首页> 外文会议>SPWLA Annual Logging Symposium;Society of Petrophysicists and Well Log Analysts, inc >INTERPRETATION OF SONIC WAVEFORMS ACQUIRED IN HIGH-ANGLE AND HORIZONTAL WELLS
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INTERPRETATION OF SONIC WAVEFORMS ACQUIRED IN HIGH-ANGLE AND HORIZONTAL WELLS

机译:高角度和水平井中声波波形的解释

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Increasingly, more high-angle (HA) and horizontal(HZ) wells have been drilled in recent yearsbecause of the accelerated development of offshoreexploration and onshore organic-shaledevelopment. Conventional waveform processingmethods are developed only for vertical wells.When used in HA/HZ wells, these methods mayyield biased estimations of P- and S-waveslownesses. New methods are needed to processsonic waveforms acquired in HA/HZ wells,specifically in the vicinity of layer boundaries andin the presence of thin layers.This paper examines several HA/HZ boreholemodels when a sonic tool operates across ahorizontal bed boundary. High-resolution 3Dnumerical simulations of sonic waveforms arecarried out with a time-domain finite-differencemethod coupled with a complex, frequency-shifted,perfectly matched layer to study the transientacoustic fields measured in and out of the borehole.These simulations assume a 3D sonic logging toolwith multipole sources and 13×8 azimuthalreceivers. Both monopole and dipole syntheticwaveforms are obtained in HA/HZ boreholespenetrating hard and soft formations. Instead of theconventional processing of monopole or dipolewaveforms that takes the average, or difference, ofwaveforms acquired with azimuthal receivers, weseparately analyze the sonic waveforms at eachazimuthal receiver. Waveforms are first processedwith a weighted spectral semblance method toyield modal dispersions; next, we reconstructformation shear slowness from these dispersioncurves with a dispersion correction method. Thetop and bottom receiver slowness is chosen whenthe tool measurement point is in the formationabove and below the well, respectively. Resultsindicate that this new procedure provides unbiasedestimations of rock formation shear slownesscompared to conventional processing. Moreover,the difference between top and bottom receiverslowness reflects the elastic property contrastbetween the formation section above and below thewell, enabling the accurate evaluation of formationheterogeneity due to bed boundary effects inHA/HZ wells.The new sonic waveform interpretation approachintroduced in this paper is ideal for theelastic/mechanical assessment of organic shale, inwhich rock heterogeneity is commonplace.
机译:越来越多的高角度(HA)和水平 (HZ)井近年来已钻探 因为近海的加速发展 勘探和陆上有机页岩 发展。常规波形处理 方法仅针对垂直井开发。 在HA / HZ井中使用时,这些方法可能会 纵波和横波的产量偏差估计 缓慢。需要新方法来处理 HA / HZ井中采集的声波波形, 特别是在层边界附近 在薄层的情况下。 本文研究了几个HA / HZ钻孔 当声波工具在 水平床边界。高分辨率3D 声波波形的数值模拟是 用时域有限差分进行 方法,加上复杂的频移 完美匹配的层来研究瞬态 在钻孔内外测量的声场。 这些模拟假设使用3D声波测井仪 具有多极源和13×8方位角 接收者。单极和偶极合成 在HA / HZ钻孔中获得波形 穿透硬地层和软地层。而不是 单极或偶极子的常规处理 取平均值或差值的波形 用方位角接收器采集的波形,我们 分别分析每个声波的波形 方位角接收器。首先处理波形 用加权光谱相似度法 产生模态色散;接下来,我们重建 这些分散作用引起的地层剪切慢度 色散校正方法绘制曲线。这 何时选择顶部和底部接收器慢度 工具测量点在地层中 分别位于井上方和下方。结果 表示此新程序提供了无偏见 岩层剪切慢度的估算 与常规处理相比而且, 顶部和底部接收器之间的区别 慢度反映出弹性对比 在上方和下方的编队段之间 好,可以对地层进行准确评估 床边界效应造成的非均质性 HA / HZ井。 新的声音波形解释方法 本文介绍的方法非常适合 有机页岩的弹性/力学评估 哪种岩石异质性很普遍。

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