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Transport and distribution of trace elements and other selected inorganic constituents by suspended particulates in the Salton Sea Basin, California, 2001

机译:2001年,加利福尼亚州萨尔顿海盆中的悬浮颗粒对微量元素和其他选定的无机成分的运输和分布

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In order to examine the transport of contaminants associated with river-derived suspended particles in the Salton Sea, California, large volume water samples were collected in transects established along the three major rivers emptying into the Salton Sea in fall 2001. Rivers in this area carry significant aqueous and particulate contaminant loads derived from irrigation water associated with the extensive agricultural activity, as well as wastewater from small and large municipalities. A variety of inorganic constituents, including trace metals, nutrients, and organic carbon were analyzed on suspended material isolated from water samples collected at upriver, near-shore, and off-shore sites established on the Alamo, New, and Whitewater rivers. Concentration patterns showed expected trends, with river-borne metals becoming diluted by organic-rich algal particles of lacustrine origin in off-shore stations. More soluble metals, such as cadmium, copper, and zinc showed a more even distribution between sites in the rivers and off-shore in the lake basin. General distributional trends of trace elements between particulate and aqueous forms were discerned by combining metal concentration data for particulates from this study with historical aqueous metals data. Highly insoluble trace metals, such as iron and aluminum, occurred almost entirely in the particulate phase, while major cations and approximately 95% of selenium were transported in the soluble phase. Evidence for greater reducing conditions in the New compared to the Alamo River was provided by the greater proportion of reduced (soluble) manganese in the New River. Evidence of bioconcentration of selenium and arsenic within the lake by algae was provided by calculating "enrichment" concentration ratios from metal concentrations on the algal-derived particulate samples and the off-shore sites.
机译:为了检查与污染物相关的污染物在加利福尼亚州萨尔顿海中的迁移,沿2001年秋季排入萨尔顿海的三大河流建立了横断面,收集了大量水样。来自大量农业活动的灌溉用水以及来自大小城市的废水产生的大量水和颗粒污染物负荷。在从阿拉莫河,新河和怀特沃特河建立的上游,近岸和近海站点采集的水样中分离出的悬浮物上,分析了多种无机成分,包括痕量金属,养分和有机碳。浓度模式显示出预期的趋势,在岸边的站台上,河流传播的金属被湖相中富含有机质的藻类湖泊微粒稀释。镉,铜和锌等易溶金属在河流站点和湖盆近海之间的分布更加均匀。通过将本研究中的颗粒物金属浓度数据与历史性含水金属数据相结合,可以辨别出颗粒状和水状之间微量元素的总体分布趋势。高度不溶的痕量金属(例如铁和铝)几乎全部出现在颗粒相中,而主要阳离子和约95%的硒在可溶性相中传输。与阿拉莫河相比,新河中还原条件更大的证据是,新河中还原(可溶)锰的比例更大。通过从藻类衍生颗粒样品和近海地点的金属浓度计算“富集”浓度比,可以提供藻类在湖泊中硒和砷生物富集的证据。

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