Using a dense seismic array to study fluvial processes in a braided river reach under flood conditions

Dense seismic array monitoring has recently allowed the detailed investigation of sources of ground vibrations and their spatiotemporal dynamics. In a context where traditional monitoring techniques for fluvial processes often do not provide data with adequate temporal and spatial resolution, the us...

Full description

Bibliographic Details
Main Authors: Marco Piantini, Florent Gimbert, Maarten Bakker, Alain Recking, Ugo Nanni
Format: Article
Language:English
Published: Taylor & Francis Group 2022-05-01
Series:LHB Hydroscience Journal
Subjects:
Online Access:https://www.tandfonline.com/doi/10.1080/27678490.2022.2053314
_version_ 1818204090885210112
author Marco Piantini
Florent Gimbert
Maarten Bakker
Alain Recking
Ugo Nanni
author_facet Marco Piantini
Florent Gimbert
Maarten Bakker
Alain Recking
Ugo Nanni
author_sort Marco Piantini
collection DOAJ
description Dense seismic array monitoring has recently allowed the detailed investigation of sources of ground vibrations and their spatiotemporal dynamics. In a context where traditional monitoring techniques for fluvial processes often do not provide data with adequate temporal and spatial resolution, the use of dense arrays could allow the identification and tracking of different sources of river-induced seismic ground vibrations (e.g. turbulence and bedload transport). Here, we study the potential of dense seismic array monitoring by investigating a high-flow event that occurred in summer 2019 along a 600-m-long braided reach of the Séveraisse River (French Alps). We use a network of 80 seismometers deployed on both river banks, and we supplement the seismic observations with flow gauging measurements and time-lapse imagery. During this event, we observe impulsive signals that are coherently detected over the array, and which we interpret as being associated with the bedload transport of clusters of coarse grains (blocks). Through phase-delay analysis we are able to locate these seismic events on the bend apex of an active branch of the reach. These results demonstrate the capability of such a method to locate bedload activity at high spatiotemporal resolution, providing crucial information for geomorphological investigations and natural risk management.
first_indexed 2024-12-12T03:35:43Z
format Article
id doaj.art-59e385a2207c4276b0d8714fae110cc1
institution Directory Open Access Journal
issn 2767-8490
language English
last_indexed 2024-12-12T03:35:43Z
publishDate 2022-05-01
publisher Taylor & Francis Group
record_format Article
series LHB Hydroscience Journal
spelling doaj.art-59e385a2207c4276b0d8714fae110cc12022-12-22T00:39:49ZengTaylor & Francis GroupLHB Hydroscience Journal2767-84902022-05-0110.1080/27678490.2022.2053314Using a dense seismic array to study fluvial processes in a braided river reach under flood conditionsMarco Piantini0Florent Gimbert1Maarten Bakker2Alain Recking3Ugo Nanni4CNRS, IRD, Institute for Geosciences and Environmental Research (IGE), University Grenoble Alpes, Grenoble, FranceCNRS, IRD, Institute for Geosciences and Environmental Research (IGE), University Grenoble Alpes, Grenoble, FranceCNRS, IRD, Institute for Geosciences and Environmental Research (IGE), University Grenoble Alpes, Grenoble, FranceINRAE, ETNA, University Grenoble Alpes, Grenoble, FranceDepartment of Geosciences, University of Oslo, Oslo, NorwayDense seismic array monitoring has recently allowed the detailed investigation of sources of ground vibrations and their spatiotemporal dynamics. In a context where traditional monitoring techniques for fluvial processes often do not provide data with adequate temporal and spatial resolution, the use of dense arrays could allow the identification and tracking of different sources of river-induced seismic ground vibrations (e.g. turbulence and bedload transport). Here, we study the potential of dense seismic array monitoring by investigating a high-flow event that occurred in summer 2019 along a 600-m-long braided reach of the Séveraisse River (French Alps). We use a network of 80 seismometers deployed on both river banks, and we supplement the seismic observations with flow gauging measurements and time-lapse imagery. During this event, we observe impulsive signals that are coherently detected over the array, and which we interpret as being associated with the bedload transport of clusters of coarse grains (blocks). Through phase-delay analysis we are able to locate these seismic events on the bend apex of an active branch of the reach. These results demonstrate the capability of such a method to locate bedload activity at high spatiotemporal resolution, providing crucial information for geomorphological investigations and natural risk management.https://www.tandfonline.com/doi/10.1080/27678490.2022.2053314Fluvial seismologydense seismic array monitoringbraided riversbedload transportSismologie fluviale reseau sismique dense 
spellingShingle Marco Piantini
Florent Gimbert
Maarten Bakker
Alain Recking
Ugo Nanni
Using a dense seismic array to study fluvial processes in a braided river reach under flood conditions
LHB Hydroscience Journal
Fluvial seismology
dense seismic array monitoring
braided rivers
bedload transport
Sismologie fluviale 
reseau sismique dense 
title Using a dense seismic array to study fluvial processes in a braided river reach under flood conditions
title_full Using a dense seismic array to study fluvial processes in a braided river reach under flood conditions
title_fullStr Using a dense seismic array to study fluvial processes in a braided river reach under flood conditions
title_full_unstemmed Using a dense seismic array to study fluvial processes in a braided river reach under flood conditions
title_short Using a dense seismic array to study fluvial processes in a braided river reach under flood conditions
title_sort using a dense seismic array to study fluvial processes in a braided river reach under flood conditions
topic Fluvial seismology
dense seismic array monitoring
braided rivers
bedload transport
Sismologie fluviale 
reseau sismique dense 
url https://www.tandfonline.com/doi/10.1080/27678490.2022.2053314
work_keys_str_mv AT marcopiantini usingadenseseismicarraytostudyfluvialprocessesinabraidedriverreachunderfloodconditions
AT florentgimbert usingadenseseismicarraytostudyfluvialprocessesinabraidedriverreachunderfloodconditions
AT maartenbakker usingadenseseismicarraytostudyfluvialprocessesinabraidedriverreachunderfloodconditions
AT alainrecking usingadenseseismicarraytostudyfluvialprocessesinabraidedriverreachunderfloodconditions
AT ugonanni usingadenseseismicarraytostudyfluvialprocessesinabraidedriverreachunderfloodconditions