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污染和未污染石灰性土壤中 Cd、Cu、Mn、Ni、Pb 和 Zn 的竞争吸附。

Competitive sorption of Cd, Cu, Mn, Ni, Pb and Zn in polluted and unpolluted calcareous soils.

机构信息

Department of Soil Science, College of Agriculture, Bu-Ali Sina University, Hamedan, Iran,

出版信息

Environ Monit Assess. 2013 Nov;185(11):8831-46. doi: 10.1007/s10661-013-3216-1. Epub 2013 May 17.

DOI:10.1007/s10661-013-3216-1
PMID:23677680
Abstract

The objectives of this study were to investigate competitive sorption behaviour of heavy metals (Cd, Cu, Mn, Ni, Pb and Zn) under different management practices and identify soil characteristics that can be correlated with the retention and mobility of heavy metals using 65 calcareous soil samples. The lowest sorption was found for Mn and Ni in competition with the other metals, indicating the high mobility of these two cations. The Freundlich equation adequately described heavy metals adsorption. On the basis of Freundlich distribution coefficient, the selectivity sequence of the metal adsorption was Cu > Pb > Cd > Zn > Ni > Mn. The mean value of the joint distribution coefficient (K dΣsp) was 182.1, 364.1, 414.7, 250.1, 277.7, 459.9 and 344.8 l kg(-1) for garden, garlic, pasture, potato, vegetables, wheat and polluted soils, respectively. The lowest observed K dΣsp in garden soil samples was due to the lower cation exchange capacity and lower carbonate content. The results of the geochemical modelling under low and high metal addition indicated that Cd, Ni, Mn and Zn were mainly retained via adsorption, while Pb and Cu were retained via adsorption and precipitation. Stepwise forward regression analysis showed that clay, organic matter and CaCO3 were the most important soil properties influencing competitive adsorption of Cd, Mn, Ni and Zn. The results in this study point to a relatively easy way to estimate distribution coefficient values.

摘要

本研究旨在探讨不同管理措施下重金属(Cd、Cu、Mn、Ni、Pb 和 Zn)的竞争吸附行为,并利用 65 个钙质土壤样本,确定与重金属保留和迁移相关的土壤特性。Mn 和 Ni 与其他金属竞争时的吸附量最低,表明这两种阳离子的迁移性较高。Freundlich 方程能很好地描述重金属的吸附。根据 Freundlich 分布系数,金属吸附的选择性顺序为 Cu > Pb > Cd > Zn > Ni > Mn。在联合分布系数(KdΣsp)的平均值方面,花园土、大蒜土、牧场土、土豆土、蔬菜土、小麦土和污染土的 KdΣsp 值分别为 182.1、364.1、414.7、250.1、277.7、459.9 和 344.8 l kg(-1)。花园土壤样本中观察到的最低 KdΣsp 值归因于较低的阳离子交换能力和较低的碳酸盐含量。在低金属添加和高金属添加下的地球化学模型结果表明,Cd、Ni、Mn 和 Zn 主要通过吸附被保留,而 Pb 和 Cu 则通过吸附和沉淀被保留。逐步正向回归分析表明,粘土、有机质和 CaCO3 是影响 Cd、Mn、Ni 和 Zn 竞争吸附的最重要土壤特性。本研究结果表明,一种相对简单的方法可以估算分布系数值。

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