Morphological and chemical characterization of calcium hydrate phases formed in alteration processes of deposited municipal solid waste incinerator bottom ash
C. Speiser et al., Morphological and chemical characterization of calcium hydrate phases formed in alteration processes of deposited municipal solid waste incinerator bottom ash, ENV SCI TEC, 34(23), 2000, pp. 5030-5037
Citations number
19
Categorie Soggetti
Environment/Ecology,"Environmental Engineering & Energy
During a study which investigates the exothermal heating of municipal solid
waste incinerator bottom ash.(MSWI) in a landfill samples were taken at a
solid waste incinerator in southern Germany operating at similar to 1000 de
greesC. The chemical and mineralogical bulk composition was determined by X
-ray fluorescence (XRF) and X-ray diffraction (XRD). Single bottom ash part
icles were investigated by optical microscopy and scanning electron microsc
opy with quantitative energy-dispersive X-ray microanalysis (SEMI EDX). The
fresh bottom ash consists of ash (42%), melting products (40%), metallic c
omponents (8%), usually aluminum, iron, and copper, and residual parts (10%
). The main phase of the bottom ash is glass (similar to 40%) with relics (
e.g, quartz) and quench phases (e.g. gehlenite). The main crystalline phase
s are silicates (e.g. gehlenite, augite, diopside, quartz), oxides (e.g. ma
gnetite, spinel, hematite), carbonates (e.g. calcite, metal-carbonates), an
d salts (e.g, chlorides and sulfides). In the deposited bottom ash endother
mic and exothermic alteration processes are observed (dissolution/precipita
tion of salts, glass corrosion, hydration and oxidation reactions of metals
, slaking of lime, cementation and carbonation processes). In the course of
these processes new mineralogical phases are formed. Among these are e.g.
anhydrite, portlandite, calcite, iron oxides and hydroxides, or gibbsite. T
hese minerals are always accompanied by different calcium-hydrate phases wi
th different mineralogical and chemical properties. The hydrate phases were
morphologically and chemically characterized by SEM/EDX. The single crysta
ls have a fibrous, ribbonlike, or tabular habit. Ca, Al, Si, and Fe were fo
und as main components, with minor amounts of Na, K, Mg, Cu, Zn, Ti, Mn, an
d CI, S, P.