Variation of some Water Quality Parameters with Fluctuation of Groundwater Table in Wana Sub-District Northern Iraq

Abstract

This study aims to investigate the effect of groundwater fluctuation on some water quality characteristics in the Wana region of Northern Iraq. The fluctuations in water table levels in 18 tube wells were monitored to find out if there is a relationship between water table levels with some water quality factors. Groundwater samples were collected monthly from September 2020 to April 2021. Electric conductivity (EC), temperature, pH, water table level, total hardness (TH), sulfate and nitrate concentrations were all measured monthly for eight months. The results showed a wide range of water salinity variation ranging from 715 to 4420 µmohs/cm, with more than half of the examined samples exceeding 3000 µmohs/cm. Even in the same wells, water salinity varied during the monthly monitoring. The depth to the water table ranged from 3.39 to 37.56 m, depending on the topography, recharge rate, and aquifer conditions in the area. All of the wells produced very hard water as a result of the dissolution of gypsum and anhydrite bedrock, with about 84% having high sulphate concentrations of over 250 mg/l. More than a quarter of the samples tested showed pollution with nitrate at concentrations extremely close to or over 50 mg/l. It was found that there is no obvious correlation between groundwater quality properties and the fluctuation of the water table.