Environmental Engineering Reference
In-Depth Information
TABLE 3.10
Values of
w
i
o
i
γ
and
γ
for Typical Organic Compounds at 298 K
o
i
w
i
Compound
γ
γ
2.4
×
10
3
Benzene
2.83
1.2
×
10
4
Toluene
3.18
1.4
×
10
5
Naphthalene
4.15
4.2
×
10
5
Biphenyl
5.30
6.1
×
10
4
p
-Dichlorobenzene
3.54
9.6
×
10
6
Pyrene
8.66
8.6
×
10
2
Chloroform
1.40
10
4
Carbon tetrachloride
3.83
1.0
×
Source:
From Mackay, D. 1982.
VolatilizationofOrganicPollutantsfromWater
.
EPA Report No: 600/3-82-019, NTIS No: PB 82-230939. Springfield,
VA: National Technical Information Service; Chiou, C.T. 1981. Parti-
tion coefficient and water solubility in environmental chemistry. In: J.
Saxena and F. Fisher (eds),
Hazard Assessment of Chemicals
, Vol. 1.
New York: Academic Press; Yalkowsky, S.H. and Banerjee, S. 1992.
Aqueous Solubilities—Methods of Estimation for Organic Compounds
.
NewYork: Marcel Dekker.
also available in pure form readily and is only sparingly soluble in water.Appendix 1
lists the log
K
ow
values for a variety of compounds.
It is important to note that generally large
K
ow
values are associated with com-
pounds that have low affinity with the aqueous phase. This becomes clear when one
notes that most solutes behave ideally in octanol, and hence
o
γ
i
varies only slightly
i
varies over several orders of magnitude (0.1-10
7
)
(see Table 3.10). Since both
V
o
and
V
w
are constants, the variation in
K
ow
is entirely
due to variations in
w
(from about 1 to 10) whereas
γ
w
i
. In other words,
K
ow
is a measure of the relative nonideality
of the solute in water as compared to that in octanol. Hence K
ow
is taken to be a
measure of the
hydrophobicity
or the
incompatibility
of the solute with water
.
K
ow
values in the literature are reported at “room temperature.” This means the
temperature is 298 K with occasional variability of about 5
◦
. It is important to note
that the temperature dependence is nearly negligible for these temperature variations.
Theremaybecaseswhenreliableexperimental
K
ow
valuesarenotavailable.Under
these circumstances it is possible to estimate
K
ow
from basic structural parameters of
the molecule (Lyman, Reehl, and Rosenblatt, 1990). Langmuir (1925) first suggested
that the interaction of a molecule with a solvent can be obtained by summing the
interactions of each fragment of the molecule with the solvent. The same principle
wasextendedtooctanol-waterpartitionratiosbyHanschandLeo(1979).Thismethod
involves assigning values of interaction parameters to the various fragments that make
up a molecule. For example, an alkane molecule (ethane, CH
3
-CH
3
)
is composed of
two -CH
3
groups, each contributing equally toward the
K
ow
of the molecule. There
are two parts to this type of calculation: a
fragmentconstant
(
b)
and
astructuralfactor
(
B)
. It is presumed that from chemical to chemical these constants are the same for a
γ
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