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Annual Report for 2010/11 and Forward Programme - Sellafield Ltd

Annual Report for 2010/11 and Forward Programme - Sellafield Ltd

Annual Report for 2010/11 and Forward Programme - Sellafield Ltd

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SSEM/20<strong>11</strong>/4730 June 20<strong>11</strong>A full copy of the Cefas report is provided to the Environment Agency as part of thesubmission package that accompanies this report.3.3.3 Progress on measurements of bed shear stress in the vicinity of the <strong>Sellafield</strong>discharge pipelineA number of packages of work were included under this task, the major piece of work beingthe deployment of an Aquadopp current profiler. Other supporting packages included anevaluation of the feasibility to deploy Woodhead drifters <strong>and</strong> a review of historical currentmeter records.As reported in the <strong>2010</strong> report, Cefas were able to confirm that the required numbers ofWoodhead drifters were available <strong>and</strong> that a supplier had been identified to produce the tagsthat would provide details of what in<strong>for</strong>mation would need to be returned by the finder of thedrifter. Un<strong>for</strong>tunately the collapse of the contract with WSC led to the decision not to pursuethe Woodhead drifter release at this stage. Whilst the release of the drifters is relativelystraight<strong>for</strong>ward (released as a package by h<strong>and</strong> from a vessel at a recorded location) thefollow-up work of waiting <strong>for</strong> the drifters to come ashore <strong>and</strong> logging <strong>and</strong> interpreting theresulting data would have taken several months. The deployment of Woodhead drifters willremain an option <strong>for</strong> future consideration.Current meter data from the <strong>Sellafield</strong> pipeline (water depth approximately 15 mbelow chart datum), were recorded by Cefas (then MAFF) at various time periods betweenMay 1981 <strong>and</strong> March 1988. These data have been reviewed to help improve the descriptionof the hydrodynamics immediately off the Cumbrian coast at <strong>Sellafield</strong>, with the aim ofreducing uncertainty in numerical model predictions. Of particular interest are the indicationsof the direction of near bed currents during episodic events (e.g., storm waves, storm surge,<strong>and</strong> wind-driven currents) when the <strong>Sellafield</strong>-derived particles are most likely to be movingalong the sea floor.The current meter data were extracted from the Cefas data archive system <strong>and</strong> subjected toa data quality analysis. The currents were measured using Plessey M021 propeller-typecurrent meters (Figure 3.33). The direction is determined from an internal compass thatregisters the change in instrument heading as the current meter vane reorients to the flow.Current directions were corrected <strong>for</strong> magnetic declination. The data were originally stored inbinary <strong>for</strong>m on magnetic tapes <strong>and</strong> have now been converted into computer data files.© Nuclear Decommissioning Authority 20<strong>11</strong>. 67

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