Development the soils on the East-Slovak Lowland is greatly influenced by soil-forming conditions from which dominated the substrate-morphological-hydrological and climatic conditions (Michaeli, Vilcek, 2013). Fluvial activity manifested depositing periglacial cones at the foot of the mountains and along the larger flows in the East-Slovak Plain were deposited fluvial sediments in the form of levee deposites (Kvitkovic, 1964), which form a very flat mild elevations along rivers. Versus the adjacent depressions stand out of 1 – 3 m (its large territory with altitudes from 94 to 120 m dissection of the relief around 26 m and with small inclination of individual forms of relief). As result of the geological-tectonic-morphological conditions in the East-Slovak Plain created specific hydrogeosystem (river network configuration and circulation of groundwater, Šútor et al., 1995). Small slope of on fluvial plains and confluence of the several rivers close to each other as well as the insufficient capacity of rivers beds lifts the levels of one to the second of the watercourse, what creates conditions for the emergence of large-scale of flooding area. Water managements adjustments solves this problem by means of the protection levees, canals, water reservoirs and dry polders. All Water Retaining Structures require a constant maintenance and repairs of, which currently absent. East-Slovak Lowland is presently almost completely deforested territory. It is a typical agrarian ecosystem with a peculiar character of soil cover (Vilcek, 2004a). The greater part of the soil cover is used as agricultural soil (about 69 % of the territory).