Investigations in the Fe – S – Se system
1)
2) MSU, Faculty
of Materials Science, GSP-3, Leninskiye Gory,
3) Forschungszentrum Jülich, Institute für Energieforschung
6, D-52425 Jülich, Germany.
*) Helmholtz
Virtual Institute „Advanced Solid-Aqueous RadioGeochemistry“,
Motivation
The long-lived fission product 79Se
(half-life >105 yrs) is one of the elements of concern for the
safe storage of High-Level nuclear Waste (HLW). The chemistry of Se resembles
that of sulfur and the Se solubility is largely controlled by its oxidation
state. The +VI and +IV oxidation states prevail as mobile aqueous oxyanions,
while Se in the oxidation states 0, -I and –II prevail as solids with low
solubility [1]. The geochemistry of Se is largely controlled by that of Fe,
with which Se is closely affiliated [2]. The redox potential (reducing
conditions) of most rock formations currently considered for the HLW disposal
is controlled by pyrite (FeS2). FeS2 is the
thermodynamically stable end product of iron compounds under reducing
conditions, and can be produced from iron monosulfide precursor (
Experimental - results
Se(IV) ions were added to a suspension of FeSam
(disordered mackinawite) and allowed to react for seven days. In a separate
experiment, a Fe(II) solution was added to a solution containing S(-II) and
Se(-II) ions and allowed to react overnight. These experiments aimed at simulating
Se retention on pre-existing mackinawite and mackinawite formation in the
presence of selenide ions, respectively. Both samples were characterized using
X-ray absorption spectroscopy (XAS) at the Se K-edge. The XANES region provided information on the Se oxidation
state and the EXAFS region on short-range structure.
In the XANES region, both the edge position and the relative intensity
of the white line [3] suggest a lower formal Se oxidation state in the
co-precipitation experiment (-II) than in the adsorption experiment (-I or 0). Analysis
of the EXAFS data indicates the presence of Se neighbors at 2.34(2) Å in the adsorption experiment. XANES
results combined with EXAFS data strongly suggests a reduction and
precipitation of a solid Se(0) phase upon Se(IV) adsorption on FeSam,
corroborating previous findings [3]. In contrast, the
presence of one Fe (interatomic Se-Fe distance = 2.37(1) Å) and two S shells
surrounding Se upon co-precipitation are found in EXAFS data modeling. The
detection of Fe and S backscatterers associated with the low Se oxidation state
may indicate that Se is located in a mackinawite-like environment. Upcoming
work will focus on the Se co-precipitation with pyrite. These results will
provide valuable information of the Se retention by iron sulfides.
Acknowledgements
N. F. acknowledges the Helmholtz Virtual Institute
“Advanced Solid-Aqueous Radiogeochemistry” (
References
[1] Elrashidi M.A.,
[2] Hatten Howard III J. (1977) Geochim. Cosmochim. Acta 41,
1665-1678.
[3] Scheinost A.C. and Charlet L. (2008) Environ. Sci. Technol. 42, 1984-1989.