Algorithm for processing dispersive waves from dipole sonic tool

M. Redaelli, R. Victor, C. Beneduzi, Pablo Batista
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Abstract

Shear sonic wave velocities can be obtained by monopole sources in logging tools only for fast formations, namely where formation shear velocity is higher than wave velocity in the drilling mud. The dipole source is used for estimating shear velocity in slow formations, by indirectly processing the flexural mode excited in the borehole. The dispersive characteristic of the flexural mode, nevertheless, renders useless the Slowness-Time Coherence method, the traditional algorithm used for processing non-dispersive sonic waveforms from monopole sources. We report the application of Dispersive Slowness-Time Coherence to process sonic log waveforms acquired using dipole sources. This method uses modeled dispersive curves created from classic wave propagation theory and can overcome the previously mentioned limitations. We tested our implementation using real data from four wells drilled in formations with distinct elastic characteristics and found our results compatible to the ones offered by service companies.
偶极子声波工具色散波处理算法
只有在快速地层中,即地层剪切速度高于钻井泥浆中的波速时,测井工具中的单极子震源才能获得剪切声波速度。偶极子源通过间接处理井内激发的弯曲模态来估计慢速地层的剪切速度。然而,弯曲模态的色散特性使得用于处理单极子源非色散声波波形的传统算法慢时相干法失效。我们报告了色散慢度-时间相干性在处理用偶极子源获得的声波测井波形中的应用。该方法利用经典波传播理论建立的模型色散曲线,克服了上述局限性。我们使用了四口井的真实数据进行了测试,这些井在具有不同弹性特性的地层中钻探,结果发现我们的结果与服务公司提供的结果一致。
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