Difference between revisions of "Forstner 1983 POS"
From Bioblast
Line 12: | Line 12: | ||
{{Labeling | {{Labeling | ||
|instruments=Theory | |instruments=Theory | ||
|additional=POS 1983, Oxygen | |additional=POS 1983, Oxygen, Oxygen solubility | ||
}} | }} |
Revision as of 18:45, 29 May 2020
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. |
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