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Solving 1-D inverse problems by Chebyshev polynomial expansion

机译:用Chebyshev多项式展开法求解一维反问题

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Seismic wave propagation described by differential equations with variable coefficients may be solved by the Chebyshev polynomial expansion method (CPEM). This method approximates a model and forward solutions by orthonormal Chebyshev polynomials. The CPEM provides an alternative to the usual formulation. In CPEM, the model is approximated globally and the forward solutions can explicitly depend on the parameters of the model. The former ensures that a smooth model is produced by inversion. The latter produces partial derivatives of the forward solutions directly with respect to the model parameters, which streamlines the inversion and also gives a quantitative tool for determining the feasibility of inversion in the presence of noise (by singular value decomposition). Two examples of inversion demonstrate the potential of the CPEM. The first is nonlinear inversion for velocity and density using borehole SH-wave data. The second is linear inversion for interval velocities from rms velocity data. Estimation of interval velocity from stacking velocity is illustrated using field data from the Gulf of Mexico.
机译:由具有可变系数的微分方程描述的地震波传播可以通过Chebyshev多项式展开法(CPEM)求解。该方法近似模型并通过正交切比雪夫多项式正解。 CPEM提供了通常配方的替代方法。在CPEM中,模型是全局近似的,正向解可以显式依赖于模型的参数。前者确保通过反演产生平滑模型。后者直接针对模型参数生成正解的偏导数,这简化了反演,还提供了一种定量工具,用于确定存在噪声(通过奇异值分解)进行反演的可行性。反演的两个例子证明了CPEM的潜力。首先是利用井下SH波数据对速度和密度进行非线性反演。第二个是均方根速度数据的区间速度线性反演。使用来自墨西哥湾的现场数据说明了根据叠加速度估算间隔速度。

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