The commercial introduction of pressurized fluidized bed combustion (P
FBC) has spurred evaluation of ash management options for this technol
ogy. Ashes used in this study were produced in the Foster Wheeler Ener
gia Oy's circulating PFBC pilot facility in Karhula, Finland and the A
merican Electric Power Tidd PFBC facility in Ohio. The fly ashes conta
in numerous compounds, including calcite (CaCO3), anhydrite (CaSO4) an
d, in the Tidd By ash, dolomite [CaMg(CO3)(2)], that have the potentia
l to be a nutrient source and a soil amendment for the reclamation of
acid and sodic soils (soils influenced by high levels of sodium). The
objective of this research was to determine if the PFBC ash could be u
sed as soil amendments for acid and sodic soils. The research effort c
onsisted of three separate tests: (1) a laboratory equilibration study
to determine the influence of By ash amendments on pH and EC (electri
cal conductivity) of actively oxidizing, acid-forming, mine spoil mate
rial, (2) a greenhouse study to determine the influence of fly ash on
plant growth; and (3) a hydraulic conductivity evaluation of sodic soi
ls treated with the PFBC fly ash materials. The study showed that the
PFBC fly ashes were effective acid spoil amendments. In a comparison w
ith ag-lime, the fly ash reacted with the spoil at a slower rate and t
he final pH of the treated material was slightly lower (similar to 7 V
ersus similar to 8). In addition, the EC of the fly-ash-treated spoil
was similar to 1 mS cm(-1) higher than that associated with the ag-lim
e-treated materials. The greenhouse study demonstrated that the By ash
was an effective amendment for the remediation of acid spoil material
s. In fact, the soils amended with fly ash supported higher plant prod
uction than those amended with ag-lime These findings are possibly due
to pH and nutritional effects. The hydraulic conductivity study demon
strated that the application of fly ash to sodic soils resulted in enh
anced permeability of the treated soil. (C) 1997 Elsevier Science Ltd.