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Chemical Reaction Equilibria Chapter 13-Part I
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Definition of reaction coordinate A A + B B C C + D D Stoichiometric coefficients: by convention are 0 for products As the rxn progresses, there is a change in the number of moles of each species, proportional to the stoichiometric numbers
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Reaction coordinate (e) We defined: dn i = i d Integrating between n i o and n i and between 0 and : n i = n i o + i Summing over all species: Mole fractions:
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example 4NH 3 (g)+ 5O 2 (g) 4NO(g)+6H 2 O(g) Initially there are 2 mol NH 3 and 5 mol O 2 Find mole fractions of reacting species as functions of the reaction coordinate, n NH3 = 2 -4
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Two or more simultaneous reactions One reaction coordinate j for each reaction
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example C 2 H 4 (g) + ½ O 2 (g) ((CH 2 ) 2 )O(g) C 2 H 4 (g) + 3 O 2 (g) 2CO 2 (g) +2H 2 O(g) Initially there are 2 mol of C 2 H 4 (g) and 3 mol of O 2 (g). Find expressions for the mole fractions of the reacting species as functions of the reaction coordinates for the two reactions.
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j iC2H4C2H4 O2O2 ((CH 2 ) 2 )OCO 2 H2OH2O j 1 2 n o = C 2 H 4 (g) + ½ O 2 (g) ((CH 2 ) 2 )O(g) C 2 H 4 (g) + 3 O 2 (g) 2CO 2 (g) +2H 2 O(g) n o (C 2 H 4 ) =2; n o (O 2 )=3
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Equilibrium criteria for chemical reactions We showed that the total Gibbs energy of a closed system at constant T and P must decrease during an irreversible process. At equilibrium: (dG) T,P =0 For a reacting system, G must be a minimum at equilibrium
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Given G=G minimize and get the value of at equilibrium. Then you can calculate the equilibrium mole fractions y( )
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how to introduce in the dG expression
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Criterion of chemical equilibrium Now we need to express the chemical potentials as functions of fugacities Solve for i and substitute in the equilibrium criterion
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Definition of equilibrium constant K
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Equilibrium constant K where K is a function of temperature
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Example: Water-gas shift reaction H 2 (g)+CO 2 (g) H 2 O(g)+CO(g) Data for G 0 is given. For a temperature of 1000 K and for a feed of 1 mol H 2 and1 mol CO 2, Determine the equilibrium value of = n o = y H2 = y CO2 = y H2O = y CO =
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G o data (J/mol) T(K)H2OH2OCOCO 2 1,000-192,420-200,240-395,790 1,100-187,000-209,110-395,960 1,200-181,380-217,830-396,020 1,300-175,720-226,530-396,080 1,400-170,020-235,130-396,130 1,500-164,310-243,740-396,160 dG/d = 0 =0.453
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