Many of the by-products from coal combustion and flue gas desulfurizat
ion are cementitious, which suggests utilization in some settings repl
acing conventional cements. Information on the long-term stability of
these materials in Nature can be obtained from studies of landfilled b
y-products. Five coal combustion by-products (CCBs) landfilled at four
sites in the USA were characterized by X-ray diffraction. Where moist
ure was available during or after disposal, the materials were changed
chemically, physically and mineralogically over time, in processes an
alogous to diagenesis of buried sediments. At three of the sites, init
ially formed crystalline-phase assemblages were transformed into an as
semblage dominated by ettringite and thaumasite. At one site where a h
igh-sodium by-product was landfilled, an assemblage of Na-rich phases,
including a zeolite and a zeolite-related nosean-hauyne phase, as wel
l as tobermorite, was observed. This assemblage is unique and previous
ly unobserved in CCBs. Diagenesis associated with many of these CCBs r
educed strength and increased permeability after only a few years in t
he natural environment. The characteristics of the altered by-products
resemble those of soils more than concrete. Initially promising 7 or
28 day laboratory tests of strength and permeability may not be charac
teristic of these materials on exposure to the environment. Blending o
f CCBs with fly ash to increase the proportion of cementitious C-S-H,
and controlling subsequent moisture additions, could minimize deleteri
ous by-product diagenesis. (C) 1997 Elsevier Science Ltd.