We examined the suitability using a flue gas desulfurization grout (FGDG) f
or the attenuation and abatement of acidic mine drainage (AMD). The FGDG us
ed was a mixture of fly ash (FA) and filter cake (FC),vith a FA/FC ratio of
1:1 to improve handling. Five percent of lime (CaO) was added to improve s
trength development and allow the use of this FGDG as a hydrologic seal for
underground mines. Acidic mine drainage solutions collect from wells locat
ed within mine voids were reacted with samples of FGDG for up to 168 d, to
evaluate the potential for grout dissolution subsequent to subterranean imp
lacement. Shortly upon reaction with AMD, FGDG released a number of ions in
to solution (As, B, Ca, K, Na, Se, SO4), concomitant with a rapid increase
in solution pH (8.5), causing decreases in the solubility of most cations (
Al, Fe, Mn, Zn). Significant increases in dissolved As and B concentrations
were noted. Both elements were present in solution at levels below respect
ive regulatory limits for drinking water. Of the original quantities of As
and B present in FGDG, 1.3 and 45.6%, respectively, were released to soluti
on over a 168-d reaction period. Concomitant with changes in solution compo
sition, reaction of FGDG with AMD resulted in a loss of ettringite and hann
ebachgite and a growth of gypsum. Additional changes in mineralogy were obs
erved as FGDG equilibrated with AMD solutions. From these reactions, the lo
ng-term stability of FGDG in underground acidic mine environments is questi
onable and warrants study in situ.