Gibbs
free energy (G)
One of the important applications of the second law of
thermodynamics is to predict the spontaneity of a reaction under a specific set
of conditions. A reaction that occurs under the given set of conditions without
any external driving force is called a spontaneous reaction. Otherwise, it is
said to be non-spontaneous. In our day today life, we observe many spontaneous
physical and chemical processes, which includes the following examples.
i.
A waterfall runs downhill, but never uphill,
spontaneously.
ii.
A lump of sugar dissolves spontaneously in a cup of
coffee, but never reappears in its original form spontaneously.
iii.
Heat flows from hotter object to a colder one, but never
flows from colder to hotter object spontaneously.
iv.
The expansion of a gas into an evacuated bulb is a
spontaneous process, the reverse process that is gathering of all molecules
into one bulb is not. Spontaneous
These examples show that the processes that occur
spontaneously in one direction, cannot take place in opposite direction
spontaneously.
Similarly a large number of exothermic reactions are
spontaneous. An example is combustion of methane.
CH4+2O2 → CO2 + 2 H2O
ΔHo =
−890.4 kJ mol−1
Another example is acid-base neutralization reaction:
H+ + OH− → H2O
ΔHo= −57.32 kJ mol−1
However, some endothermic processes are also spontaneous.
For example ammonium nitrate dissolves in water spontaneously though this
dissolution is endothermic.
NH4NO3 --H2O→ NH+4
+ NO−3
ΔHo= + 25 kJ mol−1
From the above examples we can come to the conclusion that
exothermicity favors the spontaneity but does not guarantee it. We cannot
decide whether or not a chemical reaction will occur spontaneously solely on
the basis of energy changes in the system. We know from second law of
thermodynamics that in a spontaneous process, the entropy increases. But not
all the processes which are accompanied by an increase in entropy are
spontaneous. In order to predict the spontaneity of a reaction, we need some
other thermodynamic function.
The second law of thermodynamics introduces another
thermodynamic function called Gibbs free energy which finds useful in
predicting the spontaneity of a reaction. The Gibbs free energy (G) was
developed in the 1870’s by Josiah Willard Gibbs. He originally termed this energy
as the “available energy” to do work in a system. This quantity is the energy
associated with a chemical reaction that can be used to do work.
Gibbs free energy is defined as below
G = H - TS ------------ (7.35)
Gibbs free energy (G) is an extensive property and it is a
single valued state function.
Let us consider a system which undergoes a change of state
from state (1) to state (2) at constant temperature.
G2 – G1 = (H2 – H1)
– T(S2 – S1)
ΔG =ΔH – T ΔS−−−−−−(7.36)
Now let us consider how ΔG is related to reaction
spontaneity.
We know that
ΔStotal = ΔSsys + ΔSsurr
For a reversible process (equilibrium), the change in
entropy of universe is zero. ΔStotal = 0 [∴ΔSsys = −ΔSsurr]
Similarly, for an equilibrium process ΔG=0
For spontaneous process, ΔStotal > 0 , so
TΔSsys − ΔHsys<0
−(ΔHsys− TΔSsys)>0
−(ΔG ) > 0
hence for a spontaneous process,
ΔG < 0
i.e. ΔH – T ΔS < 0
−−−−−−(7.37)
ΔHsys is the enthalpy change of a reaction, TΔSsys
is the energy which is not available to do useful work. So ΔG is the net energy
available to do useful work and is thus a measure of the ‘free energy’. For
this reason, it is also known as the free energy of the reaction. For non
spontaneous process, ΔG > 0
For any system at constant pressure and temperature
ΔG = ΔH – T ΔS −−−− (7.36)
We know that,
ΔH =ΔU + PΔV
ΔG = ΔU + PΔV – TΔS from first law of thermodynamics
ΔU = q + w
from second law of thermodynamics
ΔG = w + PΔV
−ΔG = −w − PΔV ............(7.38)
But −PΔV represents the work done due to expansion against
a constant external pressure. Therefore, it is clear that the decrease in free
energy (–ΔG) accompanying a process taking place at constant temperature and
pressure is equal to the maximum work obtainable from the system other than the
work of expansion.
The spontaneity of any process depends on three different
factors.
·
If the enthalpy change of a process is negative, then the
process is exothermic and may be spontaneous. (ΔH is negative)
·
If the entropy change of a process is positive, then the
process may occur spontaneously. (ΔS is positive)
·
The gibbs free energy which is the combination of the
above two (ΔH -TΔS) should be negative for a reaction to occur spontaneously,
i.e. the necessary condition for a reaction to be spontaneous is ΔH -TΔS < 0
The Table assumes ΔH and ΔS will remain the way indicated
for all temperatures. It may not be necessary that way. The Spontaneity of a
chemical reaction is only the potential for the reaction to proceed as written.
The rate of such processes is determined by kinetic factors, outside of
thermodynamical prediction.
In a reversible process, the system is in perfect
equilibrium with its surroundings at all times. A reversible chemical reaction
can proceed in either direction simultaneously, so that a dynamic equilibrium
is set up. This means that the reactions in both the directions should proceed
with decrease in free energy, which is impossible. It is possible only if at
equilibrium, the free energy of a system is minimum. Lets consider a general equilibrium
reaction
A+B ⇌ C + D
The free energy change of the above reaction in any state
(ΔG) is related to the standard free energy change of the reaction (ΔG0
) according to the following equation.
ΔG= ΔG0 + RT ln Q −−−−−−(7.39)
where Q is reaction quotient and is defined as the ratio
of concentration of the products to the concentrations of the reactants under
non equilibrium condition.
When equilibrium is attained, there is no further free
energy change i.e. ΔG 0 and Q becomes equal to equilibrium constant. Hence the
above equation becomes.
ΔG0 = –RT ln Keq
This equation is known as Van’t Hoff equation.
ΔG0 = –2.303 RT log Keq
----------(7.40)
We also know that
ΔG0 = ΔH0 – T ΔS0 = − RT
ln Keq
Calculate ΔG0
for conversion of oxygen to ozone 3/2 O2 ↔ O3(g) at 298 K, if Kp for this
conversion is 2.47 u 10−29 in standard pressure units.
ΔG0 = − 2.303 RT log Kp
Where
R = 8.314 JK−1mol−1
Kp = 2.47 x10−29
T = 298K
ΔG0=−2.303(8.314)(298)log(2.47u10−29)
ΔG0 = 16300 Jmol−1
ΔG0 = 16.3 KJ mol−1
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