Field measurements of cable self-burial in a sandy marine environment

Allbwn ymchwil: Cyfraniad at gyfnodolynErthygladolygiad gan gymheiriaid

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Field measurements of cable self-burial in a sandy marine environment. / Unsworth, Christopher; Austin, Martin; Van Landeghem, Katrien et al.
Yn: Coastal Engineering, Cyfrol 184, 104309, 09.2023.

Allbwn ymchwil: Cyfraniad at gyfnodolynErthygladolygiad gan gymheiriaid

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Unsworth C, Austin M, Van Landeghem K, Couldrey A, Whitehouse R, Lincoln B et al. Field measurements of cable self-burial in a sandy marine environment. Coastal Engineering. 2023 Medi;184:104309. Epub 2023 Ebr 19. doi: 10.1016/j.coastaleng.2023.104309

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TY - JOUR

T1 - Field measurements of cable self-burial in a sandy marine environment

AU - Unsworth, Christopher

AU - Austin, Martin

AU - Van Landeghem, Katrien

AU - Couldrey, Amelia

AU - Whitehouse, Richard

AU - Lincoln, Ben

AU - Doole, Siobhan

AU - Worrall, Peter

PY - 2023/9

Y1 - 2023/9

N2 - The world’s shallow continental shelves are currently experiencing a rapid pace of development from the growth of offshore renewable energy. The emplacement of infrastructure on the seabed can change the morphology of the bed, the nature of the flow above it and transport of sediment and so complicate the assessment of seabed stability for planning and designing offshore renewable infrastructure. To ascertain how much of an impact these natural processes have on cable stability, we present field results from two deployments in the Eastern Irish Sea at a location of current and planned offshore windfarms. Profiles of flow, turbulence and suspended sediment concentration were measured over a section of typical high voltage electricity cable. Even during spring tides upon deployment our observations show that sediment was deposited around the cable and self-burial occurred. The rate of deposition varied between surveys dependent on forcing and local bed conditions. Turbulence generated from the cable itself reduced as the embedment depth increased, but the relationship between bed shear stress and suspended sediment concentration was not consistent between surveys. We discuss several processes potentially responsible for the prevalence of deposition around the cable, and the difference in seabed mobility between the surveys.

AB - The world’s shallow continental shelves are currently experiencing a rapid pace of development from the growth of offshore renewable energy. The emplacement of infrastructure on the seabed can change the morphology of the bed, the nature of the flow above it and transport of sediment and so complicate the assessment of seabed stability for planning and designing offshore renewable infrastructure. To ascertain how much of an impact these natural processes have on cable stability, we present field results from two deployments in the Eastern Irish Sea at a location of current and planned offshore windfarms. Profiles of flow, turbulence and suspended sediment concentration were measured over a section of typical high voltage electricity cable. Even during spring tides upon deployment our observations show that sediment was deposited around the cable and self-burial occurred. The rate of deposition varied between surveys dependent on forcing and local bed conditions. Turbulence generated from the cable itself reduced as the embedment depth increased, but the relationship between bed shear stress and suspended sediment concentration was not consistent between surveys. We discuss several processes potentially responsible for the prevalence of deposition around the cable, and the difference in seabed mobility between the surveys.

U2 - 10.1016/j.coastaleng.2023.104309

DO - 10.1016/j.coastaleng.2023.104309

M3 - Article

VL - 184

JO - Coastal Engineering

JF - Coastal Engineering

SN - 0378-3839

M1 - 104309

ER -