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

机译:大角度和水平井中随钻声波测量的模拟和解释

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Interpretation of sonic waveforms acquired withlogging-while-drilling (LWD) tools is often non-trivialin HZ/HA wells, especially in the proximity ofboundaries between layers with high slownesscontrasts. Low-frequency components of thequadrupole mode can be affected by deleterioussuperposition effects originating from the two layers,thereby biasing the assessment of formation shearslowness. Operating companies continue to report nonnegligibledifferences between shear slownessesmeasured with LWD and wireline (WL) tools inHA/HZ wells.This paper undertakes the numerical simulation andanalysis of sonic waveforms acquired with LWDmeasurements in the vicinity of layer boundaries.Measurements simulated in HA/HZ wells are studiedfor quadrupole sources, and compared to WL loggingresults using dipole sources to estimate shear slowness.Estimations involve hard or soft formations withdifferent contrasts in shear slowness. The HZ wellsconsidered in this work have axes located at theinterface between the two layers of the formation. ForHA wells, we consider two different inclination angles.In LWD simulations with quadrupole sources in HZwells, only the first-order quadrupole wave is detected.At high frequencies, the slowness of the detected waveis the average of the slownesses of the quadrupolewaves of each layer of the formation, while at lowfrequencies the observed wave slowness approaches theslowness of the fastest formation. This is true whenboth layers are hard or soft. In WL logging simulationswith dipole sources in HZ wells, we find that thebehavior of the flexural wave is similar to that of thequadrupole wave only for the vertical dipole source andwhen both formations are soft.In HA wells, our results suggest that in formations withonly soft layers, shear slowness estimation using dipolesources in WL logging is more reliable than estimationusing LWD tool with quadrupole source. Oursimulations show that in formations with two soft layersthe effects of additional modes arising from thepresence of heterogeneities may not have a significantcontribution at low frequencies.
机译:解释用采集的声音波形 随钻测井(LWD)工具通常并非易事 在HZ / HA井中,尤其是在 高慢度层之间的边界 对比。低频成分 四极杆模式可能会受到有害影响 源自两层的叠加效果, 从而对地层剪切的评估产生偏差 缓慢。运营公司继续报告不可忽略 剪切慢度之间的差异 使用随钻测井和有线(WL)工具测量 HA / HZ井。 本文进行了数值模拟和 LWD采集的声波波形分析 层边界附近的测量。 研究了HA / HZ井中模拟的测量 用于四极子源,并与WL测井进行比较 使用偶极子源估算剪切慢度的结果。 估算涉及硬地层或软地层 剪切慢度的不同对比。 HZ井 在这项工作中考虑的轴位于 地层两层之间的界面。为了 HA井,我们考虑两个不同的倾斜角度。 在HZ中使用四极杆源进行LWD模拟中 井中,仅检测到一阶四极波。 在高频下,检测到的波的慢度 是四极慢度的平均值 地层每一层的波浪,而在低处 观察到的波慢度接近的频率 速度最快的编队。这是真的,当 这两层都是硬的或软的。在WL记录模拟中 在HZ井中使用偶极子源,我们发现 弯曲波的行为类似于 四极波仅用于垂直偶极子源和 当两个编队都是软的。 在HA井中,我们的结果表明,在具有 仅软层,使用偶极子估算剪切慢度 WL日志记录中的源比估计更可靠 使用带四极杆源的随钻测井仪。我们的 模拟表明,在具有两个软层的地层中 附加模式的影响是由于 异质性的存在可能不具有显着性 低频贡献。

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