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Determination of Formation Properties in Cased Boreholes Using Full Waveform Acoustic Logs

机译:用全波形声波测井确定套管钻孔的地层特征

摘要

Wave propagation in bonded and unbonded cased boreholes is examined through the calculation cif synthetic full waveform acoustic logs. The models consist of a central fluid borehole surrounded by a number of fluid and solid annuli. Waveforms calculated for a variety of formation and cement parameters demonstrate that the first arrivals observed on full waveform acoustic logs in well bonded cased holes are those of the formation and not the casing. Waves refracted along the casing are generally too small to be observed. The presence of the steel and cement can make the determination of formation velocities more difficult than in an open hole. The formation body wave arrivals are decreased substantially if the cement velocities are near or greater thanthe formation velocities. A fluid layer between the steel and the cement essentially frees the pipe from the cement. The steel arrival then becomes a large, ringing signal which obscures the formation arrival. The presence of this layer is a more important factor than its thickness in causing such behavior. If the fluid layer is between the cement and the formation, the cement can damp out the ringing of the pipe. If a thick cement layer is bonded to the pipe and the fluid layer is thin. the casing arrival is small and the formation arrivals are discernible. A thinner cement layer results in the observation of a body wave that has a velocity that is an average of the steel and cement velocities.
机译:通过合成全波形声波测井的计算,可以检查粘结和非粘结套管井中的波传播情况。这些模型由一个中央流体钻孔组成,周围被许多流体和固体环空所包围。为各种地层和水泥参数计算的波形表明,在粘结良好的套管孔中,在全波形声波测井上观察到的首次到达是地层的那些,而不是套管。沿套管折射的波通常太小而无法观察到。与在裸眼中相比,钢和水泥的存在会使地层速度的确定更加困难。如果水泥速度接近或大于地层速度,则地层波的到达将大大减少。钢材和水泥之间的流体层基本上使管道脱离了水泥。然后,钢的到达变为大的振铃信号,从而掩盖了地层的到达。该层的存在比引起其行为的厚度更重要。如果流体层位于水泥和地层之间,则水泥可以减弱管道的振铃。如果将较厚的水泥层粘结到管道上,并且流体层较薄。套管的到来很小,并且地层到来是可辨别的。较薄的水泥层导致观察到的体波的速度为钢和水泥速度的平均值。

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