Acoustic wave propagation in rivers: an experimental study

<p>This research has been conducted to develop the use of passive acoustic monitoring (PAM) in rivers, a surrogate method for bedload monitoring. PAM consists in measuring the underwater noise naturally generated by bedload particles when impacting the river bed. Monitored bedload acoustic sig...

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Main Authors: T. Geay, L. Michel, S. Zanker, J. R. Rigby
Format: Article
Language:English
Published: Copernicus Publications 2019-06-01
Series:Earth Surface Dynamics
Online Access:https://www.earth-surf-dynam.net/7/537/2019/esurf-7-537-2019.pdf
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spelling doaj-6a048ce466534148bbd65eb0c32f150e2020-11-24T22:04:45ZengCopernicus PublicationsEarth Surface Dynamics2196-63112196-632X2019-06-01753754810.5194/esurf-7-537-2019Acoustic wave propagation in rivers: an experimental studyT. Geay0L. Michel1L. Michel2S. Zanker3J. R. Rigby4Univ. Grenoble Alpes, CNRS, Grenoble INP, GIPSA-lab, 38000 Grenoble, FranceUniv. Grenoble Alpes, CNRS, Grenoble INP, GIPSA-lab, 38000 Grenoble, FranceEDF, Division Technique Générale, 38000 Grenoble, FranceEDF, Division Technique Générale, 38000 Grenoble, FranceUSDA-ARS National Sedimentation Laboratory, Oxford, MS, USA<p>This research has been conducted to develop the use of passive acoustic monitoring (PAM) in rivers, a surrogate method for bedload monitoring. PAM consists in measuring the underwater noise naturally generated by bedload particles when impacting the river bed. Monitored bedload acoustic signals depend on bedload characteristics (e.g., grain size distribution, fluxes) but are also affected by the environment in which the acoustic waves are propagated. This study focuses on the determination of propagation effects in rivers. An experimental approach has been conducted in several streams to estimate acoustic propagation laws in field conditions. It is found that acoustic waves are differently propagated according to their frequency. As reported in other studies, acoustic waves are affected by the existence of a cutoff frequency in the kilohertz region. This cutoff frequency is inversely proportional to the water depth: larger water depth enables a better propagation of the acoustic waves at low frequency. Above the cutoff frequency, attenuation coefficients are found to increase linearly with frequency. The power of bedload sounds is more attenuated at higher frequencies than at low frequencies, which means that, above the cutoff frequency, sounds of big particles are better propagated than sounds of small particles. Finally, it is observed that attenuation coefficients are variable within 2 orders of magnitude from one river to another. Attenuation coefficients are compared to several characteristics of the river (e.g., bed slope, surface grain size). It is found that acoustic waves are better propagated in rivers characterized by smaller bed slopes. Bed roughness and the presence of air bubbles in the water column are suspected to constrain the attenuation of acoustic wave in rivers.</p>https://www.earth-surf-dynam.net/7/537/2019/esurf-7-537-2019.pdf
collection DOAJ
language English
format Article
sources DOAJ
author T. Geay
L. Michel
L. Michel
S. Zanker
J. R. Rigby
spellingShingle T. Geay
L. Michel
L. Michel
S. Zanker
J. R. Rigby
Acoustic wave propagation in rivers: an experimental study
Earth Surface Dynamics
author_facet T. Geay
L. Michel
L. Michel
S. Zanker
J. R. Rigby
author_sort T. Geay
title Acoustic wave propagation in rivers: an experimental study
title_short Acoustic wave propagation in rivers: an experimental study
title_full Acoustic wave propagation in rivers: an experimental study
title_fullStr Acoustic wave propagation in rivers: an experimental study
title_full_unstemmed Acoustic wave propagation in rivers: an experimental study
title_sort acoustic wave propagation in rivers: an experimental study
publisher Copernicus Publications
series Earth Surface Dynamics
issn 2196-6311
2196-632X
publishDate 2019-06-01
description <p>This research has been conducted to develop the use of passive acoustic monitoring (PAM) in rivers, a surrogate method for bedload monitoring. PAM consists in measuring the underwater noise naturally generated by bedload particles when impacting the river bed. Monitored bedload acoustic signals depend on bedload characteristics (e.g., grain size distribution, fluxes) but are also affected by the environment in which the acoustic waves are propagated. This study focuses on the determination of propagation effects in rivers. An experimental approach has been conducted in several streams to estimate acoustic propagation laws in field conditions. It is found that acoustic waves are differently propagated according to their frequency. As reported in other studies, acoustic waves are affected by the existence of a cutoff frequency in the kilohertz region. This cutoff frequency is inversely proportional to the water depth: larger water depth enables a better propagation of the acoustic waves at low frequency. Above the cutoff frequency, attenuation coefficients are found to increase linearly with frequency. The power of bedload sounds is more attenuated at higher frequencies than at low frequencies, which means that, above the cutoff frequency, sounds of big particles are better propagated than sounds of small particles. Finally, it is observed that attenuation coefficients are variable within 2 orders of magnitude from one river to another. Attenuation coefficients are compared to several characteristics of the river (e.g., bed slope, surface grain size). It is found that acoustic waves are better propagated in rivers characterized by smaller bed slopes. Bed roughness and the presence of air bubbles in the water column are suspected to constrain the attenuation of acoustic wave in rivers.</p>
url https://www.earth-surf-dynam.net/7/537/2019/esurf-7-537-2019.pdf
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AT lmichel acousticwavepropagationinriversanexperimentalstudy
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AT szanker acousticwavepropagationinriversanexperimentalstudy
AT jrrigby acousticwavepropagationinriversanexperimentalstudy
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