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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Arsenic(V) sorption kinetics in long-term arsenic pesticide contaminated soils
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Arsenic(V) sorption kinetics in long-term arsenic pesticide contaminated soils

机译:长期砷农药污染土壤中的砷(V)吸附动力学

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Historic As contamination of soils occurs throughout the world from mining, industrial and agricultural activities. Sorption processes and rate may strongly influence soil As mobility, which further influences As bioavailability and toxicity. We investigated the kinetics of As(V) sorption by adding the arsenic onto both pristine (non-contaminated) and historically contaminated soils from arsenicals in two contrasting soil types (ferralitic and sandy). Results suggest both pseudo-second order (PSO) and Elovich kinetic models produce robust correlations with good data fits to linearized plots (R-2 approximate to 0.900-0.999) that describe the arsenic sorption kinetics for both contaminated and pristine soils. The arsenic sorption data are generally best described by the Elovich model with smaller normalized standard deviations (Delta q <5%) than PSO model. In addition, the surface binding to exchangeable and specific sorption of fresh arsenic (63-96%) sites has an impact on the overall low rate of As(V) sorption in the aged contaminated soils. Pristine soils "particularly ferralitic soils" show intraparticle diffusion and/or surface precipitation, which can contribute to a greater irreversibility of As(V) binding in soil. In contrast, the As(V) sorption occurred in the pristine sandy soil in a similar fashion to that of the aged contaminated soil, most likely due to both soil groups having limited strong binding sites. The detailed knowledge from this study provides new insights into the reclamation and management of As contaminated sites.
机译:历史性的土壤污染从矿业,工业和农业活动中发生。吸附过程和速率可能强烈影响土壤作为流动性,这进一步影响了生物利用度和毒性。通过将砷添加到原始(非污染物)和历史上污染的土壤中,从两种对比土壤类型(亚铁钠和桑迪)中,通过将砷(非污染)和历史污染的土壤中的砷和历史污染的土壤调查了动力学。结果表明,伪二次阶(PSO)和ELOVICH动力学模型与良好的数据相适合,符合线性化图(R-2近似为0.900-0.999),其描述了污染和原始土壤的砷吸附动力学。砷吸附数据通常由ELOVICH模型最佳地描述,具有比PSO模型更小的标准化标准偏差(Delta Q <5%)。此外,与新鲜砷(63-96%)位点的可更换和特异性吸附的表面结合对老化污染土壤中的(v)吸附的总体低速率产生影响。原始的土壤“特别是亚马拉雷蒂氏土壤”显示椎间内部扩散和/或表面沉淀,这可以有助于在土壤中的(v)结合的更大不可逆性。相比之下,在原始的砂土中发生的(v)吸附以与老化的污染土壤的类似时尚,最有可能由于具有有限的强粘结位点的土壤基团。本研究的详细知识为污染站点的填海和管理提供了新的见解。

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