Solubility Equilibria Of Sparingly Soluble Salts
OSTWALD THEORY OF INDICATORS
An indicator generally a weak organic acid or weak organic bases is a substance which is used to determine the end point in a titration. They change their colours within a certain pH range generally the colour change is due to shifting of indicator equilibrium, eg, for phenolphthalein (HPh).
HPh H+ + Ph-
Colourless pink
and shifting of this equilibrium from left to right produces pink colours
At equilibrium point [Ph-] = [HPh]
pH = pKIn. also KIn = [H+]
Where KIn is the ionization constant of the indicator
SOLUBILITY PRODUCT
Consider a binary electrolyte AxBy with solubility S mole/litre.
\begin{gathered} {A_x}{B_y} \rightleftharpoons x{A^{ + y}} + y{B^{ - x}} \hfill \\ \,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,xS\,\,\,\,\,\,\,\,\,\,yS \hfill \\ \end{gathered}
= xxyyS(x+y)
Ksp is called solubility product.
Solubility product may be defines as "the product of the concentration of ions in a saturated solution of an electrolyte at a given temperature".
From solubility product, we may conclude that;
Case I: If, [ionic product] < Ksp
Then, the solution is unsaturated i.e. more solute go into the solution.
Case II: If, [ionic product] = Ksp
The solution is just saturated i.e. no more solute can be dissolved.
Case III: If, [ionic product] > Ksp
The solution is supersaturated i.e. precipitation takes place.
Simultaneous solubility
Solubility of two sparingly soluble salt having common ion dissolved in same solution is called simultaneous solubility. Let S1 and S2 be the simultaneous solubility of AgBr and AgSCN respectively.
\begin{align} AgBr(s)A{{g}^{+}}(aq)+B{{r}^{-}}(aq)\,;\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,{{K}_{sp}}=[A{{g}^{+}}]\,[B{{r}^{-}}]=({{S}_{1}}+{{S}_{2}}){{S}_{1}}\,\,\,\,\,.......\,(1) \\ \,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,({{S}_{1}}+{{S}_{2}})\,\,\,\,\,\,\,\,\,{{S}_{1}} \\ \end{align}
\begin{align} AgSCN(s)A{{g}^{+}}(aq)+SC{{N}^{-}}(aq)\,;\,\,\,\,\,\,\,\,{{K}_{sp}}=[A{{g}^{+}}]\,[SC{{N}^{-}}]=({{S}_{1}}+{{S}_{2}}){{S}_{2}}\,\,\,\,\,.......\,(2) \\ \,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,\,({{S}_{1}}+{{S}_{2}})\,\,\,\,\,\,\,\,\,{{S}_{2}} \\ \end{align}
Thus simultaneous solubility of AgBr and AgSCN can be calculated by the above two expression.
Illustration 1. The following solutions were mixed: 500 ml of 0.01M AgNO3 and 500 ml. of solution that was both 0.01M in NaCl and 0.01M NaBr. Calculate [Ag+], [Cl–] and [Br–]
Ksp(AgCl) = 1.0 × 10–10
Ksp (AgBr) = 5 × 10–13
Fractional Precipitation
It is the technique used to separate two or more ions from a solution by adding a selective reagent that precipitates first one ion and then the second.
Considering a solution of 0.1 M Ba2+ and 0.1 M Sr2+. If K2Cr2O4 is added to this solution as a precipitating agent. Ksp of BaCrO4 is 1.2 × 10–10
and Ksp of SrCrO4 is 3.5 × 10–5
Concentration of required to precipitated BaCrO4
Concentration of required to ppt. SrCrO4 =
Since the required concentration of is low so BaCrO4 will ppt. first.
On addition of chromate ions to the solution, BaCrO4 starts precipitating in the solution when concentration reaches 1.2 × 10–9 M. On adding further chromate ions to the solution when concentration reaches upto 3.5 × 10–4, then SrCrO4 also start precipitating in the solution.
[Ba2+] left when SrCrO4 starts precipitating
= 3.4 × 10–7 M
= 0.00034%
Calculation of solubilities of salts
We shall now discuss the solubilities of different types of salts under various conditions.
(i) Solubilities of AgCl (salt of a strong acid and strong base) in water
AgCl would dissolve in water as,
AgCl (s) Ag+ (aq) + Cl– (aq)
At saturation point,
AgCl (s) Ag+(aq) + Cl– (aq)
If the solubility of the salt is x moles / L.
[Ag+] = xM, [Cl–] = xM
x2 = Ksp
or x =
(ii) Solubility of AgCl in a solution that is having 0.1M in AgNO3
AgCl would dissolve and finally reach saturation.
AgCl(s) Ag+(aq) + Cl– (aq)
The Ksp of AgCl is approximately 10–10 . If AgCl were to be dissolved in water (pure), its solubility would have been 10–5M (previous section). In the presence of 0.1M AgNO3 its solubility will decreases due to common ion effect. This means that [Ag+] from AgCl would be less than 10–5 M. Hence, we can ignore the contribution of Ag+ from AgCl.
If the solubility of AgCl is x' moles / L in the presence of 0.1M AgNO3, then
[Ag+] = 0.1 M, [Cl–] = x' M
x' = = 10–9 moles / L
(iii) Solubility of CH3COOAg (salt of weak acid and strong base) in water
CH3COOAg dissolves and reaches saturation. Since it is a salt of weak acid and strong base, it would hydrolyse. If the solubility of the salt is x moles/ l then
CH3COOAg (s) CH3COO– (aq) + Ag+ (aq)
At eqb: x –y x
CH3COO– (aq) + H2O CH3COOH (aq) + H+ (aq)
At eqb: x –y y y
Where y is the amount of CH3COO– ion that is hydrolysed.
(x –y) x = Ksp
=
Knowing the values of Ksp and Ka, solubility of the salt can be calculated.
(iv) Solubility of CH3COOAg (salt of a weak acid and strong base) in an acid buffer of pH = 4 (assuming that the buffer does not have any common ion by CH3COOAg):
CH3COOAg would dissolve and reach equilibrium. It would then be hydrolysed. If the solubility of the salt is x' M in this solution, then
At eq; CH3COOAg (s) CH3COO– (aq) + Ag+ (aq)
x' –y' x'
CH3COO– (aq) + H+ CH3COOH (aq)
x' – y' 10–4 y'
Since the solution is a buffer, the pH will be maintained.
( x' – y') x ' = Ksp
=
Since in presence of basic buffer, the degree of hydrolysis will be suppressed by already existing –OH ions, therefore the approximated formula which can be used is
x'2 = (CH3COOAg) (neglecting y'')
Knowing Ksp and Ka, the solubility can be calculated.
(v) Solubility of CH3COOAg in an buffer solution of pH = 9
Following the same logic as give in the earlier section,
CH3COOAg (s) CH3COO– (aq) + Ag+ (aq)
At eqb: x'' – y'' x''
CH3COO–(aq) + H2O CH3COOH + OH–
At eqb: x'' – y'' y'' 10–5
Where x'' M is the solubility of the salt and y'' the extent to which it is hydrolysed.
( x'' – y'') x'' = Ksp
=
Knowing, Ksp and Ka, the solubility can be calculated.
(vi) Solubility of AgCl in an aqueous solution containing NH3
Let the amount of NH3 initially be 'a' M. If the solubility of the salt is x moles/ l, then
AgCl (s) Ag+ (aq) + Cl– (aq)
At eq: x –y x
Ag+(aq) + 2NH3 (aq) Ag(NH3)2+(aq)
x–y a–2y y
Where y is the amount of Ag+ which has reacted with NH3.
( x –y) x = Ksp
= Kf (formation constant of Ag(NH3)2+)
Knowing Ksp and Kf, the solubility can be calculated.
Illustration 2. The solubility of BaSO4 in water is 2.3 x 10–4 gm/100 mL. Calculate the percentage loss in weight when 0.2 gm of BaSO4 is washed with (a) 1lt of water (b) 1lt of 0.01N Na2SO4.
Solution: (a) Solubility is in general expressed in gm/lt,
so solubility of BaSO4 = 2.3 x10–3 g /lt
Loss in weight of BaSO4 = amount of BaSO4 soluble
%loss = x 100 = 1.15%
(b) Now 0.01 N N Na2SO4 0.01 N ions
0.005 M ions
Now presence of prior to washing BaSO4 will suppress the solubility of BaSO4 (due to common ion effect). The suppression will be governed by Ksp value of BaSO4. So first calculate Ksp of BaSO4.
Solubility of BaSO4 in fresh water = 2 x 10–3 g/lt
= Mol/lt = 9.85 x 10–6 M
Ksp = [Ba2+] = (9.85 × 10–6)2 = 9.71 x 10–11
Now let x be solubility in mol/lt
[Ba2+] in solution = x mol/lt and in solution
= (x + 0.005) mol/lt
Ionic product = [Ba2+] = (x) (x + 0.005)
Ksp = Ionic Product at equilibrium (saturation)
9.71 x 10–11 = (x) (x + 0.005) x2 + 0.005 x –9.71 x 10–11 = 0
x = = 1.94 x 10–8 mol/lt = 1.94 × 10–8 x 233.4 g/lt
4.53 x 10–6 gm of BaSO4 are washed away
percentage loss = = 2.26 x 10–3%
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