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Data-driven Methods for Solving Large-scale Inverse Problems with Applications to Subsurface Imaging

机译:数据驱动方法解决大规模反问题及其在地下成像中的应用

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Seismic full-waveform inversion is a typical non-linear and ill-posed large-scale inverse problem. It is an important and widely used geophysical exploration method to obtain subsurface structures. The existing computational methods for solving full-waveform inversion are not only computationally expensive but also yield low-resolution results because of the ill-posedness and cycle skipping issues of full-waveform inversion. To resolve those issues, we employ machine-learning techniques to solve the full-waveform inversion. Specifically, we focus on applying convolutional neural network˜(CNN) to directly derive the inversion operator so that the velocity structure can be obtained without knowing the forward operator. We build a convolutional neural network with an encoder-decoder structure to model the correspondence from seismic data to subsurface velocity structures. To evaluate the performance of our inversion technique, we compare it to both existing physics-driven methods and other data-driven methods. Our numerical examples using synthetic seismic reflection data show that our CNN model significantly improves the accuracy of the velocity inversion while the computational time is reduced. Through numerical tests, we also study the robustness of our CNN model and show that our model yields some weak generalization ability.
机译:地震全波形反演是一个典型的非线性且不适定的大规模反演问题。它是获取地下构造的重要且广泛使用的地球物理勘探方法。解决全波形反演的现有计算方法不仅计算量大,而且由于全波形反演的不适定性和周期跳跃问题,还会产生低分辨率的结果。为了解决这些问题,我们采用了机器学习技术来解决全波形反演。具体而言,我们专注于应用卷积神经网络(CNN)直接推导反演算子,从而在不了解正演算子的情况下获得速度结构。我们建立了具有编码器-解码器结构的卷积神经网络,以建模从地震数据到地下速度结构的对应关系。为了评估我们的反演技术的性能,我们将其与现有的物理驱动方法和其他数据驱动方法进行了比较。我们使用合成地震反射数据的数值示例表明,我们的CNN模型显着提高了速度反演的精度,同时减少了计算时间。通过数值测试,我们还研究了CNN模型的鲁棒性,并表明我们的模型具有较弱的泛化能力。

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