推断砾石河床河流的河道内切:整合激光雷达数据、历史航拍照片和基于无人机的 SfM 地形测深技术

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL Earth Surface Processes and Landforms Pub Date : 2024-04-16 DOI:10.1002/esp.5840
Miloš Rusnák, Ján Kaňuk, Anna Kidová, Milan Lehotský, Hervé Piégay, Ján Sládek, Lukáš Michaleje
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引用次数: 0

摘要

河道内切是欧洲许多河流,尤其是西喀尔巴阡山脉河流演变的一个明显趋势,其昔日的辫状多河道游荡河系正在转变为单线河道,但通常很难区分驱动因素,也很难确定河道内切是已经结束还是仍在继续。为了跨越这些研究空白,本文提出了一种创新方法,通过基于激光雷达分析河道上方洪泛平原表面的历史航拍图像,评估西喀尔巴阡山脉贝拉河自 1949 年以来的十年内切过程。此外,还利用结构-运动(SfM)摄影测量法衍生的地形-测深模型,根据差异 DEM (DoD)计算了正在进行的侵蚀的详细分析。研究采用了 BACI(前-后-控制-影响)方法,将未受潜在外部影响的河段(控制区)与退化(受影响)河段的前状态(前)、后状态(后)进行比较,以区分驱动因素的影响。洪泛区河道表面分析表明,在退化最严重的河段,河道最大内切达 4 米,内切速率为 5.7 厘米/年。此外,横断面剖面图显示,在过去 10 年(2011-2021 年)中,由于河道向上游扩展,河道加速内切,内切速度达到 24.5 厘米/年。总体而言,无人机勘测的净变化表明,1.6 公里长的河道系统(2015-2022 年)因内切而冲刷出 22 759 立方米的砾石沉积物,而对历史河道表面的分析估计,1949 年至 2020 年期间,受影响河段的侵蚀量为 573 303 立方米。由于当地的驱动因素(河道调节,包括堤坝和砾石开采,这些因素激活了河道系统的逆向侵蚀,并使节理点向上游迁移),只有在控制断面以下的下游部分才能观察到侵蚀迹象。这项分析表明,将不同来源的数据结合起来,将长期和持续的河道反应区分开来,以及采用 BACI 方法在空间和时间上更好地确定因果关系,都是有好处的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Inferring channel incision in gravel-bed rivers: Integrating LiDAR data, historical aerial photographs and drone-based SfM topo-bathymetry

Channel incision is an evident trend for river evolution in many European rivers and notably the Western Carpathians, whose former braided and multichannel wandering river system is transforming into a single-thread channel, but it is often difficult to separate drivers and determine if incision is finished or is still ongoing. To overpass these research gaps, this paper presents an innovative approach to assess the multidecadal incision of the Belá River in the Western Carpathians since 1949 by LiDAR-based analyses of floodplain surfaces above the river channel dated from historical aerial images. Detailed analyses of ongoing incision were also calculated based on DEM of differences (DoD) using Structure-from-Motion (SfM) photogrammetry-derived topo-bathymetric models. The study applied the BACI (Before-After-Control-Impact) approach that compared pre-state (Before), post-state (After) and reach (Control) that is not affected by potential external effects with degraded (impacted) reach to be able to distinguish the driver effects. Floodplain channel surface analyses indicate the maximum incision up to 4 m and incision rate of 5.7 cm/year that occurred in the most degraded reach. Moreover, cross-section profiles point to accelerated incision of 24.5 cm/year in the last 10 years (2011–2021) by the propagation of incision upstream. Overall, the net changes from the UAV survey pointed to 22 759 m3 of gravel sediments, constituting outwash from the 1.6 km long channel system (2015–2022) by incision, whereas analyses of historical channel surfaces estimated erosion of 573 303 m3 from impacted reaches between 1949 and 2020. Incision evidence is only observed in the downstream part below the control section due to local drivers (channel regulation, comprising embankment and gravel mining that activated a backward erosion of the system with knickpoint migration upstream). This analysis shows the benefits of combining different sources of data to separate long-term and ongoing channel responses and the BACI-approach to better target cause–effect relationships in space and time.

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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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