Dissolved aluminum, indium, and cerium in the Sea of Japan and the Sea of Okhotsk : Comparison to the marginal seas of the western North Pacific
Identifieur interne : 007C34 ( Main/Repository ); précédent : 007C33; suivant : 007C35Dissolved aluminum, indium, and cerium in the Sea of Japan and the Sea of Okhotsk : Comparison to the marginal seas of the western North Pacific
Auteurs : RBID : Pascal:08-0101613Descripteurs français
- Pascal (Inist)
- Wicri :
English descriptors
- KwdEn :
Abstract
[1] Dissolved aluminum, indium, and cerium were measured in seawater from the Sea of Japan and the Sea of Okhotsk. Surface maxima of Al in the eastern Japan Basin indicate a signature of atmospheric mineral dust deposition resembling that of In. Data from all stations in this study show that Ce was markedly high in well-oxygenated bottom waters. The Ce:Al ratios of settling particles and surface sediments implicate the benthic flux of Ce as its cause. The In:Al ratios found in this study are not as high as those of the South China Sea and Sulu Sea, suggesting the minor influence of atmospheric deposition on the In:Al ratios in seawater. Fractionation between In and Al during scavenging processes, in addition to input from the bottom sediment, might contribute to the In enrichment of seawater. Apparent differences between In and Ce distributions in the marginal seas show that the benthic supply mechanism of In is not merely a simple redox-related process.
Links toward previous steps (curation, corpus...)
- to stream Main, to step Corpus: 006E54
Links to Exploration step
Pascal:08-0101613Le document en format XML
<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en" level="a">Dissolved aluminum, indium, and cerium in the Sea of Japan and the Sea of Okhotsk : Comparison to the marginal seas of the western North Pacific</title><author><name sortKey="Obata, Hajime" uniqKey="Obata H">Hajime Obata</name><affiliation wicri:level="3"><inist:fA14 i1="01"><s1>Marine Inorganic Chemistry Group, Ocean Research Institute, University of Tokyo</s1><s2>Tokyo</s2><s3>JPN</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Japon</country><placeName><settlement type="city">Tokyo</settlement></placeName></affiliation></author><author><name>DIA SOTTO ALIBO</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Department of Chemistry, University of San Carlos</s1><s2>Cebu</s2><s3>PHL</s3><sZ>2 aut.</sZ></inist:fA14><country>Philippines</country><wicri:noRegion>Cebu</wicri:noRegion></affiliation></author><author><name sortKey="Nozaki, Yoshiyuki" uniqKey="Nozaki Y">Yoshiyuki Nozaki</name><affiliation wicri:level="3"><inist:fA14 i1="01"><s1>Marine Inorganic Chemistry Group, Ocean Research Institute, University of Tokyo</s1><s2>Tokyo</s2><s3>JPN</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Japon</country><placeName><settlement type="city">Tokyo</settlement></placeName></affiliation></author></titleStmt><publicationStmt><idno type="inist">08-0101613</idno><date when="2007">2007</date><idno type="stanalyst">PASCAL 08-0101613 INIST</idno><idno type="RBID">Pascal:08-0101613</idno><idno type="wicri:Area/Main/Corpus">006E54</idno><idno type="wicri:Area/Main/Repository">007C34</idno></publicationStmt><seriesStmt><idno type="ISSN">0148-0227</idno><title level="j" type="abbreviated">J. geophys. res.</title><title level="j" type="main">Journal of geophysical research</title></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Dust fall out</term><term>Japan</term><term>Northwest Pacific</term><term>Scavenging</term><term>South China Sea</term><term>Sulu Sea</term><term>aluminum</term><term>atmospheric deposits</term><term>bottom water</term><term>enrichment</term><term>fractionation</term><term>marginal seas</term><term>particles</term><term>sea water</term><term>surface sediments</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Aluminium</term><term>Mer marginale</term><term>Eau mer</term><term>Retombée poussière</term><term>Eau fond</term><term>Particule</term><term>Sédiment surface</term><term>Dépôt atmosphérique</term><term>Fractionnement</term><term>Interception(chimie)</term><term>Enrichissement</term><term>Japon</term><term>Océan Pacifique Nord Ouest</term><term>Mer de Chine Sud</term><term>Mer Sulu</term><term>Mer de Soulou</term></keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Japon</term></keywords><keywords scheme="Wicri" type="concept" xml:lang="fr"><term>Aluminium</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">[1] Dissolved aluminum, indium, and cerium were measured in seawater from the Sea of Japan and the Sea of Okhotsk. Surface maxima of Al in the eastern Japan Basin indicate a signature of atmospheric mineral dust deposition resembling that of In. Data from all stations in this study show that Ce was markedly high in well-oxygenated bottom waters. The Ce:Al ratios of settling particles and surface sediments implicate the benthic flux of Ce as its cause. The In:Al ratios found in this study are not as high as those of the South China Sea and Sulu Sea, suggesting the minor influence of atmospheric deposition on the In:Al ratios in seawater. Fractionation between In and Al during scavenging processes, in addition to input from the bottom sediment, might contribute to the In enrichment of seawater. Apparent differences between In and Ce distributions in the marginal seas show that the benthic supply mechanism of In is not merely a simple redox-related process.</div></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0148-0227</s0></fA01><fA03 i2="1"><s0>J. geophys. res.</s0></fA03><fA05><s2>112</s2></fA05><fA06><s2>C12</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>Dissolved aluminum, indium, and cerium in the Sea of Japan and the Sea of Okhotsk : Comparison to the marginal seas of the western North Pacific</s1></fA08><fA11 i1="01" i2="1"><s1>OBATA (Hajime)</s1></fA11><fA11 i1="02" i2="1"><s1>DIA SOTTO ALIBO</s1></fA11><fA11 i1="03" i2="1"><s1>NOZAKI (Yoshiyuki)</s1></fA11><fA14 i1="01"><s1>Marine Inorganic Chemistry Group, Ocean Research Institute, University of Tokyo</s1><s2>Tokyo</s2><s3>JPN</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ></fA14><fA14 i1="02"><s1>Department of Chemistry, University of San Carlos</s1><s2>Cebu</s2><s3>PHL</s3><sZ>2 aut.</sZ></fA14><fA20><s2>C12003.1-C12003.10</s2></fA20><fA21><s1>2007</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>3144</s2><s5>354000183428660030</s5></fA43><fA44><s0>0000</s0><s1>© 2008 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>3/4 p.</s0></fA45><fA47 i1="01" i2="1"><s0>08-0101613</s0></fA47><fA60><s1>P</s1></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>Journal of geophysical research</s0></fA64><fA66 i1="01"><s0>USA</s0></fA66><fC01 i1="01" l="ENG"><s0>[1] Dissolved aluminum, indium, and cerium were measured in seawater from the Sea of Japan and the Sea of Okhotsk. Surface maxima of Al in the eastern Japan Basin indicate a signature of atmospheric mineral dust deposition resembling that of In. Data from all stations in this study show that Ce was markedly high in well-oxygenated bottom waters. The Ce:Al ratios of settling particles and surface sediments implicate the benthic flux of Ce as its cause. The In:Al ratios found in this study are not as high as those of the South China Sea and Sulu Sea, suggesting the minor influence of atmospheric deposition on the In:Al ratios in seawater. Fractionation between In and Al during scavenging processes, in addition to input from the bottom sediment, might contribute to the In enrichment of seawater. Apparent differences between In and Ce distributions in the marginal seas show that the benthic supply mechanism of In is not merely a simple redox-related process.</s0></fC01><fC02 i1="01" i2="3"><s0>001E</s0></fC02><fC02 i1="02" i2="2"><s0>001E01</s0></fC02><fC02 i1="03" i2="2"><s0>220</s0></fC02><fC03 i1="01" i2="2" l="FRE"><s0>Aluminium</s0><s5>01</s5></fC03><fC03 i1="01" i2="2" l="ENG"><s0>aluminum</s0><s5>01</s5></fC03><fC03 i1="01" i2="2" l="SPA"><s0>Aluminio</s0><s5>01</s5></fC03><fC03 i1="02" i2="2" l="FRE"><s0>Mer marginale</s0><s5>02</s5></fC03><fC03 i1="02" i2="2" l="ENG"><s0>marginal seas</s0><s5>02</s5></fC03><fC03 i1="03" i2="2" l="FRE"><s0>Eau mer</s0><s5>03</s5></fC03><fC03 i1="03" i2="2" l="ENG"><s0>sea water</s0><s5>03</s5></fC03><fC03 i1="03" i2="2" l="SPA"><s0>Agua mar</s0><s5>03</s5></fC03><fC03 i1="04" i2="X" l="FRE"><s0>Retombée poussière</s0><s5>04</s5></fC03><fC03 i1="04" i2="X" l="ENG"><s0>Dust fall out</s0><s5>04</s5></fC03><fC03 i1="04" i2="X" l="SPA"><s0>Recaída polvo</s0><s5>04</s5></fC03><fC03 i1="05" i2="2" l="FRE"><s0>Eau fond</s0><s5>05</s5></fC03><fC03 i1="05" i2="2" l="ENG"><s0>bottom water</s0><s5>05</s5></fC03><fC03 i1="05" i2="2" l="SPA"><s0>Agua fondo</s0><s5>05</s5></fC03><fC03 i1="06" i2="2" l="FRE"><s0>Particule</s0><s5>06</s5></fC03><fC03 i1="06" i2="2" l="ENG"><s0>particles</s0><s5>06</s5></fC03><fC03 i1="07" i2="2" l="FRE"><s0>Sédiment surface</s0><s5>07</s5></fC03><fC03 i1="07" i2="2" l="ENG"><s0>surface sediments</s0><s5>07</s5></fC03><fC03 i1="08" i2="2" l="FRE"><s0>Dépôt atmosphérique</s0><s5>08</s5></fC03><fC03 i1="08" i2="2" l="ENG"><s0>atmospheric deposits</s0><s5>08</s5></fC03><fC03 i1="09" i2="2" l="FRE"><s0>Fractionnement</s0><s5>09</s5></fC03><fC03 i1="09" i2="2" l="ENG"><s0>fractionation</s0><s5>09</s5></fC03><fC03 i1="10" i2="3" l="FRE"><s0>Interception(chimie)</s0><s5>10</s5></fC03><fC03 i1="10" i2="3" l="ENG"><s0>Scavenging</s0><s5>10</s5></fC03><fC03 i1="11" i2="2" l="FRE"><s0>Enrichissement</s0><s5>11</s5></fC03><fC03 i1="11" i2="2" l="ENG"><s0>enrichment</s0><s5>11</s5></fC03><fC03 i1="11" i2="2" l="SPA"><s0>Enriquecimiento</s0><s5>11</s5></fC03><fC03 i1="12" i2="2" l="FRE"><s0>Japon</s0><s2>NG</s2><s5>61</s5></fC03><fC03 i1="12" i2="2" l="ENG"><s0>Japan</s0><s2>NG</s2><s5>61</s5></fC03><fC03 i1="12" i2="2" l="SPA"><s0>Japón</s0><s2>NG</s2><s5>61</s5></fC03><fC03 i1="13" i2="2" l="FRE"><s0>Océan Pacifique Nord Ouest</s0><s2>NG</s2><s5>62</s5></fC03><fC03 i1="13" i2="2" l="ENG"><s0>Northwest Pacific</s0><s2>NG</s2><s5>62</s5></fC03><fC03 i1="14" i2="2" l="FRE"><s0>Mer de Chine Sud</s0><s2>NG</s2><s5>63</s5></fC03><fC03 i1="14" i2="2" l="ENG"><s0>South China Sea</s0><s2>NG</s2><s5>63</s5></fC03><fC03 i1="14" i2="2" l="SPA"><s0>Mar de China sur</s0><s2>NG</s2><s5>63</s5></fC03><fC03 i1="15" i2="2" l="FRE"><s0>Mer Sulu</s0><s2>NG</s2><s5>64</s5></fC03><fC03 i1="15" i2="2" l="ENG"><s0>Sulu Sea</s0><s2>NG</s2><s5>64</s5></fC03><fC03 i1="15" i2="2" l="SPA"><s0>Mar de Sulu</s0><s2>NG</s2><s5>64</s5></fC03><fC03 i1="16" i2="X" l="FRE"><s0>Mer de Soulou</s0><s2>NG</s2><s5>65</s5></fC03><fC03 i1="16" i2="X" l="ENG"><s0>Sulu Sea</s0><s2>NG</s2><s5>65</s5></fC03><fC03 i1="16" i2="X" l="SPA"><s0>Mar de Sulu</s0><s2>NG</s2><s5>65</s5></fC03><fC07 i1="01" i2="2" l="FRE"><s0>Extrême Orient</s0><s2>NG</s2></fC07><fC07 i1="01" i2="2" l="ENG"><s0>Far East</s0><s2>NG</s2></fC07><fC07 i1="01" i2="2" l="SPA"><s0>Extremo Oriente</s0><s2>NG</s2></fC07><fC07 i1="02" i2="2" l="FRE"><s0>Asie</s0><s2>564</s2></fC07><fC07 i1="02" i2="2" l="ENG"><s0>Asia</s0><s2>564</s2></fC07><fC07 i1="02" i2="2" l="SPA"><s0>Asia</s0><s2>564</s2></fC07><fC07 i1="03" i2="2" l="FRE"><s0>Océan Pacifique Nord</s0><s2>NG</s2></fC07><fC07 i1="03" i2="2" l="ENG"><s0>North Pacific</s0><s2>NG</s2></fC07><fC07 i1="04" i2="2" l="FRE"><s0>Océan Pacifique</s0><s2>564</s2></fC07><fC07 i1="04" i2="2" l="ENG"><s0>Pacific Ocean</s0><s2>564</s2></fC07><fC07 i1="04" i2="2" l="SPA"><s0>Océano Pacífico</s0><s2>564</s2></fC07><fC07 i1="05" i2="2" l="FRE"><s0>Océan Pacifique Ouest</s0><s2>NG</s2></fC07><fC07 i1="05" i2="2" l="ENG"><s0>West Pacific</s0><s2>NG</s2></fC07><fC07 i1="06" i2="X" l="FRE"><s0>Mers d'Indonésie</s0><s2>NG</s2></fC07><fC07 i1="06" i2="X" l="ENG"><s0>Indonesian Seas</s0><s2>NG</s2></fC07><fC07 i1="06" i2="X" l="SPA"><s0>Mares de Indonesia</s0><s2>NG</s2></fC07><fN21><s1>056</s1></fN21><fN44 i1="01"><s1>OTO</s1></fN44><fN82><s1>OTO</s1></fN82></pA></standard></inist></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=IndiumV3/Data/Main/Repository
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 007C34 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Main/Repository/biblio.hfd -nk 007C34 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= *** parameter Area/wikiCode missing ***
|area= IndiumV3
|flux= Main
|étape= Repository
|type= RBID
|clé= Pascal:08-0101613
|texte= Dissolved aluminum, indium, and cerium in the Sea of Japan and the Sea of Okhotsk : Comparison to the marginal seas of the western North Pacific
}}
| This area was generated with Dilib version V0.5.77. |  |