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Assessment of trace heavy metals dynamics during the interaction of aqueous solutions with the artificial OECD soil: Evaluation of the effect of soil organic matter content and colloidal mobilization

机译:水溶液与人工OECD土壤相互作用过程中痕量重金属的动力学评估:评估土壤有机质含量和胶体迁移的影响

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摘要

A micro-contamination phenomenon was reproduced and studied at lab-scale, mimicking the irrigation of a standard artificial soil with a water solution containing three Heavy Metals (HMs) at trace concentration level. To assess the dynamics of micro-pollutants accumulation and migration trough the soil, the organic matter in the soil was varied, together with sodicity of the irrigation water. Accumulation of the investigated contaminants was observed mainly in the top layer (<= 1 cm) of the irrigated soil. This was attributed to the high interaction capacity of the soil compared to the low HM concentrations in the water phase. HMs transport pattern was described assuming a multi-component mechanism including: i) the interaction of HMs with the colloidal phase of the soil; ii) the slow and constant release of small molecular weight ligands detaching from the soil immobile matrix; iii) the transportation of HMs through the soil by these low molecular weight chaperon molecules. The mobility was directly related to the soil organic matter (SOM), since higher amount of SOM correspond to a higher number of chaperon molecules. In the first centimetre of the soil the metals were mostly bound to the acid labile fraction. Very low mobilization was observed with increasing sodicity in the leaching water, since such conditions were unfavourable to the colloidal mobilization of SOM. This indicated that water/soil transfer of pollutant is not only related to the contaminant concentration in the irrigation water but also to the characteristics of the aqueous solution and to the physical-chemical properties of the soil. (C) 2016 Elsevier Ltd. All rights reserved.
机译:复制并在实验室规模进行了微污染现象的研究,模拟了用含有三种痕量浓度重金属(HMs)的水溶液灌溉标准人工土壤的过程。为了评估微量污染物在土壤中的累积和迁移动力学,对土壤中的有机物和灌溉水的碱度进行了变化。观察到的污染物的积累主要在灌溉土壤的顶层(<= 1 cm)中观察到。这归因于与水相中低HM浓度相比,土壤具有较高的相互作用能力。 HMs的传输模式是在假设多组分机理的前提下描述的:i)HMs与土壤胶体相的相互作用; ii)从土壤固定基质上缓慢而持续释放小分子量配体; iii)这些低分子量伴侣分子通过土壤运输HMs。迁移率与土壤有机质(SOM)直接相关,因为较高数量的SOM对应于较高数量的分子伴侣。在土壤的第一厘米,金属大部分与酸不稳定部分结合。随着浸出水中的碱度增加,观察到非常低的迁移率,因为这样的条件不利于SOM的胶体迁移。这表明污染物的水/土壤转移不仅与灌溉水中的污染物浓度有关,而且还与水溶液的特性以及土壤的物理化学性质有关。 (C)2016 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Chemosphere》 |2016年第11期|382-391|共10页
  • 作者单位

    Univ Cassino & Southern Lazio, Dept Civil & Mech Engn, Via Di Biasio 43, I-03043 Cassino, FR, Italy|Univ Paris Est, UPEM, Lab Geomat & Environm, EA 4508, F-77454 Marne La Vallee, France;

    Univ Paris Est, UPEM, Lab Geomat & Environm, EA 4508, F-77454 Marne La Vallee, France;

    Univ Naples Federico II, Dept Civil Architectural & Environm Engn, Via Claudio 21, I-80125 Naples, Italy;

    Univ Cassino & Southern Lazio, Dept Civil & Mech Engn, Via Di Biasio 43, I-03043 Cassino, FR, Italy;

    Univ Naples Federico II, Dept Civil Architectural & Environm Engn, Via Claudio 21, I-80125 Naples, Italy;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Agricultural wastewater reuse; Emerging contaminants; OECD soil; Trace metals; Soil colloids; Soil organic matter;

    机译:农业废水回用;新兴污染物;经合组织土壤;微量金属;土壤胶体;土壤有机质;

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