巴黎盆地潜在二氧化碳注入试验场地震监测的可行性

M. Becquey, N. Lucet, F. Huguet
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引用次数: 6

摘要

对部分枯竭油田注入二氧化碳的地震效应进行了评价。地震模拟产生了较小的时移效应,包括0.4 ms的时移和4 - 6%的储层顶部和底部的振幅变化。在大入射角下,储层水平的振幅变化应该略大,但波动方程模型表明,由于上部界面产生的剪切波的存在,挑选这些反射并不容易。原位压裂产生方位各向异性,速度和振幅随传播方向变化。这些变化包含了裂缝密度、裂缝网与多孔介质之间的关系以及孔隙和裂缝中的流体含量等信息。然而,所有这些影响都很微弱,它们的测量需要仔细的地震数据采集和处理。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Feasibility of Seismic Monitoring at a Potential CO2 Injection Test Site in the Paris Basin
Seismic effects of the injection of CO2 into a partially depleted oil field have been evaluated. Seismic modelling yields small time-lapse effects, including 0.4 ms time-shifts and 4 to 6% amplitude variations at the top and bottom of the reservoir. Amplitude variations at the reservoir level should be slightly larger at large incidence angles, but wave equation modelling shows that picking these reflections will not be easy, because of the presence of shear waves generated at upper interfaces. In-situ fracturation generates azimuthal anisotropy with velocity and amplitude variations with the propagation direction. These variations bear some information about the crack density, about the relation between the fracture nets and the porous medium, and about the fluid content in the pores and fractures. All these effects are however weak and their measurement requires careful seismic data acquisition and processing.
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