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Geostatistical interpolation model selection based on ArcGIS and spatio-temporal variability analysis of groundwater level in piedmont plains northwest China

机译:基于ArcGIS的地统计学插值模型选择和西北山前平原地下水位的时空变异性分析

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摘要

Based on the geo-statistical theory and ArcGIS geo-statistical module, datas of 30 groundwater level observation wells were used to estimate the decline of groundwater level in Beijing piedmont. Seven different interpolation methods (inverse distance weighted interpolation, global polynomial interpolation, local polynomial interpolation, tension spline interpolation, ordinary Kriging interpolation, simple Kriging interpolation and universal Kriging interpolation) were used for interpolating groundwater level between 2001 and 2013. Cross-validation, absolute error and coefficient of determination (R2) was applied to evaluate the accuracy of different methods. The result shows that simple Kriging method gave the best fit. The analysis of spatial and temporal variability suggest that the nugget effects from 2001 to 2013 were increasing, which means the spatial correlation weakened gradually under the influence of human activities. The spatial variability in the middle areas of the alluvial–proluvial fan is relatively higher than area in top and bottom. Since the changes of the land use, groundwater level also has a temporal variation, the average decline rate of groundwater level between 2007 and 2013 increases compared with 2001–2006. Urban development and population growth cause over-exploitation of residential and industrial areas. The decline rate of the groundwater level in residential, industrial and river areas is relatively high, while the decreasing of farmland area and development of water-saving irrigation reduce the quantity of water using by agriculture and decline rate of groundwater level in agricultural area is not significant.
机译:基于地统计学理论和ArcGIS地统计学模块,利用30个地下水位观测井的数据估算了北京山前地区地下水位的下降情况。在2001年至2013年之间,对地下水位进行了7种不同的插值方法(反距离加权插值,全局多项式插值,局部多项式插值,张力样条插值,普通Kriging插值,简单Kriging插值和通用Kriging插值)。交叉验证,绝对误差和测定系数(R 2 )用于评估不同方法的准确性。结果表明,简单的克里格方法最适合。对空间和时间变异性的分析表明,2001年至2013年的金块效应正在增加,这意味着空间相关性在人类活动的影响下逐渐减弱。冲积洪积扇的中间区域的空间变异性相对高于顶部和底部区域。由于土地利用的变化,地下水位也随时间变化,与2001-2006年相比,2007年至2013年之间的地下水位平均下降速度有所提高。城市发展和人口增长导致对居民区和工业区的过度开发。住宅,工业和河流地区的地下水位下降率相对较高,而农田面积的减少和节水灌溉的发展减少了农业用水量,而农业地区的地下水位下降率却没有重大。

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