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Quality improvement of crosshole georadar tomography: pre- and post-inversion data analysis strategies

机译:井孔地雷达层析成像的质量改进:反演前后的数据分析策略

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摘要

Input data of georadar tomographic inversion can be contaminated by systematic errors involved in data acquisition and preparation. Such errors are caused by mislocations of the antennas (e.g., unrecognised borehole deviation), traveltime delay problems or unconsidered anisotropy of the medium. If they are not recognised and not eliminated they may produce severe artifacts in the tomograms leading to misinterpretation of the results. However, specific errors produce significant anomalies in certain plotting schemes and certain artificial structures in the reconstructed geophysical parameter distributions. This is demonstrated using purposely contaminated synthetic data sets. These synthetic data examples illustrate how certain systematic errors, e.g., unrecognised borehole deviation, can be identified and distinguished from the expected real subsurface structure. Furthermore, a field experiment is presented carried out for fracture and void detection in a limestone formation, where such consequent data analysis helped to identify and remove discrepancies in the data. Tomographic results were clearly improved showing a more reliable and consistent behaviour. The field and synthetic data examples and calculations show that careful pre- and post-inversion analysis and handling of tomographic georadar data lead to a quality increase and to more reliable results.
机译:地雷达断层扫描反演的输入数据可能会被数据采集和准备过程中涉及的系统错误所污染。此类错误是由于天线的位置不正确(例如,无法识别的井眼偏差),传播时间延迟问题或未考虑到的介质各向异性引起的。如果无法识别并消除它们,则它们可能会在断层图中产生严重的伪像,从而导致对结果的误解。然而,在重建的地球物理参数分布中,特定误差会在某些绘图方案和某些人工结构中产生明显的异常。使用故意污染的合成数据集可以证明这一点。这些合成数据示例说明了如何识别和识别某些系统误差(例如,无法识别的井眼偏差)并将其与预期的真实地下构造相区别。此外,还进行了现场试验,以检测石灰岩地层中的裂缝和孔隙,在这种结果分析中,数据分析有助于识别和消除数据差异。断层扫描结果明显改善,表现出更加可靠和一致的行为。现场数据和合成数据示例与计算结果表明,对断层地质雷达数据进行仔细的反演前后分析和处理可提高质量,并获得更可靠的结果。

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