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Chemical structural transformations of different coal components at the similar coal rank by HRTEM in situ heating

机译:HRTEM原位加热相似煤阶煤成分的化学结构转变。

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摘要

The structural transformations in three coal components, barkinite, vitrinite and resinite, on heat-treatment from 200 to 700 degrees C were investigated by high-resolution transmission electron microscopy (HRTEM) technique. The orientation in chemical structure was examined by HRTEM image. The orientation in aromatic layers of three coal components increased gradually on heating from 200 degrees C to 700 degrees C. Vitrinite followed barkinite's transition some 50 degrees C later in temperatures of chemical structural change than barkinite. The transformations of structural parameters derived from TEM images of three coal components were different, including the interlayer spacing (d), the layer size (La), the number of aromatic layers per stack (n), and the aromatic layer stacking height (Lc). At least three temperature stages (200-400, 400-600, and 600-700 degrees C) were shown. Barkinite has similar change trends of d, Lc, and n with resinite however the La values were similar to vitrinite at 200-700 degrees C. Both barkinite and resinite had significant decreased d values at 200-400 degrees C and gradual decreased from 400 degrees C to 600 degrees C. The values of Lc and n for barkinite and resinite exhibit no obvious changes at 200-400 degrees C and increased significantly 450 degrees C. Vitrinite decrease significantly in d from 450 to 600 degrees C (4.32-3.62 angstrom) and increase greatly in Lc and d up to 450 degrees C (12.84-20.29 angstrom). Vitrinite and barkinite have two temperature ranges for increasing significantly in La from 400 degrees C to 700 degrees C. When the temperature is 600 degrees C, these coal components had much larger Lc, n, and La values with temperature increasing and decreased gradually in d values. The variation of structural parameters when heating was explained by the alteration of chemical structures in coal on pyrolysis and plastic behavior.
机译:通过高分辨率透射电子显微镜(HRTEM)技术研究了三种煤组分,重晶石,镜质石和树脂岩在200至700摄氏度的热处理条件下的结构转变。通过HRTEM图像检查化学结构的取向。从200摄氏度加热到700摄氏度,三种煤成分在芳族层中的取向逐渐增加。玻璃素体在化学结构变化的温度之后跟随着重晶石转变约50摄氏度,比重晶石更晚。从三种煤组分的TEM图像得出的结构参数的转换是不同的,包括层间间距(d),层大小(La),每堆芳烃层数(n)和芳烃层堆积高度(Lc) )。显示了至少三个温度阶段(200-400、400-600和600-700摄氏度)。重晶石的d,Lc和n与树脂岩的变化趋势相似,但是La值在200-700摄氏度时与镜质岩相似。重晶石和树脂岩在200-400摄氏度时d值显着降低,从400摄氏度逐渐降低C至600摄氏度。重晶石和树脂岩的Lc和n值在200-400摄氏度时无明显变化,并在> 450摄氏度时显着增加。玻璃体在d时从450至600摄氏度(4.32-3.62埃)显着下降。 ),直到450摄氏度(12.84-20.29埃)时Lc和d都大大增加。玻璃铁矿和轻晶石具有两个温度范围,使La从400摄氏度显着升高到700摄氏度。当温度> 600摄氏度时,这些煤组分的Lc,n和La值随温度的升高和逐渐降低而大得多。 d值。加热时结构参数的变化可以通过煤在热解和塑性行为方面化学结构的变化来解释。

著录项

  • 来源
    《Fuel》 |2018年第15期|140-147|共8页
  • 作者单位

    China Univ Min & Technol Beijing, Coll Geoscience & Surveying Engn, D11,Xueyuan Rd, Beijing 100083, Peoples R China;

    China Univ Min & Technol Beijing, Coll Geoscience & Surveying Engn, D11,Xueyuan Rd, Beijing 100083, Peoples R China;

    China Univ Min & Technol Beijing, Coll Geoscience & Surveying Engn, D11,Xueyuan Rd, Beijing 100083, Peoples R China;

    China Univ Min & Technol Beijing, Coll Geoscience & Surveying Engn, D11,Xueyuan Rd, Beijing 100083, Peoples R China;

    China Univ Min & Technol Beijing, Coll Geoscience & Surveying Engn, D11,Xueyuan Rd, Beijing 100083, Peoples R China;

  • 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

    Vitrinite; Barkinite; HRTEM; Structure; Heating; Image-analysis;

    机译:玻璃体;重晶石;HRTEM;结构;加热;图像分析;

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