(Redirected from Gibbs Free Energy)
In
thermodynamics, the 'Gibbs free energy' (
IUPAC recommended name: 'Gibbs energy' or 'Gibbs function') is a
thermodynamic potential which measures the "useful" or process-initiating work obtainable from an
isothermal,
isobaric thermodynamic system. Technically, the Gibbs free energy is the ''maximum'' amount of non-expansion work which can be extracted from a
closed system, and this maximum can be attained only in a completely
reversible process. When a system changes from a well-defined initial state to a well-defined final state, the Gibbs free energy ''ΔG'' equals the work exchanged by the system with its surroundings, less the work of the pressure forces, during a reversible transformation of the system from the same initial state to the same final state.
[ A to Z of Thermodynamics, , Pierre, Perrot, Oxford University Press, 1998, ISBN 0-19-856552-6 ].
Gibbs energy is also the chemical potential that is minimised when a system reaches equilibrium at constant pressure and temperature. As such, it is a convenient criterion of spontaineity for processes with constant pressure and temperature.
The Gibbs free energy, originally called ''available energy'', was developed in the 1870s by the American mathematical physicist
Willard Gibbs. In 1873, in a foot-note, Gibbs defined what he called the “available energy” of a body as such:
The initial state of the body, according to Gibbs, is supposed to be such that "the body can be made to pass from it to states of
dissipated energy by
reversible processes." In his 1876
magnum opus ''
On the Equilibrium of Heterogeneous Substances'', a graphical analysis of multi-phase chemical systems, he engaged his thoughts on chemical
free energy in full.
Definitions

Willard Gibbs’ 1873 'available energy' (
free energy) graph, which shows a plane perpendicular to the axis of ''v'' (
volume) and passing through point A, which represents the initial state of the body. MN is the section of the surface of
dissipated energy. Q
ε and Q
η are sections of the planes ''η'' = 0 and ''ε'' = 0, and therefore parallel to the axes of ε (
internal energy) and η (
entropy) respectively. AD and AE are the energy and entropy of the body in its initial state, AB and AC its ''available energy'' (Gibbs free energy) and its ''capacity for entropy'' (the amount by which the entropy of the body can be increased without changing the energy of the body or increasing its volume) respectively.
The Gibbs free energy, is defined as:
:
which is the same as:
:
where:
★ U is the
internal energy (SI Units:
joules)
★ p is
pressure (SI Units:
pascals)
★ V is
volume (SI Units: m
3)
★ T is the
temperature (SI Units:
kelvins)
★ S is the
entropy (SI Units: joules per kelvin)
★ H is the
enthalpy (SI Units: joules)
The expression for the infinitesimal reversible change in the Gibbs free energy, for an
open system, subjected to the operation of external forces ''X
i'', which cause the external parameters of the system ''a
i'' to change by an amount ''da
i'', is given by:
:{|cellpadding="2" style="border:2px solid #ccccff"
|
|}
★
is the
chemical potential of the ''i''-th chemical component. (SI Units: joules per particle
[1] or joules per mol
)
★
is the number of particles (or number of moles) composing the ''i''-th chemical component.
In the infinitesimal expression, the term involving the chemical potential accounts for changes in Gibbs free energy resulting from an influx of particles. In other words, it holds for an
open system only. For a
closed system, this term may be dropped.
Any number of extra terms may be added, depending on the particular system being considered. Aside from
mechanical work, a system may in addition perform numerous other types of work. For example, in the infinitesimal expression, the contractile work energy associated with a thermodynamic system that is a contractile fiber which shortens by an amount -''dl'' under a force ''f'' would result in a term ''fdl'' being added. If a quantity of energy -''de'' is acquired by a system at an electrical potential Ψ, the electrical work associated with this is -Ψ''de'', which would be included in the infinitesimal expression. Other work terms are added on per system requirements.
[2]
Each quantity in the equations above can be divided by the amount of substance, measured in
moles, to form ''molar Gibbs free energy''. The Gibbs free energy is one of the most important thermodynamic functions for the characterization of a system. It is a factor in determining outcomes such as the
voltage of an
electrochemical cell, and the
equilibrium constant for a
reversible reaction. In isothermal, isobaric systems, Gibbs free energy can be thought of as a "dynamic" quantity, in that it is a representative measure of the competing effects of the enthalpic and entropic driving forces involved in a thermodynamic process.
The temperature dependence of the Gibbs energy for an
ideal gas is given by the
Gibbs-Helmholtz equation and its pressure dependence is given by:
:
if the volume is known rather than pressure then it becomes:
:
or more conveniently as its
chemical potential:
:
In non-ideal systems,
fugacity comes into play.
Overview
In a simple manner, with respect to
STP reacting systems, a general
rule of thumb is:
Hence, out of this general natural tendency, a quantitative measure as to how near or far a potential reaction is from this minimum is when the calculated energetics of the process indicate that the change in Gibbs free energy ΔG is negative. Essentially, this means that such a reaction will be favored and will release energy. The energy released equals the maximum amount of work that can be performed as a result of the chemical reaction. Conversely, if conditions indicated a positive ΔG, then energy--in the form of work--would have to be added to the reacting system to make the reaction go.
History
The quantity called "free energy" is essentially a more advanced and accurate replacement for the outdated term “
affinity”, which was used by chemists in previous years to describe the “force” that caused
chemical reactions. The term affinity, as used in chemical relation, dates back to at least the time of
Albertus Magnus in 1250.
From the 1998 textbook ''Modern Thermodynamics'' by Nobel Laureate and chemical engineering professor
Ilya Prigogine we find: "As motion was explained by the Newtonian concept of force, chemists wanted a similar concept of ‘driving force’ for chemical change? Why do chemical reactions occur, and why do they stop at certain points? Chemists called the ‘force’ that caused chemical reactions affinity, but it lacked a clear definition."
During the entire 18th century, the dominant view in regards to heat and light was that put forward by
Isaac Newton, called the “Newtonian hypothesis”, which stated that light and heat are forms of matter attracted or repelled by other forms of matter, with forces analogous to gravitation or to chemical affinity.
In the 19th century, the French chemist
Marcellin Berthelot and the Danish chemist
Julius Thomsen had attempted to quantify affinity using
heats of reaction. In 1875, after quantifying the heats of reaction for a large number of compounds, Berthelot proposed the “
principle of maximum work” in which all chemical changes occurring without intervention of outside energy tend toward the production of bodies or of a system of bodies which liberate
heat.
In addition to this, in 1780
Antoine Lavoisier and
Pierre-Simon Laplace laid the foundations of
thermochemistry by showing that the heat given out in a reaction is equal to the heat absorbed in the reverse reaction. They also investigated the
specific heat and
latent heat of a number of substances, and amounts of heat given out in combustion. Similarly, in 1840 Swiss chemist
Germain Hess formulated the principle that the evolution of heat in a reaction is the same whether the process is accomplished in one-step or in a number of stages. This is known as
Hess' law. With the advent of the
mechanical theory of heat in the early 19th century, Hess’s law came to be viewed as a consequence of the law of
conservation of energy.
Based on these and other ideas, Berthelot and Danish chemist
Julius Thomsen, as well as others, considered the heat given out in the formation of a compound as a measure of the affinity, or the work done by the chemical forces. This view, however, was not entirely correct. In 1847, the English physicist
James Joule showed that he could raise the temperature of water by turning a paddle wheel in it, thus showing that heat and mechanical work were equivalent or proportional to each other, i.e. approximately,
. This statement came to be known as the
mechanical equivalent of heat and was a precursory form of the
first law of thermodynamics.
By 1865 the German physicist
Rudolf Clausius had shown that this equivalence principle needed amendment. That is, one can use the heat derived from a
combustion reaction in a coal furnace to boil water, and use this heat to vaporize steam, and then use the enhanced high pressure energy of the vaporized steam to push a piston. Thus, we might naively reason that one can entirely convert the initial combustion heat of the chemical reaction into the work of pushing the piston. Clausius showed, however, that we need to take into account the work that the molecules of the working body, i.e. the water molecules in the cylinder, do on each other as they pass or transform from one step of or
state of the
engine cycle to the next, e.g. from (P1,V1) to (P2,V2). Clausius originally called this the “transformation content” of the body, and then later changed the name to
entropy. Thus, the heat used to transform the working body of molecules from one state to the next cannot be used to do external work, e.g. to push the piston. Clausius defined this ''transformation heat'' as ''dQ = TdS''.
In 1873,
Willard Gibbs published ''A Method of Geometrical Representation of the Thermodynamic Properties of Substances by Means of Surfaces'' in which he introduced the preliminary outline of the principles of his new equation able to predict or estimate the tendencies of various natural processes to ensue when bodies or systems are brought into contact. By studying the interactions of homogeneous substances in contact, i.e. bodies, being in composition part solid, part liquid, and part vapor, and by using a three-dimensional
volume-
entropy-
internal energy graph, Gibbs was able to determine three states of equilibrium, i.e. "necessarily stable", "neutral", and "unstable", and whether or not changes will ensue. In 1876, Gibbs built on this framework by introducing the concept of
chemical potential so to take into account chemical reactions and states of bodies which are chemically different from each other. In his own words, to summarize his results in 1873, Gibbs states:
{| class="messagebox"
|-
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If we wish to express in a single equation the necessary and sufficient condition of
thermodynamic equilibrium for a substance when surrounded by a medium of constant
pressure ''p'' and
temperature ''T'', this equation may be written:
:
when
refers to the variation produced by any variations in the
state of the parts of the body, and (when different parts of the body are in different states) in the proportion in which the body is divided between the different states. The condition of stable equilibrium is that the value of the expression in the parenthesis shall be a minimum.
|}
In this description, as used by Gibbs, ''ε'' refers to the
internal energy of the body, ''η'' refers to the
entropy of the body, and ''ν'' is the
volume of the body.
Hence, in 1882, after the introduction of these arguments by Clausius and Gibbs, the German scientist
Hermann von Helmholtz stated, in opposition to Berthelot and Thomas’ hypothesis that chemical affinity is a measure of the heat of reaction of chemical reaction as based on the principle of maximal work, that affinity is not the heat given out in the formation of a compound but rather it is the largest quantity of work which can be gained when the reaction is carried out in a reversible manner, e.g. electrical work in a reversible cell. The maximum work is thus regarded as the diminution of the free, or available, energy of the system (''Gibbs free energy'' ''G'' at ''T'' = constant, ''P'' = constant or ''Helmholtz free energy'' ''F'' at ''T'' = constant, ''V'' = constant), whilst the heat given out is usually a measure of the diminution of the total energy of the system (
Internal energy). Thus, ''G'' or ''F'' is the amount of energy “free” for work under the given conditions.
Up until this point, the general view had been such that: “all chemical reactions drive the system to a state of equilibrium in which the affinities of the reactions vanish”. Over the next 60 years, the term affinity came to be replaced with the term free energy. According to chemistry historian Henry Leicester, the influential 1923 textbook ''Thermodynamics and the Free Energy of Chemical Reactions'' by
Gilbert N. Lewis and
Merle Randall led to the replacement of the term “affinity” by the term “free energy” in much of the English-speaking world.
What does the term ‘free’ mean?
In the 18th and 19th centuries, the
theory of heat, i.e. that heat is a form of energy having relation to vibratory motion, was beginning to supplant both the
caloric theory, i.e. that heat is a fluid, and the
four element theory in which heat was the lightest of the four elements. Many textbooks and teaching articles during these centuries presented these theories side by side. Similarly, during these years,
heat was beginning to be distinguished into different classification categories, such as “free heat”, “combined heat”, “radiant heat”,
specific heat,
heat capacity, “absolute heat”, “latent caloric”, “free” or “perceptible” caloric (''calorique sensible''), among others.
In 1780, for example,
Laplace and
Lavoisier stated: “In general, one can change the first hypothesis into the second by changing the words ‘free heat, combined heat, and heat released’ into ‘
vis viva, loss of vis viva, and increase of vis viva.’” In this manner, the total mass of caloric in a body, called ''absolute heat'', was regarded as a mixture of two components; the free or perceptible caloric could affect a thermometer while the other component, the latent caloric, could not.
[3] The use of the words “latent heat” implied a similarity to latent heat in the more usual sense; it was regarded as chemically bound to the molecules of the body. In the
adiabatic compression of a gas the absolute heat remained constant by the observed rise of temperature, indicating that some latent caloric had become “free” or perceptible.
During the early 19th century, the concept of perceptible or free caloric began to be referred to as “free heat” or heat set free. In 1824, for example, the French physicist
Sadi Carnot, in his famous “Reflections on the Motive Power of Fire”, speaks of quantities of heat ‘absorbed or set free’ in different transformations. In 1882, the German physicist and physiologist
Hermann von Helmholtz coined the phrase ‘free energy’ for the expression ''E – TS'', in which the change in F (or G) determines the amount of
energy ‘free’ for
work under the given conditions.
[4]
Thus, in traditional use, the term “free” was attached to Gibbs free energy, i.e. for systems at constant pressure and temperature, or to Helmholtz free energy, i.e. for systems at constant volume and temperature, to mean ‘available in the form of useful work.’
With reference to the Gibbs free energy, we add the qualification that it is the energy free for non-volume work.
[5]
An increasing number of books and journal articles do not include the attachment “free”, referring to G as simply Gibbs energy (and likewise for the
Helmholtz energy). This is the result of a 1988
IUPAC meeting to set unified terminologies for the international scientific community, in which the adjective ‘free’ was supposedly banished.
[6] This standard, however, has not yet been universally adopted, and many published articles and books still include the descriptive ‘free’.
Derivation
To derive the Gibbs free energy equation for an
isolated system, let ''S''
tot be the total entropy of the
isolated system, that is, a system which cannot exchange heat or mass with its surroundings. According to the
second law of thermodynamics:
:
and if
then the process is reversible. The heat transfer ''Q'' vanishes for an adiabatic system. Any
adiabatic process that is also reversible is called an
isentropic process.
Now consider diabatic systems, having internal entropy ''S''
int. Such a system is thermally connected to its surroundings, which have entropy 'S
ext'. The entropy form of the second law does not apply directly to the diabatic system, it only applies to the closed system formed by both the system and its surroundings. Therefore a process is possible if
:
.
We will try to express the left side of this equation entirely in terms of state functions. ''ΔS
ext'' is defined as:
:
Temperature ''T'' is the same for two systems in thermal equilibrium. By the
zeroth law of thermodynamics, if a system is in thermal equilibrium with a second and a third system, the latter two are in equilibrium as well. Also, ''Δq
rev'' is heat transferred ''to'' the system, so ''-Δq
rev'' is heat transferred to the surroundings, and ''−ΔQ/T'' is entropy gained by the surroundings. We now have:
:
Multiply both sides by ''T'':
:
''ΔQ'' is heat transferred ''to'' the system; if the process is now assumed to be
isobaric, then ''Δq
p = ΔH'':
:
''ΔH'' is the enthalpy change of reaction (for a chemical reaction at constant pressure and temperature). Then
:
for a possible process. Let the change Δ''G'' in Gibbs free energy be defined as
:
''(eq.1)''
Notice that it is not defined in terms of any external state functions, such as Δ''S''
ext or Δ''S''
tot. Then the second law becomes, which also tells us about the spontaneity of the reaction:
:
'favored reaction' (Spontaneous)
:
Neither the forward nor the reverse reaction prevails
:
'disfavored reaction' (Nonspontaneous)
Gibbs free energy ''G'' itself is defined as
:
''(eq.2)''
but notice that to obtain equation (2) from equation (1) we must assume that ''T'' is constant. Thus, Gibbs free energy is most useful for thermochemical processes at constant temperature and pressure: both isothermal and isobaric. Such processes don't move on a ''P''-''T'' diagram, such as phase change of a pure substance, which takes place at the saturation pressure and temperature. Chemical reactions, however, do undergo changes in
chemical potential, which is a state function. Thus, thermodynamic processes are not confined to the two dimensional ''P''-''V'' diagram. There is a third dimension for ''n'', the quantity of gas. Naturally for the study of explosive chemicals, the processes are not necessarily isothermal and isobaric. For these studies,
Helmholtz free energy is used.
If a closed system (Δ''q
rev'' = 0) is at constant pressure (Δ''q
rev'' = Δ''H''), then
:
Therefore the Gibbs free energy of a closed system is:
:
and if
then this implies that
, back to where we started the derivation of Δ''G''.
Useful identities
:
for constant temperature
:
:
:
and rearranging gives
:
:
:
which relates the electrical potential of a reaction to the equilibrium coefficient for that reaction.
where
''ΔG'' = change in Gibbs free energy, ''ΔH'' = change in
enthalpy, ''T'' = absolute
temperature, ''ΔS'' = change in
entropy, ''R'' =
gas constant, ln =
natural logarithm, ''K'' =
equilibrium constant, ''Q'' =
reaction quotient, ''n'' = number of
electrons/
mole product, ''F'' =
Faraday constant (
coulombs/
mole), and ''ΔE'' =
electrical potential of the reaction. Moreover, we also have:
:
:
which relates the equilibrium constant with Gibbs free energy.
Standard change of formation
The 'standard Gibbs free energy of formation' of a compound is the change of Gibbs free energy that accompanies the formation of 1
mole of that substance from its component elements, at their
standard states (the most stable form of the element at 25 degrees
Celsius and 100
kilopascals). Its symbol is Δ''G''
fO.
All elements in their standard states (
oxygen gas,
graphite, etc.) have 0 standard Gibbs free energy change of formation, as there is no change involved.
:Δ''G'' = Δ''G''˚ + ''RT'' ln ''Q''
At equilibrium, Δ''G''=0 and ''Q'' = ''K'' so the equation becomes Δ''G''˚= −''RT'' ln ''K''
What is Life?
Main articles: Entropy and life
To a good approximation, one of the most oft-quoted references in
thermodynamics is
Erwin Schrödinger’s 1944 postulate that an organism keeps itself alive or aloof by feeding on negative entropy from its environment.
[7][8][9] From the famous chapter six “Order, Disorder and Entropy” of his book
What is Life?, Schrödinger asks: “what is the characteristic feature of life? and “when is a piece of matter said to be alive?” To answer these questions, Schrödinger turns to thermodynamics. Life, according to Schrödinger, avoids a decay to maximum entropy, or
thermodynamic equilibrium, which Schrödinger equates with death, by feeding on
negative entropy. Specifically, according to Schrödinger, an organism avoids decay by eating, drinking, breathing, and in the case of plants assimilating, a process called
metabolism.
In the past, Schrödinger states, this process would have been considered an exchange of matter or energy, such that organisms stay alive by exchanging energy. He uses the example of how caloric values are printed in certain menus in the United States or Germany, but states that these caloric energy exchange values are useless in trying to quantify life. He then asks “what then is that precious something contained in our food which keeps us from death?” The answer, according to Schrödinger, is that because according the
second law of thermodynamics an organism continually produces “positive entropy” it must continually draw in “negative entropy” from its environment to stay alive. Or, specifically “the essential thing in metabolism is that the organism succeeds in freeing itself from all the entropy it cannot help producing while alive.”
These suppositions, because they were intended for a lay audience, however, met with great opposition in the physics community. In later editions of his book, Schrödinger attached a note to chapter six explaining his use of the term “negative entropy”. He states “the remarks on ''negative entropy'' have met with doubt and opposition from physicist colleagues. Let me say first, that if I had been catering for them alone I should have let the discussion turn on 'free energy' instead. It is the more familiar notion in this context. But this highly technical term seemed too linguistically near to ''energy'' for making the average reader alive to the contrast between the two things.”
See also
★
Enthalpy
★
Entropy
★
Free energy
★
Helmholtz free energy
★
Thermodynamics
★
Willard Gibbs
References
1. Chemical Potential - IUPAC Gold Book
2. Nonequilibrium Thermodynamics in Biophysics, , A., Katchalsky, Harvard University Press, 1965, CCN 65-22045
3. Reflections on the Motive Power of Fire – and other Papers on the Second Law of Thermodynamics by E. Clapeyron and R. Carnot, , E., Mendoza, Dover Publications, Inc., 1988, ISBN 0-486-44641-7
4. Thermal Physics, , Ralph, Baierlein, Cambridge University Press, 2003, ISBN 0-521-65838-1
5. Methods of Thermodynamics, , Howard, Reiss, Dover Publications, 1965, ISBN 0-486-69445-3
6. Glossary of Atmospheric Chemistry Terms (Recommendations 1990), , , International Union of Pure and Applied Chemistry Commission on Atomspheric Chemistry, Pure Appl. Chem., 1990 Quantities, Units and Symbols in Physical Chemistry (2nd Edition), , , International Union of Pure and Applied Chemistry Commission on Physicochemical Symbols Terminology and Units, Blackwell Scientific Publications, , ISBN 0-632-03583-8 Glossary of Terms in Quantities and Units in Clinical Chemistry (IUPAC-IFCC Recommendations 1996), , , International Union of Pure and Applied Chemistry Commission on Quantities and Units in Clinical Chemistry, Pure Appl. Chem., 1996
7. Corning, P. (2002). “Thermoeconomics – Beyond the Second Law” – source: www.complexsystems.org
8. Margulis, Lynn. & Sagan, Dorion. (1995). ''What is Life?'' Berkeley: University of California Press.
9. Schneider, Eric. D. & Sagan, Dorion. (2005). ''Into the Cool – Energy Flow, Thermodynamics, and Life''. Chicago: University of Chicago Press.
External links
★
IUPAC definition (Gibbs energy)
★
Gibbs energy - Florida State University
★
Gibbs Free Energy - Eric Weissteins World of Physics
★
Gibbs Free Energy - Chemistry Gateway
★
Entropy and Gibbs Free Energy - www.2ndlaw.com
★
Gibbs Free Energy - Georgia State University
★
Gibbs Free Energy Java Applet - University of California, Berkeley
★
Gibbs Free Energy - Illinois State University