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thermodynamics Thermodynamics is a branch of physics that deals with heat, work, and temperature, and their relation to energy, entropy, and the physical properties of matter and radiation. The behavior of these quantities is governed by the four laws ...
, the fundamental thermodynamic relation are four fundamental equations which demonstrate how four important thermodynamic quantities depend on variables that can be controlled and measured experimentally. Thus, they are essentially equations of state, and using the fundamental equations, experimental data can be used to determine sought-after quantities like ''G'' or ''H''. The relation is generally expressed as a microscopic change in
internal energy The internal energy of a thermodynamic system is the total energy contained within it. It is the energy necessary to create or prepare the system in its given internal state, and includes the contributions of potential energy and internal kinet ...
in terms of microscopic changes in
entropy Entropy is a scientific concept, as well as a measurable physical property, that is most commonly associated with a state of disorder, randomness, or uncertainty. The term and the concept are used in diverse fields, from classical thermodyna ...
, and
volume Volume is a measure of occupied three-dimensional space. It is often quantified numerically using SI derived units (such as the cubic metre and litre) or by various imperial or US customary units (such as the gallon, quart, cubic inch). ...
for a
closed system A closed system is a natural physical system that does not allow transfer of matter in or out of the system, although — in contexts such as physics, chemistry or engineering — the transfer of energy (''e.g.'' as work or heat) is allowed. In ...
in thermal equilibrium in the following way. :\mathrmU= T\,\mathrmS - P\,\mathrmV\, Here, ''U'' is
internal energy The internal energy of a thermodynamic system is the total energy contained within it. It is the energy necessary to create or prepare the system in its given internal state, and includes the contributions of potential energy and internal kinet ...
, ''T'' is
absolute temperature Thermodynamic temperature is a quantity defined in thermodynamics as distinct from kinetic theory or statistical mechanics. Historically, thermodynamic temperature was defined by Kelvin in terms of a macroscopic relation between thermodynamic ...
, ''S'' is
entropy Entropy is a scientific concept, as well as a measurable physical property, that is most commonly associated with a state of disorder, randomness, or uncertainty. The term and the concept are used in diverse fields, from classical thermodyna ...
, ''P'' is
pressure Pressure (symbol: ''p'' or ''P'') is the force applied perpendicular to the surface of an object per unit area over which that force is distributed. Gauge pressure (also spelled ''gage'' pressure)The preferred spelling varies by country a ...
, and ''V'' is
volume Volume is a measure of occupied three-dimensional space. It is often quantified numerically using SI derived units (such as the cubic metre and litre) or by various imperial or US customary units (such as the gallon, quart, cubic inch). ...
. This is only one expression of the fundamental thermodynamic relation. It may be expressed in other ways, using different variables (e.g. using thermodynamic potentials). For example, the fundamental relation may be expressed in terms of the
enthalpy Enthalpy , a property of a thermodynamic system, is the sum of the system's internal energy and the product of its pressure and volume. It is a state function used in many measurements in chemical, biological, and physical systems at a constant ...
as : \mathrmH = T\,\mathrmS + V\,\mathrmP\, in terms of the
Helmholtz free energy In thermodynamics, the Helmholtz free energy (or Helmholtz energy) is a thermodynamic potential that measures the useful work obtainable from a closed thermodynamic system at a constant temperature (isothermal). The change in the Helmholtz en ...
(''F'') as :\mathrmF= -S\,\mathrmT - P\,\mathrmV\, and in terms of the
Gibbs free energy In thermodynamics, the Gibbs free energy (or Gibbs energy; symbol G) is a thermodynamic potential that can be used to calculate the maximum amount of work that may be performed by a thermodynamically closed system at constant temperature an ...
(''G'') as :\mathrmG= -S\,\mathrmT + V\,\mathrmP\,.


The first and second laws of thermodynamics

The
first law of thermodynamics The first law of thermodynamics is a formulation of the law of conservation of energy, adapted for thermodynamic processes. It distinguishes in principle two forms of energy transfer, heat and thermodynamic work for a system of a constant am ...
states that: :\mathrmU = \delta Q - \delta W\, where \delta Q and \delta W are infinitesimal amounts of heat supplied to the system by its surroundings and work done by the system on its surroundings, respectively. According to the
second law of thermodynamics The second law of thermodynamics is a physical law based on universal experience concerning heat and energy interconversions. One simple statement of the law is that heat always moves from hotter objects to colder objects (or "downhill"), unle ...
we have for a reversible process: :\mathrmS = \frac\, Hence: :\delta Q = T\,\mathrmS\, By substituting this into the first law, we have: :\mathrmU = T\,\mathrmS - \delta W\, Letting \delta W be reversible pressure-volume work done by the system on its surroundings, :\delta W\ = P\mathrmV\, we have: :\mathrmU = T\,\mathrmS - P\,\mathrmV\, This equation has been derived in the case of reversible changes. However, since ''U'', ''S'', and ''V'' are thermodynamic
state functions In the thermodynamics of equilibrium, a state function, function of state, or point function for a thermodynamic system is a mathematical function relating several state variables or state quantities (that describe equilibrium states of a system ...
, the above relation holds also for non-reversible changes. If the composition, i.e. the amounts n_ of the chemical components, in a system of uniform temperature and pressure can also change, e.g. due to a chemical reaction, the fundamental thermodynamic relation generalizes to: :\mathrmU = T\,\mathrmS - P\,\mathrmV\ + \sum_\mu_\,\mathrmn_\, The \mu_ are the
chemical potential In thermodynamics, the chemical potential of a species is the energy that can be absorbed or released due to a change of the particle number of the given species, e.g. in a chemical reaction or phase transition. The chemical potential of a speci ...
s corresponding to particles of type i. If the system has more external parameters than just the volume that can change, the fundamental thermodynamic relation generalizes to :\mathrmU = T\,\mathrmS + \sum_X_\,\mathrmx_ + \sum_\mu_\,\mathrmn_\, Here the X_ are the
generalized forces Generalized forces find use in Lagrangian mechanics, where they play a role conjugate to generalized coordinates. They are obtained from the applied forces, Fi, i=1,..., n, acting on a system that has its configuration defined in terms of generaliz ...
corresponding to the external parameters x_. (The negative sign used with pressure is unusual and arises because pressure represents a compressive stress that tends to decrease volume. Other generalized forces tend to increase their conjugate displacements.)


Relationship to statistical mechanics

The fundamental thermodynamic relation and statistical mechanical principles can be derived from one another.


Derivation from statistical mechanical principles

The above derivation uses the first and second laws of thermodynamics. The first law of thermodynamics is essentially a definition of
heat In thermodynamics, heat is defined as the form of energy crossing the boundary of a thermodynamic system by virtue of a temperature difference across the boundary. A thermodynamic system does not ''contain'' heat. Nevertheless, the term is ...
, i.e. heat is the change in the internal energy of a system that is not caused by a change of the external parameters of the system. However, the second law of thermodynamics is not a defining relation for the entropy. The fundamental definition of entropy of an isolated system containing an amount of energy E is: :S = k \log\left Omega\left(E\right)\right, where \Omega\left(E\right) is the number of quantum states in a small interval between E and E +\delta E. Here \delta E is a macroscopically small energy interval that is kept fixed. Strictly speaking this means that the entropy depends on the choice of \delta E. However, in the thermodynamic limit (i.e. in the limit of infinitely large system size), the specific entropy (entropy per unit volume or per unit mass) does not depend on \delta E. The entropy is thus a measure of the uncertainty about exactly which quantum state the system is in, given that we know its energy to be in some interval of size \delta E. Deriving the fundamental thermodynamic relation from first principles thus amounts to proving that the above definition of entropy implies that for reversible processes we have: :dS =\frac The fundamental assumption of
statistical mechanics In physics, statistical mechanics is a mathematical framework that applies statistical methods and probability theory to large assemblies of microscopic entities. It does not assume or postulate any natural laws, but explains the macroscopic b ...
is that all the \Omega\left(E\right) states at a particular energy are equally likely. This allows us to extract all the thermodynamical quantities of interest. The temperature is defined as: : \frac\equiv\beta\equiv\frac\, This definition can be derived from the
microcanonical ensemble In statistical mechanics, the microcanonical ensemble is a statistical ensemble that represents the possible states of a mechanical system whose total energy is exactly specified. The system is assumed to be isolated in the sense that it canno ...
, which is a system of a constant number of particles, a constant volume and that does not exchange energy with its environment. Suppose that the system has some external parameter, x, that can be changed. In general, the energy eigenstates of the system will depend on ''x''. According to the adiabatic theorem of quantum mechanics, in the limit of an infinitely slow change of the system's Hamiltonian, the system will stay in the same energy eigenstate and thus change its energy according to the change in energy of the energy eigenstate it is in. The generalized force, ''X'', corresponding to the external parameter ''x'' is defined such that X dx is the work performed by the system if ''x'' is increased by an amount ''dx''. E.g., if ''x'' is the volume, then ''X'' is the pressure. The generalized force for a system known to be in energy eigenstate E_r is given by: :X = -\frac Since the system can be in any energy eigenstate within an interval of \delta E, we define the generalized force for the system as the expectation value of the above expression: :X = -\left\langle\frac\right\rangle\, To evaluate the average, we partition the \Omega(E) energy eigenstates by counting how many of them have a value for \frac within a range between Y and Y + \delta Y. Calling this number \Omega_\left(E\right), we have: :\Omega(E)=\sum_Y\Omega_Y(E)\, The average defining the generalized force can now be written: :X = -\frac\sum_Y Y\Omega_Y(E)\, We can relate this to the derivative of the entropy with respect to x at constant energy E as follows. Suppose we change ''x'' to ''x'' + ''dx''. Then \Omega\left(E\right) will change because the energy eigenstates depend on x, causing energy eigenstates to move into or out of the range between E and E+\delta E. Let's focus again on the energy eigenstates for which \frac lies within the range between Y and Y + \delta Y. Since these energy eigenstates increase in energy by ''Y'' ''dx'', all such energy eigenstates that are in the interval ranging from ''E'' − ''Y'' ''dx'' to ''E'' move from below ''E'' to above ''E''. There are :N_Y (E)=\frac Y\, dx such energy eigenstates. If Y dx\leq\delta E, all these energy eigenstates will move into the range between E and E+\delta E and contribute to an increase in \Omega. The number of energy eigenstates that move from below E+\delta E to above E+\delta E is, of course, given by N_\left(E+\delta E\right). The difference :N_Y(E) - N_Y(E+\delta E)\, is thus the net contribution to the increase in \Omega. Note that if Y dx is larger than \delta E there will be energy eigenstates that move from below E to above E+\delta E. They are counted in both N_Y (E) and N_Y(E+\delta E), therefore the above expression is also valid in that case. Expressing the above expression as a derivative with respect to E and summing over Y yields the expression: :\left(\frac\right)_E = -\sum_Y Y\left(\frac\right)_x= \left(\frac\right)_x\, The logarithmic derivative of \Omega with respect to ''x'' is thus given by: :\left(\frac\right)_E = \beta X +\left(\frac \right)_x\, The first term is intensive, i.e. it does not scale with system size. In contrast, the last term scales as the inverse system size and thus vanishes in the thermodynamic limit. We have thus found that: :\left(\frac\right)_ = \frac\, Combining this with :\left(\frac\right)_ = \frac\, Gives: :dS = \left(\frac\right)_x \, dE+\left(\frac\right)_E \, dx = \frac + \frac \, dx\, which we can write as: :dE = T \, dS - X \, dx


Derivation of statistical mechanical principles from the fundamental thermodynamic relation

It has been shown that the fundamental thermodynamic relation together with the following three postulates is sufficient to build the theory of statistical mechanics without the equal a priori probability postulate. For example, in order to derive the
Boltzmann distribution In statistical mechanics and mathematics, a Boltzmann distribution (also called Gibbs distribution Translated by J.B. Sykes and M.J. Kearsley. See section 28) is a probability distribution or probability measure that gives the probability th ...
, we assume the probability density of microstate satisfies \Pr(i)\propto f(E_i,T). The normalization factor (partition function) is therefore : Z = \sum_i f(E_i, T). The entropy is therefore given by : S = k_B \sum_i \frac \log\left(\frac\right). If we change the temperature by while keeping the volume of the system constant, the change of entropy satisfies : dS=\left(\frac\right)_V dT where : \left(\frac\right)_V = -k_B \sum_i\frac = -k_B \sum_i \frac \left(\frac\right)\cdot\log f(E_i, T) Considering that : \left\langle E\right\rangle = \sum_i \frac\cdot E_i we have : d\left\langle E\right\rangle = \sum_i \frac \left(\frac\right)\cdot E_i \cdot dT From the fundamental thermodynamic relation, we have : -\frac+\frac + \fracdV = 0 Since we kept constant when perturbing , we have dV=0. Combining the equations above, we have : \sum_i \frac \left(\frac\right)\cdot \left log f(E_i, T)+\frac\rightcdot dT = 0 Physics laws should be universal, i.e., the above equation must hold for arbitrary systems, and the only way for this to happen is : \log f(E_i, T)+\frac = 0 That is : f(E_i, T)=\exp\left(-\frac\right). It has been shown that the third postulate in the above formalism can be replaced by the following: However, the mathematical derivation will be much more complicated.


References

{{Reflist


External links


The Fundamental Thermodynamic Relation
Thermodynamics Statistical mechanics Thermodynamic equations