We have seen calculations for the entropy change for
processes. However, it is also possible
to calculate the absolute entropy. We
can begin with the definition dS = dqrev/T. The heat transferred during a process at constant volume is dqv,rev = CvdT. Substituting this value into the expression for
the entropy and assuming reversibility leads to
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If we wish to find the
entropy at a given temperature T we can integrate this expression

We have kept the
equation general by showing Cv(T) as a function of temperature. This calculation of the entropy is valid
only at constant V. At constant P we
find an analogous expression. Starting
with the heat transferred, dqp,rev = CpdT.
We have

Which leads to the
integrated expression for the absolute entropy at constant pressure
These equations tell us that if we know the entropy
at T = 0 K we can determine the absolute entropy at the temperature of interest
by integration of the temperature dependent heat capacity.
The
third law of thermodynamics states that every substance has a positive entropy,
but at zero Kelvin the entropy is zero for a perfectly crystalline
substance. The third law introduces a
numerical scale for the entropy. One of
the earliest formulations was that of Boltzmann. If we recall the function W that represents the number of ways we
can distribute N particles into a number of states the entropy can be expressed
as
S = kB ln W
At zero Kelvin the system is in its lowest energy
state. For a perfect crystal there is
only one way to distribute the energy and W = 1, therefore S = 0.

We can also begin with
the statistical view of entropy
At T = 0 K, P0 = 1 because only the
ground state will be populated. Since
ln(1) = 0, S = 0 as well.
If
there is a phase transition between 0 and T we can also calculate the
contribution to the entropy from the transition.
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A phase transition is a reversible
process. Moreover, since phase
transitions that normally consider occur at constant pressure we have qp,rev
= DHtrs.
To
calculate the absolute entropy we integrate Cp(T)/T to the first
phase transition, add a term for the phase transition and continue the integration. The absolute entropy is then calculated as

The third law of thermodynamics shows that
Cp ® 0 as T ® 0 K as well. It is necessary
to leave Cp(T) as a function of temperature for this reason
alone. The Einstein and Debye theories
of heat capacity can be used to determine the functional form of the heat
capacity of at these low temperatures (see section 17-4 and Mathchapter
I). For practical calculation of the
entropy, however, the experimental values can be used and the integrals above
are evaluated numerically (Section 21-5).
So is the
entropy not equal to zero at T = 0 K if the substance is not a perfect
crystal. The answer is yes. Let us consider the example of CO. CO has a very small dipole moment and there
is a finite chance that CO will crystallize as CO:OC:CO instead of
CO:CO:CO. For each CO molecule there
are two possible orientations of the molecule, therefore there are two ways
each CO can exist in the lattice. w = 2
for each CO. If we have N CO molecules
there are wN ways or 2N ways that all of the CO can be
distributed. Therefore, the entropy at
zero Kelvin is
S = k ln W = k ln(wN) = Nk ln w = nR ln
2.
The entropy at zero Kelvin is known as residual
entropy. The CO crystal is considered imperfect
since the sites do not all have CO aligned with the same orientation. There is significant residual entropy in a
number of common substances. For
example, water has residual entropy at zero Kelvin due to the fact that
orientation of the hydrogens and lone pairs does not have same orientation in
all of the molecules. The residual
entropy is responsible for the deviation of calculated from experimental values
of the entropy discussed in section 21-8.
We have
seen that
S = U/T + k lnQ
and that U itself can be calculated from the
partition function. This leads to a
calculation of the entropy in terms of the partition function.

This can be expressed
in terms of the molecular partition function.
Recall that the molecules in a gas are not distinguishable. Therefore, Q = qN/N!. Substituting this into the expression for
the entropy we have

Using Stirling’s
approximation: ln N! = NlnN-N, we find

Recall that the
molecular partition function is the product of the partition functions for
various molecular energy levels, translation, rotation, vibration, and
electronic, q = qtransqrotqvibqelec.

For our discussion we consider only the
translational partition function. This
one is by far the largest and this is the only one that is relevant for an
ideal gas. After all an ideal gas can
translate, but has not rotation, vibrational or electronic states. Application of the equation to real gases as
shown on page 862 of McQuarrie and Simon is complicated in appearance, but is
really no more difficult than application to qtrans. To calculate the entropy of an ideal
monatomic gas we substitute qtrans into (II).
We have already shown that

To substitute this
expression into (II) we need to take the derivative

The first an last
terms are zero since they have no temperature dpendence. The middle term evaluates to 3/2T. Substituting this into (II) we have

Recalling that Nk = nR
where N is the number of molecules and n is the number of moles we can express
the molar entropy (S = S/n) as
The dependence of entropy on molecular structure
The entropies of
gases are greater than liquids and liquids are greater than solids. This follows directly from the calculation
using equation (I). Equation (II) shown
for an ideal gas above indicates that the entropy of a gas will increase as its
mass increases. Thus, the trend in the
noble gases is for the entropy to increase as we descend the periodic table
(S(Xe) > S(Kr) > S (Ar) > S(Ne)).
Although we have not considered rotational and vibrational contributions
mathematically, it is intuitively understandable that the greater the number of
accessible levels, the greater the entropy.
Therefore, molecules with a large number of atoms (and heavier atoms)
will tend to have a larger entropy.
This is primarily because of rotational levels. A larger number of these can be populated
compared to vibrational levels.
Absolute entropies can be used to calculate reaction entropies
Entropies are
tabulated in order to facilitate the calculation of the entropy change of
chemical reactions. For the general
reaction
aA + bB ® yY + zZ
the standard entropy change is given by
DrSo
= ySo[Y] + zSo[Z] - aSo[A] - bSo[B]
where the absolute entropies So are molar
quantities.