摘要：Bedload Self-Generated Noise (SGN) measurements consist in
deploying an underwater microphone (i.e. a hydrophone) in the water
course and to record the ambient noise of a river. The use of hydrophones
is of interest as it can be easily deployed and can provide a continuous
monitoring of bedload transport. However, developments are still required
to fully understand how bedload characteristics (e.g. specific flux or
granulometry) are related to bedload SGN parameters (e.g. acoustic power
and spectrum). Laboratory experiments have shown that central and peak
frequencies of bedload noise decrease as the particle size increases, just
like in string instruments where the tone frequency decreases from a
narrow string to a broader string. In this paper, we propose to test a new
inverse method enabling the estimation of bedload grain size distributions
from SGN measurements. The inverse method is based on a theoretical
modelling of the noise generated by a bedload mixture. SGN and physical
sampling measurements have been made in 5 French alpine rivers having
several transport conditions (bedload D50 from 1 to 40 mm) and varying
slopes (0.05 to 1%). Measurements were made for specific bedload flux
varying from 10 to 150 g.m-1s-1. The proposed inverse method was used to
estimate the bedload grain size distributions. SGN results are compared to
bedload samples and are found to largely overestimate sampled
granulometries. Finally, it is observed that the spectral characteristics of
bedload SGN are not related to bedload GSD but rather to the roughness of
the river bed, acting as a source of attenuation and shaping bedload SGN
spectra.
其他摘要：Bedload Self-Generated Noise (SGN) measurements consist in deploying an underwater microphone (i.e. a hydrophone) in the water course and to record the ambient noise of a river. The use of hydrophones is of interest as it can be easily deployed and can provide a continuous monitoring of bedload transport. However, developments are still required to fully understand how bedload characteristics (e.g. specific flux or granulometry) are related to bedload SGN parameters (e.g. acoustic power and spectrum). Laboratory experiments have shown that central and peak frequencies of bedload noise decrease as the particle size increases, just like in string instruments where the tone frequency decreases from a narrow string to a broader string. In this paper, we propose to test a new inverse method enabling the estimation of bedload grain size distributions from SGN measurements. The inverse method is based on a theoretical modelling of the noise generated by a bedload mixture. SGN and physical sampling measurements have been made in 5 French alpine rivers having several transport conditions (bedload D50 from 1 to 40 mm) and varying slopes (0.05 to 1%). Measurements were made for specific bedload flux varying from 10 to 150 g.m-1s-1. The proposed inverse method was used to estimate the bedload grain size distributions. SGN results are compared to bedload samples and are found to largely overestimate sampled granulometries. Finally, it is observed that the spectral characteristics of bedload SGN are not related to bedload GSD but rather to the roughness of the river bed, acting as a source of attenuation and shaping bedload SGN spectra.
