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Experimental and mathematical model evaluation of asphaltene fractionation based on adsorption in porous media: Dolomite reservoir rock

机译:基于多孔介质吸附的沥青质分馏实验与数学模型评价:白云岩储集岩

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In this study, a whole asphaltene sample was first aged with five dolomite core samples. Then the core samples were washed with toluene; this asphaltene was named the bulk sub-fraction. Thereafter, they were washed with tetrahydrofuran, so that the n-adsorbed sub-fraction was dissolved in solvent. At the last step, the core sample was washed with an azeotrope of methanol/chloroform, which corresponded to the h-adsorbed sub-fraction, and the residual asphaltenes within the porous media were irreversibly adsorbed. According to the elemental analysis of whole asphaltene and its sub-fractions, sulfur was the most abundant element in the molecular structure of asphaltene. The presence of sulfur near dolomite increased the interaction between asphaltene and the rock surface; thus, the h-adsorbed asphaltene had the highest sulfur content. Nitrogen and oxygen content did not show a clear trend in the sub-fractions; therefore, their placements in the molecule were examined using more precise tools, such as Fourier-transform infrared spectroscopy (FTIR). Oxygen was found in asphaltene fractions in the form of a carboxylic acid functional group. From the calculation of the value of the RO-H index, the h-adsorbed asphaltene had more ability to establish a hydrogen bond (RO-H = 26.88) than the other fractions. Furthermore, by calculating the aliphatic and aromaticity indices, the sub-fraction adsorbed to the dolomite surface (h-adsorbed) had the least aliphatic compounds and the highest amount of aromaticity among the sub fractions. In addition, the h-adsorbed sub-fraction had shorter side alkyl chains than the bulk and n-adsorbed asphaltenes. Carbon number analysis was also performed to determine the number of carbons present in each molecule and to measure the molecular size of each asphaltene sub-fraction. The results showed that the C29+ fractions in the bulk sub-fraction were high (41.39%), while the C-14-C-26 and C-15-C-24 fractions had the highest frequencies in the n-adsorbed and h-adsorbed sub-fractions, respectively. A new mathematical model was tuned to determine the porosity and permeability of a resulting asphaltene deposition. The main reason for the high accuracy and innovation in the proposed relationship was the use of the fluid velocity parameter in the porous media and the volume of fluid injected into the core. In addition, the dependence of porosity and permeability reductions on parameters such as the ratio of the contribution of each asphaltene sub-fraction and the amount of the heteroatoms in each sub-fraction was studied for the first time.
机译:在这项研究中,首先将整个沥青质样品与五个白云岩岩心样品一起老化。然后将核心样品用甲苯洗涤;该沥青质被称为本体亚组分。此后,将它们用四氢呋喃洗涤,从而将n吸附的亚级分溶解在溶剂中。在最后一步,用相当于h吸附亚级分的甲醇/氯仿共沸物洗涤岩心样品,并且多孔介质中的残留沥青质被不可逆地吸附。根据整个沥青质及其子级分的元素分析,硫是沥青质分子结构中最丰富的元素。白云石附近硫的存在增加了沥青质与岩石表面之间的相互作用。因此,h吸附的沥青质的硫含量最高。氮和氧含量在亚组分中没有显示出明显的趋势。因此,使用更精确的工具(例如傅立叶变换红外光谱(FTIR))检查了它们在分子中的位置。在沥青质馏分中发现了以羧酸官能团形式存在的氧气。从RO-H指数的值的计算,与其他部分相比,h-吸附的沥青质具有建立氢键的能力(RO-H = 26.88)。此外,通过计算脂族和芳族指数,吸附到白云石表面上的子馏分(h吸附)在这些子馏分中具有最少的脂族化合物和最高的芳族量。另外,h吸附的亚级分具有比本体和n吸附的沥青质短的烷基侧链。还进行了碳数分析,以确定每个分子中存在的碳数,并测量每个沥青质亚馏分的分子大小。结果表明,本体亚组分中的C29 +组分较高(41.39%),而C-14-C-26和C-15-C-24组分在n-吸附和h-吸附中的频率最高。分别吸附子级分。调整了新的数学模型,以确定所得沥青质沉积的孔隙率和渗透率。所提出的关系的高精度和创新性的主要原因是在多孔介质中使用了流体速度参数以及注入岩心的流体量。此外,首次研究了孔隙度和渗透率降低对参数的依赖性,例如每个沥青质亚组分的贡献率和每个亚组分中杂原子的数量之比。

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