REMOVAL OF TH-230 AND PA-231 AT OCEAN MARGINS
REMOVAL OF TH-230 AND PA-231 AT OCEAN MARGINS
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DOI:
10.1016/0012-821x(83)90127-9
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发表时间:
1983-01-01
影响因子:
5.3
通讯作者:
BREWER, PG
中科院分区:
文献类型:
--
作者:
ANDERSON, RF;BACON, MP;BREWER, PG
Uranium, thorium and protactinium isotopes were measured in particulate matter collected by sediment traps deployed in the Panama Basin and by in-situ filtration of large volumes of seawater in the Panama and Guatemala Basins. Concentrations of dissolved Th and Pa isotopes were determined by extraction onto MnO2adsorbers placed in line behind the filters in the in-situ pumping systems.Concentrations of dissolved230Th and231Pa in the Panama and Guatemala Basins are lower than in the open ocean, whereas dissolved230Th/231Pa ratios are equal to, or slightly greater than, ratios in the open ocean. Particulate230Th/231Pa ratios in the sediment trap samples ranged from 4 to 8, in contrast to ratios of 30 or more at the open ocean sites previously studied. Particles collected by filtration in the Panama Basin and nearest to the continental margin in the Guatemala Basin contained230Th/231Pa ratios similar to the ratios in the sediment trap samples. The ratios increased with distance away from the continent.Suspended particles near the margin show no preference for adsorption of Th or Pa and therefore must be chemically different from particles in the open ocean, which show a strong preference for adsorption of Th. Ocean margins, as typified by the Panama and Guatemala Basins, are preferential sinks for231Pa relative to230Th. Furthermore, the margins are sinks for230Th and, to a greater extent,231Pa transported by horizontal mixing from the open ocean.