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 <front>
  <journal-meta>
   <journal-id journal-id-type="publisher-id">Russian Journal of Earth Sciences</journal-id>
   <journal-title-group>
    <journal-title xml:lang="en">Russian Journal of Earth Sciences</journal-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Russian Journal of Earth Sciences</trans-title>
    </trans-title-group>
   </journal-title-group>
   <issn publication-format="online">1681-1208</issn>
  </journal-meta>
  <article-meta>
   <article-id pub-id-type="publisher-id">46686</article-id>
   <article-categories>
    <subj-group subj-group-type="toc-heading" xml:lang="ru">
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
    <subj-group subj-group-type="toc-heading" xml:lang="en">
     <subject>ORIGINAL ARTICLES</subject>
    </subj-group>
    <subj-group>
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
   </article-categories>
   <title-group>
    <article-title xml:lang="en">Physical and chemical properties of seawater over the slopes of the northern part of the Mid-Atlantic Ridge</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Physical and chemical properties of seawater over the slopes of the northern part of the Mid-Atlantic Ridge</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Morozov</surname>
       <given-names>E G</given-names>
      </name>
      <name xml:lang="en">
       <surname>Morozov</surname>
       <given-names>E G</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Kolokolova</surname>
       <given-names>A V</given-names>
      </name>
      <name xml:lang="en">
       <surname>Kolokolova</surname>
       <given-names>A V</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-2"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <volume>15</volume>
   <issue>2</issue>
   <fpage>1</fpage>
   <lpage>7</lpage>
   <history>
    <date date-type="received" iso-8601-date="2021-10-29T13:34:45+03:00">
     <day>29</day>
     <month>10</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/46686/view">https://rjes.ru/en/nauka/article/46686/view</self-uri>
   <abstract xml:lang="ru">
    <p>We analyze physical and chemical properties of seawater east and west of the Mid-Atlantic Ridge in the tropical North Atlantic based on the historical data and our measurements in 2014. Concentration of nutrients in the bottom layer east of the ridge is smaller than west of the ridge because Antarctic Bottom Water propagated to the East Atlantic through abyssal fractures in the ridge and mixes with the overlying waters in the course of its propagations. We found a local temperature increase near the bottom in the rift zone of the Mid-Atlantic Ridge along 16° 39'~N, which can be related to hydrothermal activity in the region.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>We analyze physical and chemical properties of seawater east and west of the Mid-Atlantic Ridge in the tropical North Atlantic based on the historical data and our measurements in 2014. Concentration of nutrients in the bottom layer east of the ridge is smaller than west of the ridge because Antarctic Bottom Water propagated to the East Atlantic through abyssal fractures in the ridge and mixes with the overlying waters in the course of its propagations. We found a local temperature increase near the bottom in the rift zone of the Mid-Atlantic Ridge along 16° 39'~N, which can be related to hydrothermal activity in the region.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>Mid Atlantic Ridge</kwd>
    <kwd>abyssal fracture zones</kwd>
    <kwd>Antarctic Bottom Water</kwd>
    <kwd>seawater properties</kwd>
    <kwd>distribution of nutrients</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>Mid Atlantic Ridge</kwd>
    <kwd>abyssal fracture zones</kwd>
    <kwd>Antarctic Bottom Water</kwd>
    <kwd>seawater properties</kwd>
    <kwd>distribution of nutrients</kwd>
   </kwd-group>
  </article-meta>
 </front>
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  <p></p>
 </body>
 <back>
  <ref-list>
   <ref id="B1">
    <label>1.</label>
    <citation-alternatives>
     <mixed-citation xml:lang="ru">Morozov, E. G., Demidov, A. N., Tarakanov, R. Y., Zenk, W.  Abyssal Channels in the Atlantic Ocean, G.~Weatherly (Ed.) - Dordrecht: Springer., 2010. - 266 pp.</mixed-citation>
     <mixed-citation xml:lang="en">Morozov, E. G., Demidov, A. N., Tarakanov, R. Y., Zenk, W.  Abyssal Channels in the Atlantic Ocean, G.~Weatherly (Ed.) - Dordrecht: Springer., 2010. - 266 pp.</mixed-citation>
    </citation-alternatives>
   </ref>
   <ref id="B2">
    <label>2.</label>
    <citation-alternatives>
     <mixed-citation xml:lang="ru">Sandoval, F. J., Weatherly, G. L.  Evolution of the deep western boundary current of Antarctic bottom water in the Brazil Basin, // J. Phys. Oceanogr., 2001. - v. 31 - p. 1440.</mixed-citation>
     <mixed-citation xml:lang="en">Sandoval, F. J., Weatherly, G. L.  Evolution of the deep western boundary current of Antarctic bottom water in the Brazil Basin, // J. Phys. Oceanogr., 2001. - v. 31 - p. 1440.</mixed-citation>
    </citation-alternatives>
   </ref>
   <ref id="B3">
    <label>3.</label>
    <citation-alternatives>
     <mixed-citation xml:lang="ru">Wüst, G.  Schichtung und Zirkulation des Atlantischen Ozeans // A. Defant (Ed.), Wissenschaftliche Ergebnisse, Deutsche Atlantische Expedition auf dem Forschungs - und Vermessungsschiff ``Meteor'' 1925-1927, 6(1) - Berlin: Walter de Gruyter [ampersand] Co., 1936. - p. 1440.</mixed-citation>
     <mixed-citation xml:lang="en">Wüst, G.  Schichtung und Zirkulation des Atlantischen Ozeans // A. Defant (Ed.), Wissenschaftliche Ergebnisse, Deutsche Atlantische Expedition auf dem Forschungs - und Vermessungsschiff ``Meteor'' 1925-1927, 6(1) - Berlin: Walter de Gruyter [ampersand] Co., 1936. - p. 1440.</mixed-citation>
    </citation-alternatives>
   </ref>
  </ref-list>
 </back>
</article>
