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The catalytic effects of carbonate minerals on characteristics of heavy oil in hydrothermal reactions

机译:碳酸盐矿物催化作用对水热反应重油特性的影响

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Hydrothermal influences on heavy oil were simulated in laboratory conditions. The experimental model was composed of oil, calcite, dolomite, and manganese oxide. Oil to dominant mineral ratio was 1:1, where the content of manganese oxide was 5%. The hydrothermal reactions were carried out under the reservoir temperatures of 250-300 degrees C and a pressure of 1-2MPa. As a result of treatment, aromaticity of oil increased, while H:C ratio decreased from 1.92 to 1.61. The structures of newly formed light fractions were characterized by low molecular aromatic compounds, which were the destruction products of resins. The treatment provided removal of nitrogen and sulfur from crude oil, hence, decreasing the viscosity of products. The genotype of crude oil did not change. The quantitative changes in the ratio of isoprenoid alkanes to the linear ones were evaluated via geochemical coefficients of group composition.
机译:在实验室条件下模拟对重油的水热量影响。 实验模型由油,方解石,白云石和氧化锰组成。 含油至占优势矿物比例为1:1,其中氧化锰的含量为5%。 在250-300℃的储层温度和1-2MPa的压力下进行水热反应。 由于治疗的结果,油的芳香性增加,而H:C比率从1.92降至1.61。 通过低分子芳族化合物的特征是新形成的光级分的结构,其是树脂的破坏产物。 该处理提供了从原油中除去氮和硫,因此降低了产物的粘度。 原油的基因型没有变化。 通过Geochemical系数的基团组合物评价异戊二烯烷基与线性烷基比的定量变化。

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