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TEM CHARACTERISATION AND RAMAN SPECTROSCOPY OF VITRINITE

机译:白云母的TEM表征和拉曼光谱

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Despite of environmental concerns, coal is still a significant natural energy resource and is widely used for electricity generation and steel making, as well as for unconventional methane production (coal bed methane; CBM). Coal seams are furthermore evaluated for their carbon (CO_2) storage properties. Physicochemical and mechanical properties of coals still need to be investigated for the evaluation of long-term storage effects [1]. Coal properties are controlled by the individual distribution of its constituents, called macerals, which are divided into the main groups vitrinite, intertinite, and liptinite. According to previous studies, sorption capacity, structure and physical properties of vitrinite are more sensitive to experimental treatment with CO_2 compared to inertinite [1, 2]. Since vitrinite also seems to show a complex relationship of micromechanical properties [3] with increasing coal rank (maturity) and is usually the most abundant maceral in coal seams, our research focuses on this maceral group. Well investigated coal samples from the Ukrainian Donets Basin [4, 5], covering a maturity range from 0.62 to 1.47 %Rr (vitrinite reflectance), were selected for this study. The aim is to investigate nanopores and sub-micrometre scale mineral inclusions in organic matter via transmission electron microscopy (TEM), as these features likely have a significant impact on the material properties. Furthermore, high-resolution transmission electron microscopy (HRTEM) is employed in order to study aromatic structural features and stacking. As a complimentary characterisation method μ-Raman spectroscopy is conducted to further refine the maturity assessment and characterise changes in the aromatic vitrinite structure based on the G (graphitic) and D (disordered) bands [6]. To ensure correlation between the individual experimental techniques, vitrinite is identified based on optical microscopy under white reflected light from polished sections with randomly oriented coal fragments. Material for a single sample is obtained by careful drilling and milling out of vitrinite grains. The vitrinite powder is further diluted in isopropanol, dispersed by ultrasonification and finally dropped on a lacey carbon film for TEM investigation. Raman spectroscopy is performed on untreated specimen surfaces (Fig. 1). For a comprehensive understanding, CO_2 adsorption measurements will be conducted. This complementary approach yields valuable insights into the microstructural evolution of vitrinite with increasing maturity, as well as on micromechanics, adsorption capacity and physicochemical properties.
机译:尽管存在环境问题,但煤炭仍然是重要的自然能源,被广泛用于发电和炼钢以及非常规甲烷生产(煤层气; CBM)。此外,还评估了煤层的碳(CO_2)存储特性。评估煤的长期储藏效果还需要研究煤的理化和力学性能[1]。煤的性质受其组成的单独分布(称为“一般”)的控制,这些分布分为镜质石,互变石和锂质变石这三大类。根据以前的研究,与惰质岩相比,镜质岩的吸附能力,结构和物理性质对用CO_2进行的实验处理更为敏感[1,2]。由于镜质体似乎也显示出微机械性质与煤等级(成熟度)的增加之间的复杂关系,并且通常是煤层中最丰富的矿物,因此我们的研究集中在该矿物组上。本研究选择了来自乌克兰顿涅茨盆地[4,5]的经过充分调查的煤炭样本,其成熟度范围为0.62至1.47%Rr(镜质体反射率)。目的是通过透射电子显微镜(TEM)研究有机物质中的纳米孔和亚微米级的矿物包裹体,因为这些特征可能会对材料性能产生重大影响。此外,为了研究芳族结构特征和堆积,采用了高分辨率透射电子显微镜(HRTEM)。作为补充的表征方法,进行了拉曼光谱分析,以进一步完善成熟度评估,并基于G(石墨)带和D(无序)带表征芳族镜质体结构的变化[6]。为了确保各个实验技术之间的相关性,基于光学显微镜,在来自具有随机取向的煤碎片的抛光部分的白色反射光下,鉴定了镜质体。通过仔细钻出并研磨出镜质颗粒,可以获得单个样品的材料。将该镜质粉进一步用异丙醇稀释,通过超声处理分散,最后滴在一块花边碳膜上进行TEM研究。拉曼光谱是在未经处理的样品表面上进行的(图1)。为了全面理解,将进行CO_2吸附测量。这种互补的方法对随着增加的成熟度的镜质石的微观结构演变以及微力学,吸附能力和理化性质产生了有价值的见解。

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