Abstract
The solid-phase Se speciation after short-term (3 weeks)
contact of selenite [Se(IV)] oxyanions with pyrite (FeS2) and
troilite (FeS)wasinvestigated using X-ray absorption spectroscopy
(XAS; X-ray absorption near-edge spectroscopy-extended
X-ray absorption fine structure (XANES-EXAFS)). It was found
that the nature of the sulfide mineral dictates the final
speciation since respectively Se0 and FeSex were formed,
meaning that the reaction mechanism is different and that these
phases cannot be regarded as geochemically similar. The
experimental results support the previously proposed sorption/
reduction mechanism for the reaction of selenite with pyrite
(8). In the presence of troilite the reduction proceeds through
the intermediate formation of Se0 by reduction of selenite
with dissolved sulfide. XAS data recorded for the FeS2 and
FeS were compared with different Se reference phases, ranging
in oxidation state from —II to +IV, used for validation of the
XAS analysis methodology. This methodology can in principle be
used to analyze Se phases formed in “in situ” geochemical
conditions such as high-level radioactive waste disposal facilities.
Original language | English |
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Pages (from-to) | 3595-3601 |
Journal | Environmental Science & Technology |
Volume | 42 |
Issue number | 10 |
DOIs | |
State | Published - 12 Apr 2008 |