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Torus-nuclear magnetic resonance: Quasicontinuous airborne magnetic resonance profiling by using a helium-filled balloon

机译:圆环核磁共振:使用充氦气球的准连续机载磁共振成像

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摘要

The application of surface nuclear magnetic resonance (NMR) measurements, although proven to be valuable for various hydrogeological issues, is in practice often limited to single 1D surveys because measurement progress is slow. First, large stacking rates are necessary to overcome the low signal-to-noise ratio and, second, time and effort are required to move the equipment and to place the measurement loops in the field. We have evaluated a novel approach to cope with the latter. We have assessed and tested a data acquisition scheme based on a torus-shaped helium-filled balloon carrying the loop and moving it rapidly from one to the next measurement position along the profile lines. We have referred to this system as Torus-NMR. We have showed the feasibility of the system to deliver reliable results using common processing and inversion. Surface NMR field data are acquired at successively overlapping positions along a test profile using the Torus-NMR system. To take advantage of the faster loop setup, the overall measurement time of the single NMR soundings is reduced by reducing the number of stacks, whereas the number of soundings is increased to obtain highly overlapping coverage. Regarding a single measurement position, a significant loss of vertical resolution must be accepted that can, however, be compensated to some extent by inverting the complete profile data set simultaneously using a laterally constrained inversion. We have found that for simple subsurface models, e.g., a layered earth with up to three layers, the proposed scheme provided reasonable results, which were demonstrated using synthetic and real field data. We do not expect the Torus-NMR concept to replace 2D data acquisition schemes if high spatial resolution is required. However, we expect fields of application that aim at rapid lateral overview of how specific hydrogeological parameters of shallow aquifers are distributed over large catchment-scale areas.
机译:尽管表面核磁共振(NMR)测量对各种水文地质问题具有重要价值,但由于测量进展缓慢,因此实际上通常仅限于单次一维测量。首先,需要大的堆叠率以克服低信噪比,其次,需要时间和精力来移动设备和将测量环路放置在现场。我们评估了一种应对后者的新颖方法。我们已经评估并测试了一种基于圆环形氦气气球的数据采集方案,该气球携带该环并将其沿着轮廓线从一个快速移动到下一个测量位置。我们将该系统称为Torus-NMR。我们已经展示了该系统使用常见处理和反演提供可靠结果的可行性。使用Torus-NMR系统在沿着测试轮廓的连续重叠位置获取表面NMR场数据。为了利用更快的环路设置,通过减少烟囱的数量来减少单个NMR探测的总测量时间,而增加探测的数量以获得高度重叠的覆盖范围。对于单个测量位置,必须接受显着的垂直分辨率损失,但是可以通过使用横向约束反演同时反演完整轮廓数据集来在一定程度上进行补偿。我们发现,对于简单的地下模型(例如,具有多达三层的分层地球),所提出的方案提供了合理的结果,已使用合成和实际数据进行了证明。如果需要高空间分辨率,我们不希望Torus-NMR概念取代2D数据采集方案。但是,我们期望以快速横向概述浅层含水层的特定水文地质参数如何在大面积集水区上分布为目标的应用领域。

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