Measuring and modelling the dispersal of salmon farm organic waste over sandy sediments

Fish farm waste dispersal models are widely used but have only been directly validated to a limited extent. Two shallow (<20 m) Atlantic salmon farms (Bay of Meil and Quanterness) in Orkney, Scotland were studied. Bay of Meil has peak near-bed currents of 9.7 cm s-1 whereas Quanterness has flows...

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Main Authors: C Fox, C Webb, J Grant, S Brain, S Fraser, R Abell, N Hicks
Format: Article
Language:English
Published: Inter-Research 2023-08-01
Series:Aquaculture Environment Interactions
Online Access:https://www.int-res.com/abstracts/aei/v15/p251-269/
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author C Fox
C Webb
J Grant
S Brain
S Fraser
R Abell
N Hicks
author_facet C Fox
C Webb
J Grant
S Brain
S Fraser
R Abell
N Hicks
author_sort C Fox
collection DOAJ
description Fish farm waste dispersal models are widely used but have only been directly validated to a limited extent. Two shallow (<20 m) Atlantic salmon farms (Bay of Meil and Quanterness) in Orkney, Scotland were studied. Bay of Meil has peak near-bed currents of 9.7 cm s-1 whereas Quanterness has flows up to 31.6 cm s-1. Sediment tray traps which allow resuspension to occur were deployed at each site. The patterns of particulate organic carbon (POC) deposition into the traps were in broad agreement with the observed water current directions and results from infaunal benthic monitoring. Despite the markedly different flow regimes at the 2 sites, most of the deposition occurred within 210 m of the cage perimeters. POC footprints were then modelled using the particle tracking model NewDEPOMOD. For Bay of Meil, a footprint was obtained using the recommended parameter defaults, but the spatial extent was too constrained compared to the sediment tray results. For Quanterness, all simulated particles were lost from the model domain and the critical erosion shear stress had to be increased to unrealistic levels to obtain a footprint. The failure to find a common set of parameter values applicable to both sites, despite their similar depths and sandy seabed, suggests that there remain unresolved issues, likely in how NewDEPOMOD handles waste resuspension. The sediment trays provided a direct method for quantifying the organic carbon deposition, facilitating direct validation of the dispersal model and demonstrating that further research is needed on fish farm waste dispersal at coarser sediment sites.
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spelling doaj.art-ce75d9f6326e45c4a66129997ad1a1c12023-08-28T10:51:14ZengInter-ResearchAquaculture Environment Interactions1869-215X1869-75342023-08-011525126910.3354/aei00464Measuring and modelling the dispersal of salmon farm organic waste over sandy sedimentsC Fox0C Webb1J Grant2S Brain3S Fraser4R Abell5N Hicks6Scottish Association for Marine Science, Dunstaffnage, Oban PA37 1QA, UKCooke Aquaculture, Orkney Islands, Crowness Rd, Kirkwall KW15 1RG, UKDalhousie University, Department of Oceanography, 1355 Oxford Street, Halifax, Nova Scotia B3H 4J1, CanadaScottish Association for Marine Science, Dunstaffnage, Oban PA37 1QA, UKScottish Association for Marine Science, Dunstaffnage, Oban PA37 1QA, UKScottish Association for Marine Science, Dunstaffnage, Oban PA37 1QA, UKScottish Association for Marine Science, Dunstaffnage, Oban PA37 1QA, UKFish farm waste dispersal models are widely used but have only been directly validated to a limited extent. Two shallow (<20 m) Atlantic salmon farms (Bay of Meil and Quanterness) in Orkney, Scotland were studied. Bay of Meil has peak near-bed currents of 9.7 cm s-1 whereas Quanterness has flows up to 31.6 cm s-1. Sediment tray traps which allow resuspension to occur were deployed at each site. The patterns of particulate organic carbon (POC) deposition into the traps were in broad agreement with the observed water current directions and results from infaunal benthic monitoring. Despite the markedly different flow regimes at the 2 sites, most of the deposition occurred within 210 m of the cage perimeters. POC footprints were then modelled using the particle tracking model NewDEPOMOD. For Bay of Meil, a footprint was obtained using the recommended parameter defaults, but the spatial extent was too constrained compared to the sediment tray results. For Quanterness, all simulated particles were lost from the model domain and the critical erosion shear stress had to be increased to unrealistic levels to obtain a footprint. The failure to find a common set of parameter values applicable to both sites, despite their similar depths and sandy seabed, suggests that there remain unresolved issues, likely in how NewDEPOMOD handles waste resuspension. The sediment trays provided a direct method for quantifying the organic carbon deposition, facilitating direct validation of the dispersal model and demonstrating that further research is needed on fish farm waste dispersal at coarser sediment sites.https://www.int-res.com/abstracts/aei/v15/p251-269/
spellingShingle C Fox
C Webb
J Grant
S Brain
S Fraser
R Abell
N Hicks
Measuring and modelling the dispersal of salmon farm organic waste over sandy sediments
Aquaculture Environment Interactions
title Measuring and modelling the dispersal of salmon farm organic waste over sandy sediments
title_full Measuring and modelling the dispersal of salmon farm organic waste over sandy sediments
title_fullStr Measuring and modelling the dispersal of salmon farm organic waste over sandy sediments
title_full_unstemmed Measuring and modelling the dispersal of salmon farm organic waste over sandy sediments
title_short Measuring and modelling the dispersal of salmon farm organic waste over sandy sediments
title_sort measuring and modelling the dispersal of salmon farm organic waste over sandy sediments
url https://www.int-res.com/abstracts/aei/v15/p251-269/
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