首页> 外文期刊>Journal of Natural Gas Geoscience >Hydrocarbon phase limit and conversion process in the deep formation from Qikou Sag of Bohai Bay rift lacustrine basin, China
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Hydrocarbon phase limit and conversion process in the deep formation from Qikou Sag of Bohai Bay rift lacustrine basin, China

机译:渤海湾裂谷湖盆地奇口凹陷深层油气相限和转化过程

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It is an important research direction for the prediction of hydrocarbon phase in the reservoir during the deep exploration of rift basins in eastern China. The typical lacustrine crude oil of Shahejie Formation in Qikou Sag was used for oil cracking to gas simulation experiment by the gold tube in this paper. Then, the kinetic parameters obtained from the experimental data were studied during the cracking reactions and the hydrocarbon phase conversion process under geological conditions. The results showed that the activation energy of the oil cracking to gas from the BH-28 lacustrine crude oil ranged from 250?kJ/mol to 270?kJ/mol with an average ofEO?=?255.47?kJ/mol, and the frequency factor was aboutA?=?1014?s?1. It is higher than that of typical marine oilEO?=?246.97?kJ/mol. Using these kinetic parameters, the simulated cracking process of the lacustrine oil of Shahejie Formation was far different from that of marine oil from western China under the same geological heating rate (3?°C/Ma). And the simulated oil cracking degree in Well Niudong-1 is 73.9%, almost the same with the conversion cracking degree (60%–75%) by concentrations of 3,4-dimethyldiamantane. The kinetics of oil cracking gas could be used to investigate the oil cracking degree easily, then to get the theoretical separate oil phase depth limit. By using this model, oil in Qikou Sag, as a theoretical separate phase destruction, occurs above 5700?m depth limit (ROis about 2.0%, reservoir temperature?=?209?°C, with cracking transitionCof 62.5%), and condensate gas destruction occurs above 6700?m depth limit (ROis about 3.2%, reservoir temperature?=?240?°C, withCto 99%) under the geological conditions from Qikou Sag. Actually, the hydrocarbon phase is affected by many factors. For example, migration and changes of temperature and pressure conditions have great influence on phase conversion behavior. The injection of gas, originated from kerogen cracking gas and oil cracking gas in deeper, could increase GOR and the real separate phase depth would reduce.
机译:这是预测中国东部裂谷盆地深层油气藏中烃相的重要研究方向。本文利用金口管将奇口凹陷沙河街组的典型湖相原油用于天然气裂解实验。然后,在地质条件下,研究了在裂化反应和烃相转化过程中从实验数据获得的动力学参数。结果表明,BH-28湖相原油的油裂化为气体的活化能为250?kJ / mol至270?kJ / mol,平均EO?=?255.47?kJ / mol,且频率因子约为A?=?1014?s?1。它高于典型的船用油的EOε=?246.97?kJ / mol。利用这些动力学参数,在相同的地质升温速率(3℃/ Ma)下,沙河街组湖相油的模拟开裂过程与中国西部的海洋油相差很大。牛洞1号井的模拟油裂度为73.9%,与3,4-二甲基二金刚烷浓度下的转化裂化度(60%〜75%)几乎相同。可以利用裂化气的动力学来方便地研究裂化度,从而得到理论上单独的油相深度极限。通过使用该模型,岐口凹陷的油作为理论上的单独相破坏发生在5700?m的深度极限以上(ROis约为2.0%,油藏温度?=?209°C,裂化转变温度为62.5%),并且凝结气在奇口凹陷的地质条件下,破坏发生在6700?m的深度极限以上(ROis约为3.2%,储层温度?=?240°C,C至99%)。实际上,烃相受许多因素影响。例如,温度和压力条件的迁移和变化对相转换行为有很大的影响。源于干酪根裂化气和石油裂化气的更深层注入的天然气会增加GOR,而真正的分离相深度会减少。

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