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    <title>Gas fractionation and CO2-dynamics in natural high-CO2-systems</title>
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  <abstract type="Summary">The Okinawa Trough is a natural hydrothermal gas emission field. The flux of CO2 into the water column is dominated by hot hydrothermal CO2-rich vents. The influence of the emitted low-temperatured gas bubbles and droplets (‘condensed phase’) is very likely restricted to the lowermost part of the water column. Despite their proximity the gas composition of the condensed phases varies widely, especially in methane, which is likely caused by diverse phase transformation and thus fractionation below and above the seafloor.&lt;eng&gt;</abstract>
  <abstract type="Summary">Der Okinawa Trog ist ein natürliches hydrothermales Gasaustrittsgebiet. Der CO2-Fluss in die Wassersäule wird durch heiße hydrothermale CO2-reiche Quellen dominiert. Der Einfluss von freigesetzten kalten Gasblasen und Tropfen („kondensierte Phasen“) beschränkt sich sehr wahrscheinlich hauptsächlich auf den unteren Teil der Wassersäule. Trotz ihrer Nähe zueinander variiert die Gaszusammensetzung der einzelnen kondensierten Phasen stark, vor allem im Methangehalt. Diese basieren wahrscheinlich auf verschiedenen Phasenänderungen und damit Fraktionierungen unter- und oberhalb des Meeresbodens.&lt;ger&gt;</abstract>
  <note type="statement of responsibility">vorgelegt von Stine Beilfuhs</note>
  <note>GutachterInnen: Gregor Rehder (Universität Rostock, Leibniz-Institut für Ostseeforschung) ; Arne Körtzinger (Universität Kiel, GEOMAR Helmholtz-Zentrum für Ozeanforschung)</note>
  <note type="thesis">Dissertation Universität Rostock 2021</note>
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