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Improving riverbed sediment classification using backscatter and depth residual features of multi-beam echo-sounder systems

机译:利用多波束回声测深系统的反向散射和深度残留特征改善河床沉积物分类

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摘要

Riverbed and seafloor sediment classification using acoustic remote sensing techniques is of high interest due to their high coverage capabilities at limited cost. This contribution presents the results of riverbed sediment classification using multi-beam echo-sounder data based on an empirical method. Two data sets are considered, both taken at the Waal River, namely Sint Andries and Nijmegen. This work is a follow-up to the work carried out by Amiri-Simkooei et al. [J. Acoust. Soc. Am. 126(4), 1724–1738 (2009)]. The empirical method bases the classification on features of the backscatter strength and depth residuals. A principal component analysis is used to identify the most appropriate and informative features. Clustering is then applied to the principal components resulting from this set of features to assign a sediment class to each measurement. The results show that the backscatter strength features discriminate between different classes based on the sediment properties, whereas the depth residual features discriminate classes based on riverbed forms such as the “fixed layer” (stone having riprap structure) and riverbed ripples. Combination of these two sets of features is highly recommended because they provide complementary information on both the composition and the structure of the riverbed.
机译:由于使用声学遥感技术对河床和海底沉积物进行分类的能力有限,因此备受关注。该贡献使用基于经验方法的多波束回声数据提供了河床沉积物分类的结果。考虑了两个数据集,均在瓦尔河采集,即圣安德里斯和奈梅亨。这项工作是Amiri-Simkooei等人进行的工作的后续工作。 [J. co Soc。上午。 126(4),1724-1738(2009)]。经验方法基于反向散射强度和深度残差的特征进行分类。主成分分析用于识别最合适和最有用的功能。然后将聚类应用于这组功能所产生的主要成分,以将沉积物类别分配给每个测量。结果表明,根据沉积物的性质,后向散射强度特征可以区分不同的类别,而深度残余特征可以根据“固定层”(具有跳石结构的石头)和河床波纹等河床形式来区分。强烈建议将这两种功能组合在一起,因为它们可以提供有关河床组成和结构的补充信息。

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