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Title: “Switching on” iron in clay minerals

Abstract

We discovered a new mechanism explaining why iron in its oxidized form Fe( iii ) in clay minerals is reactive only in the presence of trace amounts of its reduced form—Fe( ii ).

Authors:
ORCiD logo [1]; ORCiD logo [2];  [1];  [1]
  1. Sandia National Laboratories, Geochemistry Department, Albuquerque, USA
  2. Pacific Northwest National Laboratory, Environmental Molecular Sciences Laboratory, Richland, USA
Publication Date:
Sponsoring Org.:
USDOE Office of Science (SC), Basic Energy Sciences (BES) (SC-22)
OSTI Identifier:
1511890
Resource Type:
Journal Article: Publisher's Accepted Manuscript
Journal Name:
Environmental Science: Nano
Additional Journal Information:
Journal Name: Environmental Science: Nano; Journal ID: ISSN 2051-8153
Publisher:
Royal Society of Chemistry (RSC)
Country of Publication:
United Kingdom
Language:
English

Citation Formats

Ilgen, A. G., Kukkadapu, R. K., Leung, K., and Washington, R. E. “Switching on” iron in clay minerals. United Kingdom: N. p., 2019. Web. doi:10.1039/C9EN00228F.
Ilgen, A. G., Kukkadapu, R. K., Leung, K., & Washington, R. E. “Switching on” iron in clay minerals. United Kingdom. doi:10.1039/C9EN00228F.
Ilgen, A. G., Kukkadapu, R. K., Leung, K., and Washington, R. E. Tue . "“Switching on” iron in clay minerals". United Kingdom. doi:10.1039/C9EN00228F.
@article{osti_1511890,
title = {“Switching on” iron in clay minerals},
author = {Ilgen, A. G. and Kukkadapu, R. K. and Leung, K. and Washington, R. E.},
abstractNote = {We discovered a new mechanism explaining why iron in its oxidized form Fe( iii ) in clay minerals is reactive only in the presence of trace amounts of its reduced form—Fe( ii ).},
doi = {10.1039/C9EN00228F},
journal = {Environmental Science: Nano},
issn = {2051-8153},
number = ,
volume = ,
place = {United Kingdom},
year = {2019},
month = {1}
}

Journal Article:
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Works referenced in this record:

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