The solubility of boric acid [B] in LiCl, NaCl, KCl, RbCl, and CsCl was determined as a function of ionic strength (0–6 mol ⋅ kg−1) at 25 ∘C. The results were examined using the Pitzer equation $$ \ln \{ [{\rm B}]^0 /[{\rm B}]\} = \ln \gamma _{\rm B} = (2\nu _{\rm c} \lambda _{{\rm Bc}} + 2\nu _{\rm a} \lambda _{{\rm Ba}})m + \nu _{\rm c} \nu _{\rm a} \zeta _{{\rm B - a - c}} m^2 $$ where [B]0 is the concentration of boric acid in water and [B] in solution, γB is the activity coefficient, νi is the number of ions (i), λBc, λBa are parameters related to the interaction of boric acid with cation c and anion a, ζB-a−c is related to the interaction of boric acid with both cation and anion and m is the salt molality. The literature values for the solubility of boric acid in a number of other electrolytes were also examined using the same equation. The results for the 2νcλBc+2νaλBa term (equal to the salting coefficient k S) were examined in terms of the ionic interactions in the solutions. The solubility of boric acid in LiCl, NaCl, and KCl solutions is not a strong function of temperature and the results can be used over a limited temperature range (5–35 ∘C). Boric acid is soluble in the order SO4 > NO3 and F > Cl > Br > I in common cation solutions. In common anion salt solutions, the order is Cs > Rb > K > Na > Li > H and Ba > Sr > Ca > Mg. The results were examined using correlations of k S with the volume properties of the ions. When direct measurements were not available, k S and ζB-c−a were estimated from known values of λBc and λBa. The values of λBc, λBa, and ζB-a−c can be used to estimate the boric acid activity coefficients γB and solubility [B] in natural mixed electrolyte solutions (seawater and brines) using the more general Pitzer equation $$ \hspace*{20pt}\ln \{ [{\rm B}]^0 /[{\rm B}]\} = \ln \lambda _{\rm B} = (2\Sigma _{\rm c} \nu _{\rm c} \lambda _{{\rm Bc}} + 2\Sigma _{\rm a} \nu _{\rm a} \lambda _{{\rm Bac}})m + \Sigma _{\rm c} \Sigma _{\rm a} \nu _{\rm c} \nu _{\rm a} \zeta _{{\rm B - a - c}} m^2 $$
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