首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >avefield simulation and data-acquisition-scheme analysis or LWD acoustic tools in very slow formations
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avefield simulation and data-acquisition-scheme analysis or LWD acoustic tools in very slow formations

机译:极慢地层中的avefield模拟和数据采集方案分析或LWD声学工具

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摘要

Propagating wavefields from monopole, dipole, and quadrupole acoustic logging-while-drilling (LWD) tools in very slow formations have been studied using the discrete wavenumber integration method. These studies examine the responses of monopole and dipole systems at different source frequencies in a very slow surrounding formation, and the responses of a quadrupole system operating at a low source frequency in a slow formation with different S-wave velocities. Analyses are conducted of coherence-velocity/slowness relationships (semblance spectra) in the time domain and of the dispersion characteristics of these waveform signals from acoustic LWD array receivers. These analyses demonstrate that, if the acoustic LWD tool is centralized properly and is operating at low frequencies (below 3 kHz), a monopole system can measure P-wave velocity by means of a "leaky" P-wave for very slow formations. Also, for very slow formations a dipole system can measure the P-wave velocity via a leaky P-wave and can measure the S-wave velocity from a formation flexural wave. With a quadrupole system, however, the lower frequency limit (cutoff frequency) of the drill-collar interference wave would decrease to 5 kHz and might no longer be neglected if the surrounding formation becomes a very slow formation, with S-wave velocities at approximately 500 m/s.
机译:使用离散波数积分方法研究了单极,偶极和四极随钻测井(LWD)工具在非常慢的地层中传播的波场。这些研究检查了在极慢的周围地层中不同源频率下的单极和偶极系统的响应,以及在具有不同S波速度的慢地层中以低源频率运行的四极系统的响应。分析了时域中的相干速度/慢度关系(相似谱)以及来自声学LWD阵列接收器的这些波形信号的色散特性。这些分析表明,如果声学随钻测井仪正确集中并且在低频(低于3 kHz)下运行,则单极系统可以通过“泄漏” P波测量非常慢的地层的P波速度。同样,对于非常慢的地层,偶极系统可以通过泄漏的P波测量P波速度,并且可以从地层弯曲波测量S波速度。但是,在四极系统中,钻-干扰波的下限频率(截止频率)将降低至5 kHz,并且如果周围地层变得非常慢,且S波速度大约为10%,则可能不再被忽略。 500 m / s。

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