Page 124 - Chemical equilibria Volume 4
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100     Chemical Equilibria
                           by equations [3.98a] and [3.98b], is  common to all the iso-composition
                           curves. The position of O depends only on the stoichiometric numbers in the
                           balance equation.
                             The  equilibrium point E for the  system under examination here
                           (Figure 3.16) is therefore at the intersection of the iso-composition curve – the
                           straight line Om (with m being fixed by the initial mixture u) and the iso-Q
                                                                                       (I)
                           curve  corresponding to the value of  the  equilibrium  constant  K  at  the
                           temperature in question. All of this is calculated for a given pressure, because
                           the diagram is isobaric.



                           3.6. Quaternary diagrams of chemical equilibria

                             It is possible to plot diagrams for equilibria involving a polycomponent
                           phase with four components of the reaction. The system  contains three
                           independent components. These diagrams are square. To demonstrate their
                           representation and their operation, we shall consider the reduction of carbon
                           dioxide by hydrogen, in accordance with:
                                CO 2 + H 2 = CO + H 2O                                  [3R.27]


                             On the horizontal abscissa axis, we shall show the proportion of carbon in
                           the CO state, and on the vertical axis, the proportion of H 2 in the state of free
                           H 2 gas. Hence, we shall have:
                                        {CO }
                                 x =                                                    [3.99a]
                                    {CO +      2 }
                                        } {CO
                                        { }
                                         H
                                 y =       2                                            [3.99b]
                                         +
                                    { } {H O   }
                                     H
                                       2
                                             2
                             Because of the conservation of carbon, we can write:
                                { } {CO+   2 } Const. k=  =  C                          [3.100]
                                 CO
                             Similarly, for the conservation of hydrogen:

                                { } {H O+  2  } Const. k=  =  H                         [3.101]
                                 H
                                   2
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