首页> 外文会议>IAHS international commission on continental erosion symposium >Driving forces in a floodplain restoration project: interaction between surface water, groundwater and morphodynamic processes during an ecological flooding
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Driving forces in a floodplain restoration project: interaction between surface water, groundwater and morphodynamic processes during an ecological flooding

机译:洪泛省恢复项目中的驱动力:在生态洪水期间,地表水,地下水和形态学过程之间的相互作用

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Erosion, transport and deposition of sediment play a major role in restoration projects and sustainable river management. The main driving variables, water and sediment dynamics resurrect the natural processes in "riverscapes" and floodplains. After the first flooding of a new river course in the flood-plain along the River Danube between Neuburg and Ingolstadt (Germany) in 2010 (up to 5 m~3/sec), new morphological activity started instantly. However, intensive erosion rates were measured during the first two controlled ecological flood events with water discharges of 10 m~3 s~(-1) and 20 m~3 s~(-1). The relatively new river banks are prone to lateral erosion and during bankfull stages new undercut slopes have developed. To understand the processes in this new river channel, its development is being recorded by a package of methods such as terrestrial laser scanning (TLS) measurements.
机译:沉积物的侵蚀,运输和沉积在恢复项目和可持续河流管理中发挥了重要作用。主要驱动变量,水和沉积动力学在“河流”和洪泛平原中复制自然过程。在2010年Neub​​urg和Ingolstadt(德国)之间的洪水河沿河河沿河河(德国)(最多5米〜3 /秒),新形态活动立即启动。然而,在前两个受控生态泛洪事件期间测量了强烈的侵蚀率,排放了10 m〜3 s〜(-1)和20 m〜3 s〜(-1)。相对较新的河岸易于侵蚀,并且在银行阶段期间新的削减斜坡已经发展起来。要了解这一新的河道中的过程,它的开发是通过诸如地面激光扫描(TLS)测量的一揽子方法来记录。

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