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The Effects of Soil/Sediment Organic Matter on Mineralization, Desorption, and Immobilization of Phenanthrene

机译:土壤/沉积物有机质对菲矿化,解吸和固定的影响

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The bioavailability, desorption profiles, and extent of immobilization of phenanthrene were assessed using three geosorbents that had been previously classified based on their relative sorption behaviors and the chemical characteristics of their associated organic matter. Contaminants sorbed to amorphous, geologically young sorbents were found to desorb at a faster rate and thus be more readily bioavailable than contaminants sorbed to geologically mature kerogens. However, the final extent of mineralization in biologically active systems was observed to be comparable for all three geosorbents tested regardless of geological age. Analysis of the geosorbents at the conclusion of the mineralization experiments implies that biological activity affects contaminant immobilization through both sequestration and transformation. Dimensional analysis of the experimental system with independent measures of phenanthrene degradation and mass transfer aided in interpretation of the mineralization data by providing a quantifiable parameter. The resulting dimensional parameter not only changes with experimental design, but also was found to change as experimental conditions changed within a single system.
机译:使用三个底片基于其相关的有机物的化学特性,使用三种地质吸水剂评估生物利用度,解吸谱和固定的固定化的固定化。发现污染物吸附到无定形的地质上幼小的吸附剂,以更快的速率解吸,因此比污染物吸附到地质上成熟的角膜的污染物更容易生物。然而,观察到生物活性系统中的矿化程度的最终程度是对所有三种地质浪潮的相当,无论地质时代如何测试。在矿化实验结束时对地质吸水剂的分析意味着生物活性通过螯合和转化来影响污染物固定。实验系统的尺寸分析,具有独立措施的菲苯乙烯降解和质量转移通过提供量化参数解释矿化数据的解释。由此产生的尺寸参数不仅用实验设计而变化,而且发现随着实验条件在单个系统内变化而变化。

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