Bahrami Jovein E, Hosseini S M
Civil Engineering Department, Ferdowsi University of Mashhad, Mashhad, Iran.
Environ Monit Assess. 2017 Feb;189(2):81. doi: 10.1007/s10661-017-5795-8. Epub 2017 Jan 26.
The primary objective of this study was to provide a detailed framework to use the spatio-temporal kriging to model the spatio-temporal variations of salinity data and predict saltwater intrusion into freshwater aquifers in the vicinity of deserts. EC data, measured in extraction wells in the Mahvelat plain located in the Northeastern part of Iran, available from 2007 to 2013, were used to demonstrate the developed framework. The source of data was not a well-designed measurement network. Therefore, to homogenize the data, spatial analysis was used to find EC distribution in the area in each year of study. To conduct the spatial analysis, a guideline and a systematic process were developed to select an appropriate kriging method and optimize its parameters. This process can be applied to different variables. After spatial analysis of EC data for all the years of the analysis period using empirical Bayesian kriging (EBK) method with manually optimized parameters, spatio-temporal and corresponding variogram analysis was conducted using R software. This process was based on a separable product-sum model applied to the data from 2007 to 2012. The data of 2013 and the data available for the years 1999 and 2006 were used for evaluating the performance of the spatio-temporal model. The EC distribution maps, developed for different years until 2021, show a high level of EC in the north, south, and west of the study area and growing saltwater intrusion into the central freshwater aquifer. This result can be attributed to the over-exploitation of the aquifer and hydraulic head and gradient distribution in the area. The framework provided in this study for spatio-temporal analysis of unstructured EC data is useful for groundwater managers in making proper decisions.
本研究的主要目的是提供一个详细框架,以利用时空克里金法对盐度数据的时空变化进行建模,并预测沙漠附近淡水含水层的海水入侵情况。利用2007年至2013年期间在伊朗东北部马赫韦拉特平原的抽水井中测量的电导率(EC)数据来演示所开发的框架。数据来源并非精心设计的测量网络。因此,为了使数据均匀化,采用空间分析来确定研究各年份该区域的EC分布。为了进行空间分析,制定了一个指南和系统流程,以选择合适的克里金方法并优化其参数。该流程可应用于不同变量。在使用手动优化参数的经验贝叶斯克里金(EBK)方法对分析期内所有年份的EC数据进行空间分析之后,使用R软件进行了时空及相应的变差函数分析。此过程基于应用于2007年至2012年数据的可分离乘积和模型。2013年的数据以及1999年和2006年可用的数据用于评估时空模型的性能。直到2021年为不同年份绘制的EC分布图显示,研究区域的北部、南部和西部EC水平较高,并且中部淡水含水层的海水入侵情况不断加剧。这一结果可归因于该地区含水层的过度开采以及水头和梯度分布。本研究提供的用于非结构化EC数据时空分析的框架对地下水管理者做出恰当决策很有用。