<mets:mets OBJID="oai:utas.edu.au:3957" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:mods="http://www.loc.gov/mods/v3" LABEL="Eprints Item" xsi:schemaLocation="http://www.loc.gov/METS/ http://www.loc.gov/standards/mets/mets.xsd http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-0.xsd" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mets="http://www.loc.gov/METS/"><mets:metsHdr CREATEDATA="2009-01-07T21:44:33Z"><mets:agent TYPE="ORGANIZATION" ROLE="CUSTODIAN"><mets:name>UTas ePrints</mets:name></mets:agent></mets:metsHdr><mets:dmdSec ID="DMD_oai:utas.edu.au:3957_mods"><mets:mdWrap MDTYPE="mods"><mets:xmlData><mods:titleInfo><mods:title>Intercomparison between FI-CL and ICP-MS for the determination of dissolved iron in Atlantic seawater</mods:title></mods:titleInfo><mods:name type="personal"><mods:namePart type="given">AR</mods:namePart><mods:namePart type="family">Bowie</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">SJ</mods:namePart><mods:namePart type="family">Ussher</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">WM</mods:namePart><mods:namePart type="family">Landing</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">PJ</mods:namePart><mods:namePart type="family">Worsfold</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:abstract>Results from a 3-laboratory blind intercomparison exercise with two widely used analytical methods for the&#13;
determination of iron in seawater are presented. The two methods used are coprecipitation followed by isotope dilution&#13;
inductively coupled plasma mass spectrometry (ICP-MS) and chemical reduction to iron(ii) followed by flow injection&#13;
with chemiluminescence detection (FI-CL). The five samples used were collected from the South Atlantic Ocean as part&#13;
of the IRONAGES intercomparison exercise. To avoid any inter-bottle variability, the same sample bottles were sent&#13;
sequentially to three laboratories in England, Australia and the United States over a 12-month period. The results show&#13;
that there is no statistical difference (P =0.05) between the shipboard FI-CL method and the directly traceable, low blank,&#13;
isotope dilution ICP-MS method for the determination of iron in surface South Atlantic seawater. There was also excellent&#13;
agreement between the overall mean of the three laboratories (0.54±0.03 nM) and the consensus value from an earlier&#13;
community-wide separate bottle intercomparison using the same IRONAGES sample water (0.59±0.21 nM).</mods:abstract><mods:classification authority="lcc">260402 Chemical Oceanography</mods:classification><mods:originInfo><mods:dateIssued encoding="iso8061">2007</mods:dateIssued></mods:originInfo><mods:originInfo><mods:publisher>CSIRO</mods:publisher></mods:originInfo><mods:genre>Article</mods:genre></mets:xmlData></mets:mdWrap></mets:dmdSec><mets:amdSec ID="TMD_oai:utas.edu.au:3957"><mets:rightsMD ID="rights_oai:utas.edu.au:3957_mods"><mets:mdWrap MDTYPE="mods"><mets:xmlData><mods:useAndReproduction>
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