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A geochemical framework for understanding residue properties

机译:用于理解残留物特性的地球化学框架

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Crude oils, and the residual fractions thereof, vary widely in many relevant properties. Thus, a detailed characterization of a single residue stream or even a number of residue streams from one region may not be very relevant to a refiner in a different part of the world. We have therefore attempted to develop a framework for understanding residue properties in a generic fashion. A detailed analysis of 11 vacuum residue fractions from a wide variety of crude oils resulted in a general model for understanding the composition and processability of residue streams. This model is based on the geochemical origin (kerogen type) and the maturity of the crude oil. The different origin of kerogen Ⅰ (paraffinic) residues, compared with the more conventional kerogen Ⅱ residues, is reflected in a large number of properties and also in a larger variability in these properties. However, upon maturation, the average properties of kerogen Ⅰ residues and kerogen Ⅱ residues converge so that mature residues of both kerogen types have much in common (low S content, low metals content, high H/C ratio etc). On a molecular basis, kerogen Ⅰ residues contain more paraffins in the form of wax compounds. Upon maturation, residues tend towards lower average molecular weights, higher H/C ratio's (lower density), lower viscosities, lower concentrations of hetero-atoms (sulphur, nitrogen, V and Ni), asphaltenes and MCRT, and higher wax contents. Maturation is found to have a negative effect on the stability and coking tendency of the residue fraction. NMR data reveal that the asphaltenes become more aromatic upon ageing, whereas the maltenes (non-asphaltenes) become less aromatic, thus causing an increasing gap in aromaticity between these fractions. Significant differences in asphaltene molecular structure between kerogen Ⅰ and kerogen Ⅱ residues were observed. Kerogen Ⅲ crudes were not included in this study as they generally contain insufficient vacuum bottoms to be of practical interest. The analytical data suggest that the concept of kerogen type and maturity may be a useful tool in describing and understanding residue characteristics and assist in optimizing feedstock selection for residue conversion processes and other residue applications (fuel oils, bitumen), as well as in understanding fouling and coking phenomena.
机译:原油及其残余馏分的许多相关性能差异很大。因此,来自一个地区的单个渣油流甚至多个渣油流的详细表征可能与世界其他地区的精炼厂关系不大。因此,我们试图开发一种框架,以通用的方式理解残留物的性质。对来自多种原油的11种减压渣油馏分的详细分析,形成了用于理解渣油流的组成和可加工性的通用模型。该模型基于地球化学来源(干酪根类型)和原油的成熟度。与更常规的干酪根Ⅱ残基相比,干酪根Ⅰ(石蜡基)残基的起源不同,这体现在大量特性上,而且这些特性的变异性也更大。然而,成熟时,干酪根Ⅰ和Ⅱ的平均性质会趋于一致,因此两种干酪根的成熟残渣有很多共同点(低S含量,低金属含量,高H / C比等)。在分子基础上,干酪根Ⅰ残基包含更多的蜡化合物形式的石蜡。成熟后,残留物趋向于降低平均分子量,提高H / C比(降低密度),降低粘度,降低杂原子浓度(硫,氮,V和Ni),沥青质和MCRT以及提高蜡含量。发现成熟对残余物部分的稳定性和结焦趋势具有负面影响。 NMR数据显示,随着时间的流逝,沥青质会变得更芳香,而麦芽烯(非沥青质)会变得更不芳香,从而导致这些馏分之间的芳香性差距越来越大。观察到干酪根Ⅰ和干酪根Ⅱ的沥青质分子结构存在显着差异。干酪根Ⅲ原油未包括在该研究中,因为它们通常含有不足的真空塔底馏出物,因此具有实际意义。分析数据表明,干酪根类型和成熟度的概念可能是描述和理解残留物特性的有用工具,并有助于优化用于残留物转化过程和其他残留物应用(燃料油,沥青)的原料选择以及理解结垢。和焦化现象。

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