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Speciation of strontium in particulates and sediments from the Mississippi River mixing zone

机译:密西西比河混合区颗粒物和沉积物中的锶形态

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Sequential extractions were performed on small amounts of particulate and sediment samples (6 to 10 mg) from the Mississippi River mixing zone. The leachates were analyzed for Sr concentration and Sr-87/Sr-86 isotope ratio. Mn and Fe contents were also measured as their oxyhydroxides are potential carrier phases for Sr. The largest fraction of Sr in the solid phase (particulates and sediments) was found to be present in the residual, refractory fraction (>70% of total). By comparison with the corresponding sediment, particulates appear to have higher concentrations of nonresidual, labile Sr (30% vs. 15%). Carbonate components seem to play an important role as carriers for labile Sr in particulates and sediments. Changes in the composition and content of the solid phase may significantly modify both the Sr-87/Sr-86 isotope ratio of the total labile fractions and that of the bulk components. However, such modifications, under normal conditions, exert little measurable influence on the Sr isotope composition of the dissolved phase. Copyright (C) 2004 Elsevier Ltd.
机译:对密西西比河混合区的少量颗粒和沉积物样品(6至10 mg)进行了连续提取。分析渗滤液的Sr浓度和Sr-87 / Sr-86同位素比。还测量了锰和铁的含量,因为它们的羟基氧化物是Sr的潜在载体相。发现固相中Sr的最大部分(颗粒和沉淀物)存在于残余的难熔部分(>总量的70%)中。与相应的沉积物相比,颗粒中非残留,不稳定的Sr浓度更高(30%比15%)。碳酸盐成分似乎在微粒和沉积物中作为不稳定Sr的载体起着重要作用。固相组成和含量的变化可能会显着改变总不稳定组分和本体组分的Sr-87 / Sr-86同位素比率。但是,这种修饰在正常条件下对溶解相的Sr同位素组成几乎没有可测量的影响。版权所有(C)2004 Elsevier Ltd.

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