Several experiments were set up to study Se speciation and solubility in the reducing
Boom clay environment, starting from oxidized Se species which were added in oversaturation with respect to the thermodynamic solubility of reduced Se solid phases. Upon introduction of SeO
32− to FeS
2-containing samples, adsorption of SeO
32− occurred at the FeS
2 surface, and led to a reduction and precipitation of a Se
0 solid phase with a solubility of 3×10
−9 M (after 60 days). In the presence of humic substances, an association of Se with these humic substances was observed and the 3×10
−9 M solubility limit was not reached in the same time delay. Upon introduction of SeO
32− to Boom
clay suspensions (equilibration up to 9 months), the initial adsorption of SeO
32− on the solid phase was increased with respect to systems containing only FeS
2, due to the presence of (illite)
clay minerals. This competing adsorption process, and the presence of humic substances, again decreased the kinetics of reduction with respect to FeS
2 samples. Also, an association of Se with Boom
clay humic substances was observed, and amounted up to
![not, vert, similar](http://www.sciencedirect.com/scidirimg/entities/223c.gif)
10
−7 M in some samples after 9 months equilibration.