Spatial Analysis of the Chemical Regime of Groundwater in the Karatal Irrigation Massif in South-Eastern Kazakhstan

Understanding the groundwater chemical regime on irrigated lands is relevant for assessing hydrogeological and reclamation processes. Water chemistry, natural climatic conditions, drainage characteristics define complex hydrochemical connections which are formed between irrigation waters, soil, water of unsaturated zone groundwater. This research paper presents results studies seasonal changes in composition Karatal massif. A detailed analysis salt have been performed based a large number samples 2019. Besides, data related to River waters quality inside basin also analyzed. Results demonstrate that salinization processes massif determined by conditions availability. In north-eastern part massif, high risk soil has observed as consequence all its Data over show influenced presence saline soil-forming rocks, depth, volume, drainage, evaporation