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Influence of discard mineral matter on slag-liquid formation and ash melting properties of coal - A FACTSAGE™ simulation study

机译:废弃矿物质对煤渣液形成和灰分熔融特性的影响-FACTSAGE™模拟研究

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摘要

The ash fusion temperature (AFT) profile of a coal is one of the parameters currently widely used in coal marketing and utilization to assess coal ash fusibility and melting characteristics, and to predict the melting behaviour of the coal ash in coal conversion processes. However, the flow temperature of a specific coal source alone does not provide enough insight into the slag formation behaviour at temperatures below the flow temperature. It has been demonstrated that ash flow temperature can be correlated with FACT™ equilibrium calculations, and that such equilibrium calculations provide useful information regarding the phase transitions that take place well below the final ash flow temperature as indicated by a standard AFT analysis. The overall objective of this study is to use the properties of different types of mineral matter and to simulate the effect on slag-liquid formation and ash flow temperature for individual mineral types as well as blends. A thermo-equilibrium simulation approach based on FACTSAGE™ was applied. The slag-liquid flow temperature simulations for coal and individual mineral types compared favourably with the actual measured ash flow temperature and are within the experimental error of an AFT analysis (±30 ℃). The slag formation of coal showed a more gradual increase in the amount of slag formed over a temperature compared to specific individual mineral types. This can be explained by the ash composition of coal which has a more even distribution of minerals compared to mineral types that have a significantly high SiO_2 or CaO content respectively. From this result it is also confirmed that flow temperature properties are non-additive and cannot be calculated from a weighted average principle. It was shown by FACTSAGE™ modelling that the addition of a discard blend to this specific coal source will have no significant effect on the flow temperature of the blend. The FACTSAGE™ modelling showed that the amount of slag-liquid of the ash that was studied is highly dependent on the temperature to which the ash is exposed. For example, the amount of slag-liquid can double by only increasing the operating temperature of a process within a small window of as little as 100 ℃ This could explain why coal conversion processes such as combustion, and entrained flow gasification, can experience periods of unstable operation despite an apparent constant feed coal quality being observed with very little variation in ash flow temperature. The important parameter is thus not the actual flow temperature, but rather the amount of slag formation at a specific operating temperature. The inability of the standard AFT analysis to reflect changes in ash melting behaviour with relatively small variations in ash composition was highlighted in this study. Even though variation in mineral matter content of the coal blend may have limited or no effect on the actual ash flow temperature, it can significantly change the amount of slag present in the ash bed. The variation in operating temperature can also result in a significant change in slag formation (positive or negative) which is not always reflected by the standard AFT analysis method. It is concluded that FACTSAGE™ thermodynamic modelling of ash melting behaviour provides a method to address the shortcomings of the standard AFT determination, which can add significant value and insight towards the improvement of the operational stability of coal conversion processes such as combustion and gasification.
机译:煤的灰分熔融温度(AFT)曲线是当前在煤炭销售和利用中广泛使用的参数之一,用于评估煤灰的易熔性和熔化特性,并预测煤灰在煤转化过程中的熔化行为。但是,仅特定煤源的流动温度不足以提供低于流动温度的炉渣形成行为的足够信息。已经证明,粉尘流温度可以与FACT™平衡计算相关联,并且这种平衡计算提供了有关发生在远远低于标准AFT分析所示的最终粉尘流温度的相变的有用信息。这项研究的总体目标是利用不同类型矿物质的特性,并模拟单个矿物质类型及其混合物对渣液形成和灰分流温度的影响。应用了基于FACTSAGE™的热平衡模拟方法。煤和各种矿物类型的矿渣-液体流动温度模拟与实际测得的灰分流动温度相比具有优势,并且在AFT分析的实验误差范围内(±30℃)。与特定的单个矿物类型相比,煤的炉渣形成在一定温度范围内形成的炉渣数量更加逐渐增加。这可以通过煤的灰分成分来解释,与分别具有显着高的SiO_2或CaO含量的矿物质类型相比,煤的矿物质分布更加均匀。从该结果还证实,流动温度特性是非加性的,并且不能根据加权平均原理来计算。 FACTSAGE™模型表明,向该特定煤源中添加废料混合物不会对混合物的流动温度产生重大影响。 FACTSAGE™模型表明,所研究的粉煤灰的渣液量在很大程度上取决于粉煤灰的暴露温度。例如,仅在低至100℃的小窗口内提高过程的操作温度,渣液的量就可以增加一倍。这可以解释为什么煤转化过程(例如燃烧和气流床气化)会经历尽管观察到了稳定的进料煤质量,但灰分流温度几乎没有变化,但运行仍不稳定。因此,重要的参数不是实际的流动温度,而是特定工作温度下的炉渣形成量。这项研究强调了标准AFT分析无法反映灰分组成相对较小变化的灰分熔融行为变化。即使煤掺混物中矿物质含量的变化可能对实际的灰分流温度产生有限的影响或没有影响,但它仍会显着改变灰分床中存在的炉渣量。工作温度的变化还会导致炉渣形成的显着变化(正或负),而标准AFT分析方法并不总是能反映出这种变化。结论是,FACTSAGE™灰烬熔融行为的热力学模型提供了一种解决标准AFT测定方法缺点的方法,该方法可以为改善煤转化工艺(如燃烧和气化)的操作稳定性提供重要的价值和见识。

著录项

  • 来源
    《Fuel 》 |2014年第1期| 834-840| 共7页
  • 作者

    J.C. van Dyk; M.J. Keyser;

  • 作者单位

    Sasol Technology R&D, Klasie Havenga Street 1, Sasolburg 1947, South Africa;

    Sasol Technology R&D, Klasie Havenga Street 1, Sasolburg 1947, South Africa;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Gasification; FACTSAGE™; Mineral matter and coal;

    机译:气化;FACTSAGE™;矿物质和煤炭;

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