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A novel velocity prediction approach in double-porosity media using the Biot-Rayleigh theory

机译:双型瑞利理论的双孔隙介质中的一种新型速度预测方法

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Wave propagation induces local fluid flow (LFF) between the inclusions and the host media due to their dissimilar compressibilities. LFF mechanism is the dominate theory on explaining the velocity dispersion and attenuation. In general, it can be well characterized by the Biot-Rayleigh theory in the case of double-porosity media. However, the obtained dry rock bulk modulus is not accurate enough for the specific high fluctuation media, in which the compressibilities of inclusion and host media are significantly different. In this paper, a modified approach for obtain dry rock bulk modulus is proposed on the basis of the original Biot-Rayleigh theory in double-porosity media. It is worth noting that equivalent stress is replaced by equivalent strain in our proposed approach. This modified method is employed to model the frequency-dependent P- and S-wave velocities and attenuation, and its comparison with Pride's theory proves the feasibility of the proposed theory. We utilize a measured well data to demonstrate the accuracy of the predicted P- and S-wave velocities of different frequency bands using the proposed theory.
机译:由于其不同的压缩,波传播引起夹杂物和主介质之间的局部流体流动(LFF)。 LFF机制是解释速度分散和衰减的主导理论。通常,在双孔隙介质的情况下,可以很好地表征Biot-rayleigh理论。然而,对于特定的高波动介质,所获得的干式岩石体积模量不够准确,其中包含夹杂物和宿主介质的压缩性显着不同。本文基于双孔隙介质中的原始BIOT-RAYLEIGH理论提出了一种改进的方法,用于获得干燥岩体模量。值得注意的是,在我们提出的方法中,等效应力被等效应变取代。这种改进的方法用于模拟频率依赖性的P和S波速度和衰减,与骄傲的理论的比较证明了提出的理论的可行性。我们利用测量的井数据来展示使用所提出的理论的预测P和S波速度的准确性。

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