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Spatial and Temporal Groundwater Level Variation Geostatistical Modeling in the City of Konya, Turkey

机译:土耳其科尼亚市的时空地下水位变化地统计模型

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摘要

Groundwater is one of the most important resources used for drinking and utility and irrigation purposes in the city of Konya, Turkey, as in many areas. The purpose of this study is to evaluate spatial and temporal changes in the level of groundwater by using geostatistical methods based on data from 91 groundwater wells during the period 1999 to 2003. Geostatistical methods have been used widely as a convenient tool to make decisions on the management of groundwater levels. To evaluate the spatial and temporal changes in the level of the groundwater, a vector-based geographic information system software package, ArcGIS 9.1 (Environmental Systems Research Institute, Redlands, California), was used for the application of an ordinary kriging method, with cross-validation leading to the estimation of groundwater levels. The average value of variogram (spherical model) for the spatial analysis was approximately 2150 m. Results of ordinary kriging for groundwater level drops were underestimated by 17%. Cross-validation errors were within an acceptable level. The kriging model also helps to detect risk-prone areas for groundwater abstraction.
机译:在许多地区,地下水是土耳其科尼亚市用于饮用水,公用事业和灌溉目的的最重要资源之一。这项研究的目的是基于1999年至2003年期间91口地下水井的数据,采用地统计方法评估地下水位的时空变化。地统计学方法已被广泛用作方便的决策依据。地下水位管理。为了评估地下水位的时空变化,使用了基于矢量的地理信息系统软件包ArcGIS 9.1(加利福尼亚州雷德兰兹的环境系统研究所),将其应用于普通的克里格法。 -验证导致对地下水位的估计。空间分析的变异函数(球形模型)的平均值约为2150 m。普通克里金法对地下水位下降的结果被低估了17%。交叉验证错误在可接受的范围内。克里金模型也有助于检测容易发生地下水抽取的区域。

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