Towards the hydrologic and bed load monitoring from high-frequency seismic noise in a braided river: The “torrent de St Pierre”, French Alps

• Published in: Journal of hydrology (Amsterdam) 2011-09, Vol.408 (1), p.43-53
• Main Authors: Burtin, Arnaud, Cattin, Rodolphe, Bollinger, Laurent, Vergne, Jérôme, Steer, Philippe, Robert, Alexandra, Findling, Nathaniel, Tiberi, Christel
• Format: Article
• Language: English
• Subjects: Applied geophysics; Bed load monitoring; Braided river; Earth sciences; Earth, ocean, space; energy; energy content; energy use and consumption; Exact sciences and technology; glaciers; Hydrology; Hydrology. Hydrogeology; Internal geophysics; Marine and continental quaternary; melting; monitoring; mountains; Noise; pollution load; rain; River seismic noise; Rivers; Sciences of the Universe; Sediment transport; Sediments; Seismic energy; Seismic engineering; Seismic phenomena; shear stress; stream channels; summer; Surficial geology; temperature; Torrents; turbulent flow; water flow; water stress
• ISSN: 0022-1694; 1879-2707
• DOI: 10.1016/j.jhydrol.2011.07.014

► High-frequency (>1 Hz) river seismic noise to continuously survey bed load transport. ► HF seismic energy is consistent with the observed hydrology and bed load changes. ► Spectral analysis helps to discriminate the signal from water and bed load transport. ► Seismic monitoring of bed load is possible in a broad range of hydraulic conditions. We explore the use of seismic noise produced by rivers to monitor the bed load transport in the case of a low-discharge braided river in the French Alps: the “torrent de St Pierre”. For this purpose, we deployed two dedicated seismic networks during summers 2007 and 2008, for which the characteristics of the recorded continuous signal are similar despite changes in the sensor locations. For dry weather conditions, only melting of nearby glaciers controls the supply of water to the stream. In these conditions, the river hydrology and the seismic energy in the 2–80 Hz frequency band both follow a diurnal fluctuation similar to the thermal amplitude. In contrast during rainfall episodes, the temperature variation fails to explain the hydrodynamic changes. Dense cloud covers reduce glacier melting and the recorded seismic energy denotes bursts of high-frequency seismic noise well correlated with water level data. Comparisons between the recorded seismic signals and the collected hydrological and sediment load data indicate that a frequency band of 3–9 Hz best explains the water level changes and thus the seismic waves coming from the flow turbulence. These analyses also reveal the presence of a seismic noise threshold that might be linked to the water shear stress exerted by the flowing water. Using the seismic energy in this frequency band as a proxy of the fluvial shear stress, the seismic–hydrologic relationship may be sensitive to variations in bed load transport. The spectral content of the seismic energy shows patterns consistent with the mobilization of sediment particles. From the interpretations of the seismic wave attenuation of river sources, we finally propose that stations at a distance from the stream less than 50 m are able to record most sediment particles. Farther stations are still useful during extreme events when largest grain sizes are mobilized. More generally this study demonstrates the feasibility of using the river seismic signal to survey bed load transport in various river types from small braided mountain rivers like the “torrent de St Pierre” to the large entrenched Himalayan rivers.