When referring to the compilation of Henry's Law Constants, please cite
this publication:
R. Sander: Compilation of Henry's law constants (version 4.0) for
water as solvent, Atmos. Chem. Phys., 15, 4399-4981 (2015),
doi:10.5194/acp-15-4399-2015
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References |
Type |
Notes |
[mol/(m3Pa)] |
[K] |
|
|
|
9.7×10−6 |
1300 |
Warneck and Williams (2012) |
L |
|
9.7×10−6 |
1300 |
Sander et al. (2011) |
L |
|
9.7×10−6 |
1300 |
Sander et al. (2006) |
L |
|
9.7×10−6 |
1300 |
Fernández-Prini et al. (2003) |
L |
1)
|
9.4×10−6 |
1300 |
Wilhelm et al. (1977) |
L |
|
7.9×10−5 |
|
Meadows and Spedding (1974) |
M |
|
7.9×10−6 |
1400 |
Douglas (1967) |
M |
148)
|
9.7×10−6 |
1500 |
Winkler (1901) |
M |
|
9.7×10−6 |
1300 |
Cargill (1990) |
X |
3)
149)
|
9.8×10−6 |
1300 |
Cargill (1990) |
X |
5)
|
8.7×10−6 |
|
Yaws (1999) |
? |
|
9.4×10−6 |
1600 |
Dean (1992) |
? |
6)
|
8.6×10−6 |
|
Yaws and Yang (1992) |
? |
92)
|
Data
The first column contains Henry's law solubility constant
at the reference temperature of 298.15 K.
The second column contains the temperature dependence
, also at the
reference temperature.
References
-
Cargill, R. W., ed.: IUPAC Solubility Data Series, vol. 43 of Carbon Monoxide, Pergamon Press, Oxford, England (1990).
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Dean, J. A.: Lange’s Handbook of Chemistry, McGraw-Hill, Inc. (1992).
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Douglas, E.: Carbon monoxide solubilities in sea water, J. Phys. Chem., 71, 1931–1933, doi:10.1021/J100865A064 (1967).
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Fernández-Prini, R., Alvarez, J. L., & Harvey, A. H.: Henry’s constants and vapor-liquid distribution constants for gaseous solutes in H2O and D2O at high temperatures, J. Phys. Chem. Ref. Data, 32, 903–916, doi:10.1063/1.1564818 (2003).
-
Meadows, R. W. & Spedding, D. J.: The solubility of very low concentrations of carbon monoxide in aqueous solution, Tellus, 26, 143–149, doi:10.3402/TELLUSA.V26I1-2.9745 (1974).
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Sander, S. P., Friedl, R. R., Golden, D. M., Kurylo, M. J., Moortgat, G. K., Keller-Rudek, H., Wine, P. H., Ravishankara, A. R., Kolb, C. E., Molina, M. J., Finlayson-Pitts, B. J., Huie, R. E., & Orkin, V. L.: Chemical Kinetics and Photochemical Data for Use in Atmospheric Studies, Evaluation Number 15, JPL Publication 06-2, Jet Propulsion Laboratory, Pasadena, CA, URL http://jpldataeval.jpl.nasa.gov (2006).
-
Sander, S. P., Abbatt, J., Barker, J. R., Burkholder, J. B., Friedl, R. R., Golden, D. M., Huie, R. E., Kolb, C. E., Kurylo, M. J., Moortgat, G. K., Orkin, V. L., & Wine, P. H.: Chemical Kinetics and Photochemical Data for Use in Atmospheric Studies, Evaluation No. 17, JPL Publication 10-6, Jet Propulsion Laboratory, Pasadena, URL http://jpldataeval.jpl.nasa.gov (2011).
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Warneck, P. & Williams, J.: The Atmospheric Chemist’s Companion: Numerical Data for Use in the Atmospheric Sciences, Springer Verlag, doi:10.1007/978-94-007-2275-0 (2012).
-
Wilhelm, E., Battino, R., & Wilcock, R. J.: Low-pressure solubility of gases in liquid water, Chem. Rev., 77, 219–262, doi:10.1021/CR60306A003 (1977).
-
Winkler, L. W.: Die Löslichkeit der Gase in Wasser (dritte Abhandlung), Ber. Dtsch. Chem. Ges., 34, 1408–1422, doi:10.1002/CBER.19010340210 (1901).
-
Yaws, C. L., ed.: Chemical Properties Handbook, McGraw-Hill, Inc. (1999).
-
Yaws, C. L. & Yang, H.-C.: Henry’s law constant for compound in water, in: Thermodynamic and Physical Property Data, edited by Yaws, C. L., pp. 181–206, Gulf Publishing Company, Houston, TX (1992).
Type
Table entries are sorted according to reliability of the data, listing
the most reliable type first: L) literature review, M) measured, V)
VP/AS = vapor pressure/aqueous solubility, R) recalculation, T)
thermodynamical calculation, X) original paper not available, C)
citation, Q) QSPR, E) estimate, ?) unknown, W) wrong. See Section 3.1
of Sander (2015) for further details.
Notes
1) |
Vapor pressure data for water from Wagner and Pruss (1993) was needed to calculate Hs. |
3) |
Value given here as quoted by Fogg and Sangster (2003). |
5) |
Value given here as quoted by Lide and Frederikse (1995). |
6) |
Only the tabulated data between T = 273 K and T = 303 K from Dean (1992) were used to derive Hs and its temperature dependence. Above T = 303 K, the tabulated data could not be parameterized very well. The partial pressure of water vapor (needed to convert some Henry's law constants) was calculated using the formula given by Sander et al. (1995). The quantities A and α from Dean (1992) were assumed to be identical. |
92) |
Yaws and Yang (1992) give several references for the Henry's law constants but don't assign them to specific species. |
148) |
Solubility in sea water at 20.99 % chlorinity. |
149) |
Erratum for page 260 of Fogg and Sangster (2003): The corresponding equation in preferred units is incorrect. The last term must be divided by 10000 (i.e. 0.0704, not 704). |
The numbers of the notes are the same as
in Sander (2015). References cited in the notes can be
found here.
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