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首页> 外文期刊>Canadian journal of earth sciences >Using a multiple variogram approach to improve the accuracy of subsurface geological models
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Using a multiple variogram approach to improve the accuracy of subsurface geological models

机译:使用多变形仪方法来提高地下地质模型的准确性

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Subsurface geological models are often used to visualize and analyze the nature, geometry, and variability of geologic and hydrogeologic units in the context of groundwater resource studies. The development of three-dimensional (3D) subsurface geological models covering increasingly larger model domains has steadily increased in recent years, in step with the rapid development of computing technology and software, and the increasing need to understand and manage groundwater resources at the regional scale. The models are then used by decision makers to guide activities and policies related to source water protection, well field development, and industrial or agricultural water use. It is important to ensure that the modelling techniques and procedures are able to accurately delineate and characterize the heterogeneity of the various geological environments included within the regional model domain. The purpose of this study is to examine if 3D stratigraphic models covering complex Quaternary deposits can be improved by splitting the regional model into multiple submodels based on the degree of variability observed between surrounding data points and informed by expert geological knowledge of the geological–depositional framework. This is demonstrated using subsurface data from the Paris Moraine area near Guelph in southern Ontario. The variogram models produced for each submodel region were able to better characterize the data variability, resulting in a more geologically realistic interpolation of the entire model domain as demonstrated by the comparison of the model output with preexisting maps of surficial geology and bedrock topography as well as depositional models for these complex glacial environments. Importantly, comparison between model outputs reveals significant differences in the resulting subsurface stratigraphy, complexity, and variability, which would in turn impact groundwater flow model predictions.
机译:地下地质模型通常用于在地下水资源研究的背景下可视化和分析地质和水文地质单位的性质,几何形状和变异性。近年来,覆盖了越来越大的模型域的三维(3D)地质地质模型的发展,在计算技术和软件的快速发展中,近年来稳步增加,并且越来越需要了解和管理区域规模的地下水资源。决策者使用该模型来指导与源防水,井场开发和工业或农业用水相关的活动和政策。重要的是要确保建模技术和程序能够准确地描绘并表征区域模型结构域内的各种地质​​环境的异质性。本研究的目的是检查是否通过将区域模型分成周围数据点之间观察到的可变性程度并由地质沉积框架的专家地质知识通知,可以改善覆盖复杂的第四室沉积物的3D地层模型。 。这是使用来自安大略省南部Guelph附近的巴黎冰碛区的地下数据来证明。为每个子模型区域产生的变形仪模型能够更好地表征数据变异性,从而通过对结构地质和基岩地形的预先存在的映射映射的模型输出的比较来实现整个模型域的更加地质逼真的插值。这些复杂冰川环境的沉积模型。重要的是,模型输出之间的比较揭示了所产生的地下地层,复杂性和可变性的显着差异,这将反过来影响地下水流模型预测。

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