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Derivation of site-specific relationships between hydraulic parameters and p-wave velocities based on hydraulic and seismic tomography

机译:基于水力和地震层析成像法推导水力参数和p波速度之间的特定位置关系

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摘要

In this study, hydraulic and seismic tomographic measurements were used to derive a site-specific relationship between the geophysical parameter p-wave velocity and the hydraulic parameters, diffusivity and specific storage. Our field study includes diffusivity tomograms derived from hydraulic travel time tomography, specific storage tomograms, derived from hydraulic attenuation tomography, and p-wave velocity tomograms, derived from seismic tomography. The tomographic inversion was performed in all three cases with the Simultaneous Iterative Reconstruction Technique algorithm, using a ray tracing technique with curved trajectories. The experimental set up was designed such that the p-wave velocity tomogram overlaps the hydraulic tomograms by half. The experiments were performed at a well-characterized sand and gravel aquifer, located in the Leine River valley near Gottingen, Germany. Access to the shallow subsurface was provided by direct-push technology. The high spatial resolution of hydraulic and seismic tomography was exploited to derive representative site-specific relationships between the hydraulic and geophysical parameters, based on the area where geophysical and hydraulic tests were performed. The transformation of thep-wave velocities into hydraulic properties was undertaken using a k-means cluster analysis. Results demonstrate that the combination of hydraulic and geophysical tomographic data is a promising approach to improve hydrogeophysical site characterization.
机译:在这项研究中,使用水力和地震层析成像测量来得出地球物理参数p波速度与水力参数,扩散率和比存储之间的特定位置关系。我们的现场研究包括从水力行进时间层析成像法得到的扩散层析X线照片,从水力衰减层析成像法得到的特定存储层析X线照片和从地震层析成像法得到的P波速度层析X射线照片。在所有三种情况下,均采用同时迭代重建技术算法,使用具有弯曲轨迹的射线跟踪技术,进行了断层图像反演。设计实验装置时,p波速度断层图与水力断层图重叠一半。实验是在德国哥廷根附近的莱因河谷地一个特征明确的砂砾石含水层进行的。通过直接推入技术可以进入浅层地下。利用水力和地震层析成像的高空间分辨率,根据进行地球物理和水力测试的区域,得出水力和地球物理参数之间具有代表性的特定地点关系。使用k均值聚类分析进行了纵波速度向水力特性的转换。结果表明,水力和地球物理层析成像数据的组合是改善水文地球物理站点特征的一种有前途的方法。

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  • 来源
    《Water resources research》 |2012年第3期|p.W03531.1-W03531.14|共14页
  • 作者单位

    Department of Earth Sciences, ETH Zurich, Zurich, Switzerland;

    Department of Earth Sciences, ETH Zurich, Zurich, Switzerland Now at Earth Sciences Division, Lawrence Berkeley National Labora tory, Berkeley, California, USA;

    Department Monitoring and Exploration Technologies, Helmholtz Centre for Environmental Research, UFZ, Leipzig, Germany;

    Geoscientiflc Centre, University of Gottingen, Gottingen, Germany;

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