Survival of Atlantic Salmon (Salmo salar) Eggs During Dewatering in a River Subjected to Hydropeaking

Hydropeaking in regulated rivers is likely to become more frequent with increasing demands for renewable energy. Sudden fluctuations affect surface and subsurface flow regimes and change hydrological interactions occurring in the hyporheic zone. The hyporheic zone plays an important role for salmon...

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Published inRiver research and applications Vol. 31; no. 4; pp. 433 - 446
Main Authors Casas‐Mulet, R, Saltveit, S. J, Alfredsen, K
Format Journal Article
LanguageEnglish
Published Bognor Regis John Wiley & Sons 01.05.2015
Blackwell Publishing Ltd
Wiley Subscription Services, Inc
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ISSN1535-1459
1535-1467
DOI10.1002/rra.2827

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Abstract Hydropeaking in regulated rivers is likely to become more frequent with increasing demands for renewable energy. Sudden fluctuations affect surface and subsurface flow regimes and change hydrological interactions occurring in the hyporheic zone. The hyporheic zone plays an important role for salmon embryonic development, and groundwater influx may create refuges for egg survival during low flow in hydropeaking regulated rivers. The links between salmon embryo survival and hyporheic hydrological processes during hydropeaking have hardly been investigated. A field experiment was undertaken in a 5 × 20 m side gravel bar subject to dewatering due to hydropeaking. Eleven cylindrical boxes composed of eight compartments were placed in the permanently wet area and the ramping zone. Sixty eggs were placed in two compartments (at 10 and 30 cm depth) in each box. Surface and interstitial water levels and temperatures were monitored at 2 min resolution. Data were collected for a period of 3 months, coinciding with early stages of salmonid egg development in this catchment. Egg compartments were checked on six occasions for survival after different hydropeaking events. Dead eggs were counted and removed. Survival rates were lower in the top compartments in the ramping zone (78%) compared with the boxes in the permanently wet area and the lowermost compartments in the ramping (survival rates >99%). With no water quality issues in the catchment and very low inputs of fine sediments in the egg compartments, exposure to dry conditions and subzero temperatures were the main factors explaining egg mortality in the top compartments of the ramping zone. The rate of survival will thus depend on the surface water and groundwater interactions. Site‐specific hydrological interactions occurring in the hyporheic zone should be actively considered when managing fish populations in rivers with hydropeaking. Copyright © 2014 John Wiley & Sons, Ltd.
AbstractList Hydropeaking in regulated rivers is likely to become more frequent with increasing demands for renewable energy. Sudden fluctuations affect surface and subsurface flow regimes and change hydrological interactions occurring in the hyporheic zone. The hyporheic zone plays an important role for salmon embryonic development, and groundwater influx may create refuges for egg survival during low flow in hydropeaking regulated rivers. The links between salmon embryo survival and hyporheic hydrological processes during hydropeaking have hardly been investigated. A field experiment was undertaken in a 520m side gravel bar subject to dewatering due to hydropeaking. Eleven cylindrical boxes composed of eight compartments were placed in the permanently wet area and the ramping zone. Sixty eggs were placed in two compartments (at 10 and 30cm depth) in each box. Surface and interstitial water levels and temperatures were monitored at 2min resolution. Data were collected for a period of 3months, coinciding with early stages of salmonid egg development in this catchment. Egg compartments were checked on six occasions for survival after different hydropeaking events. Dead eggs were counted and removed. Survival rates were lower in the top compartments in the ramping zone (78%) compared with the boxes in the permanently wet area and the lowermost compartments in the ramping (survival rates >99%). With no water quality issues in the catchment and very low inputs of fine sediments in the egg compartments, exposure to dry conditions and subzero temperatures were the main factors explaining egg mortality in the top compartments of the ramping zone. The rate of survival will thus depend on the surface water and groundwater interactions. Site-specific hydrological interactions occurring in the hyporheic zone should be actively considered when managing fish populations in rivers with hydropeaking.
Hydropeaking in regulated rivers is likely to become more frequent with increasing demands for renewable energy. Sudden fluctuations affect surface and subsurface flow regimes and change hydrological interactions occurring in the hyporheic zone. The hyporheic zone plays an important role for salmon embryonic development, and groundwater influx may create refuges for egg survival during low flow in hydropeaking regulated rivers. The links between salmon embryo survival and hyporheic hydrological processes during hydropeaking have hardly been investigated. A field experiment was undertaken in a 5 × 20 m side gravel bar subject to dewatering due to hydropeaking. Eleven cylindrical boxes composed of eight compartments were placed in the permanently wet area and the ramping zone. Sixty eggs were placed in two compartments (at 10 and 30 cm depth) in each box. Surface and interstitial water levels and temperatures were monitored at 2 min resolution. Data were collected for a period of 3 months, coinciding with early stages of salmonid egg development in this catchment. Egg compartments were checked on six occasions for survival after different hydropeaking events. Dead eggs were counted and removed. Survival rates were lower in the top compartments in the ramping zone (78%) compared with the boxes in the permanently wet area and the lowermost compartments in the ramping (survival rates >99%). With no water quality issues in the catchment and very low inputs of fine sediments in the egg compartments, exposure to dry conditions and subzero temperatures were the main factors explaining egg mortality in the top compartments of the ramping zone. The rate of survival will thus depend on the surface water and groundwater interactions. Site‐specific hydrological interactions occurring in the hyporheic zone should be actively considered when managing fish populations in rivers with hydropeaking. Copyright © 2014 John Wiley & Sons, Ltd.
Hydropeaking in regulated rivers is likely to become more frequent with increasing demands for renewable energy. Sudden fluctuations affect surface and subsurface flow regimes and change hydrological interactions occurring in the hyporheic zone. The hyporheic zone plays an important role for salmon embryonic development, and groundwater influx may create refuges for egg survival during low flow in hydropeaking regulated rivers. The links between salmon embryo survival and hyporheic hydrological processes during hydropeaking have hardly been investigated. A field experiment was undertaken in a 5×20m side gravel bar subject to dewatering due to hydropeaking. Eleven cylindrical boxes composed of eight compartments were placed in the permanently wet area and the ramping zone. Sixty eggs were placed in two compartments (at 10 and 30cm depth) in each box. Surface and interstitial water levels and temperatures were monitored at 2min resolution. Data were collected for a period of 3months, coinciding with early stages of salmonid egg development in this catchment. Egg compartments were checked on six occasions for survival after different hydropeaking events. Dead eggs were counted and removed. Survival rates were lower in the top compartments in the ramping zone (78%) compared with the boxes in the permanently wet area and the lowermost compartments in the ramping (survival rates >99%). With no water quality issues in the catchment and very low inputs of fine sediments in the egg compartments, exposure to dry conditions and subzero temperatures were the main factors explaining egg mortality in the top compartments of the ramping zone. The rate of survival will thus depend on the surface water and groundwater interactions. Site-specific hydrological interactions occurring in the hyporheic zone should be actively considered when managing fish populations in rivers with hydropeaking. Copyright © 2014 John Wiley & Sons, Ltd.
Hydropeaking in regulated rivers is likely to become more frequent with increasing demands for renewable energy. Sudden fluctuations affect surface and subsurface flow regimes and change hydrological interactions occurring in the hyporheic zone. The hyporheic zone plays an important role for salmon embryonic development, and groundwater influx may create refuges for egg survival during low flow in hydropeaking regulated rivers. The links between salmon embryo survival and hyporheic hydrological processes during hydropeaking have hardly been investigated. A field experiment was undertaken in a 5 × 20 m side gravel bar subject to dewatering due to hydropeaking. Eleven cylindrical boxes composed of eight compartments were placed in the permanently wet area and the ramping zone. Sixty eggs were placed in two compartments (at 10 and 30 cm depth) in each box. Surface and interstitial water levels and temperatures were monitored at 2 min resolution. Data were collected for a period of 3 months, coinciding with early stages of salmonid egg development in this catchment. Egg compartments were checked on six occasions for survival after different hydropeaking events. Dead eggs were counted and removed. Survival rates were lower in the top compartments in the ramping zone (78%) compared with the boxes in the permanently wet area and the lowermost compartments in the ramping (survival rates >99%). With no water quality issues in the catchment and very low inputs of fine sediments in the egg compartments, exposure to dry conditions and subzero temperatures were the main factors explaining egg mortality in the top compartments of the ramping zone. The rate of survival will thus depend on the surface water and groundwater interactions. Site‐specific hydrological interactions occurring in the hyporheic zone should be actively considered when managing fish populations in rivers with hydropeaking. Copyright © 2014 John Wiley & Sons, Ltd.
Hydropeaking in regulated rivers is likely to become more frequent with increasing demands for renewable energy. Sudden fluctuations affect surface and subsurface flow regimes and change hydrological interactions occurring in the hyporheic zone. The hyporheic zone plays an important role for salmon embryonic development, and groundwater influx may create refuges for egg survival during low flow in hydropeaking regulated rivers. The links between salmon embryo survival and hyporheic hydrological processes during hydropeaking have hardly been investigated. A field experiment was undertaken in a 5 × 20 m side gravel bar subject to dewatering due to hydropeaking. Eleven cylindrical boxes composed of eight compartments were placed in the permanently wet area and the ramping zone. Sixty eggs were placed in two compartments (at 10 and 30 cm depth) in each box. Surface and interstitial water levels and temperatures were monitored at 2 min resolution. Data were collected for a period of 3 months, coinciding with early stages of salmonid egg development in this catchment. Egg compartments were checked on six occasions for survival after different hydropeaking events. Dead eggs were counted and removed. Survival rates were lower in the top compartments in the ramping zone (78%) compared with the boxes in the permanently wet area and the lowermost compartments in the ramping (survival rates >99%). With no water quality issues in the catchment and very low inputs of fine sediments in the egg compartments, exposure to dry conditions and subzero temperatures were the main factors explaining egg mortality in the top compartments of the ramping zone. The rate of survival will thus depend on the surface water and groundwater interactions. Site‐specific hydrological interactions occurring in the hyporheic zone should be actively considered when managing fish populations in rivers with hydropeaking.
Author Alfredsen, K
Casas‐Mulet, R
Saltveit, S. J
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Becker CD, Neitzel DA, Fickeisen DH. 1982. Effects of dewatering on Chinook salmon redds: tolerance of four developmental phases to daily dewaterings. Transactions of the American Fisheries Society 111(5): 624-637.
Mills DH. 1989. Ecology and Management of Atlantic Salmon. Chapman and Hall: London.
de Gaudemar B, Schroder S, Beall E. 2000. Nest placement and egg distribution in Atlantic salmon redds, Environmental Biology of Fishes 57(1): 37-47.
Cushman RM. 1985. Review of ecological effects of rapidly varying flows downstream of hydroelectric facilities. North American Journal of Fisheries Management 5: 330-339.
Saltveit SJ, Halleraker JH, Arnekleiv JV, Harby A. 2001. Field experiments on stranding in juvenile Atlantic salmon (Salmo salar) and brown trout (Salmo trutta) during rapid flow decreases caused by hydropeaking, Regulated Rivers: Research & Management 17(4-5): 609-622.
Hansen EA. 1975. Some effects of groundwater on brown trout redds. Transactions of the American Fisheries Society 104(1): 100-110.
Cunjak RA, Prowse TD, Parrish DL. 1998. Atlantic salmon (Salmo salar) in winter: "the season of parr discontent"? Canadian Journal of Fisheries and Aquatic Sciences 55(S1): 161-180.
Malcolm I, Youngson AF, Soulsby C. 2003. Survival of salmonid eggs in a degraded gravel-bed stream: effects of groundwater-surface water interactions. River Research and Applications 19(4): 303-316.
Becker CD, Neitzel D. 1985. Assessment of intergravel conditions influencing egg and alevin survival during salmonid redd dewatering. Environmental Biology of Fishes 12(1): 33-46.
Fraser J. 1985. Shoal spawning of brook trout, Salvelinus fontinalis, in a Precambrian Shield lake. Naturaliste Canadien. 112(2): 163-174.
Sear DA, Pattison I, Collins AL, Newson MD, Jones JI, Naden PS, Carling PA. 2012. Factors controlling the temporal variability in dissolved oxygen regime of salmon spawning gravels. Hydrological Processes 28: 86-103.
Malcolm I, Middlemas CA, Soulsby C, Middlemas SJ, Youngson AF. 2010. Hyporheic zone processes in a canalised agricultural stream: implications for salmonid embryo survival. Fundamental and Applied Limnology 176(4): 319-336.
Brabrand Å, Koestler AG, Borgstrøm R. 2002. Lake spawning of brown trout related to groundwater influx. Journal of Fish Biology 60(3): 751-763.
Moir HJ, Soulsby C, Youngson AF. 2002. Hydraulic and sedimentary controls on the availability and use of Atlantic salmon (Salmo salar) spawning habitat in the River Dee system, north-east Scotland. Geomorphology 45(3): 291-308.
Curry RA, Powles P, Gunn J, Liimatainen V. 1991. Emergence chronology of brook charr,Salvenus fontinalis, alevins in an acidic stream. Environmental Biology of Fishes 31(1): 25-31.
Young P, Cech J Jr., Thompson L. 2011. Hydropower-related pulsed-flow impacts on stream fishes: a brief review, conceptual model, knowledge gaps, and research needs Reviews in Fish Biology and Fisheries 21(4): 713-731.
McMichael GA, Rakowski CL, James BB, Lukas JA. 2005. Estimated fall Chinook salmon survival to emergence in dewatered redds in a shallow side channel of the Columbia River. North American Journal of Fisheries Management 25(3): 876-884.
Schmidt SI, Hahn HJ. 2012. What is groundwater and what does this mean to fauna? - an opinion. Limnologica - Ecology and Management of Inland Waters 42(1): 1-6.
Curry RA, Gehrels J, Noakes DG, Swainson R. 1994. Effects of river flow fluctuations on groundwater discharge through brook trout, Salvelinus fontinalis, spawning and incubation habitats. Hydrobiologia 277(2): 121-134.
Baxter JS, McPhail JD. 1999. The influence of redd site selection, groundwater upwelling, and over-winter incubation temperature on survival of bull trout (Salvelinus confluentus) from egg to alevin. Canadian Journal of Zoology 77(8): 1233-1239.
1994; 277
2004; 61
1982; 39
1983; 112
1985; 5
2012
1983; 3
2011
2013; 43
1991; 31
1986; 17
2008
2005; 41
2007
2012; 19
2005
2002; 60
1992
2003; 19
1985; 27
1978
2005; 25
1998; 18
1984; 53
2000; 57
2002; 45
1982; 111
1985; 112
2010; 176
1999; 13
1999; 77
1985; 114
2011; 21
2008; 65
2012; 28
2001; 17
1975; 104
1985; 12
1979; 41
1998; 55
2012; 42
1989
2009; 17
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Snippet Hydropeaking in regulated rivers is likely to become more frequent with increasing demands for renewable energy. Sudden fluctuations affect surface and...
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SubjectTerms Boxes (containers)
Compartments
Dewatering
Eggs
embryogenesis
Embryonic growth stage
field experimentation
Fish populations
Gravel
groundwater
Hydrology
hydropeaking
hyporheic zone
Hyporheic zones
Low flow
Regulated rivers
Renewable energy
renewable energy sources
River regulations
Rivers
Salmo salar
Salmon
salmon egg survival
subsurface flow
Surface water
Surface-groundwater relations
Survival
survival rate
temperature
Water depth
Water levels
Water quality
watersheds
Title Survival of Atlantic Salmon (Salmo salar) Eggs During Dewatering in a River Subjected to Hydropeaking
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https://onlinelibrary.wiley.com/doi/abs/10.1002%2Frra.2827
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https://www.proquest.com/docview/1676351370
https://www.proquest.com/docview/1685774622
https://www.proquest.com/docview/1694496024
Volume 31
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