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Cased Borehole Effect On Downhole Seismic Measurements

机译:井下地震测量的套管钻孔效应

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摘要

Approximate and exact formulations are presented for the interaction of an incidentwave with a cased borehole. In the approximate method, the borehole coupling theoryis used to compute pressure in the fluid at a low frequency. The results are simpleand explicit. They are useful in the study of cased borehole coupling and as wellas borehole radiation. In the exact method, elastic potentials in each annulus arerepresented as a superposition of fundamental solutions to the Helmholtz equations.Continuity of displacements and stresses across layer boundaries are used to determineunknown coefficients. The global matrix method is employed to simultaneously computethese coefficients in individual layers. This method is advantageous over the Thomson Haskell propagator matrix method in handling evanescent waves. Our results show that,in a cased borehole, the borehole effects on downhole seismic measurements are moresignificant than those in an open borehole, especially when the formation is soft andthe casing is steel. For hard formations and frequency below 1 kHz, cased boreholeinfluence on downhole geophone measurement is minimal, while at high frequencies,large discrepancies occur, especially at grazing incidence. For soft formations, boththe pressure in the fluid and the solid displacement on the borehole wall show strongdependence on frequency and incidence angle, even at very low frequencies. Strongresonance occurs in the fluid for an SV incidence at angle δ = cos[superscript -1]β/C[subscript T] where CT is the tube wave velocity in a cased borehole. This resonance is prominent even at a very high frequency and large incidence angle because the tube wave velocity is raised well above the formation shear velocity by the steel pipe. This behavior is very different from that in an open borehole. At a particular angle of incidence of a plane P wave, the pressure in the fluid is near zero at low frequencies. This angle is dependent on the casing thickness and can be computed exactly. In general the casing behaves like a shield in such a way that the amplitude of both pressure in the fluid and solid motion on the borehole wall are reduced compared to those in an open borehole.
机译:给出了入射波与套管井相互作用的近似和精确公式。在近似方法中,井眼耦合理论用于计算低频流体中的压力。结果简单明了。它们可用于套管井眼耦合以及井眼辐射的研究。在精确方法中,每个环空中的弹性势表示为Helmholtz方程基本解的叠加。跨层边界的位移和应力的连续性用于确定未知系数。全局矩阵法用于同时计算各个层中的这些系数。该方法在处理e逝波方面优于Thomson Haskell传播矩阵方法。我们的结果表明,在有套管的井眼中,井眼对井下地震测量的影响比在裸眼井眼中更为明显,尤其是在地层较软且套管为钢的情况下。对于坚硬的地层和低于1 kHz的频率,套管对井下地震检波器测量的影响极小,而在高频下,会出现较大差异,尤其是在掠入射时。对于软地层,即使在非常低的频率下,流体压力和井壁上的固体位移都显示出对频率和入射角的强烈依赖性。 SV入射角为δ= cos [上标-1]β/ C [下标T]时,在流体中发生强共振,其中CT是套管井中的管波速度。即使在非常高的频率和较大的入射角下,该共振也很显着,因为管波速度远高于钢管引起的地层剪切速度。此行为与裸眼井孔的行为非常不同。在平面P波的特定入射角下,流体中的压力在低频下接近零。该角度取决于外壳厚度,可以精确计算。通常,套管的作用就像是一个屏蔽,与井壁中的流体相比,井壁中的流体压力和固体运动的振幅都减小了。

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