1999
DOI: 10.1021/ef980240o
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Effects of Heating Rate and Ion-Exchangeable Cations on the Pyrolysis Yields from a Victorian Brown Coal

Abstract: A Victorian low-rank coal (Loy Yang) was acid-washed and ion-exchanged with Na and Ca to prepare the H-form, Na-form, and Ca-form coal samples. Two more H-form samples were also prepared by rewashing the Na-form and Ca-form samples with acid. These coal samples were pyrolyzed in a wire-mesh reactor where the secondary reactions of the evolved volatiles were minimized. The ion-exchanged coal samples were found to give very different tar yields from those of the raw coal samples. While the tar yields from the py… Show more

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Cited by 184 publications
(111 citation statements)
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“…The sample preparation of two coals can be found elsewhere [14,30]. Briefly, "as mined" coal was dried 100 at low temperature (< 35 °C).…”
Section: Sample Preparationmentioning
confidence: 99%
See 1 more Smart Citation
“…The sample preparation of two coals can be found elsewhere [14,30]. Briefly, "as mined" coal was dried 100 at low temperature (< 35 °C).…”
Section: Sample Preparationmentioning
confidence: 99%
“…A wire-mesh reactor (WMR) that was frequently used in the investigation of primary pyrolysis [28][29][30][31] and gasification [32,33] can provide a wide range of heating rate from 0.1 to 5000 K s -1 and high time resolution (increment of 10 ms). It is very suitable for the production of nascent char with even milliseconds holding at a pre-set peak temperature.…”
mentioning
confidence: 99%
“…The O-Na+ group is difficult to decompose due to the strong electron adsorption [16]. Second, part of the Na may also have combined with the char matrix to form a stable cross-linked structure [42,43]. These two forms of Na attach on the char stably, but there is no enough energy to break the keys to evaporate Na in this experiment.…”
Section: Influence Of Temperature On the Occurrence Form Of The Alkalmentioning
confidence: 94%
“…4. Under our conditions, it is assumed that the coal sample has already been converted into tar, carbon gases, char, and soot by primary pyrolysis at the top non-isothermal zone of the DTR (at 500-900 °C) (Jamil et al, 2004;Sathe et al, 1999). The carbon conversion reactions in the isothermal zone of the DTR were simulated, and the feedstock was lumped into tar, carbon gases, char, and soot derived from the primary pyrolysis of the coal.…”
Section: Kinetic Modelmentioning
confidence: 99%