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Introduction Formation and distribution of the phreatic (unconfined, free, first, shallow) aquifer, groundwater layer the closest to topographic surface, primarily depends on the ruling hydrogeological conditions and relations that are perceived in the presence of rocks of intergranular porosity with favourable water collecting abilities within the top (covering) geological layer and impermeable rocks in the bottom geological layer of a certain geological complex. Main characteristics of the phreatic aquifer water regime result from the series of complex and interdependent phenomena and processes whose character is defined by numerous natural and anthropogenic factors. Among the natural factors, besides above-mentioned hydrogeological conditions, it is necessary to mention pedological, geomorphologic, fitogeographical and especially climate and hydrological circumstances. However, anthropogenic factor significantly modifies the natural regime of the phreatic aquifer in the areas with appropriate hydrotechnical works conducted or intensive irrigation/drainage of cultivated land (Pavić, 2006; Pavić et al., 2006; Pennington, Cech, 2010). Abstract

Main characteristics of water regime of the phreatic aquifer in Subotica municipality: Vojvodina, Serbia