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Geomorphology of the floodplain at the confluence of the Aventino and Sangro rivers (Abruzzo, Central Italy)

机译:阿文蒂诺河和桑格罗河交汇处的洪泛区的地貌(意大利中部阿布鲁佐)

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This paper presents a geomorphological map of the floodplain at the confluence of the Aventino and Sangro rivers (scale 1:10,000), located across the Adriatic piedmont of the Maiella Massif (Abruzzo Region, Central Italy). This area is in the lower reach of the Sangro–Aventino drainage basin, which in the mid-1900s was affected by the creation of four main artificial water reservoirs by damming of the basin's major rivers and the related network of spillway pipes for hydropower purposes. This, combined with climatic factors, induced a strong rearrangement of river channels and floodplains. The fluvial geomorphological features have been analyzed through a detailed-scale multi-temporal analysis based on geomorphological field mapping, topographic analysis, and a remote sensing analysis carried out on aerial photos, orthophotos and Lidar images. The map includes three sections: physiographic and geological setting; main geomorphological map; multi-temporal (1954–2009) and morphometric analysis of the floodplain. The mapping is focused on landforms and continental deposits, mainly linked to fluvial, slope and anthropogenic processes, and to 1954 and 2009 river channels planform analyses and the related morphometric parameters, in order to outline the changes in the river dynamics, strongly influenced by anthropogenic intervention. At a local scale, this type of map can contribute to the understanding of the causes, mechanisms and consequences of the changes in fluvial form and support river management. Finally, it may represent a tool for the assessment of natural hazards in landscapes characterized by intense and rapid geomorphological (fluvial) processes, as well as a tool for correct land management.
机译:本文介绍了位于马伊埃拉断层山(意大利中部阿布鲁佐地区)对面的阿文蒂诺河和桑格罗河(1:10,000比例)汇合处的漫滩平原的地貌图。该地区位于Sangro-Aventino流域的下游,在1900年代中期,该流域的主要河流和相关的用于水力发电的溢洪道网络被围堵,从而创建了四个主要的人工蓄水池,从而影响了该地区。再加上气候因素,导致河道和洪泛区的强烈重新布置。通过对地貌图绘制,地形分析以及对航拍照片,正射照片和激光雷达图像进行的遥感分析,通过详细的多时相分析,分析了河流的地貌特征。该地图包括三个部分:地理和地理环境;主要地貌图;多时相(1954–2009年)和洪泛区的形态计量学分析。该地图着重于地形和大陆沉积物,主要与河流,斜坡和人为过程相关,并与1954年和2009年河道平面分析和相关形态参数相关,以概述受人为影响的河流动力学变化介入。在地方尺度上,这种类型的地图可以帮助人们了解河流形态变化的原因,机制和后果,并为河流管理提供支持。最后,它可能是评估以强烈而快速的地貌(河流)过程为特征的景观中自然灾害的工具,也是正确进行土地管理的工具。

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