| Project/Area Number |
23656506
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| Research Category |
Grant-in-Aid for Challenging Exploratory Research
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| Allocation Type | Multi-year Fund |
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| Research Field |
Catalyst/Resource chemical process
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| Research Institution | Hokkaido University |
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Principal Investigator |
TSUBOUCHI Naoto 北海道大学, 大学院・工学研究院, 准教授 (90333898)
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| Project Period (FY) |
2011 – 2012
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| Project Status |
Completed (Fiscal Year 2012)
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| Budget Amount *help |
¥3,900,000 (Direct Cost: ¥3,000,000、Indirect Cost: ¥900,000)
Fiscal Year 2012: ¥1,040,000 (Direct Cost: ¥800,000、Indirect Cost: ¥240,000)
Fiscal Year 2011: ¥2,860,000 (Direct Cost: ¥2,200,000、Indirect Cost: ¥660,000)
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| Keywords | 石炭 / 乾留 / 軟化溶融 / コークス / ヘテロ元素 / 含窒素化合物 / 含硫黄化合物 / ギーセラー流動度 / アンモニア / シアン化水素 / 硫化水素 / ヘテロ化合物 |
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| Research Abstract |
The evolution of HCN, NH3 and H2S during carbonization of seven caking coals has been studied mainly with a flow-type fixed bed quartz reactor to examine the influences of nitrogen and sulfur on coal fluidity. The formation of HCN or NH3 from the coals starts at about 400〓C, and each rate profile observed provides the main and shoulder peaks around 450 and 670〓C, respectively. On the other hand, H2S evolution takes place mainly around 450 and550〓C. Each coal used also shows a maximum value in fluidity (MF) around 450〓C. There is an almost linear correlationbetween the MF value and total amount of HCN, NH3 or H2S released up to 450〓C. The addition of a commercial indole to an Australian bituminous coal can enhance the MF value at largest by a factor of about 1.3.
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