首页> 外文期刊>Estonian Journal of Earth Sciences >A radical shift from soft-water to hard-water lake: palaeolimnological evidence from Lake Kooraste K?μverj?¤rv, southern Estonia
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A radical shift from soft-water to hard-water lake: palaeolimnological evidence from Lake Kooraste K?μverj?¤rv, southern Estonia

机译:从软水湖到硬水湖的根本转变:爱沙尼亚南部Kooraste K?μverj?¤rv湖的古生物学证据

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>The Water Framework Directive (WFD) of the European Union requires the quality of all European water bodies to be >examined, and aims to achieve good status by 2015. This study was initiated to assess whether a potential reference lake for identifying lake-type specific reference conditions meets the WFD requirements, of being minimally impacted by human activity during the last centuries. The sediments of Lake Kooraste K?μverj?¤rv were analysed for diatom assemblages and sediment composition; past changes in the lake-water pH and total phosphorus were reconstructed, using quantitative models on sedimentary diatoms. The chronology of sediments was established, using spheroidal fly-ash particles stratigraphy. Palaeolimnological investigations, >supported by information from historical maps, revealed that man-made changes around the lake have severely influenced its ecological conditions. The lake, which had been oligotrophic with soft and clear water before the mid-17th century, has been trans?-formed into a hard-water lake by modifications to the inflow and outflow. The lake water quality has also been altered by the infiltration of nutrients from a nearby hypertrophic lake that was used for flax retting since the 19th century. Although the ecological status of the lake has remained good despite all these changes, it is still questionable whether to nominate it as a reference lake for stratified hard-water lake types.
机译:>欧盟的《水框架指令》(WFD)要求对所有欧洲水体的质量进行“跨度检查”,并力争在2015年之前达到良好状态。本研究旨在评估是否有潜在的参考湖泊确定湖泊类型的特定参考条件是否符合WFD要求,并且在过去的几个世纪中受到人类活动的影响最小。分析了Kooraste K?μverj?rv湖的沉积物的硅藻组合和沉积物组成。利用沉积硅藻的定量模型,重建了过去湖水pH和总磷的变化。利用球形粉煤灰颗粒地层学建立了沉积物的年代学。古生物学调查得到历史地图信息的支持,结果表明,湖周围的人为变化严重影响了其生态条件。该湖在17世纪中叶以前用软水和清澈的水富营养化,通过改变流入和流出的方式,已转变为硬水湖。自19世纪以来,附近肥大的湖泊中的营养物质的渗透也改变了湖泊的水质。尽管发生了所有这些变化,尽管湖泊的生态状况仍然保持良好,但是否将其指定为分层硬水湖泊类型的参考湖泊仍存在疑问。

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