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Modeling of sulfur retention by limestone in coal briquette

机译:煤饼中石灰石固硫的模型

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摘要

A detailed simulation model was developed for sulfur retention by limestone in a coal briquette. Four submodels, i.e., coal briquette combustion, volatile and sulfur evolution, H_2S retention, and SO_2 retention, were included in the simulation. In the model, the coal briquette combustion was divided into two successive stages: volatile ignition and char burnout. The temperature profile and its time variation, sulfur release and retention behavior within the burning coal briquette for the two stages were simulated separately. In the stage of volatile evolution and ignition, a part of coal sulfur is released as H_2S, and reacted with the calcined limestone in the area near the particle surface, where the local temperature is increased along with the volatile ignition, and the limestone in the coal briquette is partially calcined. H_2S retention in the coal briquette was thus simulated as a result of the competition among its transportation by the bulk flow of evolved volatile, its molecular diffusion due to the concentration gradient within the coal briquette, and its capture by the calcined limestone. In the stage of char burnout, the remaining part of coal sulfur is released as SO_2 with char burning which is simulated by the shrinking core model. SO_2 release rate is assumed to be proportional to the char burning rate and controlled by oxygen diffusion in the ash layer. The sulfate formation occurs in the ash layer within which oxygen exists. SO_2 retention was thus simulated as a result of the competition among the sulfate formation with the calcined limestone, SO_2 diffusion in the ash layer and its emission from the briquette surface. The sulfur retention by limestone in a spherical centimeter sized coal briquette was simulated by the model. The effects of heating rate, briquette size, calcium to sulfur ratio (Ca/S), and volatile matter of coal on the sulfur retention were predicted. The simulation results showed that rapid heating condition was good for both the H_2S retention in the volatile and the SO_2 retention in the combustion gas. The simulation also predicted a higher SO_2 retention for a larger sized coal briquette. The coals of higher rank and lower organic sulfur contents also showed a higher sulfur retention.
机译:建立了一个详细的模拟模型,用于煤饼中石灰石的固硫作用。模拟中包括了四个子模型,即煤块燃烧,挥发物和硫释放,H_2S保留和SO_2保留。在该模型中,煤饼燃烧分为两个连续的阶段:挥发性点火和炭烧尽。分别模拟了两个阶段的温度曲线及其时间变化,燃煤团块内的硫释放和保留行为。在挥发释放和着火阶段,一部分煤硫以H_2S的形式释放出来,并与煅烧的石灰石在颗粒表面附近区域发生反应,随着挥发的着火,局部温度随之升高,而在燃烧过程中,石灰石在煤中燃烧。煤饼已部分煅烧。因此,模拟了H_2S在煤球中的保留,这是由于其在挥发挥发物的大量流动中的运输,由于煤球中浓度梯度引起的分子扩散以及被煅烧石灰石捕获之间的竞争所致。在焦炭烧尽阶段,煤硫的剩余部分以焦炭燃烧形式以SO_2的形式释放,这是通过收缩核模型进行模拟的。假设SO_2的释放速率与炭燃烧速率成正比,并受灰层中氧的扩散控制。硫酸盐的形成发生在存在氧气的灰层中。因此,模拟了SO_2的保留,其原因是硫酸盐与煅烧石灰石形成之间的竞争,灰分中SO_2的扩散以及其从团块表面的排放。通过该模型模拟了石灰石在球形厘米大小的煤饼中的硫保留。预测了加热速率,团块尺寸,钙硫比(Ca / S)和煤的挥发性物质对硫保留的影响。模拟结果表明,快速加热条件对于挥发物中的H_2S保留和燃烧气体中的SO_2保留都是良好的。该模拟还预测,较大型煤饼的SO_2保留量更高。等级较高和有机硫含量较低的煤也表现出较高的硫保留率。

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