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A Wavelet-based Seismogram Inversion Algorithm for the In Situ Characterization of Nonlinear Soil Behavior

机译:基于小波的地震波反演算法用于非线性土体行为的原位表征

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We present a full waveform inversion algorithm of downhole array seismogram recordings that can be used to estimate the inelastic soil behavior in situ during earthquake ground motion. For this purpose, we first develop a new hysteretic scheme that improves upon existing nonlinear site response models by allowing adjustment of the width and length of the hysteresis loop for a relatively small number of soil parameters. The constitutive law is formulated to approximate the response of saturated cohesive materials, and does not account for volumetric changes due to shear leading to pore pressure development and potential liquefaction. We implement the soil model in the forward operator of the inversion, and evaluate the constitutive parameters that maximize the cross-correlation between site response predictions and observations on ground surface. The objective function is defined in the wavelet domain, which allows equal weight to be assigned across all frequency bands of the non-stationary signal. We evaluate the convergence rate and robustness of the proposed scheme for noise-free and noise-contaminated data, and illustrate good performance of the inversion for signal-to-noise ratios as low as 3. We finally employ the proposed scheme to downhole array data, and show that results compare very well with published data on generic soil conditions and previous geotechnical investigation studies at the array site. By assuming a realistic hysteretic model and estimating the constitutive soil parameters, the proposed inversion accounts for the instantaneous adjustment of soil response to the level and strain and load path during transient loading, and allows results to be used in predictions of nonlinear site effects during future events.
机译:我们提出了井下阵列地震图记录的完整波形反演算法,可用于估计地震地面运动过程中的非弹性土行为。为此,我们首先开发了一种新的磁滞方案,该方案通过允许针对相对少量的土壤参数调整磁滞回线的宽度和长度来改进现有的非线性场地响应模型。制定本构定律,以近似饱和粘性材料的响应,并且不考虑由于剪切导致孔隙压力发展和潜在液化的体积变化。我们在反演的正向算子中实现土壤模型,并评估本构参数,以最大化场地响应预测与地面观测值之间的互相关性。目标函数在小波域中定义,它允许在非平稳信号的所有频带上分配相等的权重。我们评估了无噪声和受噪声污染的数据的拟议方案的收敛速度和鲁棒性,并说明了信噪比低至3时反演的良好性能。我们最后将拟议的方案用于井下阵列数据,并显示结果与已发表的有关一般土壤条件的数据以及阵列现场以前的岩土工程研究结果相比较非常好。通过假设一个实际的滞回模型并估计本构土参数,所提出的反演考虑了瞬时荷载过程中土壤对水平,应变和荷载路径的瞬时调节,并允许将结果用于未来的非线性场地效应预测事件。

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