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            <gco:CharacterString>These data are from the following areas and surveys.


-   CEND072023 – North Sea (Farnes Deep, Fulmar, &amp; Dogger Bank) – May 20-   th-    to June 10-   
    th-   , 2023.
-   CEND172023 – Celtic Sea – November 9-   th-    to November 28-   th-   , 2023.
-   CEND092024 – North Sea (Farnes Deep, Fulmar, &amp; Dogger Bank) - May 24-   th-    to June 9-   
    th-   , 2024.

At each station within a survey a NIOZ Box Corer was deployed collecting up to 5 individual 
cores to a maximum sediment depth of 30cm. A 10cm diameter sub core was taken from cores 
designated for lead-210 and organic carbon &amp; nitrogen (OCN), as well as the core for 
contaminants. The lead-210 ( 210Pb) and OCN core was sliced at 2cm intervals for CEND072023 
and CEND172023, and 1cm for CEND092024. The contaminants core was sliced a 5cm intervals for all 
surveys. 

Full PSA was performed on slices from the lead-210 ( 210Pb), and the OCN cores, and a 63µm 
split on slices from the contaminant cores.

Additional Day Grab samples were taken on CEND072023. Full PSA was performed on these samples.

Full PSA sediment samples were defrosted prior to analysis, and a representative subsample was 
taken. The sediment samples were processed following the PSA methodology recommended by the 
National Marine Biological Analytical Quality Control (NMBAQC) Scheme (Mason, 2022).Laser 
diffraction is carried out on the &lt;2mm sediment. The remainder of the subsample is wet split 
using a 1mm sieve. The &gt;1mm sediment is oven dried then dry sieved at half phi intervals. The 
&lt;1mm sediment is oven dried and the weight recorded. The sieve and laser data are then merged to 
produce a full Particle Size Distribution (PSD) at half phi intervals. Gradistat software (Blott 
and Pye, 2001) was used to produce all sediment statistics (e.g., mean, mode, skewness). Each 
sample was classified using modified Folk description as defined by Long (2006). 

63 split sediment samples were defrosted prior to analysis and then wet split using a 63 μm 
sieve. The &gt;63 μm sediment fraction is then oven-dried and the weight is recorded. The &lt;63 μm 
sediment fraction is freeze-dried, the weight is recorded and then sent for metals analysis. The 
percentage mud is then calculated by ( &lt;63 μm / &gt;63 μm + &lt;63 μm )*100. 

A data point can potentially have multiple Quality Flags (QFlags) which will be semicolon 
separated. Definition of each QFlag can be found in the QFlag text file attached to this record.

This dataset was produced by work supported jointly by the Joint Nature Conservation Committee 
(JNCC) lead NC40 Offshore Marine Monitoring project funded by Department of Environment, Food, &amp; 
Rural Affairs (Defra) under its flagship marine Natural Capital and Ecosystem Assessment (mNCEA) 
programme and by the Defra funded Carbon Management Project (project number MRD333). Find out 
more about mNCEA at 
`https://www.gov.uk/government/publications/natural-capital-and-ecosystem-assessment-programme`_
.

References:

Blott, S.J. and Pye, K. (2001) GRADISTAT: a grain size distribution and statistics package for 
the analysis of unconsolidated sediments. Earth Surface Processes and Landforms 26, 1237-1248. 

Long, D. ,2006. BGS detailed explanation of seabed sediment modified Folk classification. 
`http://www.searchmesh.net/PDF/GMHM3_Detailed_explanation_of_seabed_sediment_classification.pdf`_

Mason, C. 2022. NMBAQC's Best Practice Guidance. Particle Size Analysis (PSA) for Supporting 
Biological Analysis. National Marine Biological AQC Coordinating Committee, 84pp, First 
published 2011, updated January 2016 and 2022. 
`https://www.nmbaqcs.org/media/ibzlxdej/psa-guidance_update2022.pdf`_


.. _`https://www.gov.uk/government/publications/natural-capital-and-ecosystem-assessment-programme`:
    https://www.gov.uk/government/publications/natural-capital-and-ecosystem-assessment-programme

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