Page 43 - Thermodynamics of Biochemical Reactions
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3.1 Derivation  of  the Expression  for the Equilibrium  Constant   37


            To  discuss  equilibrium  in  a  chemical  reaction  system,  it  is  convenient  to
         introduce the activity a, of a species to replace the chemical potential of  a species
         because  a, is  more  closely  related  to  partial  pressures  and  concentrations  of
         species. The activity of  a species is defined  by

                                    pi = py + RTlna,                     (3.1-7)

         where $, which is referred  to as the standard chemical potential, is the chemical
         potential when ai = 1. A superscript zero is used to designate a standard property,
         and so py is the standard chemical potential of species i. For ideal mixtures of ideal
         gases, ui can be replaced  by  P,/PO, where  Po is the standard state pressure, and
         for  ideal  solutions  a,  can  be  replaced  by  ci/cO, where  co  is  the  standard
         concentration. Note that the activity a, of  species i is dimensionless. We will use
         molar  concentrations,  but  measurements  in  physical  chemistry  are  frequently
         based  on  molal  concentrations  (mol  kg- I).  Molal  concentrations  mi have  the
         advantage that they do not change with temperature.
             From one point  of  view nothing  is gained  by  using equation 3.1-7 to define
         the activity ai of  a species and using it to replace the chemical potential pi of  the
         species. The difference between pi and ai is that pi of  an ideal gas goes from  - 00
         to  m, whereas a, goes from 0 to co. Thus the  activity of  a species in solution  is
         more  closely  related  to its  concentration  than  pi is.  However,  the  activity  of  a
         species  in  solution  is  directly  proportional  to  its  concentration  only  for  ideal
         solutions. In general,  the  activity  of  a  species  in  solution  is  given  by  a, = yici,
         where yi is the activity coefficient of species i. The activity coefficient of  a solute is
         a function  of  the concentration, especially for ions. Strictly speaking (Mills et a].,
         1993),  this  relation  should  be  written  a, = yici/cO, where  c0  is  the  standard
         concentration  (1  M).  However,  c0  is  omitted  in  this  book  to  simplify  the
         equations. Thus equation 3.1-7 is written

                                         0
                                    pi = pi + RTlnyici                   (3.1-8)
             When using the molar concentration  scale, the convention is that the activity
         coefficient  of  a  species  approaches  unity  as  the  concentration  of  the  species
         approaches zero. In discussing biochemical reactions in dilute aqueous solutions,
         effects on activity coefficients arise primarily  because of electrostatic interactions
         between  charged  species and depend  on the ionic  strength  (see Section  1.2 and
         Section 3.6). Since the ionic strength is under the control of  the investigator and
         is  nearly  constant  during  the  approach  to  equilibrium  when  a  biochemical
         reaction is carried  out in dilute aqueous solution with  a buffer, we can postpone
         discussing  the  effects  of  ionic  strength  to  Section  3.6  by  making  the  following
         observation: Equation 3.1-8 can be written

                                pi = ,UP + RTIny, + RTlnci               (3.1-9)

         In discussing biochemical thermodynamics, however, it is convenient to write this
         equation  as

                                    p, =  + RTlnc,                      (3.1 - 10)

         where pj and   are functions of the ionic strength. In equations 3.1-9 and 3.1-10,
          p, and  p:  have  been  used  in  two  different  ways,  but  in  the  rest  of  the  book
          equation 3.1-10 will always be used. In other words, chemical potentials and other
          thermodynamic properties of species in dilute aqueous solutions will be taken  to
          be functions of the ionic strength. This will allow us to avoid including y, in many
          places (even though the effect of ionic strength is taken into account) and to treat
          solutions  at a  specified  ionic  strength  as  “ideal  solutions,”  that  is  as  solutions
          following  equation  3.1-10.  We  have  already  seen  an  example  of  this  in  the
          treatment  of  pH in Section 1.2.
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