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首页> 外文期刊>Engineering Geology >Spatial estimation of the thickness of low permeability topsoil materials by using a combined ordinary-indicator kriging approach with multiple thresholds
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Spatial estimation of the thickness of low permeability topsoil materials by using a combined ordinary-indicator kriging approach with multiple thresholds

机译:通过使用具有多个阈值的组合的普通指标克里格方法,对低渗透性表土材料的厚度进行空间估算

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摘要

Accurately estimating a spatial pattern of low permeability topsoil materials, such as clay, silt, and mud, is critical because these materials are a natural barrier to groundwater recharge and flow in subsurface engineering applications. This study determined the spatial distributions and thicknesses of low permeability topsoil materials in the Choushui River alluvial fan, Taiwan by using a combined ordinary indicator kriging (OIK) approach with multiple thresholds. The thicknesses were first estimated using ordinary kriging (OK). To reduce the overestimation of low values and underestimation of high values, indicator kriging (IK) was then adopted to probabilistically categorize the thickness of the materials. The maximum occurrence probability among the categories was selected for determining the most suitable thickness category of low permeability topsoil materials. Finally, the thicknesses of the materials estimated using OK were amended according to the upper and lower limits of the most suitable category determined using multi-threshold IK. The research results reveal that the combined OIK approach with multiple thresholds can reduce the overestimation of low values and underestimation of high values for various topsoil thicknesses and characterize a reliable hydrogeological pattern in topsoil. The approach facilitates evaluating groundwater recharge and constructing a numerical model of coupled surface water and groundwater flow. (C) 2016 Elsevier B.V. All rights reserved.
机译:准确估算低渗透性表土材料(例如粘土,淤泥和泥浆)的空间格局至关重要,因为这些材料是地下工程应用中地下水补给和流动的天然屏障。这项研究使用组合的具有多个阈值的普通指示克里格(OIK)方法,确定了台湾潮水河冲积扇中低渗透性表土材料的空间分布和厚度。首先使用普通克里金法(OK)估算厚度。为了减少对低值的高估和对高值的低估,然后采用指标克里金法(IK)对材料的厚度进行概率分类。选择类别中最大的发生概率,以确定最合适的低渗透性表土材料厚度类别。最后,根据使用多阈值IK确定的最合适类别的上限和下限,修改使用OK确定的材料的厚度。研究结果表明,结合多种阈值的OIK方法可以减少各种表土厚度对低值的高估和对高值的低估,并刻画出表土中可靠的水文地质模式。该方法有助于评估地下水的补给量,并建立耦合的地表水和地下水流量的数值模型。 (C)2016 Elsevier B.V.保留所有权利。

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