Physical-chemical evaluation of groundwater quality in semi-arid areas: case study-Sabzevar plain, Iran

被引:16
作者
Panahi, Ghasem [1 ]
Eskafi, Mahya Hassanzadeh [1 ]
Rahimi, Hamidreza [2 ,3 ]
Faridhosseini, Alireza [1 ]
Tang, Xiaonan [4 ]
机构
[1] Ferdowsi Univ Mashhad, Fac Agr, Dept Water Sci & Engn, Mashhad, Razavi Khorasan, Iran
[2] Univ Liverpool, Sch Engn, 161 Brownlow Hill, Liverpool L69 3GH, Merseyside, England
[3] Hohai Univ, Yangtze Inst Conservat & Dev, Nanjing, Peoples R China
[4] Xian Jiaotong Liverpool Univ, Civil Engn Dept, Suzhou, Peoples R China
关键词
Groundwater; Drinking water; Agriculture; Water quality; Sustainable water management; GIS; DISTRICT; PATTERNS; BASIN;
D O I
10.1007/s40899-021-00576-y
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Groundwater is one of the most important water sources in arid and semi-arid areas. With the increasing world population and the water demand for agriculture and urban use, the need for water resources has increased, especially in arid and semi-arid regions, where groundwater resources play a significant role. To prevent the pollution of groundwater resources, various studies for their preservation and maintenance should be carried out, including a detailed plan for proper management of water resources and establishing a balance between water quality and how to use them. It becomes important to understand the spatial change of the quality of groundwater resources. In this study, Sabzevar plain, a typical region of semi-arid climate in Iran, was selected as a case study to assess the groundwater quality of the region, using data from 24 observation wells between 2015 and 2019. Using Arc GIS software, a map of groundwater quality parameters in the study area was prepared for quality assessment and comparison with existing international standards. The results showed that (except pH and HCO3-) the concentration of Sodium, Magnesium, and other anions and cations is higher than the corresponding WHO standard limit, suggesting that the study area is unsuitable for drinking and agricultural use. According to the Wilcox chart, 87.5% of the samples are in the C4S4 class while 8.33% are in the C4S3 class, showing the groundwater unsuitable for agricultural use due to its high salinity and alkalinity. Piper diagrams show that more than 50% of the samples are non-carbonate alkalis, indicating a very high salinity in the area. According to the pie chart, chlorine ion and sodium ion are the dominant anions and cations in the Sabzevar plain, respectively. The Schuler diagram shows that none of the samples examined were in a good class for drinking. Therefore, considering the importance of water for agricultural activities in the study area, it is recommended to have agricultural management solutions to prevent groundwater mixing with freshwater resources.
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页数:15
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