be ej(北塞尔维亚)公共供水地下水资源的水文地质和水动力特征

D. Polomcic, O. Krunić, Vesna Ristić-Vakanjac
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引用次数: 4

摘要

塞尔维亚Becej市公共供水的现有地下水来源是从三个含水层的15口井中抽取地下水,总容量超过100升/秒。水源地的特征之一是几个含水层最常被井同时开采。两层由12口井同时起孔;所有三层都由10口井开采,而一个含水层仅由3口井开采。源区的地下水位记录了30年。在对地下水状况进行的水动力分析中,得出的结论是,在上述时期,地下水位的下降幅度相对较小,远低于先前的预测值。本文介绍了两年半多来对城镇和周边水源开发制度的模拟结果,并介绍了确定抽头含水层基本水文地质参数的结果。此外,还展示了作为城镇自来水来源的含水层中每个元素的平衡。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrogeological and hydrodynamic characteristics of groundwater sources for the public water supply of Bečej (Northern Serbia)
The existing groundwater source for the public water supply of Becej City in Serbia is tapping groundwater from three water-bearing horizons over 15 wells with a summary capacity over 100 l/s. It is one of the characteristics of sources that several water-bearing layers are most frequently tapped simultaneously by wells. Two layers are tapped simultaneously by 12 wells; all three layers are tapped by ten wells, while one water-bearing layer is tapped by only three wells. The groundwater table at the source was recorded for a period of 30 years. In the conducted hydrodynamic analysis of the groundwater regime, it was concluded that in the mentioned period, a relatively low fall of the water table occurred, far lower than the previously predicted values. The results of a simulation of the exploitation regime of both the town and surrounding sources are presented in this paper for a period of more than two and a half years and the results of the identification of the basic hydrogeological parameters of the tapped water-bearing layers are presented in this paper. In addition, a balance for each element in the water-bearing layers exploited as sources of tapped water for the town are presented.
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