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The measurements include the gases He, Ne, Kr, Xe, H<jats:sub>2</jats:sub>, CH<jats:sub>4</jats:sub>, and CO<jats:sub>2</jats:sub> dissolved in distilled water in the temperature range from 5 to 35°C, and He and H<jats:sub>2</jats:sub> dissolved in seawater in the same temperature range. The maximum systematic error is estimated to be well below 5%. The isotopic fractionation in the diffusion coefficient, ∈<jats:sub><jats:italic>D</jats:italic></jats:sub>, was determined to be (−0.87 ± 0.05)‰ for <jats:sup>13</jats:sup>CO<jats:sub>2</jats:sub>/<jats:sup>12</jats:sup>CO<jats:sub>2</jats:sub> and (15 ± 3)% for <jats:sup>3</jats:sup>He/<jats:sup>4</jats:sup>He.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262943365820928","@type":"Researcher","foaf:name":[{"@value":"Bernd Jähne"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943365820930","@type":"Researcher","foaf:name":[{"@value":"Gerhard Heinz"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943365820929","@type":"Researcher","foaf:name":[{"@value":"Wolfgang Dietrich"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Oceans"}],"dc:publisher":[{"@value":"American Geophysical Union 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