Spontaneity, Entropy and Free Energy
This part of thermodynamics
predicts whether a process is spontaneous, and how much energy is available
from the process. A spontaneous process is one which occurs without
outside intervention. The speed at which it occurs is governed
by kinetics. Spontaneous processes don't necessarily occur quickly,
they just occur on their own.
There are several
factors which influence spontaneity. One is the energy involved,
DH.
Although processes which are exothermic are often spontaneous, endothermic
processes can also be spontaneous. For example, ice melts at a temperature
above 0oC, even though the process requires heat. This
example also illustrates that temperature is a factor. Some processes
are spontaneous at high temperatures, other at lower temperatures.
Lastly, entropy must be considered. Entropy is a measure of randomness
or disorder. The second law of thermodynamics states that in
any spontaneous process, the entropy of the universe increases. The
universe includes both the system's disorder and the disorder of the surroundings.
Thus, a spontaneous process can occur, in which the system becomes more
ordered, only if the entropy increase in the surroundings is greater.
For example, when ice freezes below 0oC, the liquid water goes
to a more ordered solid state. That is, the system loses entropy.
However, as the ice freezes, heat is given off the surroundings.
This heat flow increases random motion of molecules in the surroundings
and increases the entropy of the surroundings. Since the process
is spontaneous below 0oC, we know the increase in entropy of
the surroundings must be greater than the decrease in entropy of the water
molecules. The symbol for entropy change is DS.
The factors of entropy
change, temperature and enthalpy change have been combined to provide a
measure of spontaneity. This thermodynamic function, DG,
the Gibbs free energy change, not only predicts if the process is spontaneous,
but also tells us how much excess energy is available to do work.
If the process is not spontaneous, it tells us how much work is needed
to make the process happen.
If
DG
is negative, the process is spontaneous. If DG
is positive, the process is
not spontaneous.
Tables of standard
enthalpies of formation (DHfo),
free energies of formation (DGfo)
and entropy values (So) are listed in the appendix of the text.
Note that entropy values are absolute, so you must calculate entropy changes
using the following relationship:
DSo
= (sum of Soproducts) – (sum of Soreactants)
The following table summarizes
the relationship between temperature, enthalpy change and entropy change
and spontaneity.
enthalpy
change
|
entropy
change
|
spontaneity
|
(–) exothermic
|
(+) increase
|
spontaneous
at all T
|
(–) exothermic
|
(–) decrease
|
spontaneous
at lower T
|
(+) endothermic
|
(+) increase
|
spontaneous
at higher T
|
(+) endothermic
|
(–) decrease
|
never spontaneous
|
• Consider the reaction:
CaCO3(s) -->CaO(s) + CO2(g)
at 25oC. Calculate DGo
using the tables in the appendix of your textbook. Is the process
spontaneous at this temperature? Is it spontaneous at all temperatures?
If not, at what temperature does it become spontaneous?
The Relationship Between DG
and Keq
When a chemical
reaction occurs, the reaction proceeds until it reaches equilibrium.
At equilibrium, DG
= 0. The value of DG
changes during the course of the reaction as the concentrations (or pressures)
of products and reactants change. If initial conditions are not standard,
i.e., with all P=1 atm and all concentrations = 1.00M, or the temperature
is not 298K, you can calculate DG
using the following equation:
DG=DGo
+
RT lnQ where R = 8.314 J/mol-K, Q =
reaction quotient
|
Calculation of Equilibrium Constants
At
equilibrium, DG
= 0, and Q = K, so the above equation becomes:
DG
= 0 = DGo
+ RT lnK; or
Reactions with large
negative values of DGo
have
very large vales of K, showing that the driving force for the reaction
to proceed to the right is large. Reactions with positive values
of DGo
have small values of K, indicating the reaction is favored to the left.
• Calculate DHo,
DSo,
DGo
and K at 298K for: H2(g) + Cl2(g) <--> 2
HCl(g)
Copyright ©1998 Beverly
J. Volicer and Steven F. Tello, UMass Lowell. You may freely edit
these pages for use in a non-profit, educational setting. Please
include this copyright notice on all pages.