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Quantitative Formation Permeability Evaluation from Stoneley Waves

机译:斯通利波的定量地层渗透率评估

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Reservoir engineers need a continuous measurement of permeability to optimize well completion and produce the formation effectively. The borehole Stoneley wave has been shown to be sensitive to fluid mobility, the ratio of permeability and viscosity. the phenomenon is well described using the Biot theory, and models to account for the effect of the mudcake have been proposed. Existing techniques use either the Stoneley slowness or its attenuation at low frequency to estimate the fluid mobility with simplified Biot models. However, the results of these techniques usually show unexplained differences from core measured permeabilities, or with well test results. The objective of the methodology presented in this paper is to improve the reliability of the estimation and to take into account important factors that have been neglected.
机译:油藏工程师需要连续测量渗透率,以优化完井并有效生产地层。井的斯通利波已经显示出对流体流动性,渗透率和粘度之比敏感。使用比奥特理论可以很好地描述这种现象,并且已经提出了解释泥饼效应的模型。现有技术使用简化的Biot模型使用斯通利(Stoneley)慢度或其低频衰减来估计流体流动性。但是,这些技术的结果通常显示出与岩心测得的渗透率有无法解释的差异,或者具有良好的测试结果。本文介绍的方法的目的是提高估计的可靠性,并考虑已被忽略的重要因素。

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