期刊名称:Zbornik Radova: Geografski Fakultet Univerziteta u Beogradu
印刷版ISSN:1450-7552
电子版ISSN:2334-9441
出版年度:2015
卷号:63
页码:43-80
DOI:10.5937/zrgfub1563043M
语种:English
出版社:University of Belgrade - Faculty of Geography, Belgrade
摘要:In this study, we have analyzed the characteristics of deep aquifers that belong to hydrogeological area of Morava region, that is a part of Smederevo Danube region. Hydrogeological complex of Smederevo Danube region was developed in the sediments originated in Neogene. We have observed alternative rotations of hydrogeological collectors, composed of sandy and gravel sediments and hydrogeological insulatorsthat make clay creations. Based on the analysis of geological research, geophysical exploration and drilling for the need of water supply, we have tried to present a spatial position of the collectors, and dense aquifers formed in them. Mapping the dispersion of collectors and evaluating the yield of deep aquifers, it is possible to ascertain the possible usage of water under pressure. Aquifer under pressure is of sub-artesian and artesian character with the level of groundwater from +0.6 to -90 m. Exploitation yield of objects ranges over 5 l/s. Chemical analysis of groundwater from Pontic water-bearing sands, according to Alekin, shows that it belongs to the hydrocarbon-alkaline earth types of water whose mineralization is around 0.5 g/l. This means that this water is moderately hard and that it can be used for drinking. The waters of Pannonian layers belong to soft water, and in the deeper parts there is a possibility of increased mineralization.
其他摘要:У раду су обрађене карактеристике дубоке издани Смедеревског Подунавља које припадају моравској хидрогеолошкој области. Хидрогеолошки комплекс Смедеревског Подунавља развијен је у седиментима неогене старости. Запажено је наизменично смењивање хидрогеолош