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首页> 外文期刊>Sedimentology: Journal of the International Association of Sedimentologists >The sedimentary response to a pioneer geo-engineering project: Tracking the Kander River deviation in the sediments of Lake Thun (Switzerland)
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The sedimentary response to a pioneer geo-engineering project: Tracking the Kander River deviation in the sediments of Lake Thun (Switzerland)

机译:对先驱性地质工程项目的沉积响应:跟踪图恩湖(瑞士)沉积物中的坎德河偏离

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摘要

Human activities such as river corrections and deviations, lake-level regulations and installations of hydropower plants affect and often strongly modify natural processes in lacustrine systems. In 1714, the previously bypassing Kander River was deviated into peri-alpine Lake Thun. This pioneering geo-engineering project, the first river correction of such dimensions in Switzerland, doubled the water and sediment input to the lake. In order to evaluate the sedimentary consequences of the Kander River deviation, the lacustrine sediments were investigated using a combined approach of high-resolution (3·5 kHz) reflection seismic data and sediment cores (maximum length 2·5 m). The significance of this study is increased by the possible hazard represented by ammunition dumped into the lake (from 1920 to 1960) and by the recent installation of a gas pipeline on the lake floor in 2007/2008. The first 130 years after the river deviation were dominated by an extremely high sediment input, which led to the frequent occurrence of subaquatic mass movements. Slope failures primarily occur due to rapid sediment accumulation, but were occasionally triggered in combination with earthquake-induced shocks and lake-level fluctuations. After 1840, massmovement activity and sedimentation rates decreased due to a reduced sediment input as the Kander River adjusted to its new base level and, to a smaller degree, by further engineering of the Kander River bed and gravel withdrawal at the Kander Delta. A further consequence of the Kander River deviation is that the shores around Lake Thun have been more frequently affected by flooding due to the increased water input. In the time span from 1850 to 2006, six historically and/or instrumentally documented flood events could be correlated to flood turbidites in the sediment cores. This study demonstrates the significant usefulness of lacustrine sediments, not only in archiving natural hazards and human impact but also in assessing the consequences of future anthropogenic interventions on lacustrine systems.
机译:人类活动,如河流改正和改道,湖泊水位法规和水力发电厂的安装,会影响并经常强烈改变湖泊系统的自然过程。在1714年,以前绕过的坎德河(Kander River)被改道为阿尔卑斯高山的图恩湖(Thun)。这项具有开创性的地球工程项目,是瑞士首次进行这样规模的河流改正,使湖泊的水和泥沙输入量增加了一倍。为了评估坎德河偏离的沉积后果,采用高分辨率(3·5 kHz)反射地震数据和沉积岩心(最大长度2·5 m)的组合方法研究了湖相沉积物。 1920年至1960年倾倒在湖中的弹药以及最近在2007/2008年在湖面上安装了一条天然气管道,都可能带来危害,从而增加了这项研究的重要性。河流改道后的头130年主要是大量的泥沙输入,这导致了水下水肿运动的频繁发生。边坡破坏主要是由于快速的泥沙积累而引起的,但偶尔会由于地震引起的冲击和湖面波动而引发。 1840年后,由于坎德河调整至新的基准水位,泥沙运动减少,泥沙运移速率降低,并且通过对坎德河床和坎德河三角洲的砾石抽放进行了进一步工程,使泥沙运动和沉积速率降低了。坎德河偏离的另一个后果是,由于增加了水的输入,图恩湖周围的海岸更常受到洪水的影响。在1850年至2006年的这段时间里,有六个历史和/或工具记录的洪水事件可能与沉积岩心中的洪水浊度有关。这项研究表明,湖泊沉积物不仅在存档自然灾害和人类影响方面,而且在评估未来人为干预对湖泊系统的后果方面,都具有巨大的实用性。

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