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Hydrogeomorphic processes and torrent control works on a large alluvial fan in the eastern Italian Alps

机译:在意大利东部阿尔卑斯山的大型冲积扇上进行水力地貌过程和洪流控制工作

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摘要

Alluvial fans are often present at the outlet of\udsmall drainage basins in alpine valleys; their formation is\uddue to sediment transport associated with flash floods and\uddebris flows. Alluvial fans are preferred sites for human settlements\udand are frequently crossed by transport routes. In\udorder to reduce the risk for economic activities located on or\udnear the fan and prevent loss of lives due to floods and debris\udflows, torrent control works have been extensively carried\udout on many alpine alluvial fans. Hazard management\udon alluvial fans in alpine regions is dependent upon reliable\udprocedures to evaluate variations in the frequency and severity\udof hydrogeomorphic processes and the long-term performance\udof the torrent training works. An integrated approach\udto the analysis of hydrogeomorphic processes and their interactions\udwith torrent control works has been applied to a large\udalluvial fan in the southern Carnic Alps (northeastern Italy).\udStudy methods encompass field observations, interpretation\udof aerial photographs, analysis of historical documents, and\udnumerical modelling of debris flows. The overall performance\udof control works implemented in the early decades of\ud20th century was satisfactory, and a reduction of hazardous\udevents was recognised from features observed in the field and\udin aerial photographs, as well as from the analysis of historical\udrecords. The 2-D simulation of debris flows confirms\udthese findings, indicating that debris flow deposition would\udnot affect urban areas or main roads, even in the case of a\udhigh-magnitude event. Present issues in the management of\udthe studied alluvial fan are representative of situations frequently\udfound in the European Alps and deal with the need\udfor maintenance of the control structures and the pressures\udfor land use changes aimed at the economic exploitation of\udthe fan surface.
机译:冲积扇经常出现在高谷的小型排水盆地的出口。其形成是由于与洪水和泥石流有关的泥沙输送。冲积扇是人类住区的首选场所,\\经常通过运输路线穿越。为了降低位于风扇附近或附近的经济活动的风险并防止由于洪水和碎屑\溢流而造成的生命损失,洪流控制工作已在许多高山冲积扇上广泛进行。高寒地区的危害管理\乌冬面冲积扇取决于可靠的\过程,以评估水力地貌过程的频率和严重程度\ udd以及洪流培训工作的长期绩效\ ud。 \\分析水文地貌过程及其相互作用\与洪流控制工作的综合方法\已应用于卡尔尼阿尔卑斯山南部(意大利东北部)的大型\洪积扇。\ ud研究方法包括现场观察,解释\航空照片,历史文件分析和泥石流的\数字模拟。在20世纪初的几十年中实施的控制工作总体表现令人满意,从野外观察到的特征和航拍照片以及对历史记录的分析中可以看出,减少了危险事件。泥石流的二维模拟证实了这些发现,表明泥石流的沉积不会影响市区或主要道路,即使在发生高幅事件的情况下也是如此。 \研究的冲积扇的管理中的当前问题代表了欧洲阿尔卑斯山经常\未发现的情况,并处理了\控制结构的维护需求和旨在经济开发\ udthe的土地用途变化的压力\ ud风扇表面。

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