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首页> 外文期刊>Journal of Geochemical Exploration: Journal of the Association of Exploration Geochemists >Sorption and desorption of potentially toxic metals (Cd, Cu, Ni and Zn) by soil amended with bentonite, calcite and zeolite as a function of pH
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Sorption and desorption of potentially toxic metals (Cd, Cu, Ni and Zn) by soil amended with bentonite, calcite and zeolite as a function of pH

机译:用膨润土,方解石和沸石的土壤进行潜在有毒金属(CD,Cu,Ni和Zn)的吸附和解吸,作为pH值的函数

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Sorption and desorption studies of cadmium (Cd), copper (Cu), nickel (Ni) and zinc (Zn) were carried out at the pH range of 2 to 9 by a soil amended with three sorbents including bentonite, calcite and zeolite. A geochemical computer model was used to simulate the sorption of metals by control and amended soils as influenced by pH. Metals sorption on control and amended soils was dependent on pH, and increased with increasing equilibrium pH. Furthermore, metals sorption on soil amended by sorbents was greater than control, indicating the increase of soil sorption capacity by adding sorbents, while their desorption decreased. The modeling results indicated that the sorption of metals was modeled successfully using the ion exchange and surface complexation reactions. In general, the maximum sorption of metals was observed by bentonite-amended soil and calcite-amended soil, whereas the maximum desorption of all metals obtained in zeolite-amended soil, suggesting that the sorption of metals on zeolite was based on the reversible mechanism. In general, the sequence of metals sorption at pH 2 to 9 for all treatments was in order of Cu > Zn > Cd >= Ni. In addition, this sequence was observed mostly for metals activity and desorption (occasionally an exchange in the positions of Cd and Ni) but with an inverse trend. Results indicated that distribution coefficient (K-d) increased with increasing pH and, in particular, had a sharp increase at the neutral to alkaline pH.
机译:通过用三种吸附剂(包括膨润土,方解石和沸石)的土壤在2至9的pH范围内进行镉(Cd),铜(Cu),镍,镍(Ni)和锌(Zn)的吸附和解吸研究。通过PH的影响,使用地球化学计算机模型通过控制和修正的土壤来模拟金属的吸附。对照对照和修正的土壤的金属吸附依赖于pH,随着均衡pH的增加而增加。此外,吸附剂修正的土壤的金属吸附大于对照,表明通过添加吸附剂来增加土壤吸附能力,而其解吸减少。建模结果表明,使用离子交换和表面络合反应成功建模金属的吸附。通常,膨润土修正的土壤和方解石修正的土壤观察到金属的最大吸附,而在沸石修正的土壤中获得的所有金属的最大解吸,表明沸石上金属的吸附是基于可逆机制。通常,对于所有处理的pH 2至9的金属吸附序列是Cu> Zn> Cd> = Ni的顺序。此外,该序列主要用于金属活性和解吸(偶尔在CD和Ni的位置交换),但具有逆趋势。结果表明,分布系数(K-D)随着pH的增加而增加,特别是在中性至碱性pH下急剧增加。

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