Some characteristics of groundwater in Southeast Srem

Abstract

The area of Southeast Srem is rich in groundwater. Water regime of the first aquifer has a great significance from the standpoint of agricultural production. 32 piezometers were singled out and groundwater depth was measured aiming at the analysis of some groundwater characteristics. In the area of Southeast Srem, groundwater level fluctuates very widely, depending on the distance from water courses. Mean value of groundwater fluctuation in Southeast Srem amounts to 3.49m. In this area, groundwater moves in Southeast direction, i.e. in the direction of the main receiving streams of the region, the Sava and the Danube. The greatest risk of groundwater overflowing in Southeast Srem occurs in the central parts of the loess terrace and in low parts of the alluvial plain along the Sava, where groundwater level is at the depth of less than 1m.

Područje jugoistočnog Srema obiluje podzemnim vodama. Režim voda prve izdani sa stanovišta poljoprivredne proizvodnje ima veliki značaj. U cilju analize nekih karakteristika podzemnih voda područja izdvojeno je 32 pijezometra na kojima su merene dubine podzemnih voda. Nivo podzemne vode na području jugoistočnog Srema osciluju u veoma širokom opsegu, u zavisnosti od udaljenosti od vodenih tokova. Srednja vrednost oscilacija podzemnih voda na području jugoistočnog Srema iznosi 3,49m. Podzemnih vode područja kreću se u pravcu jugoistoka, tj. u pravcu prema glavnim recipijentima ovog područja, Savi i Dunavu. Najveću opasnost od izlivanja podzemnih voda na području jugoistočnog Srema imaju centralni delovi lesne terase i niski delovi aluvijalne ravni uz Savu na kojima se podzemna voda nalazi na dubini manjoj od 1m.