation spectrometry. Activities of “dissolved” (operationally defined as Th in the centrifugate) and particulate 234Th varied in the range of 1.4–6.9 and 0.9–9.3 mBq l?1, respectively. A significant correlation between Kd and SPM concentration was found. From this particle-concentration effect, the “colloidal pumping” model predicts that 98% of the “dissolved” Th is associated with colloids rather than being truly dissolved. Relative to calculated activities of the parent nuclide 238U in the Bay, the 234Th data yielded mean 234Th scavenging residence times in the range of 1.2–9.7 days. Particulate 234Th activities are inversely correlated to SPM concentrations. Particle residence times ranged from a few days in winter up to 20 days in spring characterized by less intense bottom currents. The hydrodynamic regime is the master variable controlling scavenging of Th and other similarly particle-reactive elements in Mecklenburg Bay. |
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