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                        <gco:CharacterString>Plymouth</gco:CharacterString>
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                        <gco:CharacterString>PL1 2PB</gco:CharacterString>
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                        <gco:CharacterString>dassh.enquiries@mba.ac.uk</gco:CharacterString>
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            <gco:CharacterString>Environmental Survey. Gannet Field. UKCS Blocks 21/25, 21/30, 22/21 and 22/26a
          TAKEN FROM REPORT
          SUMMARY OF SURVEY RESULTS
          Location
          All coordinates in this report are based on the International Spheroid 1924, European Datum 1950. Grid coordinates are on the Universal Transverse Mercator Projection, Central Meridian 0.
          Study Area:
          In June 2007, Fugro Survey Limited (FSLTD) were subcontracted by Fugro Rovtech Limited to performed environmental survey in the Gannet field, in the Central North Sea, UKCS blocks 21/25, 21/30, 22/21 and 22/26a. The field consists of a cluster of seven oil and gas fields (namely Gannet A, B, C, D, E, F and G). The survey was performed in order to investigate the effects of existing development in the area and to establish a baseline for future development.
          Bathymetry:
          Tidally uncorrected single beam echosounder spot depths recorded at sampling locations during the current study ranged from 93 m to 100 m, indicating an essentially flat seabed within the survey area.
          Seabed Features:
          Full seabed features information was not available for the survey area. However, a previous geophysical survey for a pipeline route from Bittern to Gannet A in the centre of the Gannet field (Fugro Geoteam Limited report number M2032.11, Shell Expro report number P97-146 / 31) found surficial sediments along the route to comprise fine to coarse, occasionally clayey and / or silty sand.
          Environmental Survey Strategy:
          A total of 38 stations were sampled using a 0.1 m2 Day grab with one or three physicochemical replicates retained for analysis and three macrofaunal replicates obtained at 21 of the 38 stations. Seabed photography was undertaken at the required locations for groundtruthing purposes.
          Granulometry:
          The sediments were similar across the survey area ranging from poorly to very poorly sorted, fine to very fine sand, with the exception of station D4, which was classified as very poorly sorted medium silt. Mean phi ranged from 2.52 to 3.69 (station C9 and C4, respectively), while station D4 showed a mean phi of 5.27. The sorting coefficient ranged from 1.03 (stations D6 and Ref2) to 2.19 (station D4).
          In general variation in the particle size composition of sediments within the survey area appeared to relate to the proximity to the historic well locations. Drill cuttings were observed in many of the samples located adjacent to the historic well locations i.e. A3, A4, C4 and D2 to D5.
          Comparison of granulometry data with 1990 survey data showed that levels of fines appeared to have increased across the entire survey, although this is probably due to a change in methodology (the current survey utilised wet sieving techniques followed by laser diffraction). However, it was considered significant that the areas adjacent to the historic well locations showed a disproportionate increase in fines, presumed to be due to the presence of drill cuttings, which were not present in the 1990 baseline survey.
          Organic Carbon:
          TOM for the majority of sediments from the survey area ranged from 1.2% to 2.9% (stations A10 and C2, respectively). Substantially higher levels of loss on ignition were recorded for stations adjacent to historic well locations i.e. D4 and C4, at 4.6% including station A3 at 4.0%. Several other stations showed elevated levels of TOM, between approximately 2.3% and 2.9%, reflecting their proximity to areas of drilling activity (stations A1, C5, D2, D3, D5, C2, C7 and C8).</gco:CharacterString>
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