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首页> 外文期刊>Environmental Geology >Geostatistical method to delineate anomalies of multi-scale spatial variation in hydrogeological changes due to the ChiChi earthquake in the ChouShui River alluvial fan in Taiwan
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Geostatistical method to delineate anomalies of multi-scale spatial variation in hydrogeological changes due to the ChiChi earthquake in the ChouShui River alluvial fan in Taiwan

机译:地统计学方法描述台湾潮水冲积扇赤池地震引起的水文地质变化的多尺度空间变化异常

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This study uses Ordinary Kriging (OK), Sequential Gaussian Simulation (SGS) and Simulated Annealing Simulation (SAS) to relocate the completely heterotopic dataset from the locations of the Standardized Satellite Oriented Control Point System (SSOCPS) stations to the Groundwater Monitoring Networks (GMNS) stations and factorial kriging to analyze and map relationships among seven variables, including the hydraulic conductivities of three aquifers, the vertical displacements of the ground and groundwater level changes in the wells of three aquifers, and also to delineate the anomalies of multi-scale spatial variation of hydrogeological properties associated with the ChiChi earthquake, measuring 7.3 on the Richter scale, in the ChouShui River alluvial fan in Taiwan. In this study, the anomalies of spatial variation of hydrogeological properties associated with the earthquake are illustrated at micro, local and regional scales of 9, 12 and 36 km, respectively. In the study area, regionalization components associated with variation at local and regional scales are obtained and mapped by factorial kriging. Factorial Kriging Analysis (FKA) also demonstrated that the main effects of the ChiChi earthquake on the spatial variations of groundwater hydrological changes include porous media compression at micro scale, hydrogeological heterogeneousness of the sediments within the aquifer at local scale and the cyclic loading of deviatoric stress at regional scale. Finally, maps of spatial variations of regional components fully depicted all of the anomalies of spatial variation of hydrogeological changes due to the ChiChi earthquake and can be used to identify, confirm and monitor the hydrogeological properties in this study area.
机译:这项研究使用普通克里金法(OK),顺序高斯模拟(SGS)和模拟退火模拟(SAS)将完全异位数据集从标准卫星定向控制点系统(SSOCPS)站的位置迁移到地下水监测网络(GMNS) )和阶乘克里金法来分析和绘制7个变量之间的关系,包括三个含水层的水力传导率,三个含水层井中地下水的垂直位移和地下水位变化,以及描绘多尺度空间异常台湾潮水河冲积扇中与ChiChi地震有关的水文地质特性的变化(以里氏7.3级测量)。在这项研究中,分别在9、12和36 km的微观,局部和区域尺度上说明了与地震有关的水文地质特征的空间变化异常。在研究区域中,获得了与局部和区域尺度上的变化相关的区域化成分,并通过阶乘克里格法进行了制图。阶乘克里格分析(FKA)还表明,ChiChi地震对地下水水文变化空间变化的主要影响包括微观尺度上的多孔介质压缩,局部尺度下含水层内沉积物的水文地质非均质性和偏应力的周期性荷载在区域范围内。最后,区域组成部分的空间变化图充分描述了由于ChiChi地震引起的水文地质变化的所有空间变化异常,可用于识别,确认和监测该研究区的水文地质特性。

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