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利用一种新的河底灾害测绘方法对冲积河底变化进行水深监测,以确保水电站结构的稳定性(波兰弗罗茨瓦夫)。

Bathymetric Monitoring of Alluvial River Bottom Changes for Purposes of Stability of Water Power Plant Structure with a New Methodology for River Bottom Hazard Mapping (Wloclawek, Poland).

机构信息

Department of Geodesy, Faculty of Geoengineering, University of Warmia and Mazury, Heweliusza 5, 10-724 Olsztyn, Poland.

Department of Geological Engineering, Faculty of Mining and Geology, VŠB-Technical University of Ostrava, 17 listopadu 15, 708 33 Ostrava, Czech Republic.

出版信息

Sensors (Basel). 2020 Sep 3;20(17):5004. doi: 10.3390/s20175004.

Abstract

The aim of this research was to produce a new methodology for a special river bottom hazard mapping for the stability purposes of the biggest Polish water power plant: Włocławek. During the operation period of the water power plant, an engineering-geological issue in the form of pothole formation on the Wisła River bed in the gravel-sand alluvium was observed. This was caused by increased fluvial erosion resulting from a reduced water level behind the power plant, along with frequent changes in the water flow rates and water levels caused by the varying technological and economic operation needs of the power plant. Data for the research were obtained by way of a 4-year geodetic/bathymetric monitoring of the river bed implemented using integrated GNSS (Global Navigation Satellite System), RTS (Robotized Total Station) and SBES (Single Beam Echo Sounder) methods. The result is a customized river bottom hazard map which takes into account a high, medium, and low risk levels of the potholes for the water power plant structure. This map was used to redevelop the river bed by filling. The findings show that high hazard is related to 5% of potholes (capacity of 4308 m), medium with 38% of potholes (capacity of 36,455 m), and low hazard with 57% of potholes (capacity of 54,396 m). Since the construction of the dam, changes due to erosion identified by the monitoring have concerned approximately 405,252 m of the bottom, which corresponds to 130 Olympic-size pools. This implies enormous changes, while a possible solution could be the construction of additional cascades on the Wisła River.

摘要

本研究的目的是为波兰最大水力发电站——沃洛科拉姆斯克(Włocławek)的稳定性开发一种特殊河底危险测绘的新方法。在水力发电站运行期间,观察到维斯瓦河砾石-砂质冲积层河床出现坑洞形成这一工程地质问题。这是由于水电站背后水位升高导致河流侵蚀加剧,加上水电站技术和经济运行需求频繁变化导致水流速度和水位频繁变化所致。研究数据是通过使用集成 GNSS(全球导航卫星系统)、RTS(机器人全站仪)和 SBES(单波束回声测深仪)方法进行的为期 4 年的河床大地测量/水深监测获得的。结果是一张定制的河底危险图,考虑了水电站结构的坑洞高、中、低风险水平。该图用于通过填充来重新开发河床。研究结果表明,高危险与 5%的坑洞(容量为 4308 立方米)有关,中等危险与 38%的坑洞(容量为 36455 立方米)有关,低危险与 57%的坑洞(容量为 54396 立方米)有关。自大坝建成以来,监测所识别的侵蚀引起的变化涉及约 405252 米的河床,相当于 130 个奥林匹克标准游泳池。这意味着巨大的变化,而可能的解决方案是在维斯瓦河上建造额外的瀑布。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2473/7506780/dc95f9895adc/sensors-20-05004-g001.jpg

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