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Difference between revisions of "Forstner 1983 POS"

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{{Publication
{{Publication
|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.
|title=Forstner H, Gnaiger E (1983) Calculation of equilibrium oxygen concentration. In: Gnaiger E, Forstner H (eds) Polarographic oxygen sensors. Aquatic and physiological applications. Springer, Berlin, Heidelberg, New York:321-33.
|info=[[Media:Forstner 1983 POS.pdf|'''Bioblast pdf''']]
|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 Erich
|year=1983
|year=1983
|journal=Springer
|journal=Springer
|mipnetlab=AT_Innsbruck_Gnaiger E, AT Innsbruck MitoCom
|abstract=[[File:Gnaiger&Forstner POS 1983.jpg|right|140px|link=Gnaiger 1983 Springer POS|Gnaiger 1983 Springer POS]] 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.
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In: [[Gnaiger 1983 Springer POS |Gnaiger E, Forstner H, eds (1983) Polarographic Oxygen Sensors. Aquatic and Physiological Applications. Springer, Berlin, Heidelberg, New York:370 pp.]]
|mipnetlab=AT Innsbruck Gnaiger E
}}
}}
== Cited by ==
{{Template:Cited by Gnaiger 2020 BEC MitoPhysiology}}
{{Labeling
{{Labeling
|instruments=Theory
|instruments=Theory
|additional=POS 1983
|additional=POS 1983, Oxygen, Oxygen solubility, BEC 2020.1
}}
}}

Latest revision as of 08:41, 27 October 2022

Publications in the MiPMap
Forstner H, Gnaiger E (1983) Calculation of equilibrium oxygen concentration. In: Gnaiger E, Forstner H (eds) Polarographic oxygen sensors. Aquatic and physiological applications. Springer, Berlin, Heidelberg, New York:321-33.

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POS1983

Bioblast pdf Springer link

Forstner H, Gnaiger Erich (1983) Springer

Abstract:

Gnaiger 1983 Springer POS

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.

In: Gnaiger E, Forstner H, eds (1983) Polarographic Oxygen Sensors. Aquatic and Physiological Applications. Springer, Berlin, Heidelberg, New York:370 pp.


β€’ O2k-Network Lab: AT Innsbruck Gnaiger E

Cited by

Gnaiger Erich et al ― MitoEAGLE Task Group (2020) Mitochondrial physiology. Bioenerg Commun 2020.1.
Gnaiger E et al ― MitoEAGLE Task Group (2020) Mitochondrial physiology. Bioenerg Commun 2020.1. doi:10.26124/bec:2020-0001.v1.



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HRR: Theory 

POS 1983, Oxygen, Oxygen solubility, BEC 2020.1