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The Waste-to-Energy Cycle |
1 Environmental Research Group, Civil Engineering Department, University of New Hampshire, Durham, NH, USA taylor.eighmy{at}unh.edu
2 Geology Department, Carnegie Science Center, Bates College, Lewiston, ME, USA deusden{at}abacus.bates.edu
The use of orthophosphate (PO43–) as a chemical stabilization agent for municipal solid waste (MSW) combustion residues is widespread in Japan and North America. The application of this technology to MSW ashes generally parallels its use with other metal contaminated wastes (e.g., soils, sediments, smelter dusts, slags, wire chopping wastes, mine tailings), especially Pb-contaminated soils. The technology relies on the fact that PO43– forms very insoluble and stable minerals for a variety of divalent metal cations (e.g., Pb, Cd, Cu, and Zn). Extensive data from phosphate-treated contaminated soil systems suggest that stabilization involves surface immobilization reactions involving sorption, heterogeneous nucleation and surface precipitation, and/or solution phase precipitation involving homogeneous nucleation and precipitation. A geochemical basis for use of PO3–4 in ash systems is presented with a focus on the wide theoretical pH distribution, pH-pE predominance and redox stability of Cd, Cu, Pb, and Zn phosphates within complex bottom ash pore water systems. Stabilization mechanisms in bottom ashes, scrubber residues, and vitrification dusts are similar to those observed in soil systems. Some longer term leaching behaviour of phosphate-stabilized ashes are presented. The roles of Ostwald ripening, solid solutions (e.g., (Pb,Ca)5(PO4)3OH), and kinetically controlled reaction pathways probably are more important than what is presently envisioned in phosphate-stabilized ash systems.
