ISSN 1673-8217 CN 41-1388/TE
主管:中国石油化工集团有限公司 主办:中国石油化工股份有限公司河南油田分公司
王瑀辉, 袁玉松. 2018: 含烃盐水包裹体PVTsim模拟的一种简化方法及应用. 石油地质与工程, 32(05): 40-43+122.
引用本文: 王瑀辉, 袁玉松. 2018: 含烃盐水包裹体PVTsim模拟的一种简化方法及应用. 石油地质与工程, 32(05): 40-43+122.
WANG Yuhui, . 2018: A simplified method of PVTsim simulation of hydrocarbon-containing saline inclusions and its application. Petroleum Geology and Engineering, 32(05): 40-43+122.
Citation: WANG Yuhui, . 2018: A simplified method of PVTsim simulation of hydrocarbon-containing saline inclusions and its application. Petroleum Geology and Engineering, 32(05): 40-43+122.

含烃盐水包裹体PVTsim模拟的一种简化方法及应用

A simplified method of PVTsim simulation of hydrocarbon-containing saline inclusions and its application

  • 摘要: 在利用PVTsim模拟地层古压力过程中发现,室温下包裹体气液体积比的模拟结果与捕获压力之间存在明显函数关系,提出了利用模拟得到的两组数据计算气液比与捕获压力的方程,再将实验室测得的室温条件下气液比代入,最后得到包裹体最大捕获压力的简化方法,可以便捷地进行批量包裹体样品捕获压力模拟,同时为包裹体成分校正及结果调整提供参考。应用此方法模拟了川东南地区林–1井下古生界地层流体压力演化过程,模拟结果揭示林–1井早期普遍存在超压,早白垩世时压力系数超过2.0,晚白垩世地层压力迅速下降,现今为常压,反映了白垩世晚期强烈构造抬升对地层超压具有显著的破坏作用。

     

    Abstract: In the process of using PVTsim to simulate the formation of the paleo-pressure, the clear relation between the simulation results of volume ratio of gas to liquid and the trapping pressure was found, the functional relation between the ratio of gas to liquid and the trapping pressure was given, then the ratio of gas to liquid measured under the room temperature in laboratory was added into the formula and finally the simplified method of hydrocarbon-containing saline inclusion was obtained, which is convenient to simulate the pressure of mass inclusion samples and provide a reference for the correcting of the components of inclusions and the simulation results. The method was applied to simulate the evolution process of fluid pressure in Paleozoic strata of well Lin-1 in southeast Sichuan, the results showed that the overpressure of well Lin-1 generally existed during early Paleozoic, the pressure coefficient of the early Cretaceous was more than 2.0. In late Cretaceous, the formation depression declined rapidly, and it is normal in present stratum, which shows that the late strong tectonic uplift had a significant damage to the overpressure of the stratum.

     

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