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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Balance and residence times of Pb-210 and Po-210 in surface waters of the northwestern Mediterranean Sea
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Balance and residence times of Pb-210 and Po-210 in surface waters of the northwestern Mediterranean Sea

机译:Pb-210和Po-210在西北地中海地表水中的平衡和停留时间

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Concentrations of the naturally occurring radionuclides Pb-210 and Po-210 were determined in both the dissolved (<0.2 mum) and particulate (>0.2mum) fractions in surface waters of the northwestern Mediterranean Sea. About 4-8% of the Pb-210 activity was observed to be associated to particles, which were determined as being mostly biogenic. The Pb-210 content in the particulate fraction was generally greater than that of Pb-210, accounting for about 20% of the total activity. Total activities of Pb-210 and Po-210 were found to be in equilibrium. Ra-226 concentrations were also determined in an effort to investigate its occurrence in Mediterranean waters. Ra-226 was in excess to both Pb-210 and Po-210 with a mean concentration of 1.72+/-0.03 Bq m(-3). Steady-state balance equations of the three radionuclides permit calculation of residence times for Pb-210 and Po-210 in surface waters (0.8 and 3.0 yr, respectively). Po-210 residence times were almost one order of magnitude higher than mostly reported values. Polonium is known to manifest higher affinity and different binding mechanisms (by entering the organic cycle) to biogenic material than Pb-210. Several processes, such as Po-210 uptake by buoyant particles and recycling of organic matter in the surface layer, could lead to such long residence times of Po-210 and, therefore, of organic particles in surface waters. Larger Po-210 atmospheric fluxes than those here considered and inputs from rivers and/or fine-grained sediment resuspension could also help to explain the observation, although presumably to a lesser extent. (C) 2002 Elsevier Science Ltd. All rights reserved. [References: 74]
机译:测定了地中海西北部地表水中溶解的(<0.2微米)和颗粒(> 0.2微米)部分中天然存在的放射性核素Pb-210和Po-210的浓度。观察到大约4-8%的Pb-210活性与颗粒相关,这些颗粒被确定为主要是生物成因的。颗粒级分中的Pb-210含量通常高于Pb-210,约占总活性的20%。发现Pb-210和Po-210的总活性处于平衡状态。还确定了Ra-226的浓度,以调查其在地中海水域的发生情况。 Ra-226超过Pb-210和Po-210,平均浓度为1.72 +/- 0.03 Bq m(-3)。三种放射性核素的稳态平衡方程可以计算Pb-210和Po-210在地表水中的停留时间(分别为0.8年和3.0年)。 Po-210的停留时间比大多数报道的值高出近一个数量级。已知与Pb-210相比具有更高的亲和力和与生物材料的不同结合机制(通过进入有机循环)。几种过程(例如,漂浮颗粒吸收Po-210以及表层中有机物的再循环)可能会导致Po-210停留时间如此长,因此导致有机颗粒在地表水中的停留时间如此长。 Po-210大气通量比此处考虑的大,河流和/或细颗粒沉积物的重悬输入也可能有助于解释这一观测结果,尽管推测程度可能较小。 (C)2002 Elsevier ScienceLtd。保留所有权利。 [参考:74]

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