设为首页 | 加入收藏
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].Acta Oceanologica Sinica,1988,(2):261-265
A study on the exchange additivity of zinc in solid mixtures in seawater——Ⅱ.Stepwise exchange in δ-MnO2/montmorrillonite mixture
A study on the exchange additivity of zinc in solid mixtures in seawater——Ⅱ.Stepwise exchange in δ-MnO2/montmorrillonite mixture
投稿时间:1987-05-23  修订日期:1987-10-06
DOI:
中文关键词:  
英文关键词:
基金项目:Project Supported by the National Natural Science Foundation of China.
作者单位
Meng Xiaoguang Shandong College of Oceanography, Qingdao, China 
Zhang Zhengbin Shandong College of Oceanography, Qingdao, China 
Liu Liansheng Shandong College of Oceanography, Qingdao, China 
摘要点击次数: 1021
全文下载次数: 659
中文摘要:
      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-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.
英文摘要:
      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-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.
查看全文   查看/发表评论  下载PDF阅读器
关闭