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首页> 外文期刊>Journal of Science and Technology of Agriculture and Natural Resources >The Effects of Constructing Irrigation and Drainage Network of Rajaei Dam on Spatial and Temporal Changes of Groundwater Quality and Quantity
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The Effects of Constructing Irrigation and Drainage Network of Rajaei Dam on Spatial and Temporal Changes of Groundwater Quality and Quantity

机译:拉惹水坝建设排灌网对地下水水质和水量时空变化的影响

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Construction of a dam in the upstream of Tajan basin, as one of the human activities in order to provide drinking water, hydropower, agriculture, flood control or other purposes, can be effective on other sectors such as water resources. The purpose of this study is investigating the impact of Rajaei dam on groundwater resources in Sari-Neka plain during 26 years period (1985-2011) using geostatistical method, parametric and non-parametric tests. The results of statistical tests showed that groundwater table variation during 26 years has experienced insignificant upward trend. Quality factors such as EC, TDS, TH, Cl, SO4, Mg, Na and SAR had significant downward trend at 5% confidence level for Pearson and Kendall test. The Quality changes of groundwater resources in the region had good condition due to construction of dam. The results of spatial analysis for the study area using Kriging interpolation method in the three years for 1985, 1999, 2011 showed that in 1999 (the year of exploitation of the dam) most of the quality factors had reached the highest level from 1985 until the dam operation (1999) and then decreased to 2011. The results of this study showed that, agricultural activities after dam construction, operation of irrigation system and drainage network design of Rajaei dams, have raised the water table in northern part of the region and consequently had a significant impact on the quality of water resources.
机译:为了提供饮用水,水力发电,农业,防洪或其他目的,在塔詹盆地上游建造水坝是人类活动之一,这对水资源等其他部门也可能是有效的。本研究的目的是使用地统计方法,参数和非参数检验方法研究拉吉大坝对Sari-Neka平原在26年期间(1985-2011年)地下水资源的影响。统计测试结果表明,26年的地下水位变化没有明显的上升趋势。对于Pearson和Kendall检验,EC,TDS,TH,Cl,SO4,Mg,Na和SAR等质量因子在5%置信度下均具有显着下降趋势。由于大坝的建设,该地区地下水资源的质量变化状况良好。 1985年,1999年和2011年这三年中使用Kriging插值法对研究区域进行的空间分析结果表明,在1999年(大坝开发之年)中,大部分质量因子从1985年到2007年达到最高水平。大坝运行(1999年),然后下降到2011年。该研究结果表明,大坝建设后的农业活动,Rajaei大坝的灌溉系统运行和排水网络设计提高了该地区北部的地下水位,因此对水资源质量产生了重大影响。

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