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The temperature-dependent release of volatile inorganic species from Victorian brown coals and German lignites under CO2 and H2O gasification conditions

机译:在CO2和H2O气化条件下维多利亚褐煤和德国褐煤中挥发性无机物的温度依赖性释放

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To promote the use of abundant low rank coal resources, and to assist with the design, development and optimisation of hot gas cleaning and downstream processes, it is necessary to understand the release mechanisms of volatile inorganic species from low rank coals under high temperature gasification conditions. Although a significant amount of work has been reported under combustion and oxygen lean gasification conditions, these studies do not sufficiently explain the role of the gasification reagents CO2 and H2O in the mechanisms. Therefore, gasification experiments under 20% CO2 and 20% H2O in He were conducted at 1100 degrees C, 1200 degrees C and 1400 degrees C for two Victorian brown coals and four Rhenish lignites. Hot gas analysis was conducted by online molecular beam mass spectrometry to determine the intensity, relative quantity and timing of the release of volatile species of interest. Two overlapping phases were clearly observed from the results - devolatilisation and char gasification. Major species detected were Na-23(+), (H2S+)-H-34, Cl-35(+), (HCl+)-H-36, K-39(+)/(NaO+)-Na-39, (NaCl+)-Na-58, (COS+)-C-60/(NaCl+)-Na-60, and (SO2+)-S-64. The release during devolatilisation was essentially independent of the bulk gas atmosphere and constituted the majority of Na and Cl species. The release of S-species occurred predominantly during gasification under both CO2 and H2O atmospheres by similar but distinct mechanisms, and was directly affected by the absence, presence and concentration of the gasification reagents. (C) 2015 Elsevier Ltd. All rights reserved.
机译:为了促进利用丰富的低阶煤资源,并协助热气净化及下游工艺的设计,开发和优化,有必要了解高温气化条件下低阶煤中挥发性无机物的释放机理。 。尽管据报道在燃烧和贫氧气化条件下进行了大量工作,但这些研究不足以解释气化剂CO2和H2O在机理中的作用。因此,针对两种维多利亚时代的褐煤和四种莱茵石褐煤,分别在1100℃,1200℃和1400℃的He中20%CO2和20%H2O下进行气化实验。通过在线分子束质谱仪进行热气分析,以确定目标挥发性物质释放的强度,相对数量和时间。从结果清楚地观察到两个重叠的阶段-脱挥发分和炭化。检测到的主要物种为Na-23(+),(H2S +)-H-34,Cl-35(+),(HCl +)-H-36,K-39(+)/(NaO +)-Na-39,( NaCl +)-Na-58,(COS +)-C-60 /(NaCl +)-Na-60和(SO2 +)-S-64。脱挥发分过程中的释放基本上不依赖于整体气体气氛,并构成了大部分Na和Cl物种。 S物种的释放主要发生在CO2和H2O气氛下的气化过程中,其机制相似但又截然不同,并且直接受到气化剂的不存在,存在和浓度的影响。 (C)2015 Elsevier Ltd.保留所有权利。

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