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FAST INVERSION OF FORMATION PERMEABILITY FROM STONELEY WAVE LOGS USING A SIMPLIFIED BIOT-ROSENBAUM MODEL

机译:使用简化的BIOT-ROSENBAUM模型从STONELEY波测井快速反演地层渗透率

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This paper describes a fast algorithm for estimating formation permeability from Stoneley wave logs. The procedure uses a simplified Biot-Rosenbaum model formulation. The input to the inversion is the Stoneley-wave spectral amplitudes at each receiver position, the bore-hole fluid properties (velocity and density), the borehole caliper log, the formation density and porosity (from log data), and the compressional and shear velocities for the interval of interest. The modal uses the borehole caliper and elastic properties to compute the Stoneley wave excitation (that is, predicted amplitude without permeability effects) as a function of frequency, and the porosity and permeability to compute the fluid flow amplitude reduction. This method also uses a reference depth of known permeability and compares amplitude variations at other depths relative to the reference depth. The permeability value obtained from the inversion represents the best fit over all receivers and all relevant frequencies. A processing example is shown to demonstrate the ability of this technique to extract formation permeability from Stoneley wave logs. [References: 16]
机译:本文介绍了一种根据Stoneley波测井估算地层渗透率的快速算法。该程序使用简化的Biot-Rosenbaum模型公式。反演的输入是每个接收器位置的斯通利波频谱振幅,井眼流体特性(速度和密度),井眼卡尺测井曲线,地层密度和孔隙度(来自测井数据)以及压缩和剪切感兴趣间隔的速度。该模态使用钻孔卡尺和弹性属性来计算斯通利波激励(即没有渗透率影响的预测振幅)随频率的变化,并使用孔隙率和渗透率来计算流体流量的振幅减小。该方法还使用已知渗透率的参考深度,并比较其他深度相对于参考深度的幅度变化。从反演获得的磁导率值表示所有接收器和所有相关频率的最佳拟合。所示的处理实例证明了该技术从斯通利波测井中提取地层渗透率的能力。 [参考:16]

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