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Partial Molal Volumes of Hydrocarbons in Water Solution
W. L. Masterton
Citation: J. Chem. Phys. 22, 1830 (1954); doi: 10.1063/1.1739928
View online: http://dx.doi.org/10.1063/1.1739928
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THF:
J O U R N A L
OF
C H E M I C A L P H Y S I C S V O L U M E 2 2 ,
N U M B E R 11
N O V E M B E R , 1 9 5 4
Partial Molal Volumes of ydrocarbons in Water Solution
W.
L.
MASTERTON*
Department of Chemistry and Chemical Engineering, University o f Illinois, Urbana, Illinois
(Received April 12 1954)
The partial molal volumes of benzene, methane, ethane and propane in water solution have been deter
mined
at
temperatures ranging from 1D-40°C. All
the
volumes measured were less
than
those of
the
same
hydrocarbons in nonpolar solvents. This decrease in volume is explained in terms of the abnormally high
internal pressure of water, which decreases the free volume available to the hydrocarbon molecules. The
temperature dependence of the partial molal volumes of the aliphatic hydrocarbons differs sharply from
. that of benzene. I t is suggested that this is caused by a difference in solution structure in the two cases.
INTRODUCTION
T
HE thermodynamics of aqueous solutions of
hydrocarbons have been investigated in this
laboratory during the past several years. Claussen and
Polglase
1
determined the solubilities, heats of solution,
and entropies of solution of methane, ethane, propane
and butane in water. Bohon and Claussen
2
carried out
a similar study for the aromatic hydrocarbons.
I t
has long been known that the lower aliphatic
hydrocarbons form solid hydrates. Structures of the
clathrate type have been proposed for these hydrates,3
and verified by x-ray diffraction studies/,r; (see urea
I C ~ ~ I I ~ 18
I
r--
6
----1"2. .
6 -
.
8
TT
oS
NJ
-
-
VI
LA
-
L.. \..
FIG. 1.
Copper block (vertical section).
*This paper is based on a thesis presented by the author in
partial fulfillment of the requirements for the Ph.D. degree at
the University of Illinois, June, 1952.
1
W. F. Claussen and M. F. Polglase, J. Am. Chern. Soc. 74
4817 (1952). '
2
R.
L.
Bohon and W. F.
Claussen,].
Am. Chern. Soc. 73 1571
(1951). '
3 W. F. Claussen,
J.
Chern. Phys.
19,259,662, 1425
(1951).
4
R. Cole, Ph.D. thesis, University of Illinois (1951).
clathrates).6 These ice-like structures contain voids
large enough to accommodate hydrocarbon molecules.
Such structures must exist in solution as well as in the
solid phase. One may then picture hydrocarbon mole
cules in solution as being surrounded by oriented cages
of water molecules. Claussen and Polglase
1
used this
concept to explain the negative enthalpies and entropies
of solution of the aliphatic hydrocarbons.
No hydrates of the aromatic hydrocarbons have ever
been reported, presumably because these molecules are
too large to fit into the voids in the hydrate structures.
I t has been found possible to explain the thermo
dynamics of aqueous solutions
of the aromatic hydro
carbons without assuming the presence of structures of
the type described above.
I t
is of interest to determine whether the partial
molal volumes of hydrocarbons in water solution agree
with this model of their solution structures. The partial
molal volume V in these extremely dilute solutions was
found to be identical with the apparent molal volume
1/- .
The latter can be determined from the specific gravities
and concentrations of the hydrocarbon solutions by the
following equation:
(1)
where M
2
=molecular weight of hydrocarbon,
y=con-
centration of hydrocarbon
in glcc,
and d do=densities
of solution and pure water, respectively, at the tem
perature at which is measured.
Since the solubilities of the hydrocarbons are ex
tremely small (benzene,
1.
70 X
10-
3
glcc; methane,
2.30X 10-
5
g/cc , an extremely sensitive method must
be chosen for the determination of the specific gravities.
Such a method should give results accurate to about
seven decimal places.
Several methods are available for the determination
of specific gravities of extremely dilute solutions.
Various modifications of the float method have been
described in the literature. They suffer from the common
problem of temperature control. A procedure in which
the solution and reference liquid were compared simul
taneously would obviously reduce this difficulty. Such
5
M. V. Stackelberg, Naturwiss. 36, 327, 359 (1949).
6 F. Cramer, Angew. Chern. 64, 437 (1952).
1830
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P A R
T I A L J\I 0
LA
L VOL U M E S 0 F H Y D ROC ARB 0 N S N \V ATE R
1831
a method is
that
of Frivold
7
which utilizes the principle
of communicating tubes.
In
this method, solution
and
reference liquid air
free conductiv ity water) are placed in two vertical tubes
connected
at
the
bottom and
near the top
by
valves.
Upon first allowing the upper valves to be opened for
equilibration
and
then opening the lower valves,.
flo.w
will occur if the solution differs from the reference hqmd
in specific gravity. Wirth, Thompson, and Utterback
8
measured indirectly the drop
of
the liquid level in one
of the tubes as a result of this flow. An alternative
procedure is to measure the volume
of
liquid which
must be withdrawn from one side of the apparatus to
prevent
flow.
This volume is simply related to the
specific gravity of the solution by the equation
Vjah l d jd
n
, (2)
where = volume of water withdrawn to achieve equi
librium, a= cross sectional area of the liquid surfaces in
the tubes,
h=distance
between the upper a.nd lower
valves, and
jd
o
=
specific gravity of the solutlOn.
EXPERIMENTAL
A. The Copper Block Specific Gravity Apparatus
t was found necessary to construct the apparatus
out of copper
so
as to allow for the rapid equilibration
FIG.2 . Glass capillary.
1 ~ 3 8 . 1
MM
1.. i
4MM.
U
T ~
.46 ii:r-
1
6
MM.
of
any
temperature difference between the two tubes.
An accuracy of one part in ten million in specific
gravity requires temperature control accurate to
±O.OOOloC
which is difficult to achieve in a glass
apparatus. The dimensions of the apparatus are indi
cated in Fig.
1.
The copper block was enclosed in a wooden insulating
chamber which formed
an
air ba
ho
Attached to the
inside of each of the walls of the chamber was a hollow
steel
tank
one inch thick.
By
circulating water from a
refrigeration bath through these tanks, experiments
could be made
at
temperatures as low as Soc. A re
sistance coil inserted inside the chamber permitted
operating temperatures up to
SO°C.
The temperature of
the air bath could be maintained to within ±O.O1 °c
while the high thermal conductivity
of
the copper block
itself insured
that
the temperatures of the two columns
of liquid would be equal within ±O.OOOOl°C. The
copper surfaces
of the block were lined with tin to
prevent corrosion.
In order to detect flow of liquid through the lower
valves, a glass capillary was inserted into the lower con-
7
O. E. Frivold, Physik. Z. 21, 529 1920).
8 Wirth, Thompson, and Utterback, J. Am. Chem. Soc. 57,
400 1935).
8 7 ~ - - ~ - - - - , - - - ~
4
BENZENE
54
... .
<
~ 5
::J
.J
5
>
41
3 9 r ~ ~ .
J
7
w
::J
..J
g
35
69
J
~ 67
...
:li
::J
..J
65
>
2 3
41
TEMP.oC
METHANE
41
FIG. 3. Change of partial molal volume with temperature.
necting tube and a dye was injected
at
one edge
of
the
capillary.
The
flow of dye through the capillary was
observed through an optical system with the eyepiece
outside the apparatus. The dimensions
of
the capillary
are quite critical; if it is too large, a significant amount
of
flow
will
occur before it can be detected, leading to
low
values of in Eq. 2). On the other hand, too fine
a capillary would greatly reduce the rate of
flow
of the
dye
and
seriously affect the sensitivity
of
the instru
ment. The capillary chosen was 1.6 mm in length and
0.4
mm
in diameter.
Its
design
is
shown in Fig.
2.
The glass tube was sealed into the lower horizontal
tube with sealing wax. t was found that the dye would
move across the capillary by diffusion and mixing in
about ten minutes while a difference
of
one
part
in ten
million in specific gravity would cause the dye to flow
across the capillary in three minutes.
The volume
of liquid withdrawn to achieve equi
librium was accurately measured in a capillary burette.
This consisted of a piece of calibrated capillary tubing
fastened to a meter stick.
Frequent blank runs were made in the course
of
the
experimental determinations. These consisted of filling
both sides of the apparatus with conductivity water
and measuring the difference in specific gravities of the
two columns
of
water. In no case was a difference de
tected greater than one part in ten million, the limit
of
accuracy
of
the experiments.
B. Preparation
and
Analysis of Solutions
Special precautions were taken to insure that the only
factor producing a difference
in
specific gravity between
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1832
W .
L. M S T E R S O N
TABLE I Apparent molal volumes of benzene in water solution.
T=IO.IOC
T
=2S.2°C
T=30.0·C
y
I d/do
'
y
I d/do
'
y
I d/do
'
10'
XlO
cc
XIO
X1O'
cc
XIO
XIO
cc
1.62 0.78 81.9 1.24 0.90 83.7
1.81
1.29 83.6
1.96 0.82 81.4 3.07 1.95 83.0 2.13 1.42
83.2
2.48
1.09 81.5 3.75
2.41
83.1
2.44 1.54
83.0
3.79 1.84 81.8
4.00
2.68 83.4 3.47 2.26 83.2
3.99 1.92 81.8 5.87 3.53 82.8 4.72 3.07 83.2
4.57 2.26 81.8
5.02 3.30 83.3
6.04 2.80 81.7 5.88 3.78 83.2
6.52 4.36 83.4
Av.=81.7 Av.=83.2 Av.=83.3
T
=34.9°C
T=39.9°C
y
I d/do
'
y
I dido
'
IO
XIO
co
XIO
XIO
cc
2.50 1.85 83.9
1.76
1.50 84.7
4.69
3.59
84.1 2.57 2.16 84.8
6.67 4.85 83.9 4.01 3.16 84.4
4.58 3.49 84.0
4.79
3.89 84.6
Av. = 84.0 Av. = 84.5
solution and standard was the presence of the solute
being investigated. A difference in concentration of dis
solved air or of isotopic composition would cause
spurious specific gravity differences.
To
avoid this a
sample of conductivity water was rendered air-free by
boiling under vacuum. t was then split into two por
tions, one of which served as the solvent for the hydro
carbon solution and the other as reference liquid.
1.
Benzene soltttions
The benzene used to prepare the solutions was
purified by the method of Mair
et al
The solutions
were prepared by placing one portion of the air-free
conductivity water in contact with benzene vapor
arising from a tube connected to the solution flask. The
solution process was hastened by stirring the water in
the solution flask with a magnetic stirrer. Solution was
carried out under vacuum.
The concentrations of the benzene solutions could be
adjusted by varying the time of exposure of the solution
flask to benzene vapor. Stirring was continued for
several minutes after the solution was shut off from
contact with the benzene vapor. This insured uniform
concentration of the solution. Solution and standard
were then successively admitted to the block. About
fifteen minutes were allowed for the liquids to come to
the temperature of the block. The specific gravity of
the solution was then determined. In each experiment
measurements were taken until three successive deter
minations agreed within one part in the seventh decimal
place.
Portions of the solution were then withdrawn from
the block
and
analyzed by means of an ultraviolet
• Mair, Termini, Willingham, a nd Rossini,
J.
Research Nat .
Bur. Standards 37 229 (1946).
spectrophotometer. t was found that the absorption
peak
at 2537
A obeyed Beer's law within
t
of 1 percent
at optical densities up to 1.0. Portions of the solution
withdrawn from various sections of the block showed
uniform concentrations within at least 1 percent.
Evaporation of benzene apparently occurred only from
the trays above the vertical tubes provided the solutions
were analyzed within two to three hours after admission
to the block.
From the concentrations of the solutions and their
specific gravities the apparent molal volumes could be
calculated
by
means of Eq. (1). The data on benzene
solutions is given in Table I
2
Aliphatic Hydrocarbon Solutions
The aliphatic hydrocarbons studied were methane,
ethane, and propane. The hydrocarbons used were all
of research grade (99 mole percent pure). They were
TABLE II. Apparent molal volumes of aliphatic hydrocarbons
in water solution.
=16.S·C
y
did .
XIO XIO
2.30 2.48
2.31
2.58
2.34 2.48
2.35 2.95
2.41
2.54
2.43 2.57
Av.=33.2
=16.9·C
cc
33.3
33.8
33.0
36.2"
33.0
33.0
Y
XIO
1.43
1.44
1.49
1.55
1.58
y
I-d/do o
XIO XIO cc
3.61 2.17 48.2
=16.9°C
y
I dido
o
X 10
XlO
cc
6.48 2.96 64.1
6.53
2.83
63.2
7.79 3.45 63.5
Av.=63.6
Methane
T=23.0°C
y
I d/do
'
10 XIO
cc
1.04
1.35 36.8
1.53 1.92 36.2
1.95 2.47 36.5
1.95 2.38 35.5
1.96 2.50 36.5
2.25
2.81
36.0
2.63 3.42 36.9
Av.=36.3
T=3S.IOC
I d/do
XIO
1.95
1.93
2.10
1.92
2.19
Av.=38.2
Ethane
T=23.0°C
y
I d/do
o
XIO
X 10
cc
3.68
2.52
50.7
4.70 3.20 50.5
5.14 3.44 50.2
5.61 3.82 50.5
Av.=50.5
Propane
T =23.0°C
Y
I d /d .
'
IO
XIO
cc
4.88 2.52 66.8
5.30
2.64 66.8
5.63 2.93 67.0
6.31 3.13
65.9
Av.=66.6
a Value omitted in obt in ing average
T =29.1 °C
y I dido
XIO XIO
1.63 2.23
1.75 2.44
1.83 2.48
Av.=38.0
cc
37.9
37.6
38.7
35.9"
38.3
y
XIO
3.35
4.59
T =29.1 °C
I dido
X 10
2.49
3.34
o
cc
38.0
38.4
37.8
o
cc
52.3
51.9
Av.=52.1
T =29.I ·C
y
I d /d .
o
X 10 X 10
cc
3.91 2.10 67.8
4.45
2.34 67.3
4.66 2.45
67.3
Av.=67.S
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PAR T I A L MOL A L VOL U M E S 0 F H Y D ROC
ARB
0 N S N W A T E R
1833
freed of traces of carbon dioxide by passing over
ascarite. The purified gases were brought into contact
with samples of air-free water stirred by means of a
magnetic stirrer in an apparatus similar to that used
for benzene.
Experiments were run to determine the time neces
sary for saturation.
It
was found
that
four hours were
sufficient to achieve saturation with the technique used.
Samples saturated for periods up to twelve hours gave
partial molal volumes identical with those obtained
after four hours contact.
Before admitting the hydrocarbon gas to the satura
tion apparatus all the air was removed from the system.
The initial pressure read on the manometer was then
the vapor pressure of water at the temperature of the
solution. Gas was admitted to the solution flask until
the desired pressure, as read on the manometer, was
reached. The final pressure of the gas after saturation
was reached was recorded.
The difference between final
and
initial pressures gave the partial pressure
of
the
hydrocarbon gas. From this pressure and the tempera
ture of the solution, it was possible to calculate the
concentration of the solution. Henry S law was used to
calculate the effect of pressure on the solubility;
data
in the literature indicates that it holds within one-half
of one percent for such extremely dilute solutions.
The
data of Claussen and Polglase
was used to calculate
the solubilities of the gases
at
one atmosphere pressure
at the temperature
of
the solution.
The specific gravities of the solutions were measured
in the same manner as those
of
the benzene solutions.
Once again it was found that the apparent molal
volumes were independent of concentration.
The data on solutions of methane, ethane, and pro
pane is given in Table
II It
will be noted
that
the
precision is considerably less than for the benzene
solutions, probably because the concentration data was
less accurate.
DISCUSSION OF RESULTS
It
is instructive to compare the partial molal volumes
of the hydrocarbons in water solution to their volumes
in nonaqueous solvents. The molal volume of pure
benzene at 25°C is 89.5 cc; the partial molal volume in
water is 83.1
cc.
This is a decrease in water solution
of
6.4
cc.
The simplest explanation of this decrease in volume
involves the large internal pressure of water as com
pared to that of benzene itself. Gjaldbaek and Hilde
brand
lO
found that the part ial molal volume of methane,
ethane, and nitrogen decreased sharply as the internal
pressure of the solvent increased. The fact that the
decrease in volume for benzene is relatively small is
10
J.
C. Gjaldbaek
and J. H
Hildebrand,
J.
Am. Chern.
Soc.
72,
1077 (1950).
TABLE
III
Partial molal volumes of methane and ethane at 25°C.
Solvent (int.)
Methane Ethane
Per-flu oro n-heptane 1430 atmos
68.4 cc 82.9 cc
n-hexane 2190
60.0
69.3
Carbon tetrachloride
3050
51.7 66.0
Water 12000
37.3
51.2
probably due to the rather small compressibility of
benzene at high pressure.
l
The coefficient of expansion
a
of benzene in water solution is independent of tem
perature and slightly smaller than
that of pure benzene,
as would be expected in a solvent of high internal
pressure.
The partial molal volumes of the aliphatic hydro
carbons in water solution are considerably less than the
corresponding values
in
nonaqueous solvents. Table III
gives the partial molal volumes of methane and ethane
at
25°C in various solvents. The values for carbon
tetrachloride are taken from Horiuti
;12
those for the
other organic liquids are from Gjaldbaek and Hilde
brand.
10
Values of the internal pre?sures are taken from
Hildebrand and ScottY
It
will be noted from the curves
that
the change of
partial molal volume with temperature for the aliphatic
hydrocarbons is of a quite different nature than
that
of benzene. The linear increase observed with benzene
does not occur with the aliphatics; instead the rate of
increase
of
the partial molal volume with temperature
(the coefficient of expansion a decreases with increasing
temperature. This leads one to believe that there are
two competing processes going on in the case of the
aliphatic hydrocarbons. The normal thermal expansion,
which increases iT would be expected to give a nearly
linear slope as it does with benzene. The other process
is apparently a breaking down
of
the cage-like structure
of water molecules around the aliphatic hydrocarbon
molecules. This produces a decrease in the part ial molal
volume analogous to that observed when ice melts. The
above curves thus represent the net result of these two
processes.
ACKNOWLEDGMENT
The author is greatly indebted to
W.
H. Rodebush,
who suggested this problem and under whose advice
and guidance the work was performed.
W.
F. Claussen
designed the apparatus and supervised its construction,
installation and testing.
The research was aided by funds supplied by the
Office
of
Naval Research and
by
a predoctoral fellow
ship provided by the U.
S.
Atomic Energy Commission.
P W. Bridgman, J. Chern. Phys. 9 794 (1941).
12
J Horiuti, Sci. Papers Inst. Phys. Chern. Research (Tokyo)
17, 125 (1931).
13 J. H Hildebrand and R. L Scott,
The Solubility oj Non-
lectrolytes
(Reinhold Publishing Corporation, New York, 1950).