石炭科学会議発表論文集
Online ISSN : 2423-8309
Print ISSN : 2423-8295
ISSN-L : 2423-8295
第40回石炭科学会議
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61.石炭の昇温熱分解時における塩素の行方
坪内 直人王 延輝大塚 康夫
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p. 124-125

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Pyrolysis of seven coals with different ranks has been carried out in a temperature-programmed mode at 10℃/min with a fixed bed quartz reactor. HCl is the predominant product among Cl-containing species observed at 800℃, followed by char-Cl and tar-Cl. The peak temperatures of HCl formation are classified roughly into 280-360, 470-510 and 580℃. It appears likely that HCl reacts with a brown coal char at 500℃ to form Cl-containing compounds, which are converted to HCl upon reheating. The HCl peak at 580℃ appears for all of the coals examined, and the yield decreases with increasing calcium content in coal.

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© 2003 一般社団法人 日本エネルギー学会
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