Difference between revisions of "Forstner 1983 POS"
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Revision as of 18:31, 16 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
Cited by
- Gnaiger E et al β MitoEAGLE Task Group (2020) Mitochondrial physiology. Bioenerg Commun 2020.1. doi:10.26124/bec:2020-0001.v1.
Labels:
HRR: Theory
POS 1983, Oxygen, Oxygen solubility, BEC 2020.1