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加压流化床气化条件下灰熔融特性的实验研究
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摘要
炭在我国一次能源的生产和消费结构中一直占主导地位,随着能源消费的持续增长,环境问题的逐渐显现,炭的清洁利用越来越受人们的关注。炭气化是发展炭洁净转化的主要技术之一,其中压力流化床炭气化以其种适应性强,污染物排放低等特点成为炭气化技术的一个重要发展方向。
     灰熔融特性是动力用和气化用的一项重要的质量指标,直接决定着炭燃烧气化过程排渣方式的选择,是影响炭燃烧和气化运行的一个重要因素。本课题拟针对压力下灰的熔融特性和烧结特性开展一系列实验和理论研究,希望为炭气化系统设计和运行提供一定的帮助。
     首先,归纳分析了不同气氛下灰碱金属化合物对灰熔融特性的影响实验结果,发现不同气氛、不同灰化学成分对灰的熔融性的影响不同,灰熔融温度不仅与Fe_2O_3和CaO总含量有关,而且与其CaO/Fe_2O_3摩尔比也有关。
     其次,利用压力热天平分析仪和X射线衍射分析仪,对不同压力、不同气氛灰矿物质的转变情况进行实验研究,研究表明压力会影响灰矿物质化学反应平衡,压力抑制方解石、硫酸钙和钾云母的分解,促进石英的相变,以及莫来石、钙长石和铁尖晶石等矿物质的生成,对灰熔融特性影响复杂。
     然后,利用搭建的压差法实验台,对课题目标进行了烧结特性的实验研究,分析了主要灰化学成分对灰烧结特性的影响规律,以及气氛条件对灰烧结特性的影响规律,结果显示,灰中的CaO、Na_2O成分降低了灰烧结温度,与氧化性气氛相比,还原性气氛降低了灰烧结温度,其降低程度与灰中Fe_2O_3含量有关。
     最后,利用热力学计算软件对不同压力、不同气氛下灰矿物质反应过程进行模拟计算,分析了各种工况下,灰各矿物质生成情况,从理论上对各种气化条件下灰矿物质反应情况进行研究。计算表明,随着加热过程的进行,灰逐渐由低温矿物质转变为高温矿物质;压力条件能够抑制硫酸钙的分解反应,促进莫来石、钙长石和堇青石的生成以及石英的相变;还原性气氛主要通过和灰中的含铁化合物反应来改变灰的矿物质组分,进而影响灰的熔融特性。
Coal is the dominant energy in the energy production and consumption structure of our country. With continued growth in energy consumption, environmental issues appear gradually, and the clean use of coal is concerned by increasing people. Coal gasification is the development of clean coal technologies, and pressurized fluidized bed coal gasification with its coal adaptability, and low emissions is to be an important development direction.
     The fusibility of coal ash is an important characteristic in pulverized coal combustion and coal gasification, which determines how to utilize coal resources in coal combustion or gasification. But there are some operation problems such as bed fusion, bed agglomeration and deposition in fluidized gasification technology, the paper mainly did experimental and theoretical research on coal ash fusibility which is important to solving these problems.
     Firstly, analyzed the influences of coal ash characteristics and atmosphere on coal ash fusibility, the results shows the fusion temperature is not only concerned with the sum of CaO and Fe_2O_3, but also with the ratio of CaO and Fe_2O_3;
     Secondly, experiments on the pressure thermal-balance apparatus and XRD, analyzed the influences of pressure and atmosphere on the mineral transformation in the coal. The results shows that the pressure will influence the balance of ash mineral chemical reactions suppress calcite, sulfuric acid Calcium and potassium mica decomposition and promote the transformation of quartz and mullite, calcium and iron spinel. The impact of pressure on the fusibility of coal ashes is complex.
     Then, analyzed the sintering temperature of coal ashes which is adding additives alter the proportion of alkaline oxides under different atmospheres. The results show the sintering temperature under coal gasification condition is lower than that under oxidizing atmosphere. And with the increase of Fe_2O_3, CaO, Na_2O content, the sintering temperature decreases.
     At last, we used the calculation software-FACTSage to simulate the influences of pressure and atmosphere on the mineral transformation in the coal ashes. Calculation shows that, with the heating process, the low-temperature minerals gradually transformed into high-temperature minerals; pressure suppress calcium sulfate decomposition and promote the transformation of mullite, anorthite, and cordierite. Reducing atmosphere, mainly through reacting with iron compounds, change the ash mineral components, thereby affecting the fusibility of coal ashes.
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