Page 65 - Vogel's TEXTBOOK OF QUANTITATIVE CHEMICAL ANALYSIS
P. 65

THE  IOMIC PROOUCT  OF  WATER   2.16

       therefore be slightly ionised in accordance with the equation:


       Applying  the  Law of  Mass Action  to this  equation, we  obtain, for any given
       temperat ure:
       a,+  x  a,,-   [H+].[OH-1   YH+.YoH-
                 -               x         = a constant
                 -
         a   ~  ,  ~  CH201          YH~O
       Since water is only slightly ionised, the ionic concentrations will be small, and
       their activity coefficients may be regarded as unity; the activity of the un-ionised
       molecules may also be taken as unity. The expression thus becomes:
       CH+] x  [OH-]
                      = a constant
           CH201
       In  pure  water  or  in  dilute  aqueous  solutions,  the  concentration  of  the
       undissociated water may be considered constant. Hence:

       CH+] x  [OH-]  = K,
       where  K,  is  the  ionic  product  of  water.  It  must  be  pointed  out  that  the
       assumption that the activity coefficients of the ions are unity and that the activity
       coefficient of  water is constant applies strictly to pure water and to very dilute
       solutions (ionic strength < 0.01); in more concentrated solutions, i.e. in solutions
       of  appreciable  ionic  strength,  the  activity  coefficients of  the ions are affected
       (compare Section 2.5), as is also the activity  of  the un-ionised  water. The ionic
       product  of  water  will  then  not  be  constant,  but  will  depend  upon  the  ionic
       strength  of  the  solution.  It  is,  however,  difficult  to  determine  the  activity
       coefficients, except  under specially selected conditions,  so that in practice  the
       ionic product K,,  although not strictly constant, is employed.
         The  ionic  product  varies  with  the  temperature,  but  under  ordinary
       experimental conditions (at about 25 OC) its value may be taken as 1 x  10-l4
       with  concentrations expressed  in mol L-'.  This is  sensibly constant  in dilute
       aqueous  solutions. If  the  product  of  [H+] and  [OH-]  in  aqueous  solution
       momentarily  exceeds this  value,  the excess ions will  immediately combine to
       form  water.  Similarly,  if  the  product  of  the  two  ionic  concentrations  is
       momentarilv  less than  10-14.  more water molecules  will  dissociate  until  the
       equilibrium value is attained.
         The  hydrogen  and  hydroxide  ion concentrations are equal in pure  water;
       therefore  CH+] = [OH-]  = z=
                                            mol L-'  at about 25 OC. A solution
       in which  the  hydrogen and  hydroxide ion concentrations are equal is termed
       an exactly neutral solution. If  [H+] is greater than   the solution is acid,
       and  if  less  than   the  solution  is  alkaline  (or basic).  It  follows  that  at
       ordinary  temperatures  [OH-]  is greater  than   in  alkaline  solution and
       less than this value in acid solution.


       *Strictly  speaking the hydrogen ion  H +  exists in water as the hydroxonium  ion  H30+ (Section
       2.4). The electrolytic dissociation of water should therefore be written:
       2H20eH30+ +OH-
       For the sake of simplicity,  the more familiar symbol H+ will be retained.
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