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首页> 外文期刊>GeoActa >Hydrochemical effects of the 'Bilancino' dam on the Sieve River basin and interactions with the Arno River (northern Tuscany, Italy)
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Hydrochemical effects of the 'Bilancino' dam on the Sieve River basin and interactions with the Arno River (northern Tuscany, Italy)

机译:“ Bilancino”大坝对Sieve流域的水化学作用以及与阿尔诺河的相互作用(意大利托斯卡纳北部)

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摘要

A hydrochemical study was carried out in order to detect some 1997 to 2002 changes in surface water composition of the catchment basin of the Sieve River. The Sieve River is the most important tributary of the Arno River with regard to the Florence water supply, as a consequence of the accomplishment of a broad artificial lake realized along the upper course of the Sieve. Moreover, the interactions between the Sieve and the Arno rivers were studied to highlight the influence of the former's discharge on the latter's water quality. An experimental classification for surface waters - developed in the Department of Earth Sciences of Florence - is used because of its excellent suitability to the whole Arno catchment basin. Two sampling surveys - before and after the dam's fulfilment - were performed, and the drawn waters were analysed to characterize their geochemical type by gauging fundamental components and environmental indicators. The analytical results point out a clear depletion in ionic concentrations following the lake realisation, with a general quality improvement of the Sieve waters inside and downstream of the reservoir. Moreover, a sort of hydrochemical stratification was observed in the water column, where contents seem to increase with increasing depth. Finally, the water supply provided by the Bilancino dam (up to 8 m~3/s for 180 days, during an average hy-drological year) will improve the quality of the Arno waters downstream of the merging with the Sieve.
机译:为了检测1997年至2002年Sieve河集水盆地地表水组成的某些变化,进行了水化学研究。就佛罗伦萨的供水而言,筛河是亚诺河最重要的支流,这是由于沿筛河上游实现了广阔的人工湖的结果。此外,还对锡耶夫河和亚诺河之间的相互作用进行了研究,以突出前者的流量对后者的水质的影响。由于地表水对整个阿诺河流域盆地的适应性极佳,因此使用了由佛罗伦萨地球科学部开发的地表水实验分类。在大坝建成之前和之后进行了两次抽样调查,并对抽水进行了分析,以通过测量基本成分和环境指标来表征其地球化学类型。分析结果指出,随着湖泊的实现,离子浓度明显减少,水库内部和下游的筛网水质量总体得到改善。此外,在水柱中观察到某种水化学分层,其含量似乎随着深度的增加而增加。最后,比兰奇诺水坝提供的水供应(在平均水文学年中,连续180天最高可达8 m〜3 / s)将改善与筛网合并后的阿诺河水质。

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