Page 222 - Introduction to Colloid and Surface Chemistry
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Colloid stability  211

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        Table 8.1  Critical coagulation  concentrations  (in  millimoles per  dm )  for hydrophobic
           96
        sols  (By courtesy  of  Elsevier  Publishing Company)
        As2$3 (~ve  so/)         Agl  (—ve  sol)     A1 2O 3 (+ve  sol)
        LiCl          58      UNO,        165     NaCl          43.5
        NaCl          51      NaNO 3      140      KCI          46
         KCI          49.5    KNO,        136      KNO 3        60
                      50      RbNO,       126
        KNO 3
        K  acetate   110      AgN0 3       0.01)
                       0.65                2.40                 0.30
        CaCI 2                Ca(N0 3) 2           K 2SO 4
                       0.72                2.60                 0.63
        MgCI 2                Mg(N0 3) 2           K 2Cr 20 7
                       0.81                2.43    K 2 oxalate  0.69
        MgSO 4                Pb(N0 3) 2
                       0.093               0.067   K 3[Fe(CN) 6]  0.08
        A1C1 3                A1(N0 3) 3
                       0.096               0.069
        M>A1 2(SO 4) 3        La(N0 3) 3
                       0.095               0.69
        AI(N0 3) 3            Ce(N0 3) 3
        electrolyte  causes  a  compression  of  the  diffuse  parts  of  the  double
        layers  around  the  particles  and  may,  in  addition,  exert  a  specific
        effect  through ion adsorption  into the Stern layer. The sol coagulates
        when  the  range  of  double-layer  repulsive interaction  is  sufficiently
        reduced  to  permit  particles  to  approach  close  enough for  van  der
        Waals forces to  predominate.
          The  critical  coagulation  concentration  (c.c.c.)  of  an  indifferent
        (inert)  electrolyte  (i.e.  the  concentration  of the  electrolyte which is
        just  sufficient  to  coagulate  a  lyophobic  sol to  an  arbitrarily defined
        extent in an arbitrarily chosen  time) shows considerable  dependence
        upon  the  charge  number  of  its  counter-ions.  In  contrast,  it  is
        practically independent  of  the  specific  character of the  various ions,
        the  charge  number of  the  co-ions  and  the  concentration of  the  sol,
        and  only  moderately  dependent  on  the  nature  of  the  sol.  These
        generalisations  are  illustrated  in  Table  8.1,  and  are  known  as  the
        Schulze-Hardy rule.

        The Deryagin-Landau and Verwey-Overbeek theory
        (introduction)

                                                     97
        Deryagin and Landau 194  and Verwey and Overbeek  independently
        developed  a  quantitative  theory in  which  the  stability  of lyophobic
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