Difference between revisions of "Forstner 1983 POS"
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{{Publication | {{Publication | ||
|title= | |title=Forstner H, Gnaiger E (1983) Calculation of equilibrium oxygen concentration. In: Polarographic Oxygen Sensors. Aquatic and Physiological Applications. Gnaiger E, Forstner H (eds), Springer, Berlin, Heidelberg, New York:321-33. | ||
|info=[[File:PDF.jpg|100px|link=http://wiki.oroboros.at/images/8/82/Forstner_1983_POS.pdf |Bioblast pdf]] [https://link.springer.com/chapter/10.1007/978-3-642-81863-9_28 Springer link] | |info=[[File:Gnaiger-Forstner 1983 POS.jpg|left|55px|link=https://www.bioblast.at/index.php/Gnaiger_1983_Springer_POS|POS1983]] [[File:PDF.jpg|100px|link=http://wiki.oroboros.at/images/8/82/Forstner_1983_POS.pdf |Bioblast pdf]] [https://link.springer.com/chapter/10.1007/978-3-642-81863-9_28 Springer link] | ||
|authors=Forstner H, Gnaiger E | |authors=Forstner H, Gnaiger E | ||
|year=1983 | |year=1983 |
Revision as of 14:18, 2 January 2021
Forstner H, Gnaiger E (1983) Calculation of equilibrium oxygen concentration. In: Polarographic Oxygen Sensors. Aquatic and Physiological Applications. Gnaiger E, Forstner H (eds), Springer, Berlin, Heidelberg, New York:321-33. |
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Forstner H, Gnaiger E (1983) Springer
Abstract:
In the chemical literature solubility of a gas is generally given as the Bunsen absorption coefficient, Ξ±, which is a function of temperature and of the electrolyte content of the solvent. Hydrostatic pressure has little effect on solubility, but with increasing head the escaping tendency of the gas increases. Therefore, at constant concentration, a POS gives a higher reading at greater depth. This effect is negligible (< 1 %) at depths less than 100 m.
β’ O2k-Network Lab: AT Innsbruck Gnaiger E
Labels:
HRR: Theory
POS 1983, Oxygen, Oxygen solubility