Thursday, July 12, 2018

thermodynamics - What is the difference between ∆G and ∆G°?



In Brady's Molecular Nature of Matter, I read that ΔrG is ΔrG at 25 C. But later, it gives a value for ΔrG at another temperature.


What is the meaning of ΔrG? Specifically:



  1. Does it only refer to 25 C?

  2. Does the ΔrG=ΔrHTΔrS equation only refer to T=298 K?

  3. If at 25 C, a system that has reached equilibrium (ΔrG=0), and thus

    • Q=K

    • ΔrG=0

    • ΔrG=0=RTlnK


    • RTlnK=0

    • lnK=0

    • K=1




But doesn't K vary from reaction to reaction? It shouldn't always equal 1, should it?



Answer







  1. Does it need to be at 25 C?



No. ΔrG can be defined at any temperature you wish to define it at, since the standard state does not prescribe a particular temperature. If you change the temperature, ΔrG will change.




  1. Does ΔrG=ΔrHTΔrS always use T=298 K?




No. You use whatever temperature you are running your reaction at.




  1. (...maths...)



Yes, at equilibrium, ΔrG=0 and Q=K.


However, everything after the first bullet point is wrong. You cannot conclude that ΔrG=0, nor can you conclude that K=1. The equation ΔrG=RTlnK does not analogously translate into ΔrG=RTlnQ! The accurate relation is:


ΔrG=ΔrG+RTlnQ


Setting Q=K and ΔrG=0 in this equation does not tell you anything about the value of K. In fact, if you try doing it, all you will find out is that ΔrG=RTlnK - no surprises there!






Any book that writes that ΔrG is the "special case" of ΔrG at T=298 K is wrong.


The Gibbs free energy of a system is defined as follows:


G=HTS


Under constant temperature and pressure (from now on, I will just assume constant T and p without stating it), all systems will seek to minimise their Gibbs free energy. Equilibrium is reached when G is minimised. When G is at a minimum, any infinitesimal change in G, i.e. dG, will be 0. Therefore, this is equivalent to saying that the condition for chemical equilibrium is dG=0.


Clearly, we need a way to relate this quantity dG to the actual reactants and products that are in the system. This can be done by using the Maxwell relation (see any physical chemistry text for details):


dG=VdpSdT+iμidni


Under constant T and p, dp=dT=0 and therefore


dG=iμidni



where μi is the chemical potential of species i, defined as a partial derivative:


μi=(Gni)nji


So, we now have a refined condition for equilibrium:


dG=iμidni=0


We can go further by noting that the values of dni for different components i, j, etc. are not unrelated. For example, if we have a reaction i+jk, then for each mole of i that is consumed, we must also use up one mole of j; this means that dni=dnj.


This can be formalised using the idea of a stoichiometric coefficient νi, which is defined to be positive for products and negative for reactants. For example, in the reaction


3HX2+NX22NHX3


we have νHX2=3, νNX2=1, and νNHX3=2.


By stoichiometry, if 1.5 mol of HX2 is consumed, then 1 mol of NHX3 has to be produced. We could write ΔnHX2=1.5 mol and ΔnNHX3=1 mol. These quantities are proportional to their stoichiometric coefficients:


ΔnHX2νHX2=1.5 mol3=0.5 mol=1 mol2=ΔnNHX3νNHX3



The quantity 0.5 mol is a constant for all chemical species J that participate in the reaction, and it is called the "extent of reaction" and denoted Δξ (that is the Greek letter xi). If the reaction is going forward, then Δξ is positive, and if the reaction is going backwards, then Δξ is negative. If we generalise the above result, we can write


Δξ=Δniνi


and if we make Δni smaller and smaller until it becomes an infinitesimal, then:


dξ=dniνidni=νidξ


If we go back to our condition for equilibrium, we can substitute in the above to get:


dG=iμiνidξ=0


Now, dξ is no longer dependent on i, since we have established already that Δξ (and by extension dξ) is a constant for all chemical species. So, we can "divide through" by it to get:


ΔrGdGdξ=iμiνi=0


where ΔrG is defined to be dG/dξ.


Note that ΔrG is an intensive property and has units of kJ mol1, since dξ has units of mol. This ensures that the units we use are consistent: since we know that ΔrG=ΔrG+RTlnQ, ΔrG must have the same units as RT.



How do we interpret the physical significance of ΔrG, or in other words, what does it even mean? There are two ways, each based on a different mathematical expression.



  1. We have ΔrG=νiμi. This means that ΔrG is simply the difference between the chemical potentials of the products and the reactants, weighted by their stoichiometric coefficients. For the reaction 3HX2+NX22NHX3, we have:


ΔrG=iμiνi=2μNHX33μHX2μNX2



  1. We have ΔrG=dG/dξ. This means that it is the slope of a curve of G against ξ:


Graph of G against xi


Note that up to this point, we have not stipulated any particular temperature, pressure, amounts of species present, or any conditions whatsoever. We have only said that the temperature and pressure must be constant.



It is important to realise that ΔrG is a well-defined quantity at all T, all p, and all possible values of ni,nj,! The shape of the curve will change when you vary the conditions. However, no matter what the curve looks like, it is always possible to find its gradient (=ΔrG) at a particular point.




What exactly, then, is ΔG? It is just a special case of ΔG, where all the reactants and products are prepared in a standard state. According to IUPAC, the standard state is defined as:



  • For a gas: pure ideal gas when the pressure p is equal to the standard pressure p.

  • For a liquid or solid: pure liquid or solid at p=p

  • For a solution: ideal solution when the concentration c is equal to the standard concentration c.


p is most commonly taken to be 1 bar, although older texts may use the value 1 atm=1.01325 bar. Since 1982, IUPAC has recommended the value 1 bar for the standard pressure (Pure Appl. Chem. 1982, 54 (6), 1239–1250; DOI: 10.1351/pac198254061239). However, depending on the context, a different value of p may prove to be more convenient. Likewise, c is most commonly – but not necessarily – taken to be 1 moldm3.


Note that in the above definitions, no temperature is specified. Therefore, by defining the standard Gibbs free energy, we are fixing a particular value of p, as well as particular values of ni,nj,. However, the value of T is not fixed. Therefore, when stating a value of ΔrG, it is also necessary to state the temperature which that value applies to.



When a reaction vessel is prepared with all its substances in the standard state, all the components of the system will have an activity of exactly 1 by definition. Therefore, the reaction quotient Q (which is a ratio of activities) will also be exactly equal to 1. So, we could also say that ΔrG is the value of ΔrG when Q=1.


Returning to the graph of G against ξ above, we note that at the left-most point, Q=0 since there are only reactants; at the right-most point, Q as there are only products. As we move from left to right, Q increases continuously, so there must be a point where Q=1. (In general, the point where Q=1 will not be the same as the equilibrium point.) Since ΔrG is the gradient of the graph, ΔrG is simply the gradient of the graph at that particular point where Q=1:


Standard reaction Gibbs free energy


The gradient of the graph, i.e. ΔrG, will vary as you traverse the graph from left to right. At equilibrium, the gradient is zero, i.e. ΔrG=0. However, ΔrG refers to the gradient at that one specific point where Q=1. In the example illustrated above, that specific gradient is negative, i.e. ΔrG<0.


Again, I reiterate that the temperature has nothing to do with this. If you were to change the temperature, you would get an entirely different graph of G versus ξ. You can still find the point on that graph where Q=1, and the gradient of that graph at the point where Q=1 is simply ΔrG at that temperature.




We have established the qualitative relationship between ΔrG and ΔrG, but it is often useful to have an exact mathematical relation.


ΔrG is exactly the same as ΔrG except for the imposition of the standard state. It follows that if we take the equation


ΔrG=iμiνi


and impose the standard state, we get



ΔrG=iμiνi


Thermodynamics tells us that


μi=μi+RTlnai


where ai is the thermodynamic activity of species i. Substituting this into the expressions for ΔG and ΔG above, we obtain the result:


ΔrG=ΔrG+RTlnQ


where the reaction quotient Q is defined as


Q=iaνii


When equilibrium is reached, we necessarily have ΔrG=0 (see the discussion above). The equilibrium constant K is defined to be the value of Q at equilibrium. Therefore, at equilibrium, Q=K. Plugging this into the equation above gives us the famous equation:


ΔrG=RTlnK


Again, no temperature is specified! In general, K depends on the temperature as well; the relationship is given by the van 't Hoff equation.



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