Riverbed sediment classification using multi-beam echo-sounder backscatter data

被引:51
作者
Amiri-Simkooei, AliReza [1 ,2 ]
Snellen, Miriam [1 ]
Simons, Dick G. [1 ]
机构
[1] Delft Univ Technol, Fac Aerosp Engn, Delft Inst Earth Observat & Space Syst DEOS, Acoust Remote Sensing Grp, NL-2629 HS Delft, Netherlands
[2] Univ Isfahan, Dept Surveying Engn, Esfahan 81744, Iran
关键词
SEA-FLOOR CHARACTERIZATION; GRAIN-SIZE DISTRIBUTION; SONAR DATA; STATISTICS; SCATTERING; SHELF; PARAMETERS; INTENSITY; CLUTTER; SURFACE;
D O I
10.1121/1.3205397
中图分类号
O42 [声学];
学科分类号
070206 ; 082403 ;
摘要
A method has recently been developed that employs multi-beam echo-sounder backscatter data to both obtain the number of sediment classes and discriminate between them by applying the Bayes decision rule to multiple hypotheses [Simons and Snellen, Appl. Acoust. 70, 1258-1268 (2009)]. In deep water, the number of scatter pixels within the beam footprint is large enough to ensure Gaussian distributions for the backscatter strengths and to increase the discriminative power between acoustic classes. In very shallow water (< 10 m), however, this number is too small. This paper presents an extension of this high-frequency methodology for these environments, together with a demonstration of its performance using backscatter data from the river Waal, The Netherlands. The objective of this work is threefold. (i) Increasing the discriminating power of the classification method: high-resolution bathymetry data allow precise bottom slope corrections for obtaining the true incident angle, and the high-resolution backscatter data reduce the statistical fluctuations via an averaging procedure. (h) Performing a correlation analysis: the dependence of acoustic backscatter classification on sediment physical properties is verified by observing a significant correlation of 0.75 (and a disattenuated correlation of 0.90) between the classification results and sediment mean grain size. (iii) Enhancing the statistical description of the backscatter intensities: angular evolution of the K-distribution shape parameter indicates that the riverbed is a rough surface, in agreement with the results of the core analysis, (C) 2009 Acoustical Society of America. [DOI: 10.1121/1.3205397]
引用
收藏
页码:1724 / 1738
页数:15
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