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Thermodynamics; Introduction

Thermodynamics describes heat and energy changes and chemical equilibria. It allows the prediction of equilibria positions, but NOT the rates of reaction or rates of change.


V The temperature scale and absolute zero

V The Zeroth Law of Thermodynamics

V The First Law of Thermodynamics
V The Second Law of Thermodynamics
V The Third Law of Thermodynamics

V Chemical potential
V Internal energy

V Heat capacity and specific heat

V Helmholtz free energy

V Power

V Boltzmann constant


'classical thermodynamics ...... is the only physical theory of universal                                                         content which I am convinced will never be overthrown'

Albert Einstein 


This webpage forms an elementary introduction to the terms and ideas of thermodynamics. Of great importance is that the laws of thermodynamics are  fundamental laws of the Universe and cannot be circumvented. Remember this, and one will not be misled by purveyors of 'too good to be true' ideas such as running cars on just water. Thermodynamics describes the energy content of systems at equilibrium and their transformations and is independent of the pathway chosen. Thermodynamics is not to be confused with kinetics, which describes the rate of change of processes and their mechanisms and depends on the pathway chosen. Biological systems (e.g., live people) are not in thermodynamic equilibrium as they are not static and are subject to the movement of matter and energy to and from other systems.


Heat is the amount of energy flowing from one body of matter to another spontaneously due to their temperature difference or by any means other than through work or the transfer of matter. Sensible heat is the energy required to change the temperature of a substance with no phase change. Latent heat is the energy required to cause phase changes between liquids, gases, and solids.


Temperature is a quantitative measure of hot and cold (K). Hotness is a body's ability to impart energy as heat to another colder body. It is a bulk property of matter (as are pressure, concentration, density, refractive index, and melting point) and should not be applied to single particles (e.g., molecules; a single particle may possess energy but does not have a temperature). Several temperature scales have been described, but the SI scale [1031] uses the kelvin.


Pressure is the force per unit area (Pa). It may be positive or negative and is not, in itself, directional. A positive pressure indicates that the system tends to expand whereas a negative pressure tends to contract.


Density of any substance is its mass (kg) divided by its volume (m3).


Energy is difficult to define precisely, being based on the Laws of thermodynamics. In different circumstances, it can be the capacity to do work, or the capacity to provide heat or radiation. There can be a conversion between different forms of energy, but energy cannot be created or destroyed. Energy has no natural zero states, so values are referred relative to (arbitrarily) chosen standard states.


Equilibrium is a state iwhen opposing forces, motions, energies, and materials are balanced and do not change with time.


Work is the energy associated with the action of a force.


Adiabatic processes occur without loss or gain of heat energy

Isobaric processes occur at constant pressure

Isothermal processes occur at a constant temperature

Isochoric processes occur at constant volume

Isenthalpic processes occur at a constant enthalpy

Isentropic processes are reversible adiabatic processes and occur at a constant entropy

Steady state processes occur without any change in the internal energy


Symbols. The symbol Δ (capital delta) means the change between the start and end states (see below). The symbol δ (small delta) means " a small change in". The symbol d (dee) is a differential (meaning "an infinitesimal change in"). The symbol ∂ (partial dee) is a mathematical symbol to denote a partial derivative, meaning the change in a function of several variables concerning one of those variables, under some constant conditions (usually the remaining conditions) as stated in the subscript(s). Thus, (∂H/∂T)P is the partial derivative of H with respect to T under conditions of constant P (see below).


dP=(dP/dT)v. dT+(dP/dV)T. dV                     (Pa)


Although advanced thermodynamics can appear daunting when first encountered, there are just three primary concepts: energy, entropy, and absolute temperature.

The temperature scale and absolute zero

Temperature is a numerical scale of relative hotness versus coldness. It is an intensive physical quantity for a material (does not depend on the amount of substance present in the system) and, when it increases, it indicates that the material has increased its energy content. The temperature may usually be considered as a measure for the average kinetic energy of particles. Absolute zero is the lowest limit for the thermodynamic temperature scale; nothing can be colder. It is defined as zero kelvin (0 K exactly; −273.15 °C , −459.67 °F) and cannot be reached (the thermodynamic temperature is often also called the absolute temperature, on the kelvin scale). The temperature scale did define the triple point of water (a triple point is a singular state with its own unique and invariant temperature and pressure) as +273.16 K precisely, and this set the kelvin temperature scale and the size of the kelvin; each kelvin increase within this scale increased the average kinetic energy by the same amount. However, the kelvin is now redefined in terms of the Boltzmann constant (kB = 1.380 649 ˣ 10−23 J ˣ K−1 exactly [2395]) e, the second, the meter and the kilogram. Withinpresently measurable bounds, the new exact kelvin is equal to the old experimental kelvin.


                                                One kelvin = 1.380 649 ˣ 10−23 J ˣ kB−1                            (exactly) [2395]


The closest approach to absolute zero achieved so far is about +0.000 000 000 038 K (38 pK).


Under special conditions, negative temperatures in which high-energy states are more occupied than low energy states are also possible [4191].

Internal energy

Thermodynamics introduces the term U, the INTERNAL ENERGY; the energy contained within the system, including its vibrational energy and bonding and interactional energy. This depends on the number of its accessible quantum states and its volume at a given pressure. The internal energy U is equivalent to the energy required to create the system.


ΔU is the change in the Internal energy; ΔU equals the heat added to a system less the work done by the system during a change to the system..

The Zeroth Law of Thermodynamics

The Zeroth Law of Thermodynamics states that two bodies in contact will come to the same temperature. It follows that If body A is in thermal equilibrium with two other bodies, B, and C, then B and C are in thermal equilibrium with one another.

The First Law of Thermodynamics

The First Law of Thermodynamics is the law of conservation of energy:

                                            'Energy can neither be created nor destroyed'


It can be expressed in everyday terms:


                                           You can't win. You can only break even

                                           You do not get anything for nothing
                                           There is no such thing as a free lunch

                                           The energy of the Universe is constant


It states that the energy in an isolated closed system is conserved, where energy is the capacity to do work. Heat energy can do work by (for example) changing a temperature or pressure. The isolated system may be a chemical reaction, a natural process, a cell, the earth, etc., If these systems are isolated, neither energy nor matter can enter or leave.


For an isolated closed system, any change in the internal energy ΔU is composed of the exchanged heat ΔQ and work ΔW done on or by the system,

ΔU = ΔQ + ΔW           (J)


and for a reversible process, the heat energy change ΔQ = TΔS and the work done ΔW = -PΔV ; (for non-spontaneous reactions , see the discussion at [3735]).



ΔU = TΔS - PΔV           (J)


Thermodynamics introduces the term H, the ENTHALPY; a measure of the heat content of the system (with units J ˣ mol−1). Enthalpy has no natural zero states, so values are referred relative to (arbitrarily) chosen standard states, with the standard states of materials being their enthalpy (heat) of formation (often at 298 K). The enthalpy H of a thermodynamic system is defined as the sum of its internal energy U and the work required to achieve its pressure and volume, P ˣ V by "making room" for the system:


H = U + PV           (J)

    ΔH is the CHANGE IN ENTHALPY; the heat lost or gained


In many biological systems, H = U as pressures and volumes, and their changes, are small.


Under constant-pressure conditions, the change in enthalpy is given


ΔH = ΔU + PΔV           (J)

By convention:

    ΔH is negative when heat is released by the system; such as in exothermic processes

    ΔH is positive when heat is absorbed by the system; such as in endothermic processes


In a sequence of reactions, the overall change in enthalpy is the sum of the enthalpies involved:


ΔHoverall = Σ ΔH

             A = B             ΔH1                     e.g.         C + ½O2       ->   CO            ΔH1 
             B = C             ΔH2                     e.g.         CO + ½O2    ->   CO2           ΔH2                 
sum      A+B = B+C    ΔH1 + ΔH2                            C + O2        ->   CO2        total ΔH = ΔH1 + ΔH2    


However, ΔH does not tell us if or how fast the process will go: e.g.,


            desk burning;       wood + O2     ->     CO2 + H2O        ΔH is negative, and heat is given out


We know that a desk will not spontaneously burn as the reaction is incredibly slow. It would burn if we created a fire'


            melting of ice;                   ice      ->    water                 ΔH is positive, and heat is absorbed


We know that ice will melt if the temperature is above 0 °C.


Therefore an enthalpy change, by itself, cannot predict the direction of a process.

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The Second Law of Thermodynamics

The Second Law of Thermodynamics tells us about the direction of processes; a hot coffee gets colder if it is let to stand—it never gets hotter. The Second Law of Thermodynamics states that the total disorder in an isolated system can only increase over time. All closed-cycle systems are irreversible.


It can be expressed in everyday terms:


                                           You can't take the cream out of the coffee

                                           If gambling, you can't even break even
                                           If gambling, the house always wins
                                           The Universe is becoming more chaotic

                                           Disorder within the Universe always increases with time
                                           A perpetual motion machine cannot exist or be built

                                           No process for converting heat into energy is 100 % efficient

                                           Heat spontaneously flows from a hot object to a cold one, not from cold to hot

                                           Isolated systems tend to move to their most probable state

                                           if you throw water into the sea, you cannot get the same water out again




Entropy explanation



The Second Law of Thermodynamics states that the total order in an isolated system cannot increase over time. The direction of both entropy change of the Universe and that of time are in the same direction and indicate that a time machine that goes back in time cannot be built, but one that goes forward can. If part of a system becomes more ordered, other parts must become even more disordered. In ideal cases, the amount of order may remain constant. There is only one way the entropy of a supposedly closed system can be decreased, and that is to transfer heat from the system (that is not closed).


The maximum fraction of the heat absorbed by an engine that can be converted into work is known as the efficiency of the heat engine and depends on the temperature of the hot and cold heat sinks, in kelvin.


% Efficiency = 100 ˣ (Thot- Tcold)/(Thot)


For example, if boiling and freezing water were the two extremes, the maximum efficiency would be 100 ˣ (373- 273)/373) = 26.8 % whereas if burning diesel oil (at 550 °C and room temperature at 25 °C were the extremes, then the maximum efficiency would be 100 ˣ (823- 298)/823) = 63.8 %. The % efficiency of a heat engine is always below one as zero kelvin can never be reached for the cold sink.


Thermodynamics introduces a term S that is the ENTROPY; a measure of disorder and chaos of the system (a measure of the number of microscopic states of a system with units of J ˣ mol−1 ˣ K−1). d An increase in disorder is an increase in entropy. More order means a decrease in entropy.  It is related to the probability that a system is in a particular state compared with all the possible states or arrangements. In a simple equiprobable system, it may be defined as


S0 = kB ˣ Ln(Ω)           (J ˣ K−1)


where kB is the Boltzmann constant (used in the definition of the kelvin), Ln() is the natural logarithm, and Ω is the probability-related number of configurations; Ω ≥ 1 with Ω -> 1 when T -> 0.

    ΔS is the CHANGE IN ENTROPY; the change in order or disorder


ΔS = Σ{SProduct } − Σ{SReagent}

ΔSoverall = Σ ΔS

By convention:  

    ΔS is positive when the disorder increases; the system is more chaotic and disorganized; e.g., a liquid turning into a gas.

    ΔS is negative when order increases; the system is more ordered and organized; e.g., a liquid turning into a crystalline



If there is no change in enthalpy but a process proceeds, there must be increased entropy; e.g., gases are mixing.

If two systems are combined, the final entropy is greater than the sum of the parts.


Entropy change, by itself, cannot predict the direction of a process


                                   2H2 + O2    ->      2H2O       clearly goes with negative entropy change as
     three molecules of a mixture     ->      two molecule of the same product


Thus, this is a process that proceeds to give a more ordered product. However, a large amount of heat (negative enthalpy change) increases the kinetic energy and disorder in the products and the surroundings.


Therefore an entropy change, by itself, cannot predict the direction of a process.

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The Third Law of Thermodynamics

The Third Law of Thermodynamics addresses the problem concerning the direction of a process. It follows from a combination of the First and Second Laws. The entropy of a system approaches a constant value as its temperature approaches absolute zero. The entropy of a perfect crystal at absolute zero is precisely equal to zero. The third law provides an absolute reference point for the entropy of a system at higher temperatures. If a system is a glass, a mixture, or an imperfect crystal, or internally disordered such as hexagonal ice, or still possessing quantum mechanical zero-point energy, or possesses other such properties, then its entropy is positive at absolute zero.


It can be expressed in everyday terms:


                                          You can't reach absolute zero

                                          If gambling, you can't stay out of the game
                                          The First and Second Laws cannot be got around


Thermodynamics introduces a term G is the GIBBS FREE ENERGY c (available energy, with units J ˣ mol−1); the ability to do work of the system at constant temperature and pressure. G is sometimes called, just, the 'free energy' or 'Gibbs energy'. b, g


G = U + PV - TS          (J)

G = H - TS                   (J)

    ΔG is the change in the Gibbs free energy. Gibbs free energy can do work at constant temperature and pressure. It determines the direction of a conceivable chemical or physical process and is zero when a system is at equilibrium at constant temperature and pressure.


In living systems (constant temperature and pressure);


ΔG = ΔH - T ΔS          (J)


    ΔG is the maximum work obtainable from a process
    ΔG is negative when the system can proceed; the process is exergonic, and

        there is a positive flow of energy from the system to the surroundings
    ΔG is positive when the system is unable to proceed; the process is endergonic, and
       it takes more energy to start the reaction than what you get out of it.

    ΔG is zero when the system is at equilibrium


Ice and water are in equilibrium at 0 °C and 101.325 kPa. When heat is absorbed from the surroundings, this ice melts. This is the enthalpy change, ΔH (6.00678 kJ ˣ mol−1). As this phase change takes place at 0 °C and 101.325 kPa, the ΔG is zero (ΔG = 0 kJ ˣ mol−1) and ΔH = +T ˣ ΔS, (ΔS = 21.9908 J ˣ mol−1 ˣ K−1). The material absorbs heat and its entropy increases when the ice melts.


Every reaction has a characteristic ΔG under defined conditions. Under standard conditions (usually 1 M reactants and products, 298.15 K (25 °C), 100 kPa), this is called the Standard Free Energy change and given the symbol, ΔG°.

Where the pH = 7, rather than [H+] = 1 M this is given the symbol, ΔG°'

For the reaction  A + B = C + D

Free energy equation

where R = gas constant (8.31 J ˣ mol−1 ˣ K−1), T is the temperature (in kelvin), and Ln is the natural logarithm;


Given ΔG is zero when the system is in equilibrium, therefore

ΔG°'= - RTLn (Keq°')         (J)  


Thus , if Keq°' =1 then ΔG°' = 0, if Keq°' =10 then ΔG°' = -5.7 kJ ˣ mol−1, and if Keq°' = 0.1 then ΔG°' = +5.7 kJ ˣ mol,


In a sequence of reactions:

ΔGoverall = Σ ΔG               (J)         



                        A + B = C + D           ΔG1
                        C + E = F                  ΔG2
sum          A + B + E = D + F            ΔG = ΔG1 + ΔG2


So long as the overall ΔG is negative, the reaction will go from left to right; A + B + E -> D + F

As an example;

                                                                                                                    ΔG°', kJ ˣ mol−1
                          Glucose + phosphate = Glucose-6-phosphate + H2O             +13.8
                                         ATP + H2O = ADP + phosphate                              - 30.5
                                    Glucose + ATP = ADP + Glucose-6-phosphate             - 16.7


Under standard conditions (at pH 7), the process directions are determined by ΔG°';

Glucose-6-phosphate + H2O -> Glucose + phosphate

ATP + H2O -> ADP + phosphate  

Glucose + ATP -> ADP + Glucose-6-phosphate  


The ATP hydrolysis pulls the phosphorylation of the glucose.


ΔG depends on the concentration of the reactants and products as well as the temperature and ΔG°'.


Process direction depends on ΔG


The fundamental equation of thermodynamics is


ΔG = V ˣ ΔP - S ˣ ΔT + ΔnA ˣ μA + ΔnB ˣ μB + ΔnC ˣ μC +. . . . . . . .

ΔG = V ˣ ΔP - S ˣ ΔT + Σi Δni ˣ μi                                                        


At a surface, a further term must be added to the right-hand side; +γΔA where γ (J ˣ m−2) and A (m2) are the surface tension and surface area, respectively.


Four Maxwell relations involve the second derivatives of each of the four thermodynamic potentials, U, H, F, and G.


partial dee T/partial dee V
partial dee T/partial dee P
partial dee S/partial dee V
partial dee S/partial dee P


partials relationship

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The chemical potential of substance A


The chemical potential of substance A
Chemical potential

The chemical potential (μ) is the energy of a material (e.g., a number of molecules) that changes with each of that number of particles. The (chemical) potential is a term established by Willard Gibbs e and is the same as the molar Gibbs free energy of formation, ΔGf, for a pure substance, with units of energy (J ˣ mol−1). In a multiphase system (such as many foods) at equilibrium, the chemical potential μi of individual components (i) is the same in all phases.


For materials in a mixture, the chemical potential (μ) is the partial molar Gibbs free energy when both temperature, pressure, and other materials present are held constant

chemical potential is thepartial molar Gibbs energy          (J ˣ mol−1)

where the substance changing is A, with nA representing the number of A molecules, and nB represents the number of molecules of all other materials present. Also,


                           dG equals the maximum work            (J ˣ mol−1)


As dG equals the maximum work that can be performed at constant P and T, this sum of chemical potentials equals the additional (non-expansion) work that can arise from changing the composition of the system. Also related to this, it may measure the tendency to diffuse.


It follows that,


dmui/dP=Vi       and         dmui/dT=Si

and                                                             dμ = -Sm dT + Vm dP                                           (The Gibbs equation)


where Sm and Vm are the molar entropy and volume of the substance.


The total Gibbs free energy of a mixture of A and B is


G = nA ˣ μA + nB ˣ μB          (J)         


The chemical potential (μ) is related to its activity (a) by


μ = μ0 + RT ln(a)           (J ˣ mol−1)


where μ0 is a constant (the standard state), given values for T and P. The activity is a measure of the "effective concentration" of a material in a mixture. It is without units as it is always divided by the respective standard activity in the same units (e.g., a single concentration unit; often = 1 mol ˣ L−1). a


The chemical potential of an aqueous solution is given by


μ = μ0 + RT ln(aw)           (J ˣ mol−1)

μ = μ0 + RT ln(xw)           (J ˣ mol−1)


where xw is the mole fraction of the ‘free’ water, aw is the water activity, and μ0 is the chemical potential of the pure water. For a graph of μ versus aw see elsewhere. There is a table of chemical potentials compiled by Dr. Georg Job.


If material is distributed between two phases in equilibrium;

μA - μB = RT ln(aA/aB)                                 (J ˣ mol−1)


The molar chemical potential of water in an electrolyte solution (molality m; activity a),H2O(T, P, m), can be written as


μH2O(T, P, m) = μH2O(T, P, 0) + RT ln {aH2O(T, P, m)}           (J ˣ mol−1)

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Heat capacity and specific heat

The heat capacity (C) is the ratio of the measurable heat added (Q) or subtracted to an object to the resulting temperature change




with units J ˣ K−1, and in the limit as ΔT tends to zero. The specific heat (mass-specific heat capacity) is the heat capacity per unit mass of a material. CP and CV are the heat capacities at constant pressure (isobaric, CP = (∂U/∂T)P and constant volume (isochoric, CV = (∂U/∂T)V), respectively. The specific heat is the amount of heat needed to raise the temperature of one kilogram of mass by 1 kelvin. The molar heat capacity is the heat capacity per mole of a pure substance, and the specific heat capacity is the heat capacity per kg of a pure substance.


As                 H = U + PV

δQ = δU + PδV         (J)         


CP = (∂H/∂T)P           (J ˣ K−1)


CV = (∂U/∂T)V           (J ˣ K−1)


where U is the internal energy and H is the system enthalpy.


The full expressions are


CP = (∂H/∂T)P= T(∂S/∂T)P = <(ΔS)2>TP /(kBN) = <(ΔH)2>TPN /(kBT2) = (∂U/∂T)P + PVαV 


 CV = (∂U/∂T)V= T(∂S/∂T)V = (∂H/∂T)V - PVαP = CP - TVαP2/βT




CP/CV = βT/βS > 1


where kB, P, T, N, V, H, S, αV, αP, βT, and βS are the Boltzmann constant, pressure (Pa), temperature (K), number of molecules, specific volume (V = 1/density; m3 mol−1), enthalpy, entropy, isobaric cubic expansion coefficient (αV=(∂V/∂T)P/V; K−1), relative pressure coefficient (αP=(∂P/∂T)V/P; K−1), isothermal compressibility (βT=-(∂V/∂P)T/V; Pa−1), and adiabatic compressibility (βS=-(∂V/∂P)S/V; Pa−1), respectively; the <> brackets indicate the fluctuations in the values about their mean values. (also see [1481]). Thus, the heat capacity measures the entropy fluctuation ΔS of N molecules at constant temperature and pressure. The isothermal compressibility measures the fluctuations ΔV of the mean volume V occupied by a given number of molecules. The expansion coefficient is related to the correlations between the entropy and volume fluctuations. In contrast to most other liquids, in which entropy and volume fluctuations are positively correlated, ΔS and ΔV are anti-correlated in water below 4 °C, with a decline in volume fluctuations associated with an enhancement of entropy fluctuations.


For an ideal gas                                                  CP − CV = nR


where n is the number of moles of the gas and R is the Gas constant.

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Power is the amount of energy used, or work done, per unit time; with units, one watt = 1 J ˣ s−1. Power may also be expressed as a force times its velocity. = N ˣ m ˣ s−1 = kg ˣ m ˣ s−2 ˣ m ˣ s−1 = kg ˣ m2 ˣ s−3 = J ˣ s−1 = watt. When power is used over a specified time, the units are of energy used (or work done) such as Kilowatt-hours (kWh) = 3.6 MJ (exactly).

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a Note: One is only allowed to take the logarithm of a dimensionless positive number, not of a physical quantity with dimensions (like m, s, L, mol, kg, V, etc.,). Thus when taking logarithms, a ≡ a/a0 where a0 is standardized as one unit in the dimensions of a. In the same manner, you cannot use trigonometric nor exponential functions of physical quantities with dimensions. [Back]


b Helmholtz free energy (A). Under conditions of where no pressure/volume work can be extracted (A ≤ G) but where pressure may change (a closed thermodynamic system, e.g., in closed explosions), G = U + PV - TS becomes.


A = U - TS                              (J)  


where A is the Helmholtz free energy c (often given in Physics textbooks as F), and as for reversible reactions,


dU=TdS - pdV        and        d(TS) =TdS +SdT

dA = -SdT - pdV



c It has been recommended that 'Gibbs free energy' and 'Helmholtz free energy' be known simply as 'Gibbs energy' [IUPAC] and 'Helmholtz energy' [IUPAC] but, at present, there is a scientific consensus to keep the historical terms. [Back]


d Entropy (S). There are several distinct (but equally applicable) "definitions" of "entropy" which results in a bit of a muddle. e.g., in equilibrium thermodynamics, entropy is a measure of a system's thermal energy per unit temperature that is unavailable for doing useful work (dispersed energy). There is some dispute over associating 'entropy' with 'disorder', F. Jeppsson, J. Haglund and H. Strömdahl, Exploiting language in teaching of entropy, Journal of Baltic Science Education, 10 (2011) 27-35. There is also confusion over associating 'static' entropy (at thermodynamic equilibrium), with dynamic entropy 'changes in entropy' during a process, i.e., 'the arrow of time', and kinetics; A. Ben-Naim, Entropy and time, Entropy, 22 (2020) 430. The present text rather likes this latter association as an aid to understanding the direction of processes.


'Changes in entropy can some times be interpreted in terms of changes in disorder' A. Ben-Naim, Entropy: Order or information, Journal of Chemical Education, 88 (2011) 594-596. [Back]


e Boltzmann constant. The Boltzmann constant (kB) s the proportionality constant relating the meam kinetic energy of particles in a gas with their thermodynamic temperature. It has the dimensions of entropy. In SI units, kB = 1.380 649 ˣ 10−23 J ˣ K−1 exactly. If expressed in terms of moles of material, one gets the gas constant R (R = kB ˣ NA = 8.314 J ˣ mol−1 ˣ K−1.


particle kinetic energy = ½m<v2> = 32kBT         (J)  


kB = m<v2>/3T                                          (J ˣ K−1)  


where < > indicates 'the mean value of'. These two equations hold for significant quantities of particles and not for single particles (it is meaningless to talk about the temperature of a single particle by itself). The value 3 in these equations derives from the 'three degrees of freedom' of the three spatial directions (x, y, z).


The Boltzmann constant is named after the Austrian physicist Ludwig Eduard Boltzmann (1844 - 1906) , also known for the definition of entropy.



f Willard Gibbs (1839-1903) introduced the term 'potential' in 1875 (J. W. Gibbs, On the equilibrium of heterogeneous substancesTransactions of the Connecticut Academy of Arts and Sciences3 (1875-1876, 1877-1878) 108-248, 343-524). [Back]


g Given an equation of state (EOS) 3-dimensional graph connecting the Gibbs energy of liquid water over Temperature and Pressure, the following properties can be calculated (IAPWS), density, specific entropy, specific isobaric heat capacity, specific enthalpy, specific internal energy, specific Helmholtz energy, thermal expansion coefficient, isentropic temperature-pressure coefficient, isothermal compressibility, isentropic compressibility, and speed of sound. [Back]


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