首页> 外文会议>SPWLA Annual Logging Symposium >ASSESSMENT OF SHOULDER-BED, INVASION, AND LAMINATION EFFECTS ON BOREHOLE SONIC LOGS: A NUMERICAL SENSITIVITY STUDY
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ASSESSMENT OF SHOULDER-BED, INVASION, AND LAMINATION EFFECTS ON BOREHOLE SONIC LOGS: A NUMERICAL SENSITIVITY STUDY

机译:钻孔声波测井的单床,侵入和层状效应评估:数值敏感性研究

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We quantify the relative effects of shoulder beds, layer thickness, invasion, and sand-shale laminations on monopole and dipole borehole sonic logs. This is accomplished through numerical simulation of sonic waveforms that includes all of the propagation modes within the 1-10 KHz range. Numerical simulations assume infinitesimal monopole and dipole sources as well as an array of infinitesimal receivers deployed in close similarity with one commercially available wireline sonic tool. Propagation modes and their velocities are assessed via slowness-time-coherence processing of the simulated waveforms. For the case of shoulder-bed and layer-thickness effects, we consider soft and hard formations bounded by shale layers. The thickness of the formation is changed to consider cases where transmitter and receivers are completely included in the bed and partially distributed across different beds. Simulations indicate that shoulder- and bed-thickness effects can account for up to 30% variations in the P-wave velocities measured with a monopole source and 31% in the measured S-wave velocities measured with a dipole source compared to those measured across infinitely thick beds. We reproduce the sonic response of sand-shale laminated formations by including thin shale layers within pay sands. The thickness of shale layers is varied to consider the effect of proportion of sand and shale on the measurements. Simulations indicate that shale laminations can account for up to 7.3% variations in the P-velocities measured with a monopole source and up to 5.8% variations in the S-velocities measured with a dipole source with respect to those of effective lamination velocities. Effects of invasion are simulated for the case of waterbase mud invading oil-bearing formations. Our simulations indicate that P-wave sonic logs can undergo up to 23% variations due to invasion under realistic assumptions of petrophysical and elastic properties of soft and hard formations.
机译:我们量化了单极和偶极井眼声波测井仪上肩床,层厚,侵入和砂页岩层合的相对影响。这是通过对包括1-10 KHz范围内的所有传播模式在内的声音波形进行数值模拟来实现的。数值模拟假定无限极的单极子和偶极子源,以及与一种市售的有线声波工具极为相似地部署的无限极小的接收器阵列。通过模拟波形的慢度-时间相干处理来评估传播模式及其速度。对于肩床和层厚效应,我们考虑了由页岩层界定的软硬层。改变地层的厚度以考虑发射器和接收器完全包含在床中并部分分布在不同床中的情况。仿真表明,与无限量测得的相比,用单极子源测得的P波速度和肩厚的影响可解释高达30%的变化,而用偶极子源测得的S波速度的变化高达31%厚床。通过将薄页岩层包括在产砂中,我们再现了砂页岩层状地层的声波响应。页岩层的厚度是变化的,以考虑砂和页岩的比例对测量的影响。模拟表明,相对于有效叠层速度,页岩层合可以解释单极震源测得的P速度变化最多7.3%,而偶极震源测得的S速度变化最多5.8%。对于水基泥浆侵入含油地层的情况,模拟了侵入的影响。我们的模拟表明,在软,硬地层的岩石物理和弹性特性的实际假设下,由于侵入,纵波声波测井曲线可能会发生高达23%的变化。

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