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Improved crosshole radar tomography by using direct and reflected arrival times

机译:通过使用直接和反射的到达时间来改善跨孔雷达层析成像

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Traveltime tomography by inverting direct arrival times is the most common technique in crosshole radar surveying. In a standard crosshole experiment, the inversion is a mathematically nonunique process due to the limited range of viewing angles producing ambiguous and smeared results. If possible, additional information should be extracted from the data or added from the outside to improve and constrain the inversion and the interpretation. In low attenuation media, reflected wave energy can also be present in the crosshole data. Reflections are often caused by well-known interfaces, such as the free earth surface or the groundwater table. Because of their differing travel paths, these reflected events contain additional information about subsurface structure and parameter distribution. We present a technique to include reflection traveltimes associated with known interfaces into tomographic traveltime inversion of crosshole radar data. If in a crosshole radar survey such reflections can be clearly identified, the total number of rays and the range of raypath angles are increased by the presented inversion strategy. Applications to a synthetic and a real field data set show the practicability and the improvements offered by this method. The results show that horizontal smearing is reduced and local anomalies are better contoured compared to standard crosshole tomography using only direct arrivals. (C) 2001 Elsevier Science BN, All rights reserved. [References: 21]
机译:通过反转直接到达时间进行的行进时间层析成像是井间雷达测量中最常用的技术。在标准的交叉孔实验中,由于视角范围有限而产生模棱两可和模糊的结果,因此反演在数学上是不唯一的过程。如果可能,应该从数据中提取其他信息,或者从外部添加其他信息,以改善和限制反演和解释。在低衰减介质中,反射波能量也可能存在于井眼数据中。反射通常是由众所周知的界面引起的,例如自由地球表面或地下水位。由于它们的传播路径不同,这些反射事件包含有关地下结构和参数分布的其他信息。我们提出一种技术,将与已知接口相关的反射传播时间包括到井间雷达数据的层析传播时间反演中。如果在井间雷达勘测中可以清楚地识别出这种反射,则通过提出的反演策略可以增加射线总数和射线路径角度范围。在合成和实地数据集上的应用表明了该方法的实用性和改进。结果表明,与仅使用直接到达的标准井眼层析成像相比,水平涂抹减少了,局部异常的轮廓更好。 (C)2001 Elsevier Science BN,保留所有权利。 [参考:21]

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