Page 184 - Geochemistry of Oil Field Waters
P. 184

PHYSICAL PROPERTIES                                                  171


            Ionic radii
              Table 5.VI contains data concerning the radii of the nonhydrated ions, the
            hydrated ions, the ionic potential, and the polarization. The size of the ions
            is of interest concerning the mobilities or the relative transport coefficient of
            a  given  ion  through  a  clayshale  membrane  system  or  the  replacement
            coefficient in  a clay ion-exchange system. The ionic potential is of  interest
            because elements with low ionic potentials are the most likely to remain in
            true solution. The polarization, which is equivalent to the valency divided by
            the ion radius, is of interest because the larger the polarization, the lower the
            replacing power in an exchange system (Collins, 1970).
              The  ionic  potentials  of  the  constituents  involved  in  the  diagenesis are
            important (Hem, 1960). Those that stay in true ionic solution to rather high
            pH  levels include Na+, K+, Mg+’,  Fe+’,  Mn+’,  Ca+’, Sr+*, and Ba+’ ; they
            are  the  soluble  cations,  and  their  ionic potentials range  from  0.3 to 1.3,
            where the ionic potential is the ratio  between the ionic charge and the ionic
            radius.  Constituents that are precipitated  by  hydrolysis are those with ionic
            potentials  of  3-12  and  include  such  ions as AP3, Fe+3, SP4, and MrP4.
            Constituents which form soluble complex ions and usually go into true ionic
            solution include B+3, C4, N+5, P+’,  S6, and Mn+’ ; their ionic potentials
            are  over  12. In general, the hydroxides of  the soluble cations possess ionic
            bonds; therefore,  they  are soluble. The hydrolysates, or those ions precipi-
            tated by hydrolysis from hydroxyl bonds, and the soluble complex ions both
            have hydrogen bonds.





           TABLE 5.VI

            Radii, valence, ionic potentials, and polarization
           Constituents        Nonhydrated   Valence   Hydrated  Ionic    Polarization
                               radius (A)              radius (A)  potential


           Lithium             0.60          +1        3.82      0.60     1.67
           Sodium              0.95          +1        3.58      0.95     1.05
           Potassium           1.33          +1        3.31      1.33      .75
           Calcium             0.99          +2        4.12      0.50     2.02
           Magnesium           0.65          +2        4.28      0.33     3.08
           Strontium           1.13          +2        4.12     0.57      1.77
           Barium              1.35          +2        4.04     0.68      1.48
           Boron               0.23          +3        -        0.08      -
           Chloride            1.81          -1        3.32      1.81     0.55
           Bromide             1.95          -1        3.30      1.95     0.51
           Iodide              2.16          -1        3.31      2.16     0.46
           Sulfate             2.90          -2        3.79     1.45      0.69
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