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Henry's Law Constants

www.henrys-law.org

Rolf Sander

NEW: Version 5.0.0 has been published in October 2023

Atmospheric Chemistry Division

Max-Planck Institute for Chemistry
Mainz, Germany


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Henry's Law Constants

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When referring to the compilation of Henry's Law Constants, please cite this publication:

R. Sander: Compilation of Henry's law constants (version 5.0.0) for water as solvent, Atmos. Chem. Phys., 23, 10901-12440 (2023), doi:10.5194/acp-23-10901-2023

The publication from 2023 replaces that from 2015, which is now obsolete. Please do not cite the old paper anymore.


Notes

ID Notetext
1) A detailed temperature dependence with more than one parameter is available in the original publication. Here, only the temperature dependence at 298.15 K according to the van 't Hoff equation is presented.
2) Clever et al. (2014) recommend the data from Rettich et al. (2000).
3) The vapor pressure for water from Wagner and Pruss (1993) was used to calculate Hs.
4) The data from Millero et al. (2002a) were fitted to the three-parameter equation: Hscp= exp( −130.91491 +6700.12242/T +17.04684 ln(T)) mol m−3 Pa−1, with T in K.
5) Almost the same data were also published in Millero et al. (2002b).
6) The data from Millero et al. (2002b) were fitted to the three-parameter equation: Hscp= exp( −118.73105 +6163.97787/T +15.22401 ln(T)) mol m−3 Pa−1, with T in K.
7) Almost the same data were also published in Millero et al. (2002a).
8) The data from Rettich et al. (2000) were fitted to the three-parameter equation: Hscp= exp( −179.13831 +8707.17767/T +24.33473 ln(T)) mol m−3 Pa−1, with T in K.
9) The data from Sherwood et al. (1991) were fitted to the three-parameter equation: Hscp= exp( −197.67462 +9515.09306/T +27.11204 ln(T)) mol m−3 Pa−1, with T in K.
10) The data from Rettich et al. (1981) were fitted to the three-parameter equation: Hscp= exp( −178.21340 +8672.23354/T +24.19307 ln(T)) mol m−3 Pa−1, with T in K.
11) Measured at high temperature and extrapolated to T = 298.15 K.
12) Value at T = 293 K.
13) Value at T = 273 K.
14) Value at T = 310 K.
15) The data from Murray and Riley (1969) were fitted to the three-parameter equation: Hscp= exp( −180.22078 +8760.50130/T +24.49289 ln(T)) mol m−3 Pa−1, with T in K.
16) The data from Shoor et al. (1969) were fitted to the three-parameter equation: Hscp= exp( −91.44799 +4548.67245/T +11.38821 ln(T)) mol m−3 Pa−1, with T in K.
17) The data from Carpenter (1966) were fitted to the three-parameter equation: Hscp= exp( −130.04464 +6687.45227/T +16.90114 ln(T)) mol m−3 Pa−1, with T in K.
18) The data from Morrison and Billett (1952) were fitted to the three-parameter equation: Hscp= exp( −167.89288 +8254.02144/T +22.62741 ln(T)) mol m−3 Pa−1, with T in K.
19) The data from Winkler (1891b) were fitted to the three-parameter equation: Hscp= exp( −155.30315 +7638.78869/T +20.77945 ln(T)) mol m−3 Pa−1, with T in K.
20) Calculated using machine learning matrix completion methods (MCMs).
21) Several references are given in the list of Henry's law constants but not assigned to specific species.
22) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −161.84252 +7966.66767/T +21.73409 ln(T)) mol m−3 Pa−1, with T in K.
23) The partial pressure of water vapor (needed to convert some Henry's law constants) was calculated using the formula given by Buck (1981). The quantities A and α from Dean and Lange (1999) were assumed to be identical.
24) Value at "room temperature".
25) Clever et al. (2014) recommend the data from Battino (1981).
26) Battino (1981) concludes that ozone aqueous chemistry needs further clarification. Data from Roth and Sullivan (1981) are recommended, in spite of limitations and assumptions of the data.
27) Roth and Sullivan (1981) found that Hs depends on the concentration of OH.
28) Value at T = 291 K.
29) Value given here as quoted by Durham et al. (1981).
30) Lide and Frederikse (1995) present an unusually low value for the Henry solubility of ozone. They refer to Battino (1981) as the source, but the quoted value cannot be found there.
31) Parker (1992) assumes that the free energy of solvation of atomic hydrogen is equal to that of He because of a similar van der Waals radius.
32) Roduner and Bartels (1992) say that the free energy of solvation ∆GHsolv (and therefore Henry's law constant) of atomic hydrogen is approximated well by that of molecular hydrogen. However, they apparently do not give a value for ∆GHsolv.
33) Fitting the temperature dependence dlnH/d(1/T) produced a low correlation coefficient (r2 < 0.9). The data should be treated with caution.
34) Data digitized from Figs. 2 and 3 in Schmidt (1979).
35) The data from Gordon et al. (1977) were fitted to the three-parameter equation: Hscp= exp( −158.95051 +6959.76267/T +21.73478 ln(T)) mol m−3 Pa−1, with T in K.
36) The data from Crozier and Yamamoto (1974) were fitted to the three-parameter equation: Hscp= exp( −129.44163 +5676.58091/T +17.31002 ln(T)) mol m−3 Pa−1, with T in K.
37) The data presented for hydrogen in Table II of Shoor et al. (1969) appear to be incorrect and are not reproduced here.
38) Value at T = 303 K.
39) The data from Morrison and Billett (1952) were fitted to the three-parameter equation: Hscp= exp( −94.36490 +4110.23880/T +12.07743 ln(T)) mol m−3 Pa−1, with T in K.
40) The data from Braun (1900) were fitted to the three-parameter equation: Hscp= exp( 171.59451 −6856.02728/T −28.14739 ln(T)) mol m−3 Pa−1, with T in K.
41) The data from Winkler (1891a) were fitted to the three-parameter equation: Hscp= exp( −103.47250 +4506.63123/T +13.44160 ln(T)) mol m−3 Pa−1, with T in K.
42) Fitting the temperature dependence dlnH/d(1/T) produced a very low correlation coefficient (r2 < 0.5). The data should be treated with caution.
43) The paper by Bunsen (1855a) was written in German. English versions with the same data were published by Bunsen (1855b) and Bunsen (1855c).
44) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −98.78036 +4298.15060/T +12.74131 ln(T)) mol m−3 Pa−1, with T in K.
45) Young (1981a) recommend the data from Muccitelli and Wen (1978).
46) The data from Muccitelli and Wen (1978) were fitted to the three-parameter equation: Hscp= exp( −103.11330 +4676.56978/T +13.28348 ln(T)) mol m−3 Pa−1, with T in K.
47) The free energy of solution was calculated based on electrochemical reduction potentials and related free energies.
48) Calculated from correlation between the polarizabilities and solubilities of stable gases. The temperature dependence is an estimate of the upper limit.
49) Jacob (1986) assumed the temperature dependence to be the same as for water.
50) In the abstract, Schwartz (1984) gives a range of 9.9 mol m−3 Pa−1 < Hscp < 3.0×101 mol m−3 Pa−1. The mean value of this range (2.0×101 mol m−3 Pa−1) has been used by Lelieveld and Crutzen (1991), Pandis and Seinfeld (1989), and Jacob (1986).
51) The value of Hs was taken from Schwartz (1984).
52) Erratum for page 264 of Fogg and Sangster (2003): the second value from their Ref. [10] refers to 291.15 K, not 281.15 K.
53) This value is a correction of the solubility published by Lind and Kok (1986).
54) This value was measured at low pH. It is superseded by a later publication of the same group (Lind and Kok, 1994).
55) Pandis and Seinfeld (1989) cite an incorrect value from Lind and Kok (1986); see erratum by Lind and Kok (1994).
56) The data from Rettich et al. (1984) were fitted to the three-parameter equation: Hscp= exp( −187.67954 +8903.42524/T +25.60079 ln(T)) mol m−3 Pa−1, with T in K.
57) The data from Murray et al. (1969) were fitted to the three-parameter equation: Hscp= exp( −174.95275 +8370.22025/T +23.67878 ln(T)) mol m−3 Pa−1, with T in K.
58) The data from Morrison and Billett (1952) were fitted to the three-parameter equation: Hscp= exp( −193.68175 +9249.63150/T +26.45117 ln(T)) mol m−3 Pa−1, with T in K.
59) Value at T = 311 K.
60) The data from Braun (1900) were fitted to the three-parameter equation: Hscp= exp( 291.66324 −11637.66767/T −46.44134 ln(T)) mol m−3 Pa−1, with T in K.
61) The data from Winkler (1891b) were fitted to the three-parameter equation: Hscp= exp( −164.15156 +7906.86704/T +22.05399 ln(T)) mol m−3 Pa−1, with T in K.
62) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −163.64571 +7887.30480/T +21.97696 ln(T)) mol m−3 Pa−1, with T in K.
63) Tsuji et al. (1990) provide effective Henry's law constants at several pH values. Here, only the value at pH = 5.8 is shown for the (acidic) S compounds and the value at pH = 8.6 for the alkaline N compounds.
64) Value given here as quoted by Betterton (1992).
65) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( 206.08500 −7165.18642/T −32.18383 ln(T)) mol m−3 Pa−1, with T in K.
66) Bone et al. (1983) give Carter et al. (1968) as the source. However, no data were found in that reference.
67) There is a typo in Sander et al. (2011): the value for A should be −10.19 not 10.19.
68) Modarresi et al. (2007) use different descriptors for their calculations. They conclude that a genetic algorithm/radial basis function network (GA/RBFN) is the best QSPR model. Only these results are shown here.
69) Incorrect data are given by Burkholder et al. (2019) for HN3. The correct parameter for the temperature dependence is A = −10.19 (Robert E. Huie, personal communication, 2021).
70) Incorrect data are given by Burkholder et al. (2015) for HN3. The correct parameter for the temperature dependence is A = −10.19 (Robert E. Huie, personal communication, 2021).
71) Solubility in sea water.
72) The data from Weiss and Price (1980) were fitted to the three-parameter equation: Hscp= exp( −180.63611 +9824.20147/T +24.46112 ln(T)) mol m−3 Pa−1, with T in K.
73) Value at T = 296 K.
74) The data from Roth (1897) were fitted to the three-parameter equation: Hscp= exp( −125.17909 +7706.80638/T +15.96486 ln(T)) mol m−3 Pa−1, with T in K.
75) Value given here as quoted by Gabel and Schultz (1973).
76) Value given here as quoted by Sy and Hasbrouck (1964).
77) The H298 and A, B, C data listed in Table 5.4 of Sander et al. (2011) are inconsistent, with 94 % difference.
78) The H298 and A, B, C data listed in Table 5.4 of Sander et al. (2006) are inconsistent, with 94 % difference.
79) A minus sign is missing in the fitting parameter presented by Young (1981b). It should be −62.8086, not 62.8086.
80) Value at T = 297 K.
81) Value at T = 288 K.
82) The data from Winkler (1901) were fitted to the three-parameter equation: Hscp= exp( −184.00012 +8924.34832/T +25.13228 ln(T)) mol m−3 Pa−1, with T in K.
83) The data from Loomis (1928) were fitted to the three-parameter equation: Hscp= exp( −223.88313 +10620.37030/T +31.13453 ln(T)) mol m−3 Pa−1, with T in K.
84) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −160.19223 +7888.02642/T +21.56401 ln(T)) mol m−3 Pa−1, with T in K.
85) Incorrect data are given by Burkholder et al. (2019) for NO. The correct parameters for the temperature dependence are A = −163.86, B = 8234, C = 22.816 (Robert E. Huie, personal communication, 2021).
86) Incorrect data are given by Burkholder et al. (2015) for NO. The correct parameters for the temperature dependence are A = −163.86, B = 8234, C = 22.816 (Robert E. Huie, personal communication, 2021).
87) The fitting parameters A, B, C, and D in Table I of Wilhelm et al. (1977) do not reproduce the data in their Table III.
88) Value at T = 295 K.
89) Pandis and Seinfeld (1989) refer to Schwartz (1984) as the source, but the quoted value cannot be found there.
90) Value obtained by estimating the diffusion coefficient for NO3 to be D = 1.0×10−5 cm2/s.
91) Jacob (1986) assumes that NO3 has the same Henry's law constant as HNO3.
92) Seinfeld and Pandis (1997) probably refer to the incorrect value given by Pandis and Seinfeld (1989).
93) Calculated from the solvation free energy.
94) Calculated from the solvation free energy.
95) Calculated from the solvation free energy.
96) This value was extrapolated from data at T = 230 K and T = 273 K.
97) Robinson et al. (1997) applied an empirical correlation between Henry's law solubilities and boiling points from Schwartz and White (1981).
98) Estimate based on the relation between boiling points and Henry's law constants for other nitrogen oxides from Schwartz and White (1981).
99) Fast, irreversible hydrolysis is assumed, which is equivalent to an infinite effective Henry's law constant.
100) Calculated based on the method by Meylan and Howard (1991).
101) Lelieveld and Crutzen (1991) assume the temperature dependence to be the same as for a(H+)a(NO3)/p(HNO3) in Schwartz and White (1981).
102) Hs′ = 2.6×107×exp(8700 K (1/T−1/T)) mol2/(m6 Pa)
103) Hs′ = 2.4×107×exp(8700 K (1/T−1/T)) mol2/(m6 Pa)
104) Pandis and Seinfeld (1989) refer to Schwartz (1984) as the source, but it is probably from Schwartz and White (1981).
105) The value is incorrect. See erratum by Brimblecombe and Clegg (1989).
106) Möller and Mauersberger (1992) assumed the solubility of HNO4 to be comparable to that of HNO3.
107) Hs′ = 9.4×101×exp(7400 K (1/T−1/T)) mol2/(m6 Pa)
108) The data from Dean et al. (1973) were fitted to the three-parameter equation: Hscp= exp( −164.52717 +8214.77776/T +21.97482 ln(T)) mol m−3 Pa−1, with T in K.
109) The data from Ashton et al. (1968) were fitted to the three-parameter equation: Hscp= exp( −279.21972 +13536.60588/T +38.97386 ln(T)) mol m−3 Pa−1, with T in K.
110) The data from Dean et al. (1973) were fitted to the three-parameter equation: Hscp= exp( −318.29953 +15733.17858/T +44.55320 ln(T)) mol m−3 Pa−1, with T in K.
111) The value presented here appears to be the total solubility of chlorine (i.e., the sum of Cl2 and HOCl) at a partial pressure of p(Cl2)  = 101325 Pa. This is different from Henry's law constant, which is defined at extrapolation to infinite dilution.
112) Young (1983) recommends values calculated from Table 1 of Adams and Edmonds (1937). Thus, the data refer to effective values that take into account the hydrolysis in the aqueous phase:
Hs,eff = ([Cl2]+[HOCl])/p(Cl2).
In addition, the values apply to a partial pressure of p(Cl2)  = 101325 Pa, and not to infinite dilution.
113) The same experimental data were also published by Whitney and Vivian (1941b).
114) The data from Yakovkin (1900) were fitted to the three-parameter equation: Hscp= exp( −122.31264 +7690.40834/T +15.63947 ln(T)) mol m−3 Pa−1, with T in K.
115) Leaist (1986) converted the total solubility of chlorine in pure water from Adams and Edmonds (1937) to an intrinsic Henry's law constant.
116) Adams and Edmonds (1937) re-analyzed the data from Yakovkin (1900) and Arkadiev (1918), considering deviations from the perfect gas law. They calculated the total solubility of chlorine (i.e., the sum of Cl2 and HOCl) at several partial pressures of Cl2. This is different from Henry's law constant, which is defined at extrapolation to infinite dilution.
117) Arkadiev (1918) re-analyzed the measurements of Yakovkin (1900). In addition to the data between 15 °C and 83.4 °C, he also analyzed the experimental results at 0 °C and obtained a dimensionless Henry solubility of Hscc = 4.115 at that temperature.
118) The value of ∆H° listed in Table 2 of Bartlett and Margerum (1999) is incorrect. The correct value can be found in the text on page 3411.
119) Wilhelm et al. (1977) present a fitting function for Cl2 based on four papers which are cited in the footnotes of Table I. However, Bunsen (1855b) and Bunsen (1855c) do not contain any data for Cl2, and the data from Whitney and Vivian (1941a) and Whitney and Vivian (1941b) are inconsistent with the fitting function.
120) Calculated from the free energy of solution by Schwarz and Dodson (1984).
121) Hs′ = 2.0×107 mol2/(m6 Pa)
122) Hs′ = 2.0×107×exp(9000 K (1/T−1/T)) mol2/(m6 Pa)
123) Hs′ = 2.0×107×exp(9000 K (1/T−1/T)) mol2/(m6 Pa)
124) Hs′ = 2.0×107×exp(9000 K (1/T−1/T)) mol2/(m6 Pa)
125) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( 9.16427 +45.13997/T −1.92853 ln(T)) mol m−3 Pa−1, with T in K.
126) Pandis and Seinfeld (1989) refer to Marsh and McElroy (1985) as the source, but the quoted value cannot be found there.
127) This value was extrapolated from data at T = 215 K and T = 263 K.
128) Value at pH = 6.5.
129) Value at T = 200 K.
130) Secoy and Cady (1941) measured the gas-aqueous equilibrium constant p(Cl2O) / c(HOCl)2 but not the intrinsic Henry's law constant of Cl2O.
131) Ourisson and Kastner (1939) measured the gas-aqueous equilibrium constant p(Cl2O) / c(HOCl)2 but not the intrinsic Henry's law constant of Cl2O.
132) The data from this work were fitted to the three-parameter equation: Hscp= exp( 1680.49677 −69933.08019/T −254.37188 ln(T)) mol m−3 Pa−1, with T in K.
133) The gas-aqueous equilibrium constant p(Cl2O) / c(HOCl)2 was combined with the temperature-dependent aqueous-phase hydration constant c(HOCl)2 / c(Cl2O) from Roth (1929) in order to calculate the intrinsic Henry's law constant of Cl2O.
134) Data for the equilibrium between gaseous Cl2O and aqueous HOCl were taken from Secoy and Cady (1941).
135) Data for the equilibrium between gaseous Cl2O and aqueous HOCl were taken from Ourisson and Kastner (1939).
136) Value at T = 277 K.
137) The recommended value from Wilhelm et al. (1977) appears to be dubious as it refers to Secoy and Cady (1941), who do not provide a value for the intrinsic Henry's law constant of Cl2O.
138) Young (1983) cites data from Secoy and Cady (1941). However, that paper only describes the equilibrium between gas-phase Cl2O and aqueous-phase HOCl. A Henry's law constant of Cl2O is not provided. In addition, the values given by Young (1983) are not extrapolated to infinite dilution but to 1 atm partial pressure of Cl2O. It is not explained how the nonlinear pressure dependence was extrapolated to 1 atm.
139) Wilhelm et al. (1977) cite Secoy and Cady (1941) as the source for their value. However, that paper only describes the equilibrium between gas-phase Cl2O and aqueous-phase HOCl. A Henry's law constant of Cl2O is not provided.
140) Even though Haller and Northgraves (1955) have been cited several times as the source of the ClO2 solubility data, they did not perform any measurements. They took the data from the 1952 edition of the Kirk-Othmer Encyclopedia of Chemical Technology which apparently reproduced data from Holst (1944).
141) Derived as a fitting parameter used in numerical modeling.
142) Robinson et al. (1997) assumed that the entropy of vaporization is the same for HOCl and ClNO3 according to Trouton's rule. On their page 3592, they mention a value of 7 M atm−1 at 250 K. However, checking their Fig. 9 and applying the temperature-dependence equation from their Table 3, it seems that the value of 7 M atm−1 refers to 298 K, not 250 K.
143) Dubik et al. (1987) measured the solubility in concentrated salt solutions (natural brines).
144) Value given here as quoted by McCoy et al. (1990).
145) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −148.75612 +9709.79389/T +19.53402 ln(T)) mol m−3 Pa−1, with T in K.
146) Hs′ = 8.2×109×exp(10000 K (1/T−1/T)) mol2/(m6 Pa)
147) Hs′ = 1.3×1010×exp(10000 K (1/T−1/T)) mol2/(m6 Pa)
148) Hs′ = 7.0×109×exp(10000 K (1/T−1/T)) mol2/(m6 Pa)
149) Chameides and Stelson (1992) give a value of Hs′ = 7.1×109×exp(6100 K (1/T−1/T)) mol2/(m6 Pa). They refer to Jacob (1986) and Chameides (1984) as the source, but this value cannot be found there.
150) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −60.28318 +2830.41867/T +8.66642 ln(T)) mol m−3 Pa−1, with T in K.
151) The value is from Table 1 of the paper. However, J. Geophys. Res. forgot to print the tables, and I received them directly from the author.
152) The value presented for HOBr is incorrect. A corrected version was later published by Burkholder et al. (2019).
153) Fickert (1998) extracted a value from wetted-wall flow tube experiments. However, it was later discovered that under the experimental conditions no evaluation of Hs is possible (John Crowley, personal communication, 1999).
154) Value at T = 275 K.
155) Value at T = 290 K.
156) Calculated using data from Wagman et al. (1982) and the aqueous-phase equilibrium Cl2 + Br2 ↔ 2 BrCl from Wang et al. (1994).
157) Thompson and Zafiriou (1983) quote a paper as the source that gives only the solubility but not the Henry's law constant.
158) Calculated from the free energy of solution by Schwarz and Bielski (1986).
159) Hs′ = 2.5×1010×exp(9800 K (1/T−1/T)) mol2/(m6 Pa)
160) Hs′ = 2.1×1010×exp(9800 K (1/T−1/T)) mol2/(m6 Pa)
161) Saiz-Lopez et al. (2014) refer to Saiz-Lopez et al. (2008) as the source, but the quoted value cannot be found there.
162) It is unclear to which isomer the value of the Henry's law constant refers to.
163) Assumed to be infinity by analogy with INO3.
164) Thompson and Zafiriou (1983) assume that Hscp(HOI) is between 4.4×10−1 mol m−3 Pa−1 and 4.4×102 mol m−3 Pa−1.
165) Badia et al. (2019) assume that INO2 has the same Henry's law constant as BrNO2.
166) Data taken from the AGRITOX database file agritox-20210608.zip.
167) Fogg and Young (1988) provide two different fitting functions: one for T < 283.2 K and one for T > 283.2 K. At T=283.2 K, the functions have different values and different slopes. Here, only the function that is valid at T is used.
168) The data from Clarke and Glew (1971) were fitted to the three-parameter equation: Hscp= exp( −133.37135 +7422.07576/T +17.82903 ln(T)) mol m−3 Pa−1, with T in K.
169) The data from Schoenfeld (1855) were fitted to the three-parameter equation: Hscp= exp( 98.96644 −3021.28876/T −16.78233 ln(T)) mol m−3 Pa−1, with T in K.
170) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −122.57010 +6962.28299/T +16.20245 ln(T)) mol m−3 Pa−1, with T in K.
171) The parameter fit for the temperature dependence is incorrect. A corrected version was later presented by Iliuta and Larachi (2007).
172) The data from Clarke and Glew (1971) were fitted to the three-parameter equation: Hscp= exp( −152.96053 +8324.82999/T +20.73129 ln(T)) mol m−3 Pa−1, with T in K.
173) Obtained with D2O as solvent.
174) Value at T = 353 K.
175) The data from Schoenfeld (1855) were fitted to the three-parameter equation: Hscp= exp( 265.79241 −9131.99684/T −42.01987 ln(T)) mol m−3 Pa−1, with T in K.
176) Value given here as quoted by Rodríguez-Sevilla et al. (2002).
177) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( 153.05871 −4328.05304/T −25.05397 ln(T)) mol m−3 Pa−1, with T in K.
178) Marti et al. (1997) give partial pressures of H2SO4 over a concentrated solution (e.g., 2.6×10−9 Pa for 54.1 wt % at 298 K). Extrapolating this to dilute solutions can only be considered an order-of-magnitude approximation for Hs.
179) Ayers et al. (1980) give partial pressures of H2SO4 over concentrated solutions at high temperatures. Extrapolating this to dilute solutions can only be considered an order-of-magnitude approximation for Hs.
180) Gmitro and Vermeulen (1964) give partial pressures of H2SO4 over a concentrated solution (e.g., 10−7 mmHg for 70 wt % at 298 K). Extrapolating this to dilute solutions can only be considered an order-of-magnitude approximation for Hs.
181) Clegg et al. (1998) estimate a Henry's law constant of 5×1011 atm−1 at 303.15 K for the reaction H2SO4(g) ↔ 2 H+(aq) + SO42−(aq) but do not give a definition for it. Probably it is defined as x2(H+)×x(SO42−)/p(H2SO4), where x is the aqueous-phase mixing ratio.
182) The data from Bullister et al. (2002) were fitted to the three-parameter equation: Hscp= exp( −281.50843 +14256.43847/T +38.73689 ln(T)) mol m−3 Pa−1, with T in K.
183) The data presented for SF6 in Table II of Shoor et al. (1969) appear to be incorrect and are not reproduced here.
184) The data from Ashton et al. (1968) were fitted to the three-parameter equation: Hscp= exp( −431.90650 +20715.81650/T +61.33841 ln(T)) mol m−3 Pa−1, with T in K.
185) Value from the validation set for checking whether the model is satisfactory for compounds that are absent from the training set.
186) Experimental value, extracted from HENRYWIN.
187) Estimation based on the quotient between vapor pressure and water solubility, extracted from HENRYWIN.
188) The data presented for helium in Table II of Shoor et al. (1969) appear to be incorrect and are not reproduced here.
189) The data from Morrison and Johnstone (1954) were fitted to the three-parameter equation: Hscp= exp( −267.15298 +11440.04263/T +37.95994 ln(T)) mol m−3 Pa−1, with T in K.
190) The data from Lannung (1930) were fitted to the three-parameter equation: Hscp= exp( 84.35043 −4135.59197/T −14.55881 ln(T)) mol m−3 Pa−1, with T in K.
191) Calculated employing molecular force field models for the solutes from Warr et al. (2015).
192) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −153.15219 +6434.36008/T +20.89911 ln(T)) mol m−3 Pa−1, with T in K.
193) The data from Morrison and Johnstone (1954) were fitted to the three-parameter equation: Hscp= exp( −171.84866 +7492.61303/T +23.58966 ln(T)) mol m−3 Pa−1, with T in K.
194) The data from Lannung (1930) were fitted to the three-parameter equation: Hscp= exp( −40.04033 +1266.80589/T +4.12574 ln(T)) mol m−3 Pa−1, with T in K.
195) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −150.94728 +6639.96438/T +20.42365 ln(T)) mol m−3 Pa−1, with T in K.
196) The data from Rettich et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −178.55165 +8674.63293/T +24.26764 ln(T)) mol m−3 Pa−1, with T in K.
197) The data from Murray and Riley (1970) were fitted to the three-parameter equation: Hscp= exp( −151.84230 +7548.13106/T +20.24085 ln(T)) mol m−3 Pa−1, with T in K.
198) The data from Shoor et al. (1969) were fitted to the three-parameter equation: Hscp= exp( −177.19900 +8740.49327/T +23.99118 ln(T)) mol m−3 Pa−1, with T in K.
199) The data from Ashton et al. (1968) were fitted to the three-parameter equation: Hscp= exp( −160.52023 +7898.05096/T +21.56102 ln(T)) mol m−3 Pa−1, with T in K.
200) The data from Morrison and Johnstone (1954) were fitted to the three-parameter equation: Hscp= exp( −159.49603 +7859.86242/T +21.39868 ln(T)) mol m−3 Pa−1, with T in K.
201) The data from Lannung (1930) were fitted to the three-parameter equation: Hscp= exp( −183.19260 +8856.79081/T +24.97248 ln(T)) mol m−3 Pa−1, with T in K.
202) Calculated employing molecular force field models for the solutes from Vrabec et al. (2001).
203) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −143.77232 +7158.59719/T +19.05403 ln(T)) mol m−3 Pa−1, with T in K.
204) The data from Morrison and Johnstone (1954) were fitted to the three-parameter equation: Hscp= exp( −153.87925 +7855.39037/T +20.51280 ln(T)) mol m−3 Pa−1, with T in K.
205) Two series of measurements with considerably different results are presented by von Antropoff (1910) for krypton.
206) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −220.92114 +10903.79433/T +30.49407 ln(T)) mol m−3 Pa−1, with T in K.
207) The value b for Xe given by Himmelblau (1960) in their Table III is incorrect. Most likely, only a minus sign is missing.
208) The data from Morrison and Johnstone (1954) were fitted to the three-parameter equation: Hscp= exp( −165.83721 +8808.62019/T +22.15186 ln(T)) mol m−3 Pa−1, with T in K.
209) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −199.40126 +10306.10786/T +27.18844 ln(T)) mol m−3 Pa−1, with T in K.
210) The data from Lewis et al. (1987) were fitted to the three-parameter equation: Hscp= exp( 5.03587 +1555.37916/T −3.42648 ln(T)) mol m−3 Pa−1, with T in K.
211) Calculated employing molecular force field models for the solutes from Mick et al. (2016).
212) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −240.66156 +12686.97685/T +33.12171 ln(T)) mol m−3 Pa−1, with T in K.
213) The data from Sisi et al. (1971) were fitted to the three-parameter equation: Hscp= exp( −81.82525 +4954.57763/T +10.19950 ln(T)) mol m−3 Pa−1, with T in K.
214) Solubility in natural sea water. Measurements at different salinities were also performed but only at a fixed temperature of 296.15 K.
215) Temperature dependence calculated using linear free energy relationships (LFERs).
216) Petersen et al. (1998) give the invalid unit "mol L−1 ppm−1". Here, it is assumed that "ppm" is used as a synonym for "10−6 atm".
217) Shon et al. (2005) refer to Petersen et al. (1998) as the source, but a different value is listed there.
218) Value at T = 333 K.
219) Calculated using linear free energy relationships (LFERs).
220) More than one reference is given as the source of this value.
221) Hedgecock et al. (2005) refer to Hedgecock and Pirrone (2004) as the source, but this value cannot be found there.
222) Clever and Young (1987) recommend the data from Rettich et al. (1981).
223) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −133.87728 +6629.97157/T +17.62624 ln(T)) mol m−3 Pa−1, with T in K.
224) The data from Scharlin and Battino (1995) were fitted to the three-parameter equation: Hscp= exp( −206.41168 +10058.77208/T +28.34417 ln(T)) mol m−3 Pa−1, with T in K.
225) The data from Shoor et al. (1969) were fitted to the three-parameter equation: Hscp= exp( −201.05778 +9920.37989/T +27.48020 ln(T)) mol m−3 Pa−1, with T in K.
226) The same value was also published in McAuliffe (1963).
227) The same value was also published in McAuliffe (1966).
228) The data from Morrison and Billett (1952) were fitted to the three-parameter equation: Hscp= exp( −195.92072 +9624.37184/T +26.74976 ln(T)) mol m−3 Pa−1, with T in K.
229) The data from Winkler (1901) were fitted to the three-parameter equation: Hscp= exp( −203.15902 +9951.75251/T +27.82679 ln(T)) mol m−3 Pa−1, with T in K.
230) Yao et al. (2002) compared two QSPR methods and found that radial basis function networks (RBFNs) are better than multiple linear regression. In their paper, they provide neither a definition nor the unit of their Henry's law constants. Comparing the values with those that they cite from Yaws (1999), it is assumed that they use the variant Hvpx and the unit atm.
231) English and Carroll (2001) provide several calculations. Here, the preferred value with explicit inclusion of hydrogen bonding parameters from a neural network is shown.
232) Value from the training dataset.
233) Calculated with a principal component analysis (PCA); see Suzuki et al. (1992) for details.
234) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −185.72813 +9197.97387/T +25.21142 ln(T)) mol m−3 Pa−1, with T in K.
235) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −109.51433 +6313.03876/T +13.60483 ln(T)) mol m−3 Pa−1, with T in K.
236) The data from Morrison and Billett (1952) were fitted to the three-parameter equation: Hscp= exp( −215.51394 +10861.98666/T +29.50128 ln(T)) mol m−3 Pa−1, with T in K.
237) The data from Winkler (1901) were fitted to the three-parameter equation: Hscp= exp( −277.60377 +13887.90452/T +38.63046 ln(T)) mol m−3 Pa−1, with T in K.
238) Value given here as quoted by Gharagheizi et al. (2010).
239) Calculated using linear free energy relationships (LFERs).
240) Calculated using SPARC Performs Automated Reasoning in Chemistry (SPARC).
241) Calculated using COSMOtherm.
242) Temperature is not specified.
243) Value from the training dataset.
244) Calculated using the GROMHE model.
245) Calculated using the SPARC approach.
246) Calculated using the HENRYWIN method.
247) Calculated using a combination of a group contribution method and neural networks.
248) Modarresi et al. (2005) use different descriptors for the QSPR models. They conclude that their "COSA" method and the artificial neural network (ANN) are best. However, as COSA is not ideal for hydrocarbons with low solubility, only results obtained with ANN are shown here.
249) Yaffe et al. (2003) present QSPR results calculated with the fuzzy ARTMAP (FAM) and with the back-propagation (BK-Pr) method. They conclude that FAM is better. Only the FAM results are shown here.
250) Value from the training set.
251) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −249.13770 +12672.58357/T +34.34947 ln(T)) mol m−3 Pa−1, with T in K.
252) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −275.67877 +14048.75446/T +38.16041 ln(T)) mol m−3 Pa−1, with T in K.
253) The data from Morrison and Billett (1952) were fitted to the three-parameter equation: Hscp= exp( −257.69118 +13189.22089/T +35.51019 ln(T)) mol m−3 Pa−1, with T in K.
254) The H298 and A, B, C data listed in Table 5-4 of Burkholder et al. (2019) are inconsistent, with 14 % difference.
255) The H298 and A, B, C data listed in Table 5-4 of Burkholder et al. (2015) are inconsistent, with 14 % difference.
256) The H298 and A, B, C data listed in Table 5.4 of Sander et al. (2011) are inconsistent, with 14 % difference.
257) The H298 and A, B, C data listed in Table 5.4 of Sander et al. (2006) are inconsistent, with 14 % difference.
258) The data from Morrison and Billett (1952) were fitted to the three-parameter equation: Hscp= exp( −257.40529 +13425.82235/T +35.27658 ln(T)) mol m−3 Pa−1, with T in K.
259) Value given here as quoted by Dupeux et al. (2022).
260) Calculated using the COSMO-RS method.
261) Value from the validation dataset.
262) The H298 and A, B, C data listed in Table 5-4 of Burkholder et al. (2019) are inconsistent, with 6 % difference.
263) The H298 and A, B, C data listed in Table 5-4 of Burkholder et al. (2015) are inconsistent, with 6 % difference.
264) The H298 and A, B, C data listed in Table 5.4 of Sander et al. (2011) are inconsistent, with 6 % difference.
265) The H298 and A, B, C data listed in Table 5.4 of Sander et al. (2006) are inconsistent, with 6 % difference.
266) Fogg and Sangster (2003) cite an incorrect fitting function from Hayduk (1986).
267) The fitting function and the data in the table on page 34 of Hayduk (1986) are inconsistent by a factor of about 3. A comparison with the original measurements by Wetlaufer et al. (1964) shows that the data in the table are correct. Refitting the data suggests that the third fitting parameter should be 52.4651, not 53.4651.
268) Value from the test set.
269) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 15 % difference.
270) The data from Jou and Mather (2000) were fitted to the three-parameter equation: Hscp= exp( −400.38105 +20169.61328/T +56.35286 ln(T)) mol m−3 Pa−1, with T in K.
271) The paper by Jou and Mather (2000) also contains high-temperature data. However, only data up to 373.2 K were used here to calculate the temperature dependence.
272) Value from the validation dataset.
273) Value from the test set.
274) The data from Shoor et al. (1969) were fitted to the three-parameter equation: Hscp= exp( −311.59148 +15699.27148/T +43.32183 ln(T)) mol m−3 Pa−1, with T in K.
275) Value from the test dataset.
276) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 6 % difference.
277) Apparently, the values in Table 2 of Park et al. (1997) show log10(Kaw) and not Kaw as their figure caption states.
278) Extrapolated from data measured between 40 °C and 80 °C.
279) Data are taken from the report by Howe et al. (1987).
280) Value from the training set.
281) In their Table 8, Staudinger and Roberts (1996) incorrectly cite a value given by Ashworth et al. (1988).
282) The same data were also published in Hansen et al. (1995).
283) Hansen et al. (1993) found that the solubility of 2-methylhexane increases with temperature.
284) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 5 % difference.
285) The data from Dohányosová et al. (2004) were fitted to the three-parameter equation: Hscp= exp( −670.94997 +33188.34075/T +95.95541 ln(T)) mol m−3 Pa−1, with T in K.
286) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 21 % difference.
287) The data from Dohányosová et al. (2004) were fitted to the three-parameter equation: Hscp= exp( −792.29258 +38089.35992/T +114.36667 ln(T)) mol m−3 Pa−1, with T in K.
288) Data taken from the supplement.
289) Calculated using the EPI Suite (v4.0) method.
290) Calculated using the SPARC (v4.2) method.
291) Calculated using the COSMOtherm (v2.1) method.
292) Calculated using the ABSOLV (ADMEBoxes v4.1) method.
293) Mackay et al. (2006a) list a vapor pressure p, a solubility c, and a Henry's law constant calculated as p/c. However, the data are internally inconsistent and deviate by more than 10 %.
294) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 23 % difference.
295) Value at T = 294 K.
296) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 13 % difference.
297) The data listed in Tables 2 and 3 of Dewulf et al. (1999) are inconsistent, with 5 % difference.
298) Value at T = 301 K.
299) Value given here as quoted by Staudinger and Roberts (1996).
300) Value from the test set for true external validation.
301) The data from Dohányosová et al. (2004) were fitted to the three-parameter equation: Hscp= exp( −365.40645 +19821.40051/T +50.78223 ln(T)) mol m−3 Pa−1, with T in K.
302) The data from Dohányosová et al. (2004) were fitted to the three-parameter equation: Hscp= exp( −383.72514 +20514.87228/T +53.42859 ln(T)) mol m−3 Pa−1, with T in K.
303) The data from Dohányosová et al. (2004) were fitted to the three-parameter equation: Hscp= exp( −369.42853 +19642.40603/T +51.34116 ln(T)) mol m−3 Pa−1, with T in K.
304) Haynes (2014) refers to Mackay and Shiu (1981), but that article lists this value for 1,4-dimethylcyclohexane, not for 1,2-dimethylcyclohexane.
305) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 6 % difference.
306) The data from Dohányosová et al. (2004) were fitted to the three-parameter equation: Hscp= exp( −346.32561 +18710.63122/T +47.87398 ln(T)) mol m−3 Pa−1, with T in K.
307) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −187.57836 +9639.75245/T +25.50544 ln(T)) mol m−3 Pa−1, with T in K.
308) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −166.44394 +8613.39266/T +22.39721 ln(T)) mol m−3 Pa−1, with T in K.
309) The data from Morrison and Billett (1952) were fitted to the three-parameter equation: Hscp= exp( −175.14997 +9028.26949/T +23.67675 ln(T)) mol m−3 Pa−1, with T in K.
310) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −221.00286 +11107.47493/T +30.50401 ln(T)) mol m−3 Pa−1, with T in K.
311) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −168.51157 +9378.22622/T +22.33127 ln(T)) mol m−3 Pa−1, with T in K.
312) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −241.54655 +12718.75981/T +33.18333 ln(T)) mol m−3 Pa−1, with T in K.
313) The data from Serra and Palavra (2003) were fitted to the three-parameter equation: Hscp= exp( −261.78355 +13728.91505/T +36.10688 ln(T)) mol m−3 Pa−1, with T in K.
314) According to Donahue and Prinn (1993), the value is incorrect.
315) Wang et al. (2017) provide separate data for cis and trans. However, since both isomers are identified by the same SMILES string in their study, it is unclear how the stereochemistry has been taken into account.
316) Values for the Henry's law constants shown in Fig. 3 of Martins et al. (2017) were obtained from Simão Pinho (personal communication, 2022).
317) Ebert et al. (2023) present "curated experimental" Henry's law constants from the literature but do not provide any references. It is only mentioned that the value is from multiple sources and obtained from experimental vapor pressure and water solubility.
318) The data from Dohányosová et al. (2004) were fitted to the three-parameter equation: Hscp= exp( −169.70973 +10843.51763/T +21.91320 ln(T)) mol m−3 Pa−1, with T in K.
319) Ebert et al. (2023) present "curated experimental" Henry's law constants from the literature but do not provide any references. It is only mentioned that the value is from a single database or data collection and obtained from experimental vapor pressure and water solubility.
320) Approximate value extracted from Fig. 1 of Maillard and Rosenthal (1952).
321) The same article was also published in Monatshefte für Chemie 23, 489-501 (1902).
322) Value given here as quoted by Fogg et al. (2002).
323) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −143.25283 +7542.89338/T +19.33269 ln(T)) mol m−3 Pa−1, with T in K.
324) Incorrect data are given by Burkholder et al. (2019) for 1-butyne. The number in their table should probably be 0.0569, not 0.569.
325) Regression and individual data points of Simpson and Lovell (1962) are inconsistent, with 5 % difference.
326) Using the theoretical initial concentration (H0); see Zhang et al. (2013) for details.
327) Average of all duplicates (H1); see Zhang et al. (2013) for details.
328) Sieg et al. (2009) also provide data for supercooled water. Here, only data above 0 °C were used to calculate the temperature dependence.
329) Extrapolated from data above 298 K.
330) It was found that Hs changes with the concentration of the solution.
331) The data from Görgényi et al. (2002) were fitted to the three-parameter equation: Hscp= exp( −346.88030 +18421.52810/T +48.91393 ln(T)) mol m−3 Pa−1, with T in K.
332) Value obtained by applying a modified batch air-stripping method, otherwise called the vapor entry loop (VEL) method; see Kochetkov et al. (2001) for details.
333) Value obtained by applying the static head space (HS) method; see Kochetkov et al. (2001) for details.
334) The data from Khalfaoui and Newsham (1994b) were fitted to the three-parameter equation: Hscp= exp( −129.36095 +8999.48627/T +16.29087 ln(T)) mol m−3 Pa−1, with T in K.
335) The data from Robbins et al. (1993) were fitted to the three-parameter equation: Hscp= exp( 189.41389 −5855.10843/T −30.90289 ln(T)) mol m−3 Pa−1, with T in K.
336) Value at T = 302 K.
337) The data from Cooling et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −231.38331 +13640.47358/T +31.46504 ln(T)) mol m−3 Pa−1, with T in K.
338) Calculated using Gh and Hh from Table 2 in Andon et al. (1954). Note that the thermodynamic functions in that table are not based on their α in Table 1. Instead, the expression exp(−Gh/(RT)) yields the Henry's law constant Hsxp in the unit 1/atm.
339) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 11 % difference.
340) Values for salt solutions are also available from this reference.
341) The data from Görgényi et al. (2002) were fitted to the three-parameter equation: Hscp= exp( −468.28203 +24099.39947/T +66.85565 ln(T)) mol m−3 Pa−1, with T in K.
342) Value obtained by applying the EPICS method; see Ayuttaya et al. (2001) for details.
343) Value obtained by applying the static cell (linear form) method; see Ayuttaya et al. (2001) for details.
344) Value obtained by applying the direct phase concentration ratio method; see Ayuttaya et al. (2001) for details.
345) Value obtained by applying the static cell (nonlinear form) method; see Ayuttaya et al. (2001) for details.
346) The data from Robbins et al. (1993) were fitted to the three-parameter equation: Hscp= exp( −573.76928 +28956.65188/T +82.51911 ln(T)) mol m−3 Pa−1, with T in K.
347) The temperature dependence is recalculated using the data in Table 4 of Lamarche and Droste (1989) and not taken from their Table 5.
348) Apparently, the vapor pressure of toluene was used to calculate its Henry's law constant. However, no source is provided.
349) Value given here as quoted by Dewulf et al. (1995).
350) The data from Robbins et al. (1993) were fitted to the three-parameter equation: Hscp= exp( −1350.74178 +64760.28328/T +197.85937 ln(T)) mol m−3 Pa−1, with T in K.
351) The data from Schwardt et al. (2021) were fitted to the three-parameter equation: Hscp= exp( 100.47045 −2603.76722/T −17.31043 ln(T)) mol m−3 Pa−1, with T in K.
352) Value given here as quoted by HSDB (2015).
353) The regression parameters for ethylbenzene in Table 1 of Schwardt et al. (2021) are wrong. Corrected values from Schwardt et al. (2022) are used here.
354) The data from Schwardt et al. (2021) were fitted to the three-parameter equation: Hscp= exp( −176.88587 +11290.74921/T +23.22869 ln(T)) mol m−3 Pa−1, with T in K.
355) Different types of Henry's law constants of Ryu and Park (1999) are inconsistent, with 14 % difference.
356) The data from Robbins et al. (1993) were fitted to the three-parameter equation: Hscp= exp( −371.46947 +20514.07888/T +51.95086 ln(T)) mol m−3 Pa−1, with T in K.
357) The value listed as A for diethylbenzene is probably not A but the Henry's law volatility constant Hvpx at 298 K.
358) Yaffe et al. (2003) list this species twice in their table, with different values. As it is unclear which is correct, the data are not reproduced here.
359) Erratum for page 365 of Fogg and Sangster (2003): data from Kondoh and Nakajima (1997) are cited incorrectly, giving the same values at 308.2 K and 318.2 K, respectively.
360) Value from the external prediction set.
361) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 8 % difference.
362) Because of discrepancies between the values shown in Tables 4 and 5 of Shiu and Ma (2000), the data are not used here.
363) Effective Henry's law constants at several pH values are provided by van Ruth and Villeneuve (2002). Here, only the value at pH = 3 is shown.
364) The values of Dewulf et al. (1999) are not used here because, according to them, the calculated regression does not match the theoretical expectation for this species.
365) Calculated using the COSMO-RS method.
366) Value given here as quoted by Haynes (2014).
367) Ebert et al. (2023) present "curated experimental" Henry's law constants from the literature but do not provide any references. It is only mentioned that the value is from a single database or data collection and measured directly.
368) Literature-derived value.
369) Final adjusted value.
370) Value given here as quoted by Petrasek et al. (1983).
371) Calculated using COSMOtherm.
372) Calculated using the COSMO-RS method.
373) Ebert et al. (2023) present "curated experimental" Henry's law constants from the literature but do not provide any references. It is only mentioned that the value is from a single original paper and obtained from experimental vapor pressure and water solubility.
374) Value at T = 299 K.
375) Value at T = 283 K.
376) Cargill (1990) recommends the data from Rettich et al. (1982).
377) The data from Rettich et al. (1982) were fitted to the three-parameter equation: Hscp= exp( −188.21737 +8974.05844/T +25.72558 ln(T)) mol m−3 Pa−1, with T in K.
378) The data from Douglas (1967) were fitted to the three-parameter equation: Hscp= exp( −180.92848 +8514.05914/T +24.68060 ln(T)) mol m−3 Pa−1, with T in K.
379) Solubility in sea water at 20.99 % chlorinity.
380) The data from Winkler (1901) were fitted to the three-parameter equation: Hscp= exp( −163.07031 +7890.85881/T +21.94517 ln(T)) mol m−3 Pa−1, with T in K.
381) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −161.93492 +7852.78262/T +21.76812 ln(T)) mol m−3 Pa−1, with T in K.
382) The data from Zheng et al. (1997) were fitted to the three-parameter equation: Hscp= exp( −144.44443 +8071.06186/T +19.20040 ln(T)) mol m−3 Pa−1, with T in K.
383) The data from Murray and Riley (1971) were fitted to the three-parameter equation: Hscp= exp( −167.86941 +9146.24434/T +22.67331 ln(T)) mol m−3 Pa−1, with T in K.
384) The data from Morrison and Billett (1952) were fitted to the three-parameter equation: Hscp= exp( −126.83009 +7302.88179/T +16.55553 ln(T)) mol m−3 Pa−1, with T in K.
385) The data from Bohr (1899) were fitted to the three-parameter equation: Hscp= exp( −140.70007 +7951.73013/T +18.60961 ln(T)) mol m−3 Pa−1, with T in K.
386) As mentioned by Fogg and Sangster (2003), the fitting equation by Scharlin (1996) is erroneous. It appears that a correction factor of about 106 is necessary for consistency with their own data in Table 1.
387) The data from Dean and Lange (1999) were fitted to the three-parameter equation: Hscp= exp( −138.54120 +7859.16351/T +18.28486 ln(T)) mol m−3 Pa−1, with T in K.
388) Keßel et al. (2017) provide data at several pH values. Here, only the value at pH = 2 is shown because hydrolysis occurs in more alkaline solutions.
389) The H298 and A, B, C data listed in Table 5.4 of Sander et al. (2011) are inconsistent, with 92 % difference.
390) This paper supersedes earlier work with more concentrated solutions (Butler et al., 1933).
391) Value given here as quoted by Gaffney et al. (1987).
392) Value given here as quoted by Hine and Weimar (1965).
393) The H298 and A, B, C data listed in Table 5-4 of Burkholder et al. (2019) are inconsistent, with 10 % difference.
394) The H298 and A, B, C data listed in Table 5-4 of Burkholder et al. (2015) are inconsistent, with 10 % difference.
395) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 8 % difference.
396) The H298 and A, B, C data listed in Table 5.4 of Sander et al. (2011) are inconsistent, with 10 % difference.
397) Extrapolated from data above 298 K.
398) Koga (1995) found that tert-butanol does not obey Henry's law at c > 3.8 mM.
399) Incorrect data are given by Burkholder et al. (2019) for 2-methyl-2-propanol. The correct parameter for the temperature dependence is C = 37.98 (Robert E. Huie, personal communication, 2021).
400) Incorrect data are given by Burkholder et al. (2015) for 2-methyl-2-propanol. The correct parameter for the temperature dependence is C = 37.98 (Robert E. Huie, personal communication, 2021).
401) Calculated for an aqueous solution containing 60 % ethanol by volume as the solvent.
402) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 6 % difference.
403) Value obtained by Saxena and Hildemann (1996) using the group contribution method.
404) Value at T = 300 K.
405) The error given by Suzuki et al. (1992) is not the difference between the observed and the calculated value, as it should be. It is unclear which of the numbers is wrong.
406) The species is probably 2,3-dimethyl-2-butanol and not 2,3-dimethylbutanol as listed in Hine and Mookerjee (1975).
407) Rumble (2021) refers to Moore et al. (1995) as the source, but this value cannot be found there.
408) It is assumed here that entry number 72 in Table 1 of Yaws et al. (1997) refers to 2-methyl-1-heptanol, not 2-methyl-2-heptanol.
409) KWAC and KAWp from Table 2 of Lei et al. (2007) are inconsistent, with 10 % difference.
410) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 8 % difference.
411) Different types of Henry's law constants of Yaws and Yang (1992) are inconsistent, with 16 % difference.
412) Different types of Henry's law constants of Yaws and Yang (1992) are inconsistent, with 10 % difference.
413) Value at T = 307 K.
414) Value given here as quoted by Mackay et al. (1995).
415) Calculated using SPARC Performs Automated Reasoning in Chemistry (SPARC). It is assumed here that the value refers to T = 298.15 K.
416) Value given here as quoted by Hine and Mookerjee (1975).
417) Value at T = 373 K.
418) Value at T = 281 K.
419) It is assumed here that the thermodynamic data refer to the units [mol dm−3] and [atm] as standard states.
420) Value given here as quoted by Shiu et al. (1994).
421) HSDB (2015) refers to Abraham et al. (1994b) as the source, but this value cannot be found there. Maybe the value is taken from Abraham et al. (1990).
422) Mackay et al. (2006c) list a vapor pressure p, a solubility c, and a Henry's law constant calculated as p/c. However, the data are internally inconsistent and deviate by more than 10 %.
423) Betterton (1992) gives Buttery et al. (1969) as the source. However, no data were found in that reference.
424) Intermediate of estimates employing the bond method from the EPI HENRYWIN software.
425) Although Mansfield (2020) writes that his "Table 6 summarizes numerical calculations for formaldehyde and acetaldehyde assuming the values given in Tables 4 and 5", different values for the Henry's law constants are shown in these tables.
426) Saxena and Hildemann (1996) say that this value is unreliable.
427) Calculated using the free energy perturbation (FEP) method.
428) Calculated using the thermodynamic integration (TI) method.
429) Calculated using the Bennett acceptance ratio (BAR) method.
430) Saxena and Hildemann (1996) give a range of 9.9×102 mol m−3 Pa−1 < Hscp < 5.9×104 mol m−3 Pa−1.
431) Saxena and Hildemann (1996) give a range of 5.9×106 mol m−3 Pa−1 < Hscp < 3.9×109 mol m−3 Pa−1.
432) The formula of 1,2-butanediol is incorrectly given as "HOCH(OH)C2H5" by Burkholder et al. (2019).
433) The formula of 1,2-butanediol is incorrectly given as "HOCH(OH)C2H5" by Burkholder et al. (2015).
434) Saxena and Hildemann (1996) give a range of 9.9×102 mol m−3 Pa−1 < Hscp < 4.9×104 mol m−3 Pa−1.
435) Saxena and Hildemann (1996) give a range of 3.9×102 mol m−3 Pa−1 < Hscp < 3.9×104 mol m−3 Pa−1.
436) Calculated based on atmospheric measurements.
437) Calculated using EPI.
438) Calculated using SPARC.
439) Henry's law constants calculated using the GROMHE model. Temperature dependences calculated with the method of Kühne et al. (2005).
440) Isaacman-VanWertz et al. (2016) refer to Raventos-Duran et al. (2010) as the source, but the quoted value cannot be found there.
441) Calculated using GROMHE.
442) Isaacman-VanWertz et al. (2016) refer to a paper by Hilal et al. as the source, but the quoted value cannot be found there.
443) Calculated using SPARC.
444) Calculated using the bond contribution of HENRYWIN.
445) Compernolle and Müller (2014b) recommend Hscp for 1,7-heptanediol in the range of 4.5×104 mol m−3 Pa−1 < Hscp < 8.3×104 mol m−3 Pa−1.
446) Compernolle and Müller (2014b) recommend Hscp for 1,9-nonanediol in the range of 2.4×104 mol m−3 Pa−1 < Hscp < 3.9×104 mol m−3 Pa−1.
447) Compernolle and Müller (2014b) recommend Hscp for 1,10-decanediol in the range of 2.5×104 mol m−3 Pa−1 < Hscp < 3.0×104 mol m−3 Pa−1.
448) Value given here as quoted by Hilal et al. (2008).
449) Calculated using the EPI Suite method at https://www.epa.gov/tsca-screening-tools/epi-suitetm-estimation-program-interface (last access: 18 September 2023).
450) Value for the temperature range from 261 K to 281 K.
451) Value at T = 278 K.
452) Leriche et al. (2000) assume Hs(ROO) = Hs(ROOH) ×Hs(HO2) / Hs(H2O2).
453) Lelieveld and Crutzen (1991) assume Hs(CH3OO) = Hs(HO2).
454) Jacob (1986) assumes Hs(CH3OO) = Hs(CH3OOH) ×Hs(HO2) / Hs(H2O2).
455) Calculated using EVAPORATION and AIOMFAC.
456) Calculated using the GROMHE model.
457) Effective value that takes into account the hydration of HCHO:
Hs= ([HCHO]+[CH2(OH)2])/p(HCHO).
458) Data from Table 1 by Zhou and Mopper (1990) were used to redo the regression analysis. The data for acetone in their Table 2 are incorrect.
459) Dong and Dasgupta (1986) found that the Henry's law constant for HCHO is not a true constant but that it increases with increasing concentration. Note that their expression does not converge asymptotically to a constant value at infinite dilution.
460) Ledbury and Blair (1925) (and also Blair and Ledbury (1925)) measured the solubility of HCHO at very high concentrations around 5 to 15 M. Their value of Hs increases with HCHO concentration. Lelieveld and Crutzen (1991), Hough (1991), and Pandis and Seinfeld (1989) all use these solubility data but do not specify how they extrapolated to lower concentrations. Since the concentration range is far from typical values in atmospheric chemistry, the value is not reproduced here.
461) Value given here as quoted by Möller and Mauersberger (1992).
462) Effective value that takes into account the hydration of the aldehyde:
Hs= ([RCHO]+[RCH(OH)2])/p(RCHO).
463) The data from Wieland et al. (2015) were fitted to the three-parameter equation: Hscp= exp( 25.01220 +3596.11696/T −6.81730 ln(T)) mol m−3 Pa−1, with T in K.
464) Value given here as quoted by Bone et al. (1983).
465) Value suitable for the conditions of a case study in Mexico City.
466) Volkamer et al. (2009) found average effective Henry's law constants for CHOCHO in the range 1.6×106 mol m−3 Pa−1 < Hscp < 5.9×106 mol m−3 Pa−1 for solutions containing ammonium sulfate and/or fulvic acid. A salting-in effect by fulvic acid was observed even in the absence of sulfate.
467) Solubility in sulfate aerosol.
468) Woo and McNeill (2015) say that the Henry's law constant was updated based on advances in the literature since McNeill et al. (2012) but do not provide further details.
469) Value at T = 372 K.
470) The data from Wieland et al. (2015) were fitted to the three-parameter equation: Hscp= exp( −176.35942 +12895.73116/T +22.70566 ln(T)) mol m−3 Pa−1, with T in K.
471) The formula of propenal is incorrectly given as "CH2CHO" by Burkholder et al. (2019).
472) The temperature dependence parameter C for 2-butenal is missing in Burkholder et al. (2019). The correct value is C = 24.42 (Robert E. Huie, personal communication, 2021).
473) The data from Buttery et al. (1971) for trans-2-octenal are incorrectly cited by Betterton (1992).
474) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 6 % difference.
475) Calculated under the assumption that ∆G and ∆H are based on [mol L−1] and [atm] as the standard states.
476) Calculated using the experimental value adjusted (EVA) method; see McFall et al. (2020) for details.
477) Value at T = 359 K.
478) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 5 % difference.
479) Calculated from the slope of yacP vs xac, using data from Table VIII in Lichtenbelt and Schram (1985).
480) Value at T = 313 K.
481) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 6 % difference.
482) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 7 % difference.
483) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 6 % difference.
484) Table S2 in the supplement of Wu et al. (2022a) contains incorrect data for 3-octanone. Here, the corrected data (Shuang Wu, personal communication, 2022) were used: 2.88×10−2 and 1.52×10−2 at 25 °C and 35 °C, respectively.
485) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 7 % difference.
486) The value listed as A for 2,6,8-trimethyl-4-nonanone is probably not A but the Henry's law volatility constant Hvpx at 298 K.
487) The data from Wieland et al. (2015) were fitted to the three-parameter equation: Hscp= exp( 116.85779 −1341.05519/T −19.91967 ln(T)) mol m−3 Pa−1, with T in K.
488) The data from Wieland et al. (2015) were fitted to the three-parameter equation: Hscp= exp( −74.84087 +9452.88617/T +7.41865 ln(T)) mol m−3 Pa−1, with T in K.
489) The value given here was measured at a liquid-phase mixing ratio of 1 μmol mol−1. Servant et al. (1991) found that the Henry's law constant changes at higher concentrations.
490) Abraham (1984) smoothed the values from a plot of enthalpy against carbon number.
491) The value of Hs was taken from Keene and Galloway (1986).
492) Calculated using thermodynamic data from Latimer (1952).
493) Value at pH = 4.
494) Calculated using HENRYWIN 3.2 (bond contribution method).
495) At pH = 7.
496) At pH = 10.8.
497) Value at T = 289 K.
498) Value at T = 338 K.
499) Pecsar and Martin (1966) are quoted as the source. However, only activity coefficients and no vapor pressures are listed there.
500) The H298 and A, B, C data listed in Table 5-4 of Burkholder et al. (2019) are inconsistent, with 6 % difference.
501) The formula of methyl ethanoate is incorrectly given as "CH3C(O)CH3" by Burkholder et al. (2015).
502) The H298 and A, B data listed in Table 5-4 of Burkholder et al. (2015) are inconsistent, with 74 % difference.
503) The same data were also published in Kieckbusch and King (1979a).
504) The H298 and A, B, C data listed in Table 5-4 of Burkholder et al. (2019) are inconsistent, with 7 % difference.
505) The formula of propyl ethanoate is incorrectly given as "CH3C(O)C3H8" by Burkholder et al. (2019).
506) Katritzky et al. (1998) list this species twice in their table, with different values. As it is unclear which of them is correct, the data are not reproduced here.
507) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 5 % difference.
508) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 6 % difference.
509) The value listed as A for n-heptyl acetate is probably not A but the Henry's law volatility constant Hvpx at 298 K.
510) The value listed as A for n-octyl acetate is probably not A but the Henry's law volatility constant Hvpx at 298 K.
511) Betterton (1992) gives Kieckbusch and King (1979b) as the source. However, no data were found in that reference.
512) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 6 % difference.
513) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 5 % difference.
514) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 6 % difference.
515) The data from Wieland et al. (2015) were fitted to the three-parameter equation: Hscp= exp( 34.46832 +3269.29552/T −8.76905 ln(T)) mol m−3 Pa−1, with T in K.
516) Burkholder et al. (2019) refer to Dohnal et al. (2010) but the quoted value cannot be found there.
517) Burkholder et al. (2015) refer to Dohnal et al. (2010) but the quoted value cannot be found there.
518) Dipropyl phthalate is listed twice with different values.
519) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 9 % difference.
520) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 17 % difference.
521) Hwang et al. (2010) present regression parameters in their Table 6 and values extrapolated to 298.15 K in their Table 5. However, I was not able to reproduce their calculation. The data shown here are from my own regression of the measured data between 318.15 K and 333.15 K.
522) The data from Haimi et al. (2006) were fitted to the three-parameter equation: Hscp= exp( 752.39274 −29351.83448/T −115.55407 ln(T)) mol m−3 Pa−1, with T in K.
523) Different types of Henry's law constants of Arp and Schmidt (2004) are inconsistent, with 5 % difference.
524) The data from Robbins et al. (1993) were fitted to the three-parameter equation: Hscp= exp( −4264.16032 +202439.46180/T +628.54371 ln(T)) mol m−3 Pa−1, with T in K.
525) The data from Haimi et al. (2006) were fitted to the three-parameter equation: Hscp= exp( 224.10069 −4205.03828/T −37.65761 ln(T)) mol m−3 Pa−1, with T in K.
526) The data from Haimi et al. (2006) were fitted to the three-parameter equation: Hscp= exp( −780.30940 +40758.59752/T +112.07468 ln(T)) mol m−3 Pa−1, with T in K.
527) The data from Haimi et al. (2006) were fitted to the three-parameter equation: Hscp= exp( −565.00561 +31411.46240/T +79.73748 ln(T)) mol m−3 Pa−1, with T in K.
528) Ebert et al. (2023) present "curated experimental" Henry's law constants from the literature but do not provide any references. It is only mentioned that the value is from a single original paper and obtained from experimental vapor pressure and the infinite-dilution activity coefficient.
529) The data from Haimi et al. (2006) were fitted to the three-parameter equation: Hscp= exp( −1125.52184 +56732.54277/T +163.04749 ln(T)) mol m−3 Pa−1, with T in K.
530) The data from Haimi et al. (2006) were fitted to the three-parameter equation: Hscp= exp( −1315.53726 +64110.36765/T +191.89554 ln(T)) mol m−3 Pa−1, with T in K.
531) The value listed as A for di-n-pentyl ether is probably not A but the Henry's law volatility constant Hvpx at 298 K.
532) The value listed as A for di-n-hexyl ether is probably not A but the Henry's law volatility constant Hvpx at 298 K.
533) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 5 % difference.
534) The data from Wieland et al. (2015) were fitted to the three-parameter equation: Hscp= exp( −157.10556 +10203.60762/T +20.42555 ln(T)) mol m−3 Pa−1, with T in K.
535) Betterton (1992) gives Hine and Weimar (1965) as the source. However, no data were found in that reference.
536) Betterton (1992) gives Vitenberg et al. (1975) as the source. However, no data were found in that reference.
537) Based on gas chromatograph retention indices (GC-RIs).
538) Warneck (2005) refers to Saxena and Hildemann (1996) as the source, but the quoted value cannot be found there.
539) The formula of hydroxyethanoic acid is incorrectly given as "HC(OH)C(O)OH" by Burkholder et al. (2019).
540) The formula of hydroxyethanoic acid is incorrectly given as "HC(OH)C(O)OH" by Burkholder et al. (2015).
541) Temperature dependencies in Tables 1 and 2 of Ashworth et al. (1988) are inconsistent, with 31 % difference.
542) Compernolle and Müller (2014a) recommend Hscp for tartaric acid in the range of 6.9×1014 mol m−3 Pa−1 < Hscp < 9.2×1015 mol m−3 Pa−1.
543) Chan et al. (2010) give a range of 1.9×105 mol m−3 Pa−1 < Hscp < 9.5×106 mol m−3 Pa−1.
544) Calculated using the HENRYWIN program and calibration to 1,3-propanediol.
545) The value was chosen for a model study because it gave the best agreement with measurements.
546) Center of the range (2.3... 4.0) mol m−3 Pa−1.
547) Calculated based on the method by Hine and Mookerjee (1975).
548) Compernolle and Müller (2014a) recommend Hscp for citric acid in the range of 2.0×1014 mol m−3 Pa−1 < Hscp < 5.9×1015 mol m−3 Pa−1.
549) The data from Wieland et al. (2015) were fitted to the three-parameter equation: Hscp= exp( −96.39127 +11107.87195/T +10.76466 ln(T)) mol m−3 Pa−1, with T in K.
550) In their Fig. 5b, Kish et al. (2013) apply an unspecified factor to the Henry's law constant, and it is not clear if the temperature dependence shown there is correct (Yong Liu, personal communication, 2014).
551) Calculated using the method from Nguyen (2013).
552) Calculated from the slope of y1P vs x1, using the tabulated VLE data from Kim et al. (2008) between 40 °C and 100 °C. Only dilute solutions with x1 ≤ 0.1 were considered.
553) Value at T = 309 K.
554) The data from Christie and Crisp (1967) for dipropylamine are incorrectly cited by Betterton (1992).
555) Value at T = 323 K.
556) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 6 % difference.
557) Value at T = 308 K.
558) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 5 % difference.
559) Value at T = 285 K.
560) Mackay et al. (2006d) list a vapor pressure p, a solubility c, and a Henry's law constant calculated as p/c. However, the data are internally inconsistent and deviate by more than 10 %.
561) Calculated using ∆Gsg→ H2O and ∆Hsg→ H2O from Table IV of Arnett and Chawla (1979). Since some of the values in this table are taken directly from Andon et al. (1954), it is assumed that the thermodynamic properties are defined in the same way. Since ∆Hsg→ H2O is defined relative to pyridine, a value of −11.93 kcal mol−1 from Arnett et al. (1977) was added.
562) Due to an apparently incorrect definition of the Henry's law constant by Andon et al. (1954), Staudinger and Roberts (2001) quote incorrect values from that paper.
563) The data from Wieland et al. (2015) were fitted to the three-parameter equation: Hscp= exp( −12.48322 +7833.96799/T −2.23379 ln(T)) mol m−3 Pa−1, with T in K.
564) Value given here as quoted by Feigenbrugel and Le Calvé (2021).
565) Value calculated from the solubility of 9.4×10−3 mol L−1 and the vapor pressure of 0.255 mmHg, as shown on pages 7142-7143 of Arnett and Chawla (1979). It is inconsistent with the entry in Table IV of that paper.
566) Value given here as quoted by Ma et al. (2010a).
567) Nguyen (2013) refer to Kim et al. (2008) as the source, but this value cannot be found there.
568) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 7 % difference.
569) Value given here as quoted by Goodarzi et al. (2010).
570) Goodarzi et al. (2010) compared several QSPR methods and found that the Levenberg-Marquardt algorithm with Bayesian regularization produces the best results. Values obtained with other methods can be found in their supplement.
571) Value from the validation set.
572) At pH = 5.
573) Value from the test set.
574) At pH = 10.
575) At pH = 9.
576) At pH = 5.2.
577) At pH = 7.4.
578) At pH = 9.3.
579) At pH = 4.
580) Kames and Schurath (1992) were unable to assign the values to the isomers.
581) Ebert et al. (2023) present "curated experimental" Henry's law constants from the literature but do not provide any references. It is only mentioned that the value is from a single original paper and measured directly.
582) The same data were also published in Fischer and Ballschmiter (1998a).
583) The formula of 1,3-propanediol dinitrate is incorrectly given as "O2NO2CH2CH2CH2ONO2" by Burkholder et al. (2019).
584) The formula of 1,3-propanediol dinitrate is incorrectly given as "O2NO2CH2CH2CH2ONO2" by Burkholder et al. (2015).
585) Comparing the value with that from the cited publication (Kames and Schurath, 1995), it can be seen that the unit and the temperature listed in Table 3 of Warneck et al. (1996) are incorrect.
586) The data from Kames and Schurath (1995) for peroxyacetyl nitrate are incorrectly cited by Schurath et al. (1996).
587) The data from Kames and Schurath (1995) for peroxypropionyl nitrate are incorrectly cited by Schurath et al. (1996).
588) The data from Kames and Schurath (1995) for peroxy-n-butyl nitrate are incorrectly cited by Schurath et al. (1996).
589) The data from Kames and Schurath (1995) for peroxymethacryloyl nitrate are incorrectly cited by Schurath et al. (1996).
590) The data from Kames and Schurath (1995) for peroxy-i-butyl nitrate are incorrectly cited by Schurath et al. (1996).
591) Estimate based on Raventos-Duran et al. (2010).
592) The value at T is the intrinsic Henry's law constant, but the temperature dependence refers to the effective Henry's law constant at pH = 3.0.
593) The value at T is the intrinsic Henry's law constant, but the temperature dependence refers to the effective Henry's law constant at pH = 3.08.
594) Burkholder et al. (2019) refer to Borduas et al. (2016), but the quoted temperature dependence cannot be found there.
595) The values for nitroethane in Tables VI and VIII of Friant and Suffet (1979) differ by a factor of 10. Apparently, the value in Table VIII is wrong.
596) The data listed in Tables 2 and 3 of Dewulf et al. (1999) are inconsistent, with 27 % difference.
597) Mackay et al. (2006d) list two values for dinoseb which differ by a factor of 1000. It is unclear which number is correct (if any), and the data are not reproduced here.
598) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 6 % difference.
599) The data from Glew and Moelwyn-Hughes (1953) were fitted to the three-parameter equation: Hscp= exp( −135.82151 +7593.40134/T +18.05983 ln(T)) mol m−3 Pa−1, with T in K.
600) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −163.70243 +8973.31702/T +22.17142 ln(T)) mol m−3 Pa−1, with T in K.
601) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −142.70480 +8025.53525/T +19.04459 ln(T)) mol m−3 Pa−1, with T in K.
602) The data from Zheng et al. (1997) were fitted to the three-parameter equation: Hscp= exp( −190.61883 +10088.26604/T +25.94088 ln(T)) mol m−3 Pa−1, with T in K.
603) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −177.44258 +9554.69077/T +23.94054 ln(T)) mol m−3 Pa−1, with T in K.
604) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −350.64777 +16708.21486/T +49.40261 ln(T)) mol m−3 Pa−1, with T in K.
605) The data from Scharlin and Battino (1995) were fitted to the three-parameter equation: Hscp= exp( −552.21779 +25529.81258/T +79.59510 ln(T)) mol m−3 Pa−1, with T in K.
606) The data from Scharlin and Battino (1994) were fitted to the three-parameter equation: Hscp= exp( −552.21779 +25529.81258/T +79.59510 ln(T)) mol m−3 Pa−1, with T in K.
607) The data from Wen and Muccitelli (1979) were fitted to the three-parameter equation: Hscp= exp( −356.93310 +16943.80173/T +50.37092 ln(T)) mol m−3 Pa−1, with T in K.
608) The data from Ashton et al. (1968) were fitted to the three-parameter equation: Hscp= exp( −320.94892 +15261.58540/T +45.04995 ln(T)) mol m−3 Pa−1, with T in K.
609) The data from Morrison and Johnstone (1954) were fitted to the three-parameter equation: Hscp= exp( −174.44927 +8434.85415/T +23.34667 ln(T)) mol m−3 Pa−1, with T in K.
610) The H298 and A, B data listed in Table 5-7 of Burkholder et al. (2019) are inconsistent, with 8 % difference.
611) The H298 and A, B data listed in Table 5-7 of Burkholder et al. (2015) are inconsistent, with 8 % difference.
612) The data from Zheng et al. (1997) were fitted to the three-parameter equation: Hscp= exp( −203.78636 +11097.46295/T +27.89781 ln(T)) mol m−3 Pa−1, with T in K.
613) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −184.82864 +10260.68840/T +25.06659 ln(T)) mol m−3 Pa−1, with T in K.
614) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −175.64793 +9805.36391/T +23.71997 ln(T)) mol m−3 Pa−1, with T in K.
615) The data from Zheng et al. (1997) were fitted to the three-parameter equation: Hscp= exp( −244.13803 +12963.44791/T +33.68869 ln(T)) mol m−3 Pa−1, with T in K.
616) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −225.56576 +12186.49271/T +30.88527 ln(T)) mol m−3 Pa−1, with T in K.
617) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −208.89051 +11387.65726/T +28.42219 ln(T)) mol m−3 Pa−1, with T in K.
618) The data from Chang and Criddle (1995) were fitted to the three-parameter equation: Hscp= exp( −1003.84803 +45506.40253/T +147.89569 ln(T)) mol m−3 Pa−1, with T in K.
619) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −164.25882 +9381.26592/T +21.50848 ln(T)) mol m−3 Pa−1, with T in K.
620) The data from Wen and Muccitelli (1979) were fitted to the three-parameter equation: Hscp= exp( −499.57565 +23563.38593/T +71.28478 ln(T)) mol m−3 Pa−1, with T in K.
621) Value at T = 287 K.
622) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −78.74672 +5836.90728/T +8.41930 ln(T)) mol m−3 Pa−1, with T in K.
623) The data from Clever et al. (2005) were fitted to the three-parameter equation: Hscp= exp( −588.11467 +28143.61522/T +84.26598 ln(T)) mol m−3 Pa−1, with T in K.
624) In their Table 13, Clever et al. (2005) list Ostwald coefficients that are probably incorrect by a factor of 100. Therefore, these values are not used. Instead, Hs is calculated using the amount fraction x1 from the same table.
625) The data from Scharlin and Battino (1994) were fitted to the three-parameter equation: Hscp= exp( −630.69809 +30309.09484/T +90.46889 ln(T)) mol m−3 Pa−1, with T in K.
626) The data from Wen and Muccitelli (1979) were fitted to the three-parameter equation: Hscp= exp( −673.45393 +31915.35190/T +97.01332 ln(T)) mol m−3 Pa−1, with T in K.
627) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −197.14327 +10473.25304/T +26.34780 ln(T)) mol m−3 Pa−1, with T in K.
628) Calculated using the COSMO-RS method.
629) Value given here as quoted by Kanakidou et al. (1995).
630) Comparing with Abraham et al. (1994a), it seems that the compound called "trifluoroethanol" by Goss (2005) refers to 2,2,2-trifluoroethanol.
631) Comparing with Abraham et al. (1994a), it seems that the compound called "hexafluoropropanol" by Goss (2005) refers to 1,1,1,3,3,3-hexafluoro-2-propanol.
632) Value at T = 284 K.
633) Measured in aqueous hydrochloric acid and extrapolated to pure water as the solvent at 25 °C. Measurements were also made at other temperatures; however, those were not extrapolated to pure water as the solvent.
634) Calculated using the EPI Suite Bond estimation method.
635) Calculated using the new SPARC method; see Arp et al. (2006) for details.
636) Calculated using the COSMOtherm method; see Arp et al. (2006) for details.
637) A refit yields A = −18.99, B = 5493, and H(298 K) = 0.57 M atm−1 (Robert E. Huie, personal communication, 2021).
638) A refit yields A = −18.99, B = 5493, and H(298 K) = 0.57 M atm−1 (Robert E. Huie, personal communication, 2021).
639) A refit yields A = −21.67, B = 5776, and H(298 K) = 0.10 M atm−1 (Robert E. Huie, personal communication, 2021).
640) The H298 and A, B data listed in Table 5-4 of Burkholder et al. (2019) are inconsistent, with 29 % difference.
641) A refit yields A = −21.67, B = 5776, and H(298 K) = 0.10 M atm−1 (Robert E. Huie, personal communication, 2021).
642) The H298 and A, B data listed in Table 5-4 of Burkholder et al. (2015) are inconsistent, with 29 % difference.
643) The H298 and A, B data listed in Table 5.4 of Sander et al. (2011) are inconsistent, with 29 % difference.
644) The data from Clever et al. (2005) were fitted to the three-parameter equation: Hscp= exp( 289.52696 −11352.27202/T −46.16631 ln(T)) mol m−3 Pa−1, with T in K.
645) The Ostwald coefficient given by Clever et al. (2005) at 313.2 K is probably incorrect. Therefore, the Ostwald coefficients are not used. Instead, Hs is calculated using the amount fraction x1 from the same table.
646) Extrapolated based on number of carbons.
647) Measured with the wetted-wall column at room temperature.
648) The H298 and A, B data listed in Table 5.4 of Sander et al. (2011) are inconsistent, with 9 % difference.
649) The H298 and A, B data listed in Table 5.4 of Sander et al. (2006) are inconsistent, with 9 % difference.
650) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −251.05500 +13259.10200/T +35.01685 ln(T)) mol m−3 Pa−1, with T in K.
651) The same data were also published in McConnell et al. (1975).
652) The data from Glew and Moelwyn-Hughes (1953) were fitted to the three-parameter equation: Hscp= exp( −171.13914 +9743.00524/T +23.09616 ln(T)) mol m−3 Pa−1, with T in K.
653) Values at different temperatures are from different sources. Thus a temperature dependence was not calculated.
654) Chiang et al. (1998) show vinyl chloride in their Table 2 but most probably they meant to refer to dichloromethane instead.
655) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −444.17924 +22456.73010/T +63.76504 ln(T)) mol m−3 Pa−1, with T in K.
656) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 7 % difference.
657) The data from Görgényi et al. (2002) were fitted to the three-parameter equation: Hscp= exp( −378.59438 +20174.67146/T +53.50889 ln(T)) mol m−3 Pa−1, with T in K.
658) The data from Moore et al. (1995) were fitted to the three-parameter equation: Hscp= exp( 32.52949 +1878.33965/T −7.88669 ln(T)) mol m−3 Pa−1, with T in K.
659) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −109.09283 +8000.75665/T +13.39152 ln(T)) mol m−3 Pa−1, with T in K.
660) Probably an interpolation of the data from Balls (1980).
661) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 5 % difference.
662) The data from Bullister and Wisegarver (1998) were fitted to the three-parameter equation: Hscp= exp( −704.15798 +34144.64622/T +102.06046 ln(T)) mol m−3 Pa−1, with T in K.
663) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −426.63883 +22457.44484/T +60.22986 ln(T)) mol m−3 Pa−1, with T in K.
664) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −221.58683 +12291.19608/T +30.42274 ln(T)) mol m−3 Pa−1, with T in K.
665) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −233.85465 +12927.81251/T +32.20905 ln(T)) mol m−3 Pa−1, with T in K.
666) The data from Görgényi et al. (2002) were fitted to the three-parameter equation: Hscp= exp( −372.18420 +19566.35271/T +52.67600 ln(T)) mol m−3 Pa−1, with T in K.
667) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −1295.59488 +61538.96732/T +190.02999 ln(T)) mol m−3 Pa−1, with T in K.
668) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −309.75754 +17275.24359/T +43.35857 ln(T)) mol m−3 Pa−1, with T in K.
669) The data from Robbins et al. (1993) were fitted to the three-parameter equation: Hscp= exp( 313.50875 −12121.71831/T −49.20602 ln(T)) mol m−3 Pa−1, with T in K.
670) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( 255.46482 −8896.18926/T −40.90189 ln(T)) mol m−3 Pa−1, with T in K.
671) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 5 % difference.
672) The data from Schwardt et al. (2021) were fitted to the three-parameter equation: Hscp= exp( 200.57633 −7128.32092/T −31.87111 ln(T)) mol m−3 Pa−1, with T in K.
673) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −304.31063 +17046.46392/T +42.59182 ln(T)) mol m−3 Pa−1, with T in K.
674) The data from Schwardt et al. (2021) were fitted to the three-parameter equation: Hscp= exp( −1784.40256 +88283.19114/T +260.26556 ln(T)) mol m−3 Pa−1, with T in K.
675) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( 608.52671 −23622.70039/T −93.86675 ln(T)) mol m−3 Pa−1, with T in K.
676) The value for A in the table of Kondoh and Nakajima (1997) is incorrect. Recalculating the regression, it can be seen that it should be 13.95 and not 1.395.
677) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( 2638.58362 −114985.14319/T −396.08684 ln(T)) mol m−3 Pa−1, with T in K.
678) The H298 and A, B data listed in Table 5-4 of Burkholder et al. (2019) are inconsistent, with 9 % difference.
679) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −573.71583 +28877.33987/T +82.70652 ln(T)) mol m−3 Pa−1, with T in K.
680) The data from Sarraute et al. (2006) were fitted to the three-parameter equation: Hscp= exp( −503.53929 +28223.72051/T +70.89539 ln(T)) mol m−3 Pa−1, with T in K.
681) As explained by Miller and Stuart (2003), the measurements were performed at 296 K.
682) Value for T = 295... 298 K.
683) Value for T = 293... 298 K.
684) The data from Schwardt et al. (2021) were fitted to the three-parameter equation: Hscp= exp( −20.66741 +2604.13624/T +0.71646 ln(T)) mol m−3 Pa−1, with T in K.
685) Mackay et al. (2006b) list a vapor pressure p, a solubility c, and a Henry's law constant calculated as p/c. However, the data are internally inconsistent and deviate by more than 10 %.
686) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 6 % difference.
687) The data from Schwardt et al. (2021) were fitted to the three-parameter equation: Hscp= exp( −214.72727 +12076.60512/T +29.20360 ln(T)) mol m−3 Pa−1, with T in K.
688) A typo in Ashworth et al. (1988) has been corrected by Howe et al. (1987).
689) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −332.68901 +17925.88529/T +46.77838 ln(T)) mol m−3 Pa−1, with T in K.
690) The data from Schwardt et al. (2021) were fitted to the three-parameter equation: Hscp= exp( −6.68864 +2211.35284/T −1.35565 ln(T)) mol m−3 Pa−1, with T in K.
691) The data from Khalfaoui and Newsham (1994b) were fitted to the three-parameter equation: Hscp= exp( −593.56757 +30300.79738/T +85.11672 ln(T)) mol m−3 Pa−1, with T in K.
692) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −294.54970 +16409.35487/T +40.82700 ln(T)) mol m−3 Pa−1, with T in K.
693) The data from Cooling et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −511.78322 +26710.11950/T +72.88403 ln(T)) mol m−3 Pa−1, with T in K.
694) The data from Schwardt et al. (2021) were fitted to the three-parameter equation: Hscp= exp( −265.05147 +15058.79780/T +36.44507 ln(T)) mol m−3 Pa−1, with T in K.
695) The data from Görgényi et al. (2002) were fitted to the three-parameter equation: Hscp= exp( −480.92432 +24776.46284/T +68.60174 ln(T)) mol m−3 Pa−1, with T in K.
696) The data from Knauss et al. (2000) were fitted to the three-parameter equation: Hscp= exp( −389.28726 +21123.08804/T +54.69871 ln(T)) mol m−3 Pa−1, with T in K.
697) The data from Khalfaoui and Newsham (1994b) were fitted to the three-parameter equation: Hscp= exp( −511.93773 +26713.30359/T +72.90551 ln(T)) mol m−3 Pa−1, with T in K.
698) The data from Robbins et al. (1993) were fitted to the three-parameter equation: Hscp= exp( 176.56015 −5511.47473/T −28.96682 ln(T)) mol m−3 Pa−1, with T in K.
699) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( 681.41357 −27448.54898/T −104.63745 ln(T)) mol m−3 Pa−1, with T in K.
700) The data from Cooling et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −574.03630 +29404.80442/T +82.22224 ln(T)) mol m−3 Pa−1, with T in K.
701) The data from Schwardt et al. (2021) were fitted to the three-parameter equation: Hscp= exp( −330.94781 +18207.73829/T +46.05991 ln(T)) mol m−3 Pa−1, with T in K.
702) The data from Knauss et al. (2000) were fitted to the three-parameter equation: Hscp= exp( −281.09217 +15955.08953/T +38.60107 ln(T)) mol m−3 Pa−1, with T in K.
703) The data from Robbins et al. (1993) were fitted to the three-parameter equation: Hscp= exp( −1145.60543 +55089.35358/T +167.32916 ln(T)) mol m−3 Pa−1, with T in K.
704) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −224.85290 +13463.70772/T +30.65123 ln(T)) mol m−3 Pa−1, with T in K.
705) Henry's law constants were evaluated using data from Florida sandy field soil.
706) According to Thomas et al. (2006), theoretical Henry's law constants were calculated using the "normal boiling point, the critical temperature, and the enthalpy of volatilization at the normal boiling point".
707) Haynes (2014) refers to Mackay and Shiu (1981), but that article lists this value for 1-chloro-2-methylpropane (the saturated compound), not for 1-chloro-2-methylpropene.
708) The regression parameters for chlorobenzene in Table 1 of Schwardt et al. (2021) are wrong. Corrected values from Schwardt et al. (2022) are used here.
709) The data from Schwardt et al. (2021) were fitted to the three-parameter equation: Hscp= exp( −266.69788 +14811.78372/T +37.00246 ln(T)) mol m−3 Pa−1, with T in K.
710) The data from Khalfaoui and Newsham (1994b) were fitted to the three-parameter equation: Hscp= exp( −757.46460 +35956.18738/T +110.75693 ln(T)) mol m−3 Pa−1, with T in K.
711) The data from Cooling et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −820.00716 +38880.20610/T +120.01460 ln(T)) mol m−3 Pa−1, with T in K.
712) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 8 % difference.
713) Erratum for page 344 of Fogg and Sangster (2003): their reference [89] does not contain 1,2-dichlorobenzene.
714) The data listed in Tables 2 and 3 of Dewulf et al. (1999) are inconsistent, with 7 % difference.
715) The data listed in Tables 2 and 3 of Dewulf et al. (1999) are inconsistent, with 7 % difference.
716) Rumble (2021) refers to Oliver (1985) as the source, but this value cannot be found there.
717) Value for T = 298... 303 K.
718) Ebert et al. (2023) present "curated experimental" Henry's law constants from the literature but do not provide any references. It is only mentioned that the value is from multiple sources and obtained from the experimental octanol-water partition coefficient and the octanol-air partition coefficient.
719) Ebert et al. (2023) present "curated experimental" Henry's law constants from the literature but do not provide any references. It is only mentioned that the value is from a single database or data collection and obtained from the experimental octanol-water partition coefficient and the octanol-air partition coefficient.
720) Odabasi and Adali (2016) provide the parameters A and B for an equation to calculate temperature-dependent Henry's law constants. Values calculated with this equation at 298 K are slightly different than those measured at 298 K and given as H in their Table 1. Here, the values H and B are used.
721) Modified gas-stripping method (MGSM); see Lau et al. (2006) for details.
722) Integrated gas-stripping method (IGSM); see Lau et al. (2006) for details.
723) Calculated with the principal component regression (PCR) method; see Lee (2007) for details.
724) Calculated with the partial least-square regression (PLSR) method; see Lee (2007) for details.
725) The same data were also published in Dunnivant et al. (1988).
726) Value given here as quoted by Dunnivant et al. (1988).
727) Calculated using the EPICS method.
728) Calculated using the "Direct" method.
729) Westcott et al. (1981) give a range of 1.9×10−2 mol m−3 Pa−1 < Hscp < 3.2×10−2 mol m−3 Pa−1.
730) Westcott et al. (1981) give a range of 2.8×10−2 mol m−3 Pa−1 < Hscp < 9.0×10−2 mol m−3 Pa−1.
731) Erratum for page 350 of Fogg and Sangster (2003): the equation describing the recommended temperature-dependent data appears to be incorrect and is not used here.
732) Value at pH = 4.
733) When comparing H in Table 4 with Kgw in Table 5 of Pfeifer et al. (2001), it can be seen that the values refer to Kgw×100 and not Kgw/100.
734) Measured at pH = 1.
735) The same data were also published in Brandsch et al. (1993).
736) Erratum for page 376 of Fogg and Sangster (2003): data from Santl et al. (1994) are cited incorrectly; it should be 3.64, not 3.84.
737) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 8 % difference.
738) Although pronamide and propyzamide are the same species, Mackay et al. (2006d) list two different values for them. It is unclear which number is correct (if any), and the data are not reproduced here.
739) The value at 20 °C was calculated from published values of vapor pressure and water solubility. Data between 25 °C and 40 °C were calculated from the measured evaporation rate.
740) At pH = 5.4.
741) Ebert et al. (2023) present "curated experimental" Henry's law constants from the literature but do not provide any references. It is only mentioned that the value is from multiple sources and measured directly.
742) The data from Zheng et al. (1997) were fitted to the three-parameter equation: Hscp= exp( −206.94328 +11372.60160/T +28.22232 ln(T)) mol m−3 Pa−1, with T in K.
743) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −200.57402 +11192.93914/T +27.21798 ln(T)) mol m−3 Pa−1, with T in K.
744) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −208.06388 +11491.48483/T +28.35421 ln(T)) mol m−3 Pa−1, with T in K.
745) The data from Chang and Criddle (1995) were fitted to the three-parameter equation: Hscp= exp( −1756.79407 +80807.02552/T +259.24906 ln(T)) mol m−3 Pa−1, with T in K.
746) The data from McLinden (1989) were fitted to the three-parameter equation: Hscp= exp( −387.81156 +19950.78638/T +54.91348 ln(T)) mol m−3 Pa−1, with T in K.
747) The temperature dependence was recalculated from the data on p. 20 of McLinden (1989).
748) The data from McLinden (1989) for HCFC-22 are incorrectly cited by Kanakidou et al. (1995).
749) The H298 and A, B data listed in Table 5-4 of Burkholder et al. (2019) are inconsistent, with 5 % difference.
750) The H298 and A, B data listed in Table 5-4 of Burkholder et al. (2015) are inconsistent, with 5 % difference.
751) The H298 and A, B data listed in Table 5.4 of Sander et al. (2011) are inconsistent, with 5 % difference.
752) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( 100.23590 −3339.68982/T −17.66849 ln(T)) mol m−3 Pa−1, with T in K.
753) The data from Scharlin and Battino (1995) were fitted to the three-parameter equation: Hscp= exp( −291.40685 +14224.53456/T +40.73325 ln(T)) mol m−3 Pa−1, with T in K.
754) The data from Scharlin and Battino (1994) were fitted to the three-parameter equation: Hscp= exp( −291.40685 +14224.53456/T +40.73325 ln(T)) mol m−3 Pa−1, with T in K.
755) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −147.53824 +8643.05363/T +18.97752 ln(T)) mol m−3 Pa−1, with T in K.
756) The data from Scharlin and Battino (1995) were fitted to the three-parameter equation: Hscp= exp( −211.99699 +11400.41036/T +28.66283 ln(T)) mol m−3 Pa−1, with T in K.
757) The data from Scharlin and Battino (1994) were fitted to the three-parameter equation: Hscp= exp( −211.99699 +11400.41036/T +28.66283 ln(T)) mol m−3 Pa−1, with T in K.
758) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −278.68448 +15169.41095/T +38.36974 ln(T)) mol m−3 Pa−1, with T in K.
759) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −129.78084 +8533.77911/T +16.20428 ln(T)) mol m−3 Pa−1, with T in K.
760) The data from Bu and Warner (1995) were fitted to the three-parameter equation: Hscp= exp( −415.59157 +21411.24346/T +58.50528 ln(T)) mol m−3 Pa−1, with T in K.
761) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( 0.13353 +5070.08549/T −4.84639 ln(T)) mol m−3 Pa−1, with T in K.
762) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −113.07654 +6884.36758/T +13.75470 ln(T)) mol m−3 Pa−1, with T in K.
763) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −149.62353 +7869.46528/T +19.40044 ln(T)) mol m−3 Pa−1, with T in K.
764) The data from Chang and Criddle (1995) were fitted to the three-parameter equation: Hscp= exp( −402.28495 +20229.16189/T +57.28419 ln(T)) mol m−3 Pa−1, with T in K.
765) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −277.88370 +14905.51805/T +38.38688 ln(T)) mol m−3 Pa−1, with T in K.
766) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −195.56650 +11207.08869/T +26.12575 ln(T)) mol m−3 Pa−1, with T in K.
767) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −249.15404 +13774.89590/T +34.23234 ln(T)) mol m−3 Pa−1, with T in K.
768) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −210.55601 +11968.42846/T +28.54087 ln(T)) mol m−3 Pa−1, with T in K.
769) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −155.04312 +9704.04801/T +20.06575 ln(T)) mol m−3 Pa−1, with T in K.
770) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −270.78344 +14413.03953/T +37.48366 ln(T)) mol m−3 Pa−1, with T in K.
771) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −184.96240 +10541.13831/T +24.70437 ln(T)) mol m−3 Pa−1, with T in K.
772) The data from Chang and Criddle (1995) were fitted to the three-parameter equation: Hscp= exp( −190.58060 +10602.65774/T +25.66197 ln(T)) mol m−3 Pa−1, with T in K.
773) The data from Maaßen (1995) were fitted to the three-parameter equation: Hscp= exp( −237.50724 +13032.41274/T +32.48569 ln(T)) mol m−3 Pa−1, with T in K.
774) The data from Reichl (1995) were fitted to the three-parameter equation: Hscp= exp( −200.95912 +11406.81841/T +27.03092 ln(T)) mol m−3 Pa−1, with T in K.
775) The data from Smith et al. (1981b) were fitted to the three-parameter equation: Hscp= exp( 678.00770 −27346.39638/T −103.92351 ln(T)) mol m−3 Pa−1, with T in K.
776) Kanakidou et al. (1995) assume Hs(CClF2OONO2) = Hs(PAN).
777) The H298 and A, B data listed in Table 5-4 of Burkholder et al. (2019) are inconsistent, with 11 % difference.
778) The data from De Bruyn and Saltzman (1997) were fitted to the three-parameter equation: Hscp= exp( −521.17646 +25057.64644/T +75.60914 ln(T)) mol m−3 Pa−1, with T in K.
779) The data from Glew and Moelwyn-Hughes (1953) were fitted to the three-parameter equation: Hscp= exp( −184.73597 +10636.09284/T +25.03175 ln(T)) mol m−3 Pa−1, with T in K.
780) Values at 298 K in Tables C2 and C5 of Brockbank (2013) are inconsistent, with 6 % difference.
781) The data from Moore et al. (1995) were fitted to the three-parameter equation: Hscp= exp( −395.20167 +20638.03484/T +56.40082 ln(T)) mol m−3 Pa−1, with T in K.
782) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( −82.06673 +6867.92071/T +9.56720 ln(T)) mol m−3 Pa−1, with T in K.
783) The data from Moore et al. (1995) were fitted to the three-parameter equation: Hscp= exp( −408.59491 +21699.59623/T +58.19801 ln(T)) mol m−3 Pa−1, with T in K.
784) The data from Wright et al. (1992) were fitted to the three-parameter equation: Hscp= exp( 1124.79951 −46767.40872/T −170.54217 ln(T)) mol m−3 Pa−1, with T in K.
785) Erratum for page 274 of Fogg and Sangster (2003): the value in the table is kH, not lnkH.
786) Value at T = 50 K.
787) Rumble (2021) refers to Hiatt (2013) as the source, but this value cannot be found there.
788) Haynes (2014) refers to Mackay et al. (1993) as the source, but this value cannot be found there.
789) The data from Sarraute et al. (2006) were fitted to the three-parameter equation: Hscp= exp( −370.06283 +22192.71634/T +51.12683 ln(T)) mol m−3 Pa−1, with T in K.
790) Erratum for page 321 of Fogg and Sangster (2003): data from Yates and Gan (1998) are cited with a typo. The value at 313.2 K should probably be 4.78×10−6, not 4.78×10−2.
791) Ebert et al. (2023) present "curated experimental" Henry's law constants from the literature but do not provide any references. It is only mentioned that the value is from a single original paper and obtained from the experimental octanol-water partition coefficient and the octanol-air partition coefficient.
792) Diaz et al. (2005) also cite a Henry's law constant from Pfeifer et al. (2001) even though this species is not mentioned there. There might be a mix up of the different haloanisoles.
793) Erratum for page 285 of Fogg and Sangster (2003): data in their table look strange (9.70R) and are not used here.
794) The data from Moore et al. (1995) were fitted to the three-parameter equation: Hscp= exp( −76.31131 +7250.73360/T +8.15388 ln(T)) mol m−3 Pa−1, with T in K.
795) The data from Moore et al. (1995) were fitted to the three-parameter equation: Hscp= exp( −265.18008 +15516.80509/T +36.54803 ln(T)) mol m−3 Pa−1, with T in K.
796) The data from Moore et al. (1995) were fitted to the three-parameter equation: Hscp= exp( −229.06923 +13418.39257/T +31.15669 ln(T)) mol m−3 Pa−1, with T in K.
797) The data from Glew and Moelwyn-Hughes (1953) were fitted to the three-parameter equation: Hscp= exp( −384.31677 +19391.25580/T +54.93602 ln(T)) mol m−3 Pa−1, with T in K.
798) The data from Moore et al. (1995) were fitted to the three-parameter equation: Hscp= exp( −247.93525 +14910.30572/T +34.08071 ln(T)) mol m−3 Pa−1, with T in K.
799) The regression given by Fogg and Sangster (2003) does not produce the data in their table. Thus the regression was recalculated.
800) The value listed as A for iodobenzene is probably not A but the Henry's law volatility constant Hvpx at 298 K. For the value of B, a minus sign is probably missing.
801) The data from Moore et al. (1995) were fitted to the three-parameter equation: Hscp= exp( −242.58767 +14043.89458/T +33.48497 ln(T)) mol m−3 Pa−1, with T in K.
802) Karagodin-Doyennel et al. (2021) probably assume that CH2BrI has the same Henry's law constant as CH2ClI.
803) The data from Haimi et al. (2006) were fitted to the three-parameter equation: Hscp= exp( −266.45850 +15036.99733/T +36.80758 ln(T)) mol m−3 Pa−1, with T in K.
804) Yaws et al. (2003) present Henry's law constants based on water solubility and vapor pressure. The water solubility is calculated using a correlation to the boiling point. For the vapor pressures, no references are provided.
805) The data from Zin et al. (2016) were fitted to the three-parameter equation: Hscp= exp( −419.66332 +22034.35758/T +59.55571 ln(T)) mol m−3 Pa−1, with T in K.
806) The data from Haimi et al. (2006) were fitted to the three-parameter equation: Hscp= exp( −166.97891 +10357.07398/T +22.04420 ln(T)) mol m−3 Pa−1, with T in K.
807) The data from Haimi et al. (2006) were fitted to the three-parameter equation: Hscp= exp( −406.56800 +21428.82541/T +57.60207 ln(T)) mol m−3 Pa−1, with T in K.
808) The data from Zin et al. (2016) were fitted to the three-parameter equation: Hscp= exp( 10.26074 +2303.75755/T −4.36399 ln(T)) mol m−3 Pa−1, with T in K.
809) Presumably, the species called "42-methyl-2-butanethiol" in Table 1 of Yao et al. (2002) should be 2-methyl-2-butanethiol.
810) Schäfer and Lax (1962) present data based on Booth and Jolley (1943). However, these data appear to be incorrect.
811) Booth and Jolley (1943) converted data from Rex (1906) to another unit. However, this was apparently not done correctly.
812) Booth and Jolley (1943) present data from Chancel and Parmentier (1885). However, in that paper only the solubility at an unknown partial pressure of CS2 was measured.
813) Value extracted from their Fig. 46.
814) The data from Haimi et al. (2006) were fitted to the three-parameter equation: Hscp= exp( −233.39763 +13839.16150/T +31.85189 ln(T)) mol m−3 Pa−1, with T in K.
815) Hs′ = 6.4×1014 mol2/(m6 Pa)
816) It is unclear how Fogg and Sangster (2003) obtained the data. Apparently, limiting activity coefficients γ were taken from Trampe and Eckert (1993), but a source for vapor pressure data is not mentioned. Also, the γ values listed in the table are different from those found in the original paper.
817) At pH = 3.9.
818) At pH = 4.8.
819) Mackay et al. (2006d) list two values for thiobencarb which differ by a large factor. It is unclear which number is correct (if any), and the data are not reproduced here.
820) Extrapolated from data at elevated temperatures.
821) Calculated using HENRYWIN 3.21.
822) Calculated using vapor pressures and water solubilities from HENRYWIN 3.21.
823) Calculated using vapor pressures and water solubilities from the EPA Toxicity Estimation Software Tool (TEST).
824) Wilhelm et al. (1977) and Abraham (1979) are quoted as the source. However, the data cannot be found there.
825) Shon et al. (2005) refer to Petersen et al. (1998) as the source, but this value cannot be found there.
826) The value from their experiment 7 at 10 °C is not used in the determination of the temperature dependence because of very different ionic strengths and concentrations for that experiment.

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