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首页> 外文期刊>Boreal Environment Research >A model study of the effects of sulfide-oxidizing bacteri(Beggiatoa spp.) on phosphorus retention processes in hypoxic sediments: implications for phosphorus management in the Baltic sea
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A model study of the effects of sulfide-oxidizing bacteri(Beggiatoa spp.) on phosphorus retention processes in hypoxic sediments: implications for phosphorus management in the Baltic sea

机译:硫化物氧化细菌(Beggiatoa spp。)对低氧沉积物中磷滞留过程影响的模型研究:对波罗的海磷管理的意义

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Ongoing eutrophication increases phosphorus storage in surficial sediments of the Baltic Sea which can then be released during hypoxic/anoxic events. Such sediments are suit- able habitats for sulfide-oxidizing bacteria, Beggiatoa spp. The objective of this paper is toinvestigate the effects of these bacteria on the P retention processes in hypoxic sediments using a diagenetic model. This model simulates interactions of the processes controlling P mobility in the sediments with redox reactions from the Beggiatoa metabolism. Modeling results demonstrate that P retention capability is limited when dissolved iron is mineralized as iron sulfides in the sediments. In this regard, sulfide consumption by Beggiatoa spp. potentially decreases the rate of iron sulfide formation and consequently increases the P retention capability in local-scale sediment.
机译:持续的富营养化增加了波罗的海表层沉积物中的磷储存,然后在缺氧/缺氧事件中释放磷。这种沉积物是硫化物氧化细菌(Beggiatoa spp)的适宜生境。本文的目的是使用成岩模型研究这些细菌对低氧沉积物中磷保留过程的影响。该模型模拟了沉积物中P迁移过程与Beggiatoa代谢的氧化还原反应之间的相互作用。模拟结果表明,当溶解的铁矿化为沉积物中的硫化铁时,磷的保留能力受到限制。在这方面,Beggiatoa spp消耗了硫化物。可能会降低硫化铁的形成速度,从而提高局部尺度沉积物中磷的保留能力。

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