Ljiljana Dimitrijevic, Aleksandar Radivojevic, Ninoslav Golubovic
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摘要

拉西纳河发源于韦利卡河和缅曼斯卡河的泉水,发源于Goc山和Zeljin山的山坡。经过92公里后,它流入海拔134米的扎帕德纳莫拉瓦河,位于克鲁塞瓦茨下游5公里处。在本研究中,将分析位于切列杰人工湖下游35公里处的克鲁塞瓦茨境内的拉西纳河的水质,以及其合流的水质,如:加格洛夫斯卡河,特姆卡尔斯卡河,隆尼克河。对拉西纳河水质的测试是在河本身的五个侧面进行的,在它的大汇合处的入口处进行的。我们还将讨论Krusevac工业的废水及其对Rasina河水质的影响,以及废水控制和去除潜在污染物的可能性。
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Kvalitet vode reke Rasine nizvodno od akumulacije "Ćelije"
The Rasina river begins on the slopes of the mountains Goc and Zeljin from the springs of the rivers Velika and Burmanska. After 92 km it flows into the Zapadna Morava, 5 km downstream from Krusevac, at 134m altitude. In this study, the water quality of the Rasina in the territory of Krusevac will be analyzed, 35 km downstream from the Celije artificial lake, and also the quality of its confluents like: Gaglovska river, Trmcarska river, Lomnicka river. The testing of the Rasina water quality is performed on five profiles on the river itself, and on the mouths of its larger confluents. We will also talk about effluents of Krusevac industry and their influence on the water quality of the Rasina river, and about the possibilities of effluent control and removal of potential pollutants as well.
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