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首页> 外文期刊>Fuel Processing Technology >The mineralogy, morphology and sintering characteristics of ash deposits on a probe at different temperatures during combustion of blends of Zhundong lignite and a bituminous coal in a drop tube furnace
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The mineralogy, morphology and sintering characteristics of ash deposits on a probe at different temperatures during combustion of blends of Zhundong lignite and a bituminous coal in a drop tube furnace

机译:准东褐煤与烟煤在滴管炉中燃烧过程中,不同温度下探针上灰分的矿物学,形貌和烧结特性

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摘要

Ash deposits formed on an air-cooled probe at different temperatures during combustion of coal blends of a Zhundong lignite (ZL) and an Australian bituminous (AB) were studied in the present work. The blends with various AB ratios were combusted in a drop tube furnace in air at 1400 degrees C, and the ash deposits formed on the probe top surface maintained at 500 degrees C, 600 degrees C, 700 degrees C, and 750 degrees C, were collected and characterised using XRD and SEM-EDS for their mineralogy, morphology and elemental composition. The size distributions and sintering temperatures of the ash deposits were also determined. At the probe temperature of 500 degrees C, the ZL ash deposit was dominated by fluxing minerals where significant amounts of fine particles (<10 mu m) and their aggregates existed, leading to low ash sintering temperatures. As the AB ratio increased to 20 wt% and above, the amount of the fluxing minerals in the deposits decreased while the amount of refractory quartz and mullite minerals increased. Morphologically, the refractory ash particles from AB coal diluted the Na-bearing mineral phases and the contacts between fine ash particles, leading to the absence of nepheline and, correspondingly, an increase in the ash sintering temperature. In addition, as the probe temperature increased, mineral interactions and ash sintering were facilitated when the AB ratio was less than 20 wt%, leading to the formation of new mineral phases and an increase in ash particle sizes. However, no significant mineralogical and morphological changes were observed when the AB ratio was higher than 40 wft, indicating that these ash deposits were more refractory and resistant to the temperature change. (C) 2016 Elsevier B.V. All rights reserved.
机译:在本工作中,研究了准东褐煤(ZL)和澳大利亚沥青(AB)的煤共混物燃烧期间在不同温度下在风冷探头上形成的灰烬沉积物。将具有各种AB比的共混物在滴管炉中于1400摄氏度的空气中燃烧,并在探头顶面上形成的灰分沉积保持在500摄氏度,600摄氏度,700摄氏度和750摄氏度。使用XRD和SEM-EDS收集并表征其矿物学,形态和元素组成。还确定了灰渣沉积物的尺寸分布和烧结温度。在探针温度为500摄氏度时,ZL灰分沉积物以助熔矿物为主,其中存在大量的细颗粒(<10微米)及其聚集体,导致灰分烧结温度低。随着AB比率增加到20wt%或更高,沉积物中助熔矿物的量减少,而耐火石英和莫来石矿物的量增加。从形态上讲,来自AB煤的耐火灰颗粒稀释了含Na的矿物相和细灰颗粒之间的接触,从而导致了霞石的缺失,并相应地提高了灰烧结温度。另外,随着探针温度的升高,当AB比小于20wt%时,促进了矿物相互作用和灰分烧结,导致形成新的矿物相并增加了灰分粒径。然而,当AB比高于40wft时,没有观察到明显的矿物学和形态学变化,表明这些灰烬沉积物更耐火并且对温度变化具有抵抗力。 (C)2016 Elsevier B.V.保留所有权利。

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