首页> 外文期刊>Journal of African Earth Sciences >Long term groundwater balance and water quality monitoring in the eastern plains of Urmia Lake, Iran: A novel GIS based low cost approach
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Long term groundwater balance and water quality monitoring in the eastern plains of Urmia Lake, Iran: A novel GIS based low cost approach

机译:伊朗乌尔米亚湖东部平原的长期地下水平衡和水质监测:基于GIS的新型低成本方法

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摘要

Groundwater quality and quantity are two major challenges in arid and semi-arid regions, due to their critical roles in sustainable agricultural development. Irrigated lands are spread all over Urmia Lake's surrounding plains in Iran. Due to the risk of saltwater intrusion as a result of over-exploitation from groundwater resources, it is important to monitor the groundwater quality and quantity through time and space. In this paper, the groundwater quantity was assessed over 11 years applying a novel groundwater balance estimation method based on water table data and 3D modeling; groundwater quality were monitored over 10 years using GIS and geostatistics; and the saltwater intrusion were investigated through generated quality maps and regression analysis. Results indicate that the groundwater balance was negative during the study period. Furthermore, the aquifers quality decreased over the study period, which was severe in west and southwest of the study area. The saltwater intrusion was proved and salty water was spread from west to other zones. The saltwater intrusion into aquifers increased electrical conductivity, chloride and sodium concentrations and will cause many ecological and agricultural problems. The novel and practicable approach utilized for groundwater balance quantitative assessment is suitable for countries lacking hydrological properties databases.
机译:由于其在可持续农业发展中的关键作用,地下水的质量和数量是干旱和半干旱地区的两个主要挑战。灌溉土地遍及伊朗Urmia湖周围的平原。由于地下水资源过度开采而导致咸水入侵的风险,因此在时间和空间上监控地下水的质量和数量非常重要。本文基于地下水位数据和3D建模,采用一种新颖的地下水平衡估算方法对11年间的地下水量进行了评估。使用GIS和地统计学方法对地下水质量进行了10年的监测;通过生成的质量图和回归分析研究了盐水入侵。结果表明,在研究期间地下水平衡为负。此外,在研究期间,含水层质量下降,在研究区的西部和西南部较为严重。咸水入侵得到证实,咸水从西部扩散到其他地区。盐水侵入含水层增加了电导率,氯化物和钠的浓度,将引起许多生态和农业问题。用于地下水平衡定量评估的新颖可行的方法适用于缺乏水文特性数据库的国家。

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