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Stoneley Wave Propagation Across Borehole Permeability Heterogeneities

机译:斯通利波在钻孔渗透率非均质性中的传播

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摘要

An important application of borehole acoustic logging is the determination of formationpermeability using Stoneley waves. Heterogeneous permeable structures, such as fractures,sand-shale sequences, etc., are commonly encountered in acoustic logging. The purpose of this study is to investigate the effects of the permeability heterogeneities on the borehole Stoneley wave propagation. We have studied the effects of formation permeability heterogeneities on the Stoneley wave propagation when the heterogeneity changes in radial and azimuthal directions (Zhao et al, 1993). To further study the problem of acoustic logging in heterogeneous porous formations, we study the case where the formation permeability varies in the borehole axial and radial directions. This is a very important problem because vertical heterogeneity variations are commonly encountered in acoustic logging applications. Using the finite difference approach, such heterogeneities as random heterogeneous permeability variations, multiple fracture zones, permeable (sand) - non-permeable (shale) sequences, can be readily modeled, and the results are presented. Our numerical simulation results show that the continuous permeability variations in the formation have only minimal effects on the Stoneley wave propagation. Whereas the discontinuous variation (e.g., permeable sand and non-permeable shale sequences) can have significant effeces on the Stoneley wave propagation. However, when the Stoneley wavelength is considerably large compared to the scale of heterogeneity variations, the Stoneley wave is sensitive only to the overall fluid transmissivity of the formation heterogeneity,To demonstrate the effects of heterogeneity on the Stoneley wave propagation. anexperimental data set (Winkler et aI., 1989) has been modeled using a randomly layeredpermeability model. The heterogeneous permeability model results agree with the datavery well, while the data disagree with the results from homogeneous permeabilitymodels.The numerical technique for calculating Stoneley wave propagation across permeabilityheterogeneities has been applied to interpret the acoustic logging data across aheeerogeneous fraceure zone (paillet. 1984). The modeling technique, in conjunctionwith a variable permeability model, successfully explains the non-symmetric patternsof the Stoneley wave attenuation and reileceion at the top and bottom of the fracturezone, while it is difficult to explain these patterns using a homogeneous permeable zonemodel. The technique developed in this study can be used as an effective means forcharacterizing permeability heterogeneities using borehole Stoneley waves.
机译:钻孔声波测井的重要应用是利用斯通利波确定地层渗透率。声波测井通常会遇到非均质的渗透性结构,例如裂缝,砂页岩层序等。这项研究的目的是研究渗透率非均质性对钻孔斯通利波传播的影响。我们研究了当非均质性沿径向和方位角变化时,地层渗透率非均质性对斯通利波传播的影响(Zhao等,1993)。为了进一步研究非均质多孔地层中的声波测井问题,我们研究了地层渗透率沿井眼轴向和径向变化的情况。这是一个非常重要的问题,因为在声波测井应用中通常会遇到垂直异质性变化。使用有限差分方法,可以很容易地模拟异质性,例如随机异质渗透率变化,多个裂缝带,可渗透(砂)-不可渗透(页岩)序列,并给出结果。我们的数值模拟结果表明,地层中连续的渗透率变化对斯通利波传播的影响很小。而不连续的变化(例如,可渗透的砂岩和不可渗透的页岩层序)对斯通利波传播具有显着影响。然而,当斯通利波的波长比非均质性变化的尺度大得多时,斯通利波仅对地层非均质性的整体流体透射率敏感,以证明非均质性对斯通利波传播的影响。实验数据集(Winkler等,1989)已使用随机分层的渗透率模型进行了建模。非均质渗透率模型的结果与数据非常吻合,但数据与均质渗透率模型的结果不一致。将计算斯通利波跨渗透率非均质性传播的数值技术用于解释非均质裂缝带的声波测井资料(Paillet.1984) 。该建模技术与可变渗透率模型相结合,成功地解释了裂缝区顶部和底部的斯通利波衰减和回缩的非对称模式,而使用均质的渗透区模型很难解释这些模式。这项研究中开发的技术可以用作表征井眼斯通利波渗透性非均质性的有效手段。

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