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    <identifier>10.57760/sciencedb.02782</identifier>
    <datestamp>2022-09-22T11:27:06Z</datestamp>
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  <dc:date>2022-09-22</dc:date>
  <dc:title>Vertical distribution of total and particulate 234Th, particulate organic carbon (POC) and nutrients with their physical forcings (temperature, salinity, fluorescence-based Chl a)</dc:title>
  <dc:identifier>doi:10.57760/sciencedb.02782</dc:identifier>
  <dc:language>en</dc:language>
  <dc:description>Temperature, salinity, fluorescence-based Chl a were accessed from sensors attached to a Seabird 911 conductivity-temperature-depth (CTD); Total 234Th was precipitated by using the small-volume (4 L) MnO2 co-precipitation method (Benitez-Nelson et al., 2001; Cai et al., 2006). Particulate 234Th and POC were filterd by quartz microfiber (QMA) filters (25 mm diameter, 1.0 &amp;mu;m pore size) as particulate samples following method described in the JGOFS cookbook (Knap et al., 1996); the activity of 234Th was determined by a gas-flow proportional low-level RIS&amp;Oslash; beta counter (Model GM-25-5). Precipitation efficiency was determined by ICP-MS. Nutrients were analysed onboard using a Four-channel Continuous Flow Technicon AA3 Auto-Analyzer (Bran-Lube GmbH). The detection limits for both N+N (nitrate plus nitrite, termed as dissolved inorganic nitrogen, DIN) and SRP (soluble reactive phosphate) were 0.03 &amp;mu;mol L-1.</dc:description>
  <dc:subject>234Th; POC; Nutrients</dc:subject>
  <dc:creator>Yifan Ma</dc:creator>
  <dc:creator>Minhan Dai</dc:creator>
  <dc:rights>PUBLIC</dc:rights>
  <dc:rights>https://creativecommons.org/licenses/by/4.0/</dc:rights>
  <dc:type>dataset</dc:type>
  <dc:relation>http://www.doi.org/10.5194/bg-20-2013-2023</dc:relation>
  <dc:publisher>Science Data Bank</dc:publisher>
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