S. Fendorf et al., Pyrolusite surface transformations measured in real-time during the reactive transport of Co(II)EDTA(2-), GEOCH COS A, 63(19-20), 1999, pp. 3049-3057
Oxidation of Co(II)EDTA(2-) to Co(III)EDTA(-) by manganese and iron hydrous
oxide minerals enhances the transport of Co-60 in subsurface environments.
Until now, reduction of the oxidant MnO2 has not been identified in hydrod
ynamic systems, leaving the fate and transport mechanisms involving Co-60 i
n natural environment!; unresolved. We investigated the transport of Co(II)
EDTA(2-) through packed beds of beta-MnO2 and identified the reaction mecha
nism using a novel hydrodynamic how cell coupled with X-ray absorption near
edge structure (XANES) spectroscopy. Using this technique we are able to d
etermine both solution and solid-phase species of cobalt and manganese in r
eal-time. Co(II)EDTA(2-) is produced while Mn(IV) is reduced to Mn(III) whi
ch forms an alpha-Mn2O3 layer on pyrolusite. This layer passivates the surf
ace after an initial reaction period and ultimately limits the production o
f Co(III)EDTA(-). As a consequence, the enhanced transport of Co-60 by oxid
ative processes may be diminished by continual exposure to pyrolusite-an ad
vantage from an environmental quality perspective. It has also been clarifi
ed that Mn(III) is formed rather than Mn(II) resulting in formation of a st
able trivalent manganese solid (alpha-Mn2O3). Copyright (C) 1999 Elsevier S
cience Ltd.