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Combined Methods of Thermal Analysis for Characterization of Rocks Containing Hydrocarbon

机译:含烃岩石岩体表征的热分析的综合方法

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Combined methods of thermal analysis TG/DTA/MS and TG/DSC in conjunction with Thermomechanical Analyzer (TMA) were used for characterization of thermal properties of hydrocarbon bearing shales. Results were obtained on three different samples: oil shale, high carbonate content shale, and a shale bearing natural gas. The analysis was performed in temperature range RT-950°C under helium atmosphere with heating rate 10°C/min. All samples were crushed but not powdered, and a weight of 100 mg was used. Combined TG/DTA/MS indicates that each sample shows three transitions: 1. A minimal mass loss between 100°C-300°C and during this period water (masses 18 and 17 used as water signatures) is being detected by the mass spectrometer. 2. The second mass loss is attributed to the decomposition of organic material between the temperatures of 350°C-500°C, and the mass spectrometer shows a hydrocarbon fragmentation trend with the dominant evolving ions with masses 41, 43, 55, 57, and 71. There is a small endothermic reaction that occurs during this decomposition. 3. At ~650°C the calcium carbonate begins to decompose, and lasts until ~900°C. The evolving gas measured during this period is carbon dioxide. Combined TG/DSC registered an endothermic reaction occurring during organic/kerogen decomposition and calcium carbonate decomposition. The carbonate rich sample shows similar trends but with a more prominent dehydration event occurring at ~110°C-140°C, the hydrocarbon within the sample shows a similar fragmentation trend but it accounted for only 4% in weight of the sample. The carbonate rich sample has a greater carbonate decomposition of ~22% (which equivocates to 50% of the rock being calcium carbonate). The information on physicochemical transitions of sample materials were correlated to dimensional changes measured by dilatometry (TMA) results and proved useful in understanding the nature of expansion and contraction of the shale with changing temperature.
机译:热分析TG / DTA / MS和TG / DSC结合热机械分析仪(TMA)的组合方法用于表征碳氢化合物轴承HALES的热性能。结果是在三种不同的样品上获得:油页岩,高碳含量页岩和轴承天然气。该分析在温度范围RT-950℃下在氦气气氛下进行,加热速率为10℃/ min。将所有样品粉碎但不粉末,使用重量为100mg。组合的TG / DTA / MS表示每个样品显示三个过渡:1。通过质谱仪检测到100°C-300°C和100°C-300°C和在此时段水(用作水签名的质量18和17)之间的最小质量损失。 2.第二种质量损失归因于350℃-500℃的温度之间的有机材料的分解,质谱仪显示烃类碎片趋势,其具有质量41,43,55,57的主要进化离子,和71.在这种分解过程中发生了小的吸热反应。 3.在〜650℃下,碳酸钙开始分解,持续直到〜900°C。在此期间测量的不断发展的气体是二氧化碳。组合Tg / DSC在有机/角蛋白分解和碳酸钙分解期间注册了一种吸热反应。碳酸盐富含量显示出类似的趋势,但在〜110℃-140℃下发生更显着的脱水事件,样品内的烃显示出类似的碎裂趋势,但它仅占样品重量的4%。碳酸盐富含样品具有较大的碳酸盐分解〜22%(其等易于50%的岩石是碳酸钙)。关于样品材料的物理化学转变的信息与稀释物(TMA)结果测量的尺寸变化相关,并证明了了解物流变化温度的扩展和收缩性质。

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