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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Fast 3D multichannel deconvolution of electromagnetic induction loop-loop apparent conductivity data sets acquired at low induction numbers
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Fast 3D multichannel deconvolution of electromagnetic induction loop-loop apparent conductivity data sets acquired at low induction numbers

机译:快速3D多通道解卷积的电磁感应回路循环表观电导率数据集在低感应号中获取

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摘要

Electromagnetic induction (EMI) sensors using sufficiently low-frequency harmonic sources and sufficiently small loop separations operate in the low-induction-number (LIN) domain for a relatively wide range of background conductivity. These systems are used in diverse near-surface investigations including applications from soil sciences, hydrology, and archaeology. The special case of portable multiconfiguration EMI sensors operating at frequencies = 20 kHz offers the possibility of using a fast linear deconvolution method to interpret multichannel data sets in three dimensions. Here, we have developed a fast 3D inversion/deconvolution method regularized with 3D smoothness constraints and formulated in the hybrid spectral-spatial domain. Compared with other linear approaches, the spectral-spatial domain formulation significantly reduces the computational cost of the processing and opens the door for real-time 3D interpretation of large data sets consisting of more than 100,000 data points. First, we test our proposed algorithm on synthetic data sets computed with the full Maxwell theory. Then, we apply our method to a real four-configuration EMI data set acquired to map the thickness of peat layers embedded in a sandy environment. For the synthetic and the field example, we compared our result with the result obtained using a standard point-by-point 1D nonlinear inversion approach. This comparison demonstrates that the proposed methodology provides superior lateral resolution compared with the 1D nonlinear inversion, at the same time significantly reducing the computational cost of the processing.
机译:电磁感应(EMI)传感器使用足够低频谐波源和足够小的环路分离在低感应 - 数(LIN)域中操作,以进行相对宽的背景电导率。这些系统用于不同的近表面调查,包括土壤科学,水文和考古学的应用。在频率下操作的便携式多组件EMI传感器的特殊情况& 20 kHz提供了使用快速线性解卷积方法来解释三维的多声道数据集的可能性。在这里,我们开发了一种用3D平滑度约束进行规范的快速3D反转/解卷积方法,并配制在混合谱 - 空间域中。与其他线性方法相比,光谱空间域制剂显着降低了处理的计算成本,并打开了由大于100,000多个数据点组成的大数据集的实时3D解释门。首先,我们在用全麦克斯韦理论计算的合成数据集上测试所提出的算法。然后,我们将我们的方法应用于真正的四配置EM​​I数据集以映射嵌入沙质环境中的泥炭层的厚度。对于合成和领域示例,我们将结果与使用标准点逐1D非线性反转方法获得的结果进行了比较。该比较表明,与1D非线性反转相比,该方法提供了卓越的横向分辨率,同时显着降低了处理的计算成本。

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