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Evaluation of the salt accumulation process during inundation in water resource of Contas river basin (Bahia-Brazil) applying principal component analysis

机译:应用主成分分析法评价康塔斯河流域(巴伊亚-巴西)水资源中的盐分积累过程。

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摘要

The high salinization in some reservoirs of the Contas river basin (Bahia-Brazil) has been erroneously attributed only to concentration by evaporation. However, recent studies of this basin have shown that in period of intense rainfalls, occur an increase of the saline concentration in the flowing rivers of the reservoirs. The application of statistical methods (cluster and principal components analysis) have shown that this fact can be attributed to the discharge of saline waters from the small reservoirs of every drained area, provoked by inundation, is also an important factor in the salinization process. Thus the study of the geochemical variables: Na~+ , K~+, Ca~(2+), Mg~(2+), Cl~-, SO_4~(2-) and CO_3~(2-), showed one group formed by Na~+ and Cl~-, attributed to the discharge of saline water provoked by inundation from a small reservoir, and a second group constituted by Ca~(2+) , Mg~(2+), K~+ and SO_4~(2-), due to an increase provoked by the evaporation in the salinization process.
机译:在Contas河盆地(巴伊亚-巴西)的某些水库中,高盐碱化被错误地归因于蒸发浓缩。但是,该盆地的最新研究表明,在强降雨期间,水库的河流中的盐分浓度会增加。统计方法(聚类和主成分分析)的应用表明,这一事实可以归因于每个流域小型水库的咸水排放,这些水是由于淹没引起的,也是盐碱化过程中的重要因素。因此,对地球化学变量Na〜+,K〜+,Ca〜(2 +),Mg〜(2 +),Cl〜-,SO_4〜(2-)和CO_3〜(2-)的研究表明:由Na〜+和Cl〜-组成的组,归因于从小型水库中淹没引起的盐水排放,第二组由Ca〜(2 +),Mg〜(2 +),K〜+和SO_4〜(2-),由于盐化过程中蒸发引起的增加。

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