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The Evolution of Pyritic and Organic Sulfur from Pulverized Coal Particles during Combustion

机译:燃烧过程中粉煤颗粒中粉煤颗粒的耐热与有机硫的演变

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A detailed evaluation of the evolution of sulfur forms during the combustion of three pulverized coals illustrates that a more careful consideration of the behavior of included sulfur is necessary. Although this sample set is quite limited, the following approaches to the development of an initial model for the evolution of included pyritic and organic sulfur appear warranted for these specific coals: · The thermal decomposition of pyritic sulfur is coal specific and, under the reducing conditions within a coal particle, the amount of sulfur released has been observed to exceed that which would result from decomposition of pyrite to troilite (Fe{sub}1.0S). A predictive correlation will require a broader range of coals and further study. · Pyrolysis of organic sulfur appears to be similar to that of the remaining organic structure. · During char oxidation, total sulfur evolves at a rate similar to that of the remaining organic structure.
机译:在三个粉碎煤的燃烧期间对硫形式的演化的详细评估说明需要更仔细地考虑所包括的硫的行为。虽然该样品集非常有限,但对于这些特异性煤的概念出现以下对初始模型的开发方法的初始模型:·硫酸硫的热分解是煤特异性的,并且在还原条件下在煤颗粒内,已经观察到释放的硫的量超过将黄铁矿分解成毒液(Fe {Sub} 1.0s)。预测相关性需要更广泛的煤和进一步研究。 ·有机硫的热解似乎类似于剩余的有机结构的热解。 ·在氧化氧化过程中,总硫以类似于剩余有机结构的速率演变。

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