2000
DOI: 10.1021/ef990080w
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The Effect of Pressure on Ash Formation during Pulverized Coal Combustion

Abstract: A bituminous coal with a size faction of 63−90 μm was combusted under oxidizing atmosphere (air) in a drop tube furnace (DTF) and a pressurized drop tube furnace (PDTF) at a gas temperature of 1573 K and pressures of 0.1, 0.5, 1.0, and 1.5 MPa. Ash generated at high pressure was found to be much finer than ash generated at low pressure due to the differences in char structure. Pressure influcences ash formation by its effect on the structure of char particles after devolatilisation. Char samples produced at hi… Show more

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Cited by 69 publications
(42 citation statements)
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“…41 The stages can be broadly categorized as evaporation of moisture, devolatilization (decomposition), and char burnout and fragmentation. 13,15,42 During decomposition, volatile species present in the fuel (alkali metals, SO 2 /SO 3 , and chlorides) are released into the vapor phase. When these vapors cool, they condense to form the fine fraction of the ash, 15 whereas char burnout and fragmentation generally give rise to the coarse fraction of the ash due to coalescence of the nonvolatile components contained within the fuel matrix (included minerals).…”
Section: ■ Introductionmentioning
confidence: 99%
“…41 The stages can be broadly categorized as evaporation of moisture, devolatilization (decomposition), and char burnout and fragmentation. 13,15,42 During decomposition, volatile species present in the fuel (alkali metals, SO 2 /SO 3 , and chlorides) are released into the vapor phase. When these vapors cool, they condense to form the fine fraction of the ash, 15 whereas char burnout and fragmentation generally give rise to the coarse fraction of the ash due to coalescence of the nonvolatile components contained within the fuel matrix (included minerals).…”
Section: ■ Introductionmentioning
confidence: 99%
“…Consequently, the transition from porous char to molten slag at 1400 and 1500 °C is responsible for the sharp decrease in the surface area at around 90% conversion observed in Figure 26. Wu et al (1999Wu et al ( , 2000 concluded that fragmentation plays a key role in the formation of large amounts of fine ash particles in the early and middle stage of pulverized coal combustion, while coalescence of included minerals results in the formation of coarse ash in the later stage of combustion, depending on the structure of the char. Baxter (1992) found that the fragmentation of bituminous coal char is strongly dependent on the size of the particle.…”
Section: Sem Imagesmentioning
confidence: 99%
“…For a lower vitrinite content of 50 percent, again at 25 atmospheres, 75 percent of the particles are predicted to be present as cenospheres. The increase in cenosphere content with increasing pressure increases the char fragmentation during gasification with an attendant increase on char reaction rates 22 and a decrease in the particle size of ash produced (Wu et al, 2000). 18 The microporosity and therefore total surface area of the char is also impacted by the increase in total pressure.…”
Section: Char Morphologymentioning
confidence: 99%
“…The increase in cenosphere content with increasing pressure increases the char fragmentation during gasification with an attendant increase on char reaction rates 22 and a decrease in the particle size of ash produced (Wu et al, 2000). 18 The microporosity and therefore total surface area of the char is also impacted by the increase in total pressure. These changes in surface area and porosity will also influence the high pressure reactivity of the chars.…”
Section: Char Morphologymentioning
confidence: 99%