Characterization of Candiota (South Brazil) coal and combustion by-product

Abstract

Elemental composition and mineralogy of a high ash feed coal (ash: 49.7 wt.%), and its bottom and fly ash from a Brazilian power plant (Presidente Médici Power Plant or UTPM-446 MW) was determined using ICP-MS, ICP-AES, X-ray diffraction (XRD) and scanning electron micrography (SEM). Most trace elements in coal fall in the usual range determined for world coals. However, concentrations of some elements were higher than the expected for coals, including Cs Rb and heavy rare earth elements (REEs). This might be due to the high content of detrital minerals of the studied coal, given that these elements are usually associated with clay minerals. Elements were classified into three groups based on the analysis of trace element concentrations in fly and bottom ashes, and enrichments or depletions of these concentrations in relation to the coal: Group I (volatile elements with subsequent condensation): As, B, Bi, Cd, Ga, Ge, Mo, Pb, S, Sb, Sn, Tl and Zn; Group II (no volatile elements enriched in bottom ash vs. fly ash): Ca, Fe, Mn, P, Ti and Zr; Group III (low volatile elements with no partitioning between fly and bottom ashes): Al, Ba, Be, Co, Cr, Cs, Hf, K, Li, Mg, Na, Ni, Rb, Sr, Th, U, W, Y and most of REE. The mass balance for trace elements obtained demonstrated that the volatile emission of the trace elements studied is very low. According to the leachable proportion obtained, the elements may be classified as follows: B (40–50%)>Mo>Cu>Ge=Li=Zn=As>, Ni, Sb, Tl, U>Ba, Cd, Sr, V (0.3–2%). For the other elements studied, the leachable fraction is in most cases <1% of the bulk content.