Morphological and chemical characterization of calcium hydrate phases formed in alteration processes of deposited municipal solid waste incinerator bottom ash

Citation
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
Journal title
ENVIRONMENTAL SCIENCE & TECHNOLOGY
ISSN journal
0013936X → ACNP
Volume
34
Issue
23
Year of publication
2000
Pages
5030 - 5037
Database
ISI
SICI code
0013-936X(200012)34:23<5030:MACCOC>2.0.ZU;2-E
Abstract
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.