Quantifying changes in groundwater level and chemistry in Shahrood, northeastern Iran

Ajdary, Khalil; Kazemi, Gholam A.

Quantifying changes in groundwater level and chemistry in Shahrood, northeastern Iran | Quantification des variations du niveau et de la chimie de la nappe de Shahrood, Nord-Est de l’Iran Cuantificación de cambios en el nivel y química del agua subterránea en Shahrood, noreste de Irán 定量分析伊朗东北部Shahrood地区地下水位和化学成分变化 ارزیابی کمی تغییرات سطح آب و شیمی آب زیرزمینی در شاهرود، شمال شرق ایران Quantificação das alterações do nível piezométrico e do estado químico das águas subterrâneas em Shahrood, nordeste do Irão

2014

Ajdary, Khalil | Kazemi, Gholam A.

Temporal changes in the quantity and chemical status of groundwater resources must be accurately quantified to aid sustainable management of aquifers. Monitoring data show that the groundwater level in Shahrood alluvial aquifer, northeastern Iran, continuously declined from 1993 to 2009, falling 11.4 m in 16 years. This constitutes a loss of 216 million m³from the aquifer’s stored groundwater reserve. Overexploitation and reduction in rainfall intensified the declining trend. In contrast, the reduced abstraction rate, the result of reduced borehole productivity (related to the reduction in saturated-zone thickness over time), slowed down the declining trend. Groundwater salinity varied substantially showing a minor rising trend. For the same 16-year period, increases were recorded in the order of 24% for electrical conductivity, 12.4% for major ions, and 9.9% for pH. This research shows that the groundwater-level declining trend was not interrupted by fluctuation in rainfall and it does not necessarily lead to water-quality deterioration. Water-level drop is greater near the aquifer’s recharging boundary, while greater rates of salinity rise occur around the end of groundwater flow lines. Also, fresher groundwater experiences a greater rate of salinity increase. These findings are of significance for predicting the groundwater level and salinity of exhausted aquifers.

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