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General Chemistry Principles, Patterns, and Applications, 2011

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continue to precipitate until the system reaches equilibrium, which occurs when [Ba 2+ ][SO 4<br />

2−<br />

] = K sp =<br />

1.08 × 10 −10 .<br />

Exercise<br />

The solubility product of calcium fluoride (CaF 2) is 3.45 × 10 −11 . If 2.0 mL of a 0.10 M solution of NaF is<br />

added to 128 mL of a 2.0 × 10 −5 M solution of Ca(NO 3) 2, will CaF 2precipitate?<br />

Answer: yes (Q = 4.7 × 10 −11 > K sp)<br />

The Common Ion Effect <strong>and</strong> Solubility<br />

The solubility product expression tells us that the equilibrium concentrations of the cation <strong>and</strong> the anion<br />

are inversely related. That is, as the concentration of the anion increases, the maximum concentration of<br />

the cation needed for precipitation to occur decreases—<strong>and</strong> vice versa—so that Ksp is constant.<br />

Consequently, the solubility of an ionic compound depends on the concentrations of other salts that<br />

contain the same ions. This dependency is another example of the common ion effect discussed inChapter<br />

16 "Aqueous Acid–Base Equilibriums", Section 16.6 "Buffers": adding a common cation or anion shifts a<br />

solubility equilibrium in the direction predicted by Le Châtelier’s principle. As a result, the solubility of<br />

any sparingly soluble salt is almost always decreased by the presence of a soluble salt that contains a<br />

common ion. [2]<br />

Consider, for example, the effect of adding a soluble salt, such as CaCl2, to a saturated solution of calcium<br />

phosphate [Ca3(PO4)2]. We have seen that the solubility of Ca3(PO4)2 in water at 25°C is 1.14 × 10 − 7<br />

M (Ksp =<br />

2.07 × 10 − 33 ). Thus a saturated solution of Ca3(PO4)2 in water contains 3 × (1.14 × 10 − 7<br />

M) = 3.42 × 10 − 7<br />

M<br />

Ca 2+ <strong>and</strong> 2 × (1.14 × 10 − 7<br />

M) = 2.28 × 10 − 7<br />

M PO4 3− , according to the stoichiometry shown inEquation<br />

17.1 (neglecting hydrolysis to form HPO4 2− as described in Chapter 16 "Aqueous Acid–Base Equilibriums").<br />

If CaCl2 is added to a saturated solution of Ca3(PO4)2, the Ca 2+ ion concentration will increase such that<br />

[Ca 2+ ] > 3.42 × 10 − 7<br />

M, making Q > Ksp. The only way the system can return to equilibrium is for the<br />

reaction inEquation 17.1 to proceed to the left, resulting in precipitation of Ca3(PO4)2. This will decrease<br />

the concentration of both Ca 2+ <strong>and</strong> PO4 3− until Q = Ksp.<br />

Note the Pattern<br />

The common ion effect usually decreases the solubility of a sparingly soluble salt.<br />

E X A M P L E 4<br />

Calculate the solubility of calcium phosphate [Ca 3(PO 4) 2] in 0.20 M CaCl 2.<br />

Saylor URL: http://www.saylor.org/books<br />

Saylor.org<br />

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