Characterizing the effects of morphological microstructures and hydropeaks on fish stranding in rivers
Fish stranding in rivers, due to rapid shoreline dewatering, often occurs during the down‐ramping phase of hydropeaks, which enables peak energy production. Multiple hydropeaking characteristics and river morphology influence stranding, but little is known about the effects of riverbed microstructur...
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Published in | River research and applications Vol. 40; no. 5; pp. 834 - 849 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Chichester, UK
John Wiley & Sons, Ltd
01.06.2024
Wiley Subscription Services, Inc Wiley |
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Abstract | Fish stranding in rivers, due to rapid shoreline dewatering, often occurs during the down‐ramping phase of hydropeaks, which enables peak energy production. Multiple hydropeaking characteristics and river morphology influence stranding, but little is known about the effects of riverbed microstructures. Our goal was to identify how the combination of hydropeaking characteristics and the occurrence of morphological microstructures (e.g., puddles and scour pools) influences fish stranding. For this purpose, we used an extensive dataset of fish stranding observations collected over 3 years in spring at 48 sites along a 50 km‐long reach of the Ain River, France. We aimed (1) to characterize stranding events and their associated fish assemblages and (2) to identify the spatial and temporal determinants of stranding. The occurrence of morphological microstructures was the main factor explaining fish stranding. Scour pools had a strong impact, followed by scour puddles, humid zones, and alluvial puddles. Then, hydropeaking characteristics interacted with morphology and modulated the intensity of stranding. Low flow ranges (low peak flow and low base flow) occurring after periods without hydropeaks induced ‘salmonid fry’ stranding events and ‘super‐stranding’ events (massive stranding of many taxa). Other flow ranges induced ‘regular cyprinid fry’ stranding events. Salmonids were particularly subject to stranding at the beginning of the sampling period. Recommendations are (1) to act in priority on sites where stranding is most likely, by morphological operations or by installing attractive structures in the perennial area and (2) to maintain attractive, perennial habitats in the low flow range of hydropeaks, for example, by increasing base flow. |
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AbstractList | Fish stranding in rivers, due to rapid shoreline dewatering, often occurs during the down‐ramping phase of hydropeaks, which enables peak energy production. Multiple hydropeaking characteristics and river morphology influence stranding, but little is known about the effects of riverbed microstructures. Our goal was to identify how the combination of hydropeaking characteristics and the occurrence of morphological microstructures (e.g., puddles and scour pools) influences fish stranding. For this purpose, we used an extensive dataset of fish stranding observations collected over 3 years in spring at 48 sites along a 50 km‐long reach of the Ain River, France. We aimed (1) to characterize stranding events and their associated fish assemblages and (2) to identify the spatial and temporal determinants of stranding. The occurrence of morphological microstructures was the main factor explaining fish stranding. Scour pools had a strong impact, followed by scour puddles, humid zones, and alluvial puddles. Then, hydropeaking characteristics interacted with morphology and modulated the intensity of stranding. Low flow ranges (low peak flow and low base flow) occurring after periods without hydropeaks induced ‘salmonid fry’ stranding events and ‘super‐stranding’ events (massive stranding of many taxa). Other flow ranges induced ‘regular cyprinid fry’ stranding events. Salmonids were particularly subject to stranding at the beginning of the sampling period. Recommendations are (1) to act in priority on sites where stranding is most likely, by morphological operations or by installing attractive structures in the perennial area and (2) to maintain attractive, perennial habitats in the low flow range of hydropeaks, for example, by increasing base flow. Abstract Fish stranding in rivers, due to rapid shoreline dewatering, often occurs during the down‐ramping phase of hydropeaks, which enables peak energy production. Multiple hydropeaking characteristics and river morphology influence stranding, but little is known about the effects of riverbed microstructures. Our goal was to identify how the combination of hydropeaking characteristics and the occurrence of morphological microstructures (e.g., puddles and scour pools) influences fish stranding. For this purpose, we used an extensive dataset of fish stranding observations collected over 3 years in spring at 48 sites along a 50 km‐long reach of the Ain River, France. We aimed (1) to characterize stranding events and their associated fish assemblages and (2) to identify the spatial and temporal determinants of stranding. The occurrence of morphological microstructures was the main factor explaining fish stranding. Scour pools had a strong impact, followed by scour puddles, humid zones, and alluvial puddles. Then, hydropeaking characteristics interacted with morphology and modulated the intensity of stranding. Low flow ranges (low peak flow and low base flow) occurring after periods without hydropeaks induced ‘salmonid fry’ stranding events and ‘super‐stranding’ events (massive stranding of many taxa). Other flow ranges induced ‘regular cyprinid fry’ stranding events. Salmonids were particularly subject to stranding at the beginning of the sampling period. Recommendations are (1) to act in priority on sites where stranding is most likely, by morphological operations or by installing attractive structures in the perennial area and (2) to maintain attractive, perennial habitats in the low flow range of hydropeaks, for example, by increasing base flow. |
Author | Cattaneo, Franck Insulaire, Flora Paillex, Amael Capra, Hervé Lamouroux, Nicolas Barillier, Agnès Gouraud, Véronique |
Author_xml | – sequence: 1 givenname: Flora surname: Insulaire fullname: Insulaire, Flora email: insulaire.flora@gmail.com organization: EDF R&D LNHE, Laboratoire National d’Hydraulique et Environnement – sequence: 2 givenname: Nicolas orcidid: 0000-0002-9184-2558 surname: Lamouroux fullname: Lamouroux, Nicolas organization: RiverLy research unit, INRAE – sequence: 3 givenname: Agnès surname: Barillier fullname: Barillier, Agnès organization: EDF CIH, Savoie Technolac – sequence: 4 givenname: Amael surname: Paillex fullname: Paillex, Amael organization: ECOTEC Environment SA – sequence: 5 givenname: Hervé orcidid: 0000-0002-3965-4314 surname: Capra fullname: Capra, Hervé organization: RiverLy research unit, INRAE – sequence: 6 givenname: Franck surname: Cattaneo fullname: Cattaneo, Franck organization: Hepia – University of Applied Sciences and Arts Western Switzerland – sequence: 7 givenname: Véronique surname: Gouraud fullname: Gouraud, Véronique organization: EDF R&D LNHE, Laboratoire National d’Hydraulique et Environnement |
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Keywords | dam yprinids stranding flow management Ain Riverc rsalmonids hydropowe |
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Snippet | Fish stranding in rivers, due to rapid shoreline dewatering, often occurs during the down‐ramping phase of hydropeaks, which enables peak energy production.... Abstract Fish stranding in rivers, due to rapid shoreline dewatering, often occurs during the down‐ramping phase of hydropeaks, which enables peak energy... |
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SubjectTerms | Ain River Base flow Cyprinidae cyprinids dam data collection Dewatering energy Environmental Sciences Fish flow management Fluvial morphology France Fry hydropower Low flow Microstructure Morphology Physical characteristics Puddles River beds Riverbeds Rivers Salmonidae Salmonids shorelines spring Stranding stream channels |
Title | Characterizing the effects of morphological microstructures and hydropeaks on fish stranding in rivers |
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