Natural waters may be chemically studied as mixed electrolyte
solutions. Some important equilibrium properties of natural waters are
intimately related to the activity-concentration ratios (i.e., activity
coefficients) of the ions in solution. An Ion Interaction Model, which
is based on Pitzer's (1973) thermodynamic model, is proposed in this
dissertation. The proposed model is capable of describing the activity
coefficient of ions in mixed electrolyte solutions. The effects of
temperature on the equilibrium conditions of natural waters and on the
activity coefficients of the ions in solution, may be predicted by means
of the Ion Interaction Model presented in this work. The bicarbonate ion, HCO3-, is commonly found in natural waters.
This anion plays an important role in the chemical and thermodynamic
properties of water bodies. Such properties are usually directly related
to the activity coefficient of HCO3- in solution. The Ion Interaction
Model, as proposed in this dissertation, is used to describe
indirectly measured activity coefficients of HCO3- in mixed electrolyte
solutions. Experimental pH measurements of MCl-MHCO3 and MCl-H2CO3 solutions
at 25°C (where M = K+, Na+, NH4+, Ca2+ or Mg2+) are used in this
dissertation to evaluate indirectly the MHCO3 virial coefficients. Such
coefficients permit the prediction of the activity coefficient of HCO3-
in mixed electrolyte solutions. The Ion Interaction Model is found to
be an accurate method for predicting the activity coefficient of HCO3-
within the experimental ionic strengths (0.2 to 3.0 m). The virial
coefficients of KHCO3 and NaHCO3 and their respective temperature variations
are obtained from similar experimental measurements at 10° and
40°C. The temperature effects on the NH4HCO3, Ca(HCO3)2, and Mg(HCO3)2
virial coefficients are estimated based on these results and the temperature
variations of the virial coefficients of 40 other electrolytes. Finally, the Ion Interaction Model is utilized to solve various
problems of water chemistry where bicarbonate is present in solution.