Published in
Royal Society of Chemistry, Environmental Science: Nano, 6(6), p. 1704-1715, 2019
DOI: 10.1039/c9en00228f
Links
Tools
“Switching on” iron in clay minerals
This paper was not found in any repository, but could be made available legally by the author.
Full text: Unavailable
Published version:
archiving forbidden
Data provided by 
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).