Phase-mineral and chemical composition of fractions separated from composite fly ashes at the Soma power station, Turkey

Vassilev S., Vassileva C., Karayigit A. İ., Bulut Y., Alastuey A., Querol X.

INTERNATIONAL JOURNAL OF COAL GEOLOGY, cilt.61, ss.65-85, 2005 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 61
  • Basım Tarihi: 2005
  • Doi Numarası: 10.1016/j.coal.2004.05.004
  • Dergi Adı: INTERNATIONAL JOURNAL OF COAL GEOLOGY
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.65-85
  • Anahtar Kelimeler: mineral and chemical composition, trace elements, coal, fly ash, Turkey, SOLID-WASTE PRODUCTS, TRACE-ELEMENTS, FEED COALS, COMBUSTION WASTES, GEOCHEMISTRY, PARTICLES, BEHAVIOR, FORMS
  • Hacettepe Üniversitesi Adresli: Evet

Özet

The phase-mineral and chemical composition of six fractions recovered from two fly ashes (FAs) produced in the Soma power station (Turkey) was characterized to predict their possible environmental concerns and potential utilization directions. A combination of conventional separation procedures including sieving, hand picking, sink-float and magnetic separations, as well as leaching and evaporation, was used to isolate the following fractions: (1) char concentrates (CCs); (2) light fractions (<1 g cm(-3)) (LFs); (3) water-soluble residues (WRs); (4) magnetic fractions (Ws); (5) nonmagnetic coarse-grained fractions (>63 pm) (NCFs); and (6) nonmagnetic fine-grained fractions (<63 mum) (NFFs). CCs (3.3-3.4%) are composed of char (61-68%) and some inorganic phases, and are highly enriched in U>S>Mn>Mo>Fe>Sb. Us (0.4-0.8%) contain porous cenosphere, spongy, and vesicular char types (21-54%) impregnated by calcite, anhydrite, portlandite, and clay minerals. These fractions show high concentrations of Sb>Se>As. WRs (1.7-2.6%) consist of gypsum, portlandite, Ca oxalate, and calcite (92-98%), and are highly enriched in water-soluble Sb>Mo>S>Ca. The greatest amounts (1-37%) leached from FAs reveal Sb>Mo>S>Ca>Sr>Se>(B, Na)>Li. MFs (1.4-2.3%) are concentrated in magnetite, hematite, and Fe-spinel (31-39%), and are highly enriched in Mn>Fe>Co>Cu>Ni>Zn>(Mo, Yb)>(Lu, Tm, Y)>(Er, Ho, Mg)>Sb. NCFs (49-56%) include mostly coarse-grained glass, quartz, calcite, and mullite, and these are the poorest in trace elements fractions. NFFs (39-47%) contain dominantly fine-grained glass, calcite, quartz, char, and mullite, and are slightly enriched in some chalcophile elements. Possible environmental concerns are related mainly to the trace element mobility in WRs, Us, and CCs, while the potential utilization directions are connected mostly with the composition of MFs, WRs, CCs, Us, and NFFs. (C) 2004 Elsevier B.V. All rigths reserved.