压力变化对盖层和储层岩石完整性及断层活化的影响

M. Abdideh, Yaghob Hamid
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引用次数: 0

摘要

盖层是阻止碳氢化合物向上运移的堤坝。它们有差异和弱点,包括不连续、破碎区域和断层。注气是提高原油采收率和孔隙压力的有效机制。随着孔隙压力的增大,正应力减小,不透水边界(盖层、断层等)的完整性变得不稳定。对储层进行地质力学研究和建模是油藏开发的必然要求。综合地质力学模型的建立,包括应力状态是深度(方向和数量)、储层岩石及其地层物理性质(岩石阻力和弹性模量)、孔隙压力估算以及裂缝和断层的描述和分布的函数。在这项工作中,分析和数值方法被用于地质力学建模,用于建模和岩石物理信息的数据是井下测试。对伊朗西南部Asmari油藏和Marun油田盖层进行了注气地质力学建模,并进行了相应的操作。计算了断层恢复阈值和诱发断裂的临界压力,并将计算结果以解析模型和数值模型的形式呈现。此外,除了分析深层应力场外,还确定了地层的阻力参数。结果表明,井口、裂缝和油田边缘的变化和不稳定性最大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
An Evaluation of Rock Integrity and Fault Reactivation in the Cap Rock and Reservoir Rock Due to Pressure Variations
Cap rocks are dams which can prevent the upward movement of hydrocarbons. They have disparities and weaknesses including discontinuities, crushed areas, and faults. Gas injection is an effective mechanism for oil recovery and pore pressure. With increasing pore pressure, normal stress is reduced, and the integrity of impermeable boundaries (cap rock, fault, etc.) becomes instable. A successful strategy for reservoir development is the inevitable necessity of conducting geomechanical studies and modeling the reservoir. The construction of a comprehensive geomechanical model, including the stress state is a function of depth (direction and amount), physical properties of the reservoir rock and its formations (rock resistance and elastic moduli), pore pressure estimation, and description and distribution of fractures and faults. In this work, analytical and numerical methods have been used in geomechanical modeling, and the data used for modeling and petrophysical information are downhole tests. The geomechanical modeling of gas injection into the reservoir and, simultaneously, the operation of Asmari reservoir and Marun oilfield cap rock in the southwest of Iran were carried out. The threshold of reactivating faults and the critical pressure of induced fracture were calculated, and the results were presented as analytical and numerical models. Moreover, in addition to analyzing the stress field at depths, the resistance parameters of the formations were determined. The results showed that the most changes and instabilities were around the wellheads, fractures, and the edges of the field.
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