Properties
of Liquids
Critical
Temperature and Critical Pressure
The obvious way to turn a gas into a liquid is to cool it
to a temperature below its boiling point. There is another
way of condensing a gas to form a liquid, however, which
involves raising the pressure on the gas. Liquids boil at the
temperature at which the vapor pressure is equal to the
pressure on the liquid from its surroundings. Raising the
pressure on a gas therefore effectively increases the boiling
point of the liquid.
Suppose that we have water vapor (or steam) in a closed
container at 120oC and 1 atm. Since the
temperature of the system is above the normal boiling point
of water, there is no reason for the steam to condense to
form a liquid. Nothing happens as we slowly compress the
container
thereby raising the pressure on the gas
until
the pressure reaches 2 atm. At this point, the system is at
the boiling point of water, and some of the gas will condense
to form a liquid. As soon as the pressure on the gas exceeds
2 atm, the vapor pressure of water at 120oC is no
longer large enough for the liquid to boil. The gas therefore
condenses to form a liquid, as shown in the figure below.
In theory, we should be able to predict the
pressure at which a gas condenses at a given temperature by
consulting a
plot of vapor pressure vs. temperature . In
practice, every compound has a critical temperature
(Tc).
If the temperature of the gas is above the critical
temperature, the gas can't be condensed, regardless of the
pressure applied.
The existence of a critical temperature was discovered by
Thomas Andrews in 1869 while studying the effect of
temperature and pressure on the behavior of carbon dioxide.
Andrews found that he could condense CO2 gas into
a liquid by raising the pressure on the gas, as long as he
kept the temperature below 31.0oC. At 31.0oC,
for example, it takes a pressure of 72.85 atm to liquify CO2
gas. Andrews found that it was impossible to turn CO2
into a liquid above this temperature, no matter how much
pressure was applied.
Gases can't be liquified at temperatures above the
critical temperature because at this point the properties of
gases and liquids become the same, and there is no basis on
which to distinguish between gases and liquids. The vapor
pressure of a liquid at the critical temperature is called
the critical pressure (Pc).
The vapor pressure of a liquid never gets larger than this
critical pressure.
The critical temperatures, critical pressures, and boiling
points of a number of gases are given in the table below.
There is an obvious correlation between the critical
temperature and boiling point of these gases. These
properties are related because they are both indirect
measures of the force of attraction between particles in the
gas phase.
Critical Temperatures, Critical
Pressures and Boiling Points of Common Gases
Gas |
|
Tc(oC) |
|
Pc (atm) |
|
BP (oC) |
He |
|
-267.96 |
|
2.261 |
|
-268.94 |
H2 |
|
-240.17 |
|
12.77 |
|
-252.76 |
Ne |
|
-228.71 |
|
26.86 |
|
-246.1 |
N2 |
|
-146.89 |
|
33.54 |
|
-195.81 |
CO |
|
-140.23 |
|
34.53 |
|
-191.49 |
Ar |
|
-122.44 |
|
48.00 |
|
-185.87 |
O2 |
|
-118.38 |
|
50.14 |
|
-182.96 |
CH4 |
|
-82.60 |
|
45.44 |
|
-161.49 |
CO2 |
|
31.04 |
|
72.85 |
|
-78.44 |
NH3 |
|
132.4 |
|
111.3 |
|
-33.42 |
Cl2 |
|
144.0 |
|
78.1 |
|
-34.03 |
The experimental values of the critical
temperature and pressure of a substance can be used to
calculate the a and b constants in the van
der Waals equation.

Surface
Tension
There is a force of attraction between molecules in
liquids, and liquids can flow until they take on the shape
that maximizes this force of attraction. Below the surface of
the liquid, the force of cohesion (literally,
"sticking together") between molecules is the same
in all directions, as shown in the figure below. Molecules on
the surface of the liquid, however, feel a net force of
attraction that pulls them back into the body of the liquid.
As a result, the liquid tries to take on the shape that has
the smallest possible surface area
the shape of a sphere. The
magnitude of the force that controls the shape of the liquid
is called the surface tension. The stronger
the bonds between the molecules in the liquid, the larger the
surface tension.
There is also a force of adhesion (literally,
"sticking") between a liquid and the walls of the
container. When the force of adhesion is more than half as
large as the force of cohesion between the liquid molecules,
the liquid is said to "wet" the solid. A good
example of this phenomenon is the wetting of paper by water.
The force of adhesion between paper and water combined with
the force of cohesion between water molecules explains why
sheets of wet paper stick together.
Water wets glass because of the force of adhesion that
results from interactions between the positive ends of the
polar water molecules and the negatively charged oxygen atoms
in glass. As a result, water forms a meniscus
that curves upward in a small-diameter glass tube, as shown
in the figure below. (The term meniscus comes from
the Greek word for "moon" and is used to describe
anything that has a crescent shape.) The meniscus that water
forms in a buret results from a balance between the force of
adhesion pulling up on the column of water to wet the walls
of the glass tube and the force of gravity pulling down on
the liquid.
 |
Water climbs the walls of a small-diameter tube
to form a meniscus that curves upward, whereas
mercury forms a meniscus that curves downward. |
The force of adhesion between
water and wax is very small compared to the force of cohesion
between water molecules. As a result, rain doesn't adhere to
wax. It tends to form beads, or drops, with the smallest
possible surface area, thereby maximizing the force of
cohesion between the water molecules. The same thing happens
when mercury is spilled on glass or poured into a narrow
glass tube. The force of cohesion between mercury atoms is so
much larger than the force of adhesion between mercury and
glass that the area of contact between mercury and glass is
kept to a minimum, with the net result being the meniscus
shown in the above figure.

Viscosity
Viscosity is a measure of the resistance
to flow. Motor oils are more viscous than gasoline, for
example, and the maple syrup used on pancakes is more viscous
than the vegetable oils used in salad dressings.
Viscosity is measured by determining the rate at which a
liquid or gas flows through a small-diameter glass tube. In
1844 Jean Louis Marie Poiseuille showed that the volume of
fluid (V) that flows down a small-diameter capillary
tube per unit of time (t) is proportional to the
radius of the rube (r), the pressure pushing the
fluid down the tube (P), the length of the tube (l),
and the viscosity of the fluid (
).
Viscosity is reported in units called poise
(pronounced "pwahz"). The viscosity of water at
room temperature is roughly 1 centipoise, or 1 cP. Gasoline
has a viscosity between 0.4 and 0.5 cP; the viscosity of air
is 0.018 cP.
Because the molecules closest to the walls of a
small-diameter tube adhere to the glass, viscosity measures
the rate at which molecules in the middle of the stream of
liquid or gas flow past this outer layer of more or less
stationary molecules. Viscosity therefore depends on any
factor that can influence the ease with which molecules slip
past each other. Liquids tend to become more viscous as the
molecules become larger, or as the amount of intermolecular
bonding increases. They become less viscous as the
temperature increases. The viscosity of water, for example,
decreases from 1.77 cP at 0oC to 0.28 cP at 100oC.

Hydrogen
Bonding and the Anomalous Properties of Water
We are so familiar with the properties of water that it is
difficult to appreciate the extent to which its behavior is
unusual.
- Most solids expand when they melt. Water expands when
it freezes.
- Most solids are more dense than the corresponding
liquids. Ice (0.917 g/cm3) is not as dense
as water.
- Water has a melting point at least 100oC
higher than expected on the basis of the melting
points of H2S, H2Se, and H2Te.
- Water has a boiling point almost 200oC
higher than expected from the boiling points of H2S,
H2Se, and H2Te.
- Water has the largest surface tension of any common
liquid except liquid mercury.
- Water has an unusually large viscosity.
- Water is an excellent solvent. It can dissolve
compounds, such as NaCl, that are insoluble or only
slightly soluble in other liquids.
- Water has an unusually high heat capacity. It takes
more heat to raise the temperature of 1 gram of water
by 1oC than any other liquid.
These anomalous properties all result from the strong
intermolecular bonds in water. Water is best described as a polar
molecule in which there is a partial separation of charge
to give positive and negative poles. The force of attraction
between a positively charged hydrogen atom on one water
molecule and the negatively charged oxygen atom on another
gives rise to an intermolecular bond, as shown in the figure
below. This dipole-dipole interaction between water molecules
is known as a hydrogen bond.
Hydrogen bonds are separated from other
examples of van der Waals forces because they are unusually
strong: 10-12 kJ/mol. The hydrogen bonds in water are
particularly important because of the dominant role that
water plays in the chemistry of living systems. Hydrogen
bonds are not limited to water, however.
Hydrogen-bond donors include substances that contain
relatively polar H-X bonds, such as NH3,
H2O, and HF. Hydrogen-bond acceptors include
substances that have nonbonding pairs of valence electrons.
The H-X bond must be polar to create the partial
positive charge on the hydrogen atom that allows
dipole-dipole interactions to exist. As the X atom
in the H-X bond becomes less electronegative,
hydrogen bonding between molecules becomes less important.
Hydrogen bonding in HF, for example, is much stronger than in
either H2O or HCl.
The hydrogen bonds between water molecules in ice produce
the open structure shown in the figure below. When ice melts,
some of these bonds are broken, and this structure collapses
to form a liquid that is about 10% denser. This unusual
property of water has several important consequences. The
expansion of water when it freezes is responsible for the
cracking of concrete, which forms potholes in streets and
highways. But it also means that ice floats on top of rivers
and streams. The ice that forms each winter therefore has a
chance to melt during the summer.
 |
The structure of ice. Note that the hydrogen
atoms are closer to one of the oxygen atoms than the
other in each of the hydrogen bonds. |
The figure below shows another consequence
of the strength of the hydrogen bonds in water. There is a
steady increase in boiling point in the series CH4,
GeH4, SiH4, and SnH4. The
boiling points of H2O and HF, however, are
anomalously large because of the strong hydrogen bonds
between molecules in these liquids. If this doesn't seem
important, try to imagine what life would be like if water
boiled at -80oC.
The surface tension and viscosity of water
are also related to the strength of the hydrogen bonds
between water molecules. The surface tension of water is
responsible for the capillary action that brings water up
through the root systems of plants. It is also responsible
for the efficiency with which the wax that coats the surface
of leaves can protect plants from excessive loss of water
through evaporation.
The unusually large heat capacity of water is also related
to the strength of the hydrogen bonds between water
molecules. Anything that increases the motion of water
molecules, and therefore the temperature of water, must
interfere with the hydrogen bonds between these molecules.
The fact that it takes so much energy to disrupt these bonds
means that water can store enormous amounts of thermal
energy. Although the water in lakes and rivers gets warmer in
the summer and cooler in the winter, the large heat capacity
of water limits the range of temperatures that would
otherwise threaten the life that flourishes in this
environment. The heat capacity of water is also responsible
for the ocean's ability to act as a thermal reservoir that
moderates the swings in temperature that occur from winter to
summer.

