荷兰北海F3区块的超压产生机制

Khusmia Karin, Sudarmaji
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引用次数: 0

摘要

北海F3区块是一个由于埋藏和各种沉积带等复杂地质条件而导致孔隙压力值随时间变化的区块。孔隙压力是需要分析的重要方面之一,作为识别区域和超压机制的基础。超压是一种比正常压力更大的孔隙压力条件,可能会导致钻井问题,如井涌、井喷等。本研究使用eaton方法结合井数据和地震数据计算孔隙压力值。这两个数据被集成以生成1D和3D中的孔隙压力值。1D建模使用交互式岩石物理3.5,而3D建模使用Petrel软件。在三维建模中,使用的变量是通过声阻抗反演获得的层速度和反演速度。使用的子变量是反演密度和从井密度声阻抗反演获得的回归密度。1100–1800 m深处存在1D超压区,超压值为3836–18975 kPa。此外,基于3D模型的超压值为8000–18000 kPa。使用声阻抗反演模型验证超压区,该模型的高值为5200–5380(m/s)*(gr/cc)。F3区块的超压预计由不平衡压实引起。。
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Overpressure-generating mechanisms in the Blok F3, North Sea, Netherland
Block F3 North Sea is a block with pore pressure values that vary over time due to complex geological conditions such as burial and various sedimentation zones. Pore pressure is one of the important aspects that need to be analyzed as a basis for the identification of zones and overpressure mechanisms. Overpressure is a greater pore pressure condition than normal pressure and may cause drilling problems, such as kicks, blowouts, etc. This study calculated pore pressure values using the eaton method approach with well data and seismic data. Both data are integrated for generating pore pressure values in 1D and 3D. 1D Modelling uses Interactive Petrophysics 3.5, while 3D modeling uses Petrel software. In 3D modeling, the variables used are interval velocity and inversion velocity obtained by acoustic impedance inversion. The sub-variables used are the inversion density and the regression density obtained from well density acoustic impedance inversion. The existence of a 1D overpressure zone at a depth of 1,100 – 1,800 m with an overpressure value of 3,836 – 18,975 kPa. In addition, the overpressure value based on the 3D model is 8,000 – 18,000 kPa. The overpressure zone is validated using an acoustic impedance inversion model with a high value of 5,200 – 5,380 (m/s)*(gr/cc). Overpressure in Block F3 is predicted to occur from disequilibrium compaction..
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审稿时长
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