Uncovering Hidden Secrets: Using Geophysics to Study Sedimentary Deposits Upstream of Dams

Friday 07 March 2025


Scientists have long been fascinated by the mysterious world of sedimentary deposits upstream of run-of-the-river dams, and for good reason. These deposits can have a significant impact on the operation and safety of the dam, as well as the surrounding environment.


To better understand these deposits, researchers from the University of Lyon and the Centre d’Analyse Comportementale des Ouvrages Hydrauliques (CACOH) in France used a combination of geophysical methods to study sedimentary deposits upstream of dams. They focused on two specific techniques: Sub Bottom Profiling (SBP) and Ground Penetrating Radar (GPR).


The SBP method uses low-frequency sound waves to penetrate the sediment and scan for underlying layers, while GPR uses electromagnetic radiation to create high-resolution images of subsurface structures. By combining these methods, researchers were able to gain a deeper understanding of the internal structures of the sedimentary deposits.


One of the key findings was that different sediment units could be identified using the geophysical signals. These units corresponded to distinct events in the sedimentological evolution of the deposits, such as dredging and flood periods. By analyzing these events, researchers were able to reconstruct the history of sediment deposition upstream of the dam.


The implications of this study are significant. By understanding the internal structures of sedimentary deposits, dam operators can better manage the risk of sediment accumulation and optimize field campaigns. This approach can also help reduce management costs by identifying areas where new sediment cores may be necessary.


The researchers tested their methodology on several dam reservoirs in the Upper Rhône region of France, including the Chautagne reservoir. Their findings were impressive: they were able to identify two distinct events that had a significant impact on the sedimentological evolution of the deposits.


One event was a dredging operation in 2009, which compacted the sediments due to the weight of the dredging machine. The second event was a flood period that created an erosion surface. By analyzing these events, researchers were able to gain a better understanding of how sedimentary deposits are formed and evolve over time.


The use of geophysical methods in this study provides a powerful tool for dam operators and environmental scientists. By combining SBP and GPR techniques, researchers can non-invasively examine the internal structures of sedimentary deposits without disrupting the surrounding environment.


This approach has significant implications for our understanding of sedimentary deposits and their impact on water management.


Cite this article: “Uncovering Hidden Secrets: Using Geophysics to Study Sedimentary Deposits Upstream of Dams”, The Science Archive, 2025.


Sedimentary Deposits, Run-Of-The-River Dams, Geophysical Methods, Sub Bottom Profiling, Ground Penetrating Radar, Sedimentological Evolution, Dam Operation, Risk Management, Upper Rhône Region, France


Reference: Anne Weit, Thierry Winiarski, Brice Mourier, Thierry Fretaud, Christophe Peteuil, “Interest of geophysical methods to determine the evolution and the spatial distribution of sedimentary deposits upstream of run-of-the-river dams (Upper Rh{ô}ne, France)” (2025).


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