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Time Course Transformations and Fate of Mercury in Aquatic Model Ecosystems

机译:水生模型生态系统中的时程变化和汞的命运

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摘要

Model aquatic ecosystems have been used to study the natural mechanisms involved in the distribution and transformation of inorganic mercury (IHg) in the different compartments and its interactions with the biota. Laboratory incubations in indoor freshwater microcosms, presenting a simple biological organization, were carried out at various spiked concentrations (3, 25 and 257 nmol l~(-1) of IHg, as mercuric chloride) and from a single initial contamination of the water column. The different compartments of the model ecosystems (water, sediment, macrophytes Elodea canadensis and snails Lymnaea stagnalis) were investigated for mercury distribution and speciation during a 2-month experimental period. The principal results obtained have evidenced different Hg biogeochemical pathways including biotic IHg methylation and reduction and transfer to the biota. A fast transfer of IHg from the water to the aquatic organisms and to the sediment was first observed with IHg half-lives of 24 h and 8 days, respectively. IHg methylation, clearly related to biogenic processes, was also demonstrated in all contaminated microcosms after 1 week of exposure. Finally, gaseous mercury species were determined in the different microcosms and significant biological induced production of elemental Hg (Hg°) and dimethyl Hg (DMHg) was observed. This overall investigation, based on the time courses evolution of IHg and in situ produced monomethylmercury (MMHg) concentrations allows to determine uptake and elimination rate constants for IHg as well as the bioaccumulation kinetics of MMHg in macrophytes and snails. The applicability of these aquatic model ecosystems to provide real insights for pollution impact and ecotoxicological risk assessments has been demonstrated.
机译:已将模型水生生态系统用于研究不同隔室中无机汞(IHg)的分布和转化及其与生物群相互作用的自然机制。在室内淡水的微观世界中,以简单的生物组织进行实验室培养,采用各种浓度的浓度(3,25和257 nmol l〜(-1)的IHg,作为氯化汞),并且受到水柱的单个初始污染。在两个月的实验期内,研究了模型生态系统的不同区室(水,沉积物,大型植物加拿大伊乐藻和蜗牛Lymnaea stagnalis)的汞分布和形态。获得的主要结果证明了不同的汞生物地球化学途径,包括生物IHg甲基化以及还原和转移至生物区系。首次观察到IHg从水到水生生物和沉积物的快速转移,IHg的半衰期分别为24小时和8天。暴露1周后,在所有受污染的微观世界中也证实了IHg甲基化,与甲基化过程明显相关。最后,在不同的微观世界中确定了气态汞物种,并观察到了明显的生物诱导的元素汞(Hg°)和二甲基汞(DMHg)产生。基于IHg的时程演变和原位产生的一甲基汞(MMHg)浓度的整体研究,可以确定IHg的吸收和消除速率常数,以及MMHg在大型植物和蜗牛体内的生物蓄积动力学。这些水生模型生态系统的适用性为污染影响和生态毒理风险评估提供了真正的见识。

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