CO2气氛对煤热解过程中硫逸出的影响

Effect of CO2 atmosphere on sulfur release during coal pyrolysis

  • 摘要: 采用热解-质谱(Py-MS)与热解-气相色谱(Py-GC)相结合的方法对平朔(PS)和义马(YM)原煤、脱灰煤及其脱黄铁矿煤进行了热解实验,考察了CO2气氛对煤热解过程中硫逸出行为的影响。并采用质谱在线分析H2S、COS和SO2的逸出曲线,利用气相色谱分析H2S、COS和SO2在气相中的逸出量。结果表明,CO2气氛有利于H2S、COS和SO2进入气相,且逸出量增加,而COS增加幅度更大。同时,CO2气氛有利于H2S和SO2最大逸出峰温提前。另外,CO2气氛对原煤的H2S、COS和SO2逸出温度影响较大,但对脱灰煤的影响较小。在较高的温度下,CO2有利于煤中稳定有机硫的分解。这进一步验证了在较高温度下COS形成与CO相关,而在较低温度下与CO无关。

     

    Abstract: Yima (YM) coal and Pingshuo (PS) coal as well as their deashed coals and depyrited coals were used to investigate the effects of CO2 and Ar on the sulfur release behavior during coal pyrolysis by pyrolysis connected with mass spectrometer (Py-MS) and pyrolysis connected with gas chromatogram (Py-GC). It is found that CO2 atmosphere can promote the release of H2S, COS and SO2, especially the remarkable releasing of COS. In addition, CO2 atmosphere can decrease the maximum release peak temperature of H2S, COS and SO2 for raw coals, while there is no obvious effect for their deashed coals. At the same time, CO2 is beneficial to the decomposition of organic sulfur at higher temperature. That the COS formation is related to CO at higher temperatures and has nothing to do with CO at lower temperatures is validated.

     

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