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The subthermal potential of karstic groundwater of Kucaj-Beljanica region in Serbia estimated by the multivariate analysis

机译:塞尔维亚甘济岛喀斯贾卡岛地区喀斯特地下水的分解潜力估计多元分析

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摘要

To define the potential uses of groundwater, a detailed hydrochemical analysis was carried out in the Kuaj-Beljanica Massif at seven locations, in the eastern part of the Republic of Serbia. The hydrogeochemical analysis led to a better understanding of the hydrogeochemical processes occurring underground, as well as the existence and origin of groundwater heat sources. The chemical composition of the thermal groundwater indicates different formation conditions, the influence of different rock types and different physico-chemical processes with time and temperature variations on water quality. Better insight into the geochemical and thermal conditions of groundwater can identify the most prospective locations for geothermal applications such as indoor and outdoor space heating, sports, recreation and tourism, as well as industrial applications, with or without the additional use of heat pumps. Factor analysis (FA), especially principal component analysis (PCA) and cluster analysis (CA) were applied for the evaluation of the spatial/temporal variations of Kuaj-Beljanica thermal groundwater. It was concluded that PCA was the optimum method for explaining functional relationships between the chemical elements. After data reduction, three main factors controlling variability were identified. Hierarchical cluster analysis (HCA) was applied for sample differentiation according to sample location which resulted in the grouping of the examined location into three main groups according to their thermal or geochemical potential: Group I: lowest potential for any purpose; Group II: best thermal potential (wellness centres, agriculture and heating of different facilities and Group III: specific hydrogeochemical potential suitable for bottling or balneal tourism.
机译:为了定义地下水的潜在用途,在塞尔维亚共和国东部的七个地区的Kuaj-Beljanica Massif中进行了详细的水化学分析。水文地球化学分析导致​​了对地下发生的水文地球化学过程的更好理解,以及地下水热源的存在和起源。热地水的化学成分表示不同的形成条件,不同岩石类型的影响和不同的物理化学过程随时间和温度变化对水质。更好地洞察地球化学和地下水的热条件可以识别地热应用的最前景位置,如室内和室外空间加热,运动,娱乐和旅游以及工业应用,有或没有额外使用热泵。因子分析(FA),尤其是主要成分分析(PCA)和聚类分析(CA)用于评估Kuaj-Beljanica热地水的空间/时间变化。得出结论,PCA是解释化学元素之间的功能关系的最佳方法。在减少数据后,确定了控制变异性的三个主要因素。根据样品位置施加分层聚类分析(HCA),根据样品位置施加样品分化,导致将检查的位置分组为三个主要组,根据其热量或地球化学潜力:I组:任何目的的最低潜力;第II组:最佳热潜力(健康中心,农业和不同设施和III集团的加热:适用于装瓶或空地的特定水文层。

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