2015
DOI: 10.1016/j.fuproc.2014.12.005
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An experimental investigation on the drying kinetics of a single coarse particle of Belchatow lignite in an atmospheric superheated steam condition

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Cited by 45 publications
(50 citation statements)
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“…Pores, in which water is kept in the sample, become vacant after the water removal and they are crushed due to thermal stress mostly in the DDRP at which the sample's surface and core temperatures start increasing from the saturation temperature to the test temperature. This behavior was previously shown [18]. The water transported from the inside sample to the shell at the CDRP might occur not as vapor, but in the form of liquid.…”
Section: Methodssupporting
confidence: 71%
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“…Pores, in which water is kept in the sample, become vacant after the water removal and they are crushed due to thermal stress mostly in the DDRP at which the sample's surface and core temperatures start increasing from the saturation temperature to the test temperature. This behavior was previously shown [18]. The water transported from the inside sample to the shell at the CDRP might occur not as vapor, but in the form of liquid.…”
Section: Methodssupporting
confidence: 71%
“…The drying rate curve plot, at each test temperature of 110, 130, 150 and 170 °C, is also summarized in Figure 10. The clearly visible influence of the particle size and superheated steam temperature was explained in previous work [18], but the additional variety from individual properties of coal is observed. Because of the diversification of the petrographic lithotype texture, it is very difficult to determine the representative characteristics of drying behavior for each case.…”
Section: Methodsmentioning
confidence: 49%
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