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A study on the exchange additivity of zinc in solid mixtures in seawater——Ⅱ.Stepwise exchange in δ-MnO2/montmorrillonite mixture
引用本文:Meng Xiaoguang,Zhang Zhengbin,Liu Liansheng. A study on the exchange additivity of zinc in solid mixtures in seawater——Ⅱ.Stepwise exchange in δ-MnO2/montmorrillonite mixture[J]. 海洋学报(英文版), 1988, 7(2): 261-265
作者姓名:Meng Xiaoguang  Zhang Zhengbin  Liu Liansheng
作者单位:Shandong College of Oceanography, Qingdao, China;Shandong College of Oceanography, Qingdao, China;Shandong College of Oceanography, Qingdao, China
基金项目:Project Supported by the National Natural Science Foundation of China
摘    要:In this study the zinc exchange process and the reason for the non-additive exchange of δ-MnO2/montmorrillonite have been investigated. The results suggest that with pH increasing from 2 to 8, the stepwise exchange of zinc occurs on δ-MnO. and montmorrillonite in their mixture.At low pH zinc ions are bound on δ-MnO2, while at high pH, the exchange on montmorrillonite dominates the surface interaction in the mixture. The study demonstrates that the stepwise exchange and the heterogeneity of the binding sites on δ-MnO2 surface are the reason for the non-additive exchange. It is also shown that when δ-MnO2 amounts to 5 %, zinc exchange on sea sediments is controlled by 8-MnO2.

收稿时间:1987-05-23
修稿时间:1987-10-06

A study on the exchange additivity of zinc in solid mixtures in seawater——Ⅱ.Stepwise exchange in δ-MnO2/montmorrillonite mixture
Meng Xiaoguang,Zhang Zhengbin and Liu Liansheng. A study on the exchange additivity of zinc in solid mixtures in seawater——Ⅱ.Stepwise exchange in δ-MnO2/montmorrillonite mixture[J]. Acta Oceanologica Sinica, 1988, 7(2): 261-265
Authors:Meng Xiaoguang  Zhang Zhengbin  Liu Liansheng
Affiliation:Shandong College of Oceanography, Qingdao, China
Abstract:In this study the zinc exchange process and the reason for the non-additive exchange of δ-MnO2/montmorrillonite have been investigated. The results suggest that with pH increasing from 2 to 8, the stepwise exchange of zinc occurs on δ-MnO2 and montmorrillonite in their mixture.At low pH zinc ions are bound on δ-MnO2, while at high pH, the exchange on montmorrillonite dominates the surface interaction in the mixture. The study demonstrates that the stepwise exchange and the heterogeneity of the binding sites on δ-MnO2 surface are the reason for the non-additive exchange. It is also shown that when δ-MnO2 amounts to 5%, zinc exchange on sea sediments is controlled by δ-MnO2.
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