Y. Fujikawa et M. Fukui, RADIONUCLIDE SORPTION TO ROCKS AND MINERALS - EFFECTS OF PH AND INORGANIC ANIONS .2. SORPTION AND SPECIATION OF SELENIUM, Radiochimica Acta, 76(3), 1997, pp. 163-172
Sorption of Se-75 to rocks (metamorphosed chert and shale, and ganodio
rite) and minerals (hematite, magnetite and calcite) was investigated
in 0.001 N, 0.01 N and 0.1 N solutions of Na2SO4, NaCl, Na2CO3 and NaH
CO3. The effect of pH and co-existing anions on the sorption of this r
adionuclide is discussed in terms of surface complex formation. Variat
ion in the speciation of Se-75 during the sorption experiment was exam
ined. A low pH solution produced a protonated surface on the sorbent w
hich attracted the selenium anions. Of the co-existing anions (SO42-,
Cl-, CO32- and HCO3-) which compete with selenium anions for sorption
sites, SO42- was the most effective competitor. Oxidation of radioacti
ve Se (first added as selenite) to selenate was promoted in the presen
ce of sorbents. There was a positive correlation between the ratio of
selenate in solution and the ratio of Se sorbed. One explanation for t
his correlation is that the oxidation reaction of selenite to selenate
is caused in part by electron transfer in the surface complex formed
between the sorbent and selenite, resulting in the release of selenate
into solution. Greater selenite sorption therefore leads to a larger
amount of selenate in the solution. Because Se is one of the most mobi
le radionuclides contained in the final form of radioactive wastes, we
compared its affinity for geological materials with other nuclides. N
uclide affinity for the solid phase, with the exception of calcite, wa
s in the order Co greater than or equal to Cs greater than or equal to
Mn greater than or equal to Sr greater than or equal to Se in slightl
y acidic to basic solutions (pH 5.5 to 10.1) and Cs > Se greater than
or equal to Co greater than or equal to Mn congruent to Sr in acidic s
olutions (pH 4.5 to 4.8). Radionuclide sorption to calcite differed fr
om that to other geological samples, the affinity for which decreased
in the order Mn greater than or equal to Co greater than or equal to S
r greater than or equal to Se greater than or equal to Cs (pH 6.5 to 1
0.2).