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Minimization of Hg and trace elements during coal combustion and gasification processes  67

           being vaporized from the fuel, the TEs may undergo reactions both with the ash par-
           ticles and the gaseous species in the flue gas. The reactions between the vaporized TEs
           and the ash particles constitute an important mechanism for the retention of TEs in
           large fly ash particles that are easier to be captured by the air pollution control systems
           (Senior et al., 2000a). Very few elements remain in the vapor state, probably only var-
           iable proportions of the total amount of Hg and the halogens, but even these may be
           associated with the surfaces of very fine fly ash particles.
              The final fate of TEs is determined by complex and interrelated processes such as
           vaporization, reaction, nucleation, condensation, and coagulation. Fig. 3.3 shows a
           general model of fine ash formation mechanisms for TEs which involves a series of
           complex processes. Attalla et al. (2004) concluded the elemental form of trace species
           has an influence on its final partitioning; the more volatile elements seem to vaporize
           independently of the mode of occurrence; and the char particle temperature determines
           the degree of volatilization. Moreover, some postcombustion zone transformations
           have been identified which affect TE partitioning. For example, the interaction of
           Ca with As, Se, and Cd dictates that for coals, which contain significant CaO, the par-
           titioning behavior of these elements is controlled by surface reactions rather than
           condensation.


                                                Nucleation / condensation/
                              Metal vapor            coagulation     Submicron
                                                                      particles
                                        Surface reaction/
                                         condensation
                                                            Attritive
                                Vaporization   Porous      fragmentation
                                                          fragmentation
                                               particle
                                                            Explosive


                                                                 Submicron inclusions,
                                                                  residual particles,
                                                                secondary atomization
              Coal
                                          Inherently
                      Porous char                Cenospheric
                                         bound metal
                                                   particle
                          Mineral  Excluded
                          inclusions  ash
                                               Dense
                                               particle

                                                               Supermicron
                                                                particle
           Figure 3.3 Ash formation mechanism for trace elements.
           Adapted from Attalla, M.I., Morgan, S., Riley, K., Bryant, G., Nelson, P.F., 2004. Trace Element
           Deportment in Combustion Processes. Research Report 50, Pullenvale, Queensland, Australia,
           84 pp.
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