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Use of four-dimensional ground penetrating radar and advanced visualization methods to determine subsurface fluid migration

机译:使用四维地面穿透雷达和先进的可视化方法来确定地下液体迁移

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摘要

Four-dimensional (4D) or time-lapse three-dimensional (3D) ground penetrating radar surveys can be used to monitor and image subsurface fluid flow. This information can be used to create a model of hydrogeological properties. The massive amount of data, which is present in and can possibly be generated from 4D GPR data sets, precludes a manual interpretation. Consequently, 4D data sets have to be processed and visualized in a way that extracts models and allows for data visualization in a semi-automatic way. The principles behind such an approach are applied to the Borden data set, which is used to demonstrate how advanced visualization can assist in the interpretation of raw and processed data. In the Borden data set, changes in reflectivity between different time-steps unveil areas of fluid migration in three dimensions. The combination of these reflectivity changes (between different combinations of the 3D subsets of the 4D data set) is used to create a model of hydrogeological properties. While this model does not yield a quantitative description of porosity, permeability or hydraulic conductivity, it is a qualitative proxy for a combination of these properties. (C) 2000 Elsevier Science B.V. All rights reserved. [References: 11]
机译:四维(4D)或延时三维(3D)接地穿透雷达调查可用于监测和图像地下流体流动。该信息可用于创建水文地质性质的模型。存在的大量数据,它可以从4D GPR数据集生成,排除了手动解释。因此,必须以提取模型的方式处理和可视化4D数据集并允许以半自动方式进行数据可视化。这种方法背后的原则应用于Borden数据集,用于演示高级可视化可以帮助解释原始和处理数据的解释。在Borden数据集中,不同时间步骤之间的反射率的变化揭示了三维流体迁移区域。这些反射率变化的组合(在4D数据集的3D子集的不同组合之间)用于产生水文地质性质的模型。虽然该模型不产生孔隙率,渗透性或液压导电性的定量描述,但是对于这些性质的组合是一种定性代理。 (c)2000 Elsevier Science B.V.保留所有权利。 [参考:11]

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