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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Use of terrestrial photosieving and airborne topographic LiDAR to assess bed grain size in large rivers: a study on the Rhine River
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Use of terrestrial photosieving and airborne topographic LiDAR to assess bed grain size in large rivers: a study on the Rhine River

机译:使用陆地的光相和空中地形利达评估大型河流的床粒大小:莱茵河研究

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摘要

Most grain size monitoring is still being conducted by manual sampling in the field, which is time consuming and has low spatial representation. Due to new remote sensing methods, some limitations have been partly overcome, but methodological progress is still needed for large rivers as well as in underwater conditions. In this article, we tested the reliability of two methods along the Old Rhine River (France/Germany) to estimate the grain size distribution (GSD) in above-water conditions: (i) a low-cost terrestrial photosieving method based on an automatic procedure using Digital Grain Size (DGS) software and (ii) an airborne LiDAR topo-bathymetric survey. We also tested the ability of terrestrial photosieving to estimate the GSD in underwater conditions. Field pebble counts were performed to compare and calibrate both methods. The results showed that the automatic procedure of terrestrial photosieving is a reliable method to estimate the GSD of sediment patches in both above-water and underwater conditions with clean substrates. Sensitivity analyses showed that environmental conditions, including solar lighting conditions and petrographic variability, significantly influence the GSD from the automatic procedure in above-water conditions. The presence of biofilm in underwater conditions significantly altered the GSD estimation using the automatic procedure, but the proposed manual procedure overcame this problem. The airborne LiDAR topographic survey is an accurate method to estimate the GSD of above-water bedforms and is able to generate grain size maps. The combination of terrestrial photosieving and airborne topographic LiDAR methods is adapted to assess the GSD over several kilometers long reaches of large rivers. (c) 2020 John Wiley & Sons, Ltd.
机译:大多数粒度监测仍然是通过该领域的手动抽样进行的,这是耗时的并且空间表示低。由于新的遥感方法,部分克服了一些局限性,但大型河流以及水下条件仍然需要方法。在本文中,我们测试了沿着旧莱茵河(法国/德国)的两种方法的可靠性,以估算上述水条件中的粒度分布(GSD):(i)基于自动的低成本地面点击性方法使用数字粒度(DGS)软件和(ii)机载LIDAR Topo-Bathy-Bathy-Search的程序。我们还测试了陆地的能力,以估计水下条件中的GSD。进行场鹅卵石计数以比较和校准两种方法。结果表明,陆地度量的自动过程是一种可靠的方法,以估计高于水和水下条件的沉积物斑块的可靠方法。敏感性分析表明,环境条件,包括太阳能照明条件和岩体变异性,显着影响了GSD在水上的自动过程中。使用自动程序显着改变了水下条件中生物膜的存在显着改变了GSD估计,但是所提出的手动程序会克服这个问题。空中激光雷达的地形调查是估计上面水床形的GSD的准确方法,能够产生晶粒尺寸图。地面光相和空中地形激发乐队方法的结合适用于评估GSD在几公里长到达大型河流。 (c)2020 John Wiley&Sons,Ltd。

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