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Uranium-238<\/strong> Thorium-234<\/strong> Water-column total Th-234 with 4 L method and U-238 from U-salinity relationship from the 2010 and 2011 U.S. GEOTRACES cruises.<\/p><\/div>","@type":"rdf:HTML"}],"http:\/\/www.w3.org\/2000\/01\/rdf-schema#label":[{"@value":"GT10-11 - Th234_Total_and_U238","@type":"xsd:string"}],"http:\/\/ocean-data.org\/schema\/hasProcessingDescription":[{"@value":" Data were flagged with quality indicators: 1 = Good; 2 = Questionable; 3 = Bad.<\/p>\n BCO-DMO made the following modifications: Additional GEOTRACES Processing:<\/strong> Bottle parameters in the master file were taken from the GT-C_Bottle_GT10, GT-C_Bottle_GT11, ODF_Bottle_GT10, and ODF_Bottle_GT11 datasets. Non-bottle parameters, including those from GeoFish tows, Aerosol sampling, and McLane Pumps, were taken from the Event_Log_GT10 and Event_Log_GT11 datasets. 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(2020) Water-column total Thorium-234 and Uranium-238 from R\/V Knorr cruises KN199-04 and KN204-01 in the Subtropical northern Atlantic Ocean from 2010-2011 (U.S. GEOTRACES NAT project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). 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\nValue and uncertainty from equation derived in Owens et al. (2011)
\n\u00a0\u00a0\u00a0 \u00a0\u00a0\u00a0 U-238 (dpm\/L) = (Salinity * 0.0786) - 0.315
\nSalinity was measured onboard the ship by the Scripps Ocean Data Facility.<\/p>\n
\nDetermined by the widely-adopted 4 L method. Shallow (< 1000 m) samples were collected from the SIO ODF Rosette and deep samples (>1000 m) were collected from Niskin bottles hung above in situ pumps. Data are decay corrected to the mid-point time between when bottles 1 and 12 were fired for shallow casts and when the messenger was dropped for deep cast. All surface samples were collected using a deck-mounted pump (denoted as bottle 13). All data have been recovery-corrected using the Th-230\/Th-229 recovery method (see references below) to account for any loss of sample material during processing. All samples were analyzed using RISO Laboratory Anti-coincidence Beta Counters, using a helium\/1% butane mixture. Overall method efficiency was determined by minimizing the percent difference between mean U-238 and Th-234 values for samples from >1000 m to > 1000 m from the bottom (44.5 % for KN 199-4 and 46.4 % for KN 204-01a and KN 204-01b).<\/p><\/div>","@type":"rdf:HTML"}],"http:\/\/ocean-data.org\/schema\/hasBriefDescription":[{"@value":"Water-column total Thorium-234 and Uranium-238.","@language":"en-US"}],"http:\/\/purl.org\/dc\/terms\/description":[{"@value":"
\n- Parameter names have been modified to conform with BCO-DMO naming conventions.
\n- cruise_part was separated from the official cruise ID for cruise KN204-01.
\n- Added Cast_ISO_DateTime_UTC from the original cast dates and times.<\/p>\n
\nAfter the data were submitted to the International Data Management Office, BODC, the office noticed that important identifying information was missing in many datasets. With the agreement of BODC and the US GEOTRACES lead PIs, BCO-DMO added standard US GEOTRACES information, such as the US GEOTRACES event number, to each submitted dataset lacking this information. To accomplish this, BCO-DMO compiled a 'master' dataset composed of the following parameters: station_GEOTRC, cast_GEOTRC (bottle and pump data only), event_GEOTRC, sample_GEOTRC, sample_bottle_GEOTRC (bottle data only), bottle_GEOTRC (bottle data only), depth_GEOTRC_CTD (bottle data only), depth_GEOTRC_CTD_rounded (bottle data only), BTL_ISO_DateTime_UTC (bottle data only), and GeoFish_id (GeoFish data only). This added information will facilitate subsequent analysis and inter comparison of the datasets.<\/p>\n