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ANALYSIS OF WATER LEAKAGE IN DOWNSTREAM DAM TOE OF KOMANI DAM

机译:小谷坝下游坝趾渗水分析

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Koman dam is one of most important high dams in Drin River Cascade. Safety of these dam is very important not only in power production but also in social and environmental aspects connected with vital activity of local people living in downstream of Drini River and in economic development of the country. In December 2014, during the rehabilitation works on some protection measures at the downstream dam toe, a considerable amount of water leakage emerged from the dam toe. This was noticed even before, but its amount and physical-chemical properties were not evaluated. In order to study the origin and flow direction of this water leakage, KESH sh.a. (Albanian Power Corporation) realized Geophysical and Hydro chemical surveys, turbidity and flow measurements and respective analyses of them. Geophysical survey consist in Apparent Resistivity surveys and Self Potential survey. The survey was done in 3 lines using Resistivity "Real Section" technique. Results are plotted in Sections and plan maps of resistivity and SP parameter. There are defined possible leakage areas and the main flow directions are defined. Also, there is done a hydro chemical analyse. Nine water samples were taken from the different places as Komani lake, service galleries of dam, dam toe and two karst springs which were analysed for both physical-chemical parameters and isotopic composition of 0-18 and D. The attained analytical data found that water from the dam toe leakages shows the same chemical signature and isotopic composition of 0-18 and D as the water from the lake, thus confirming the hydraulic connection between them. Also, There is done the analyse of water leakage turbidity and amount of this leakage.
机译:科曼水坝是德林河喀斯喀特最重要的高水坝之一。这些大坝的安全不仅在电力生产中而且在与居住在Drini河下游的当地人的重要活动以及该国的经济发展有关的社会和环境方面都非常重要。 2014年12月,在下游坝脚趾的一些保护措施的修复工程中,坝脚趾出现大量漏水。这甚至在以前就已注意到,但尚未评估其量和理化性质。为了研究这种漏水的起因和流向,请参考KESHsh.a。 (阿尔巴尼亚电力公司)实现了地球物理和水化学勘测,浊度和流量测量以及对它们的相应分析。地球物理调查包括表观电阻率调查和自电势调查。使用电阻率“实际剖面”技术以3条线进行了调查。将结果绘制在电阻率和SP参数的剖面图和平面图中。定义了可能的泄漏区域,并定义了主要的流向。另外,进行了水化学分析。从科马尼湖,大坝,坝脚趾和两个喀斯特泉水等不同地点采集了9个水样,分析了其物理化学参数以及0-18和D的同位素组成。获得的分析数据发现,水从大坝脚趾泄漏出来的水与湖中的水显示出相同的化学特征和0-18和D的同位素组成,从而证实了两者之间的水力联系。另外,还进行了漏水浊度和漏水量的分析。

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