Tc(VII) and Cr(VI) Interaction with Naturally Reduced Ferruginous Smectite from a Redox Transition Zone.
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DOI: 10.1021/acs.est.7b02191
Abstract: Fe(II)-rich clay minerals found in subsurface redox transition zones (RTZs) can serve as important sources of electron equivalents limiting the transport of redox-active contaminants. While most laboratory reactivity studies are based on reduced model clays,… read more here.
Keywords: interaction naturally; vii interaction; redox transition; naturally reduced ... See more keywords