The Performance of Several Current Interpolation Methods for Variability of cations in Groundwater in Esfarayen Plain, Iran: A Case Study

A. Mahmoodnia, Morteza Mousavi, Farshad Golbabaei Kootenaei, M. Asadi-Ghalhari
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Abstract

Acquiring information about groundwater quality is essential in developing management strategies. In this article, spatio-temporal variations of cations in groundwater in Esfarayen plain were investigated using data monitored in 134 groundwater wells, active in 1988, and 47 wells, active in 2019. To evaluate groundwater quality, interpolation methods have been used to interpolate existing limited spatial data. The performance of 8 current interpolation methods on the data for the two selected years (1988 and 2019) was compared. Finding the optimum interpolation method for the considered groundwater quality parameters is essential. Cross-validation and three indexes of R2, mean absolute error (MAE), and root mean square error (RMSE) were used to compare the performance of the methods. By identifying universal kriging (UK) and global polynomial interpolation (GPI) methods as the optimum methods and using those for the selected years (1988 and 2019), spatial variation of the concentration of cations in groundwater across the plain has been presented. In 1988, the maximum concentration of the cations occurred in the southwest of the plain (about 80 mg/L), and the minimum concentration of the cations was observed in the northwest of the plain (approximately 8 mg/L). Similarly, in 2019, the highest concentration of the cations was found in the southwest of the plain (almost 64 mg/L), and its lowest concentration was observed in the northeast of the plain (roughly 13 mg/L). Moreover, temporal variations of the concentration of cations in groundwater from 1988 to 2019 have also been presented. The concentration of the cations increased by approximately 23 mg/L in the northwest and decreased to about 37 mg/L in the southwest of the study area from 1988 through 2019. According to the results, changes in the quality of groundwater are a complex problem and it is necessary to adopt proper strategies to reduce its adverse effects.
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伊朗Esfarayen平原地下水阳离子变化的几种电流插值方法的性能:一个案例研究
获取有关地下水质量的信息对于制定管理战略至关重要。在本文中,使用1988年活跃的134口地下水井和2019年活跃的47口水井的监测数据,调查了Esfarayen平原地下水中阳离子的时空变化。为了评估地下水质量,插值方法已被用于对现有的有限空间数据进行插值。比较了当前8种插值方法对所选两年(1988年和2019年)数据的性能。为所考虑的地下水质量参数找到最佳插值方法是至关重要的。交叉验证和R2、平均绝对误差(MAE)和均方根误差(RMSE)三个指标用于比较两种方法的性能。通过将通用克里格法(UK)和全局多项式插值法(GPI)确定为最佳方法,并使用选定年份(1988年和2019年)的方法,呈现了平原地下水中阳离子浓度的空间变化。1988年,阳离子的最大浓度出现在平原的西南部(约80 mg/L),而阳离子的最小浓度出现在该平原的西北部(约8 mg/L)。同样,2019年,在平原西南部发现了最高浓度的阳离子(约64 mg/L),在平原东北部观察到了最低浓度(约13 mg/L)。此外,还介绍了1988年至2019年地下水中阳离子浓度的时间变化。从1988年到2019年,研究区域西北部的阳离子浓度增加了约23 mg/L,西南部的阳离子含量降至约37 mg/L。根据研究结果,地下水水质的变化是一个复杂的问题,有必要采取适当的策略来减少其不利影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Avicenna Journal of Environmental Health Engineering
Avicenna Journal of Environmental Health Engineering Environmental Science-Health, Toxicology and Mutagenesis
CiteScore
1.00
自引率
0.00%
发文量
8
审稿时长
8 weeks
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