Effect of Zn coprecipitation on the structure of layered Mn oxides
Effect of Zn coprecipitation on the structure of layered Mn oxides
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DOI:
10.1016/j.chemgeo.2018.05.044
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发表时间:
2018-08
期刊:
影响因子:
3.9
通讯作者:
Shiliang Zhao;Qian Wang;Jingying Sun;O. Borkiewicz;Rixiang Huang;E. M. Saad;Benjamin P. Fields
中科院分区:
文献类型:
--
作者:
Shiliang Zhao;Qian Wang;Jingying Sun;O. Borkiewicz;Rixiang Huang;E. M. Saad;Benjamin P. Fields
Mn oxides (MnOx) are a group of ubiquitous metal oxides in the environment and can significantly affect the biogeochemical cycles of metals, nutrients, and contaminants. Due to their negative surface charge across a wide range of environmental conditions, metal cations have strong affinities for MnOx, and the presence of metal cations during or after the formation of MnOxmight significantly affect their structure and reactivity. This study systematically investigates the effects of Zn2+presence during mineral formation (i.e. coprecipitation) on the structure of acid birnessite and δ-MnO2, two synthetic analogs that are structurally similar to fresh biogenic MnOxbut with different crystallinity. For both acid birnessite and δ-MnO2, Zn2+existed as surface adsorbed species at vacancy sites, interrupted layer stacking alongcaxis, and caused reductions of the lateral particle size. Zn2+also reduced Mn(III) contents in δ-MnO2layers, leaving more vacancy sites (capped by adsorbed Zn2+). The reduction of layer stacking was more obvious for acid birnessite, while the modification of layer structure was more significant for δ-MnO2. These structural changes will likely lead to modified reactivity of MnOxin natural systems.