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A geochemical framework for understanding residue properties

机译:理解残留物业的地球化学框架

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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:原油和其残留级分,在许多相关性质中变化很大。因此,单个残基流或甚至来自一个区域的许多残留物流的详细表征可能与世界的不同部分中的炼油厂非常相关。因此,我们试图以通用方式制定理解残留物业的框架。对来自各种原油的11个真空残留级分的详细分析导致了解残留物流的组成和加工性的一般模型。该模型基于地球化学来源(Kerogen Type)和原油的成熟度。与更常规的基因Ⅱ残基相比,基因Ⅰ(链烷烃)残基的不同起源在大量的性质中反映,并且在这些性质中也处于较大的可变性。然而,在成熟的平均性质干酪根Ⅰ残基和油母岩Ⅱ的残基汇聚,以使这两种类型的干酪根成熟残基具有很多共同点(低S含量,低金属含量,高H / C比等)。在分子的基础上,KerogenⅠ残基含有更多以蜡化合物形式的链烷烃。成熟后,残留物倾向于较低的平均分子量,较高的H / C比(较低密度),较低的粘度,较低浓度的杂原子(硫,氮,V和Ni),沥青质和MCRT,以及更高的蜡含量。发现成熟对残留部分的稳定性和焦化趋势产生了负面影响。 NMR数据显示,沥青质在老化时变得更加芳族,而麦芽酮(非沥青质)变得较低,因此在这些级分之间导致芳香性的差距增加。观察到KerogenⅠ和KerogerⅡ残基之间沥青质分子结构的显着差异。在本研究中未包括KerogenⅢ的丘,因为它们通常含有不足的真空底部是实际兴趣的。分析数据表明,Cherogen型和成熟度的概念可以是描述和理解残留特性的有用工具,并有助于优化残留转换方法和其他残留件应用(燃料油,沥青)以及理解污垢的原料选择和焦化现象。

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