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Magnetic resonance sounding dataset of a hard-rock headwater catchment for assessing the vertical distribution of water contents in the subsurface

机译:硬岩水源流域的磁共振测深数据集用于评估地下含水量的垂直分布

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摘要

Magnetic Resonance Sounding (MRS) measurements are acquired at 16 stations in the Strengbach headwater catchment (Vosges Mountains – France). These data, rendering the vertical distribution of water contents in the subsurface, are used to show their potential in conditioning a hydrological model of the catchment, as described in the article “Magnetic resonance sounding measurements as posterior information to condition hydrological model parameters: Application to a hard-rock headwater catchment” – Journal of Hydrology (2020). Acquisition protocols follow a free induction decay scheme. Data are filtered by applying a band-pass filter at the Larmor frequency. A filter removing the 50 Hz noise is also applied with the exception of data at a Larmor frequency close to the 50 Hz harmonic. The signal envelopes are then fitted by a decaying exponential function over time to estimate the median characteristic relaxation time of each MRS sounding.
机译:在Strengbach上游流域(法国孚日山脉)的16个站进行了磁共振测深(MRS)测量。这些数据显示了地下含水量的垂直分布,用于显示它们在调节集水区水文模型中的潜力,如文章“磁共振测深作为条件信息来调节水文模型参数”所述:坚硬的源头流域” –水文学杂志(2020)。采集协议遵循自由感应衰减方案。通过在拉莫尔频率上应用带通滤波器来过滤数据。除拉莫尔频率接近50 Hz谐波的数据外,还应用了去除50 Hz噪声的滤波器。然后,信号包络通过随时间的衰减指数函数进行拟合,以估计每个MRS探测的中值特征弛豫时间。

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