声波斯通利波衰减测量的渗透率推导:在中东巨型碳酸盐岩油田的应用

H. Yin, Xianyun Wu, L. Yose
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引用次数: 1

摘要

渗透率是油藏模拟、油田开发和油藏管理中最重要的参数之一。利用斯通利波衰减机制(而不是先前研究中讨论的斯通利波速),开发了一种创新的渗透率推导方法和工作流程。将该工作流程应用于中东某大型碳酸盐岩油田直井的声波波形数据。工作流程包括:(a)从波形数据中严格提取斯通利波衰减,(b)从斯通利波衰减到渗透率的快速反演。通过将结果与岩心渗透率和MDT流度数据进行比较,验证了方法和工作流程。应用结果表明,低频单极子波形提供了高质量的斯通利波数据,斯通利波衰减响应渗透率的变化。低频单极子波形提取的斯通利波衰减测井具有变异性,不同储层段的渗透率测井与岩心渗透率具有较好的整体相关性。主储层厚度超过100英尺。孔隙度在整个储层中普遍较高,但由于孔隙类型的变化,渗透率会发生好几个数量级的变化。斯通利波衰减渗透率趋势与优势孔隙系统的垂向变化非常吻合。斯通利推导的渗透率区分了渗透率在1 ~ 20毫达西范围内的下段微孔和渗透率在10 ~ 100毫达西范围内的上段混合孔。声波渗透率也可以探测到致密条纹(具有胶结的柱面岩带),这些条纹具有低孔隙度和渗透率,可以在储层中充当流动挡板。这些结果表明,斯通利波衰减是对碳酸盐岩孔隙系统变化的响应,并且斯通利推导的渗透率可以在没有岩心数据的情况下提供有用的渗透率估计。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Permeability Derivation from Sonic Stoneley Wave Attenuation Measurements: Application in a Giant Carbonate Field from Middle East
Permeability is one of the most important parameters that is required in reservoir simulation, field development, and reservoir management. An innovative permeability derivation method and workflow has been developed using Stoneley wave attenuation mechanism (not Stoneley wave velocity as discussed in some previous studies). The workflow was applied to the sonic waveform data acquired from a vertical well in a giant carbonate field in Middle East. The workflow includes (a) extraction of Stoneley-wave attenuation rigorously from the waveform data, and (b) fast inversion from Stoneley-wave attenuation to permeability. Validation of the method and workflow were performed by comparing the results with core permeability and MDT mobility data. Results from this application indicate that low-frequency monopole waveforms provide good quality Stoneley wave data, and that Stoneley wave attenuation responds to permeability changes. The Stoneley-wave attenuation log extracted from the low-frequency monopole waveforms shows variability, and the permeability log obtained using the inversion workflow through different reservoir intervals has a good overall correlation with core permeability. The main reservoir interval is over 100 feet thick. Porosities are generally high throughout the interval, but permeabilities vary by several orders of magnitude due to pore type changes. The Stoneley wave attenuation permeability trend corresponds very well to vertical changes in the dominant pore system. Stoneley-derived permeabilities distinguish between microporosity in lower section with permeabilities in 1-20 millidarcy range, and mixed-pores in the upper section with permeabilities in the 10's to 100's of millidarcy range. The sonic permeability is also picking up tight streaks (stylolite zones with cementation) that have low porosity and permeability and can act as flow baffles within the reservoir. These results show that Stoneley wave attenuation is responding to changes in carbonate pore systems, and that Stoneley-derived permeabilities can provide useful permeability estimates in the absence of core data.
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