菱镁矿
煅烧
甲烷
一氧化碳
催化作用
无机化学
镁
化学
二氧化碳
氢
二氧化碳电化学还原
碳纤维
氧化物
材料科学
有机化学
复合数
复合材料
作者
Georg Baldauf‐Sommerbauer,Susanne Lux,Wolfgang Aniser,Matthäus Siebenhofer
标识
DOI:10.1002/ceat.201600094
摘要
Abstract The conversion of mineral magnesite to magnesium oxide, methane, carbon dioxide, and carbon monoxide in a hydrogen atmosphere at ambient pressure and overpressure without catalysts is discussed. Low temperature and elevated pressure facilitate CH 4 formation whereas moderate to high temperature and low pressure facilitate CO formation. Methane is formed directly without any additional catalyst. CO 2 emissions are decreased substantially in reductive calcination. Additional experiments revealed that reductively calcined magnesium oxide is a highly active reverse water‐gas shift catalyst. CO formation from gaseous CO 2 and H 2 at catalytically active magnesium oxide was reproducibly confirmed. Further reduction of carbon monoxide to methane is not catalyzed by reductively calcined magnesium oxide.
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