The diffusion coefficients \$D\$ of important gas tracers dissolved in water and seawater were measured with a modified Barrer method. The measurements include the gases He, Ne, Kr, Xe, H\$\_2\$, CH\$\_4\$, and CO\$\_2\$ dissolved in distilled water in the temperature range from 5 to 35\$\circ\$C, and He and H\$\_2\$ 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, \$\varepsilon\_D\$, was determined to be (−0.87 ± 0.05)‰ for \$^13\$CO\$\_2\$/\$^12\$CO\$\_2\$ and (15 \$\pm\$ 3)\% for \$^3\$He/\$^4\$He.
%0 Journal Article
%1 citeulike:3038316
%A Jähne, Bernd
%A Heinz, Gerhard
%A Dietrich, Wolfgang
%D 1987
%J Journal of Geophysical Research
%K material-properties, measurement 80a20-heat-and-mass-transfer diffusivity
%N C10
%P 10767--10776
%T Measurement of the Diffusion Coefficients of Sparingly Soluble Gases in Water
%U http://www.agu.org/journals/ABS/1987/JC092iC10p10767.shtml
%V 92
%X The diffusion coefficients \$D\$ of important gas tracers dissolved in water and seawater were measured with a modified Barrer method. The measurements include the gases He, Ne, Kr, Xe, H\$\_2\$, CH\$\_4\$, and CO\$\_2\$ dissolved in distilled water in the temperature range from 5 to 35\$\circ\$C, and He and H\$\_2\$ 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, \$\varepsilon\_D\$, was determined to be (−0.87 ± 0.05)‰ for \$^13\$CO\$\_2\$/\$^12\$CO\$\_2\$ and (15 \$\pm\$ 3)\% for \$^3\$He/\$^4\$He.
@article{citeulike:3038316,
abstract = {The diffusion coefficients \$D\$ of important gas tracers dissolved in water and seawater were measured with a modified Barrer method. The measurements include the gases He, Ne, Kr, Xe, H\$\_2\$, CH\$\_4\$, and CO\$\_2\$ dissolved in distilled water in the temperature range from 5 to 35\$\circ\$C, and He and H\$\_2\$ 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, \$\varepsilon\_D\$, was determined to be (−0.87 ± 0.05)‰ for \$^{13}\$CO\$\_2\$/\$^{12}\$CO\$\_2\$ and (15 \$\pm\$ 3)\% for \$^3\$He/\$^4\$He.},
added-at = {2017-06-29T07:13:07.000+0200},
author = {J\"{a}hne, Bernd and Heinz, Gerhard and Dietrich, Wolfgang},
biburl = {https://www.bibsonomy.org/bibtex/2568f7b3a17eea7f2314fcff08edfe7a1/gdmcbain},
citeulike-article-id = {3038316},
citeulike-linkout-0 = {http://www.agu.org/journals/ABS/1987/JC092iC10p10767.shtml},
interhash = {957566aca453ce91860259eaf079d393},
intrahash = {568f7b3a17eea7f2314fcff08edfe7a1},
journal = {Journal of Geophysical Research},
keywords = {material-properties, measurement 80a20-heat-and-mass-transfer diffusivity},
number = {C10},
pages = {10767--10776},
posted-at = {2008-07-24 07:56:28},
priority = {2},
timestamp = {2021-04-06T00:03:16.000+0200},
title = {{Measurement of the Diffusion Coefficients of Sparingly Soluble Gases in Water}},
url = {http://www.agu.org/journals/ABS/1987/JC092iC10p10767.shtml},
volume = 92,
year = 1987
}