Probing the importance of planar surfaces and crystal edges for electron transfer within iron-bearing clays

Zhaohui Wang

doi:10.1039/c4ra04521a

Probing the importance of planar surfaces and crystal edges for electron transfer within iron-bearing clays

Zhaohui Wang^*

^*Corresponding author for this work

Donghua University

Research output: Contribution to journal › Article › peer-review

6 Scopus citations

Abstract

We demonstrated the importance of basal planes and crystal edge for electron transfer within montmorillonite (MK10) and nontronite (NAu-2) by a facile dye-sensitized photoreduction method. It was found that not all structural Fe in the clay matrix was redox-active. The results are vital to the utilization of naturally abundant clays in environmental redox chemistry. This journal is

Original language	English
Pages (from-to)	31476-31480
Number of pages	5
Journal	RSC Advances
Volume	4
Issue number	59
DOIs	https://doi.org/10.1039/c4ra04521a
State	Published - 2014
Externally published	Yes

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10.1039/c4ra04521a

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abstract = "We demonstrated the importance of basal planes and crystal edge for electron transfer within montmorillonite (MK10) and nontronite (NAu-2) by a facile dye-sensitized photoreduction method. It was found that not all structural Fe in the clay matrix was redox-active. The results are vital to the utilization of naturally abundant clays in environmental redox chemistry. This journal is",

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AB - We demonstrated the importance of basal planes and crystal edge for electron transfer within montmorillonite (MK10) and nontronite (NAu-2) by a facile dye-sensitized photoreduction method. It was found that not all structural Fe in the clay matrix was redox-active. The results are vital to the utilization of naturally abundant clays in environmental redox chemistry. This journal is

UR - https://www.scopus.com/pages/publications/84904816756

U2 - 10.1039/c4ra04521a

DO - 10.1039/c4ra04521a

M3 - 文章

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JO - RSC Advances

JF - RSC Advances

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Probing the importance of planar surfaces and crystal edges for electron transfer within iron-bearing clays

Abstract

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