17.6 Precipitation and Dissolution

Learning Objectives

By the end of this section, you will be able to:
  • Write chemical equations and equilibrium expressions representing solubility equilibria
  • Carry out equilibrium computations involving solubility, equilibrium expressions, and solute concentrations

The preservation of medical laboratory blood samples, mining of sea water for magnesium, formulation of over-the-counter medicines such as Milk of Magnesia and antacids, and treating the presence of hard water in your home’s water supply are just a few of the many tasks that involve controlling the equilibrium between a slightly soluble ionic solid and an aqueous solution of its ions.

In some cases, we want to prevent dissolution from occurring. Tooth decay, for example, occurs when the calcium hydroxylapatite, which has the formula Ca5(PO4)3(OH), in our teeth dissolves. The dissolution process is aided when bacteria in our mouths feast on the sugars in our diets to produce lactic acid, which reacts with the hydroxide ions in the calcium hydroxylapatite. Preventing the dissolution prevents the decay. On the other hand, sometimes we want a substance to dissolve. We want the calcium carbonate in a chewable antacid to dissolve because the CO32- ions produced in this process help soothe an upset stomach.

In this section, we will find out how we can control the dissolution of a slightly soluble ionic solid by the application of Le Châtelier’s principle. We will also learn how to use the equilibrium constant of the reaction to determine the concentration of ions present in a solution.

The Solubility Product Constant

Silver chloride is what’s known as a sparingly soluble ionic solid (Figure 17.6a). Recall from the solubility rules in an earlier chapter that halides of Ag+ are not normally soluble. However, when we add an excess of solid AgCl to water, it dissolves to a small extent and produces a mixture consisting of a very dilute solution of Ag+ and Cl– ions in equilibrium with undissolved silver chloride:

[latex]\text{AgCl}(s)\;\underset{\text{precipitation}}{\overset{\text{dissolution}}{\rightleftharpoons}}\;\text{Ag}^{+}(aq)\;+\;\text{Cl}^{-}(aq)[/latex]

This equilibrium, like other equilibria, is dynamic; some of the solid AgCl continues to dissolve, but at the same time, Ag+ and Cl– ions in the solution combine to produce an equal amount of the solid. At equilibrium, the opposing processes have equal rates.

Two beakers are shown with a bidirectional arrow between them. Both beakers are just over half filled with a clear, colorless liquid. The beaker on the left shows a cubic structure composed of alternating green and slightly larger grey spheres. Evenly distributed in the region outside, 11 space filling models are shown. These are each composed of a central red sphere with two smaller white spheres attached in a bent arrangement. In the beaker on the right, the green and grey spheres are no longer connected in a cubic structure. Nine green spheres, 10 grey spheres, and 11 red and white molecules are evenly mixed and distributed throughout the liquid in the beaker.
Figure 17.6a Silver chloride is a sparingly soluble ionic solid. When it is added to water, it dissolves slightly and produces a mixture consisting of a very dilute solution of Ag+ and Cl– ions in equilibrium with undissolved silver chloride (credit: Chemistry (OpenStax), CC BY 4.0).

The equilibrium constant for the equilibrium between a slightly soluble ionic solid and a solution of its ions is called the solubility product (Ksp) of the solid. Recall from the chapter on solutions and colloids that we use an ion’s concentration as an approximation of its activity in a dilute solution. For silver chloride, at equilibrium:

[latex]\text{AgCl}(s)\;{\rightleftharpoons}\;\text{Ag}^{+}(aq)\;+\;\text{Cl}^{-}(aq)\;\;\;\;\;\;\;K_{\text{sp}} = [\text{Ag}^{+}(aq)][\text{Cl}^{-}(aq)][/latex]

When looking at dissolution reactions such as this, the solid is listed as a reactant, whereas the ions are listed as products. The solubility product constant, as with every equilibrium constant expression, is written as the product of the concentrations of each of the ions, raised to the power of their stoichiometric coefficients. Here, the solubility product constant is equal to Ag+ and Cl– when a solution of silver chloride is in equilibrium with undissolved AgCl. There is no denominator representing the reactants in this equilibrium expression since the reactant is a pure solid; therefore [AgCl] does not appear in the expression for Ksp.

Some common solubility products are listed in Table 17.6a according to their Ksp values. Each of these equilibrium constants is much smaller than 1 because the compounds listed are only slightly soluble. A small Ksp represents a system in which the equilibrium lies to the left, so that relatively few hydrated ions would be present in a saturated solution.

Table 17.6a Common Solubility Products by Decreasing Equilibrium Constants
Substance Ksp at 25 °C
CuCl 1.2 × 10–6
CuBr 6.27 × 10–9
AgI 1.5 × 10–16
PbS 7 × 10–29
Al(OH)3 2 × 10–32
Fe(OH)3 4 × 10–38

Example 17.6a

Writing Equations and Solubility Products

Write the ionic equation for the dissolution and the solubility product expression for each of the following slightly soluble ionic compounds:

  1. AgI, silver iodide, a solid with antiseptic properties
  2. CaCO3, calcium carbonate, the active ingredient in many over-the-counter chewable antacids
  3. Mg(OH)2, magnesium hydroxide, the active ingredient in Milk of Magnesia
  4. Mg(NH4)PO4, magnesium ammonium phosphate, an essentially insoluble substance used in tests for magnesium
  5. Ca5(PO4)3OH, the mineral apatite, a source of phosphate for fertilizers

(Hint: When determining how to break (d) and (e) up into ions, refer to the list of polyatomic ions in the section on chemical nomenclature.)

Solution

  1. [latex]\text{AgI}(s)\;{\rightleftharpoons}\;\text{Ag}^{+}(aq)\;+\;\text{I}^{-}(aq)\;\;\;\;\;\;\;K_{\text{sp}} = [\text{Ag}^{+}][\text{I}^{-}][/latex]
  2. [latex]\text{CaCO}_3(s)\;{\rightleftharpoons}\;\text{Ca}^{2+}(aq)\;+\;\text{CO}_3^{\;\;2-}(aq)\;\;\;\;\;\;\;K_{\text{sp}} = [\text{Ca}^{2+}][\text{CO}_3^{\;\;2-}][/latex]
  3. [latex]\text{Mg(OH)}_2(s)\;{\rightleftharpoons}\;\text{Mg}^{2+}(aq)\;+\;2\text{OH}^{-}(aq)\;\;\;\;\;\;\;K_{\text{sp}} = [\text{Mg}^{2+}][\text{OH}^{-}]^2[/latex]
  4. [latex]\text{Mg(NH}_4)\text{PO}_4(s)\;{\rightleftharpoons}\;\text{Mg}^{2+}(aq)\;+\;\text{NH}_4^{\;\;+}(aq)\;+\;\text{PO}_4^{\;\;3-}(aq)\;\;\;\;\;\;\;K_{\text{sp}} = [\text{Mg}^{2+}][\text{NH}_4^{\;\;+}][\text{PO}_4^{\;\;3-}][/latex]
  5. [latex]\text{Ca}_5(\text{PO}_4)3\text{OH}(s)\;{\rightleftharpoons}\;5\text{Ca}^{2+}(aq)\;+\;3\text{PO}_4^{\;\;3-}(aq)\;+\;\text{OH}^{-}(aq)\;\;\;\;\;\;\;K_{\text{sp}} = [\text{Ca}^{2+}]^5[\text{PO}_4^{\;\;3-}]^3[\text{OH}^{-}][/latex]

Exercise 17.6a

Write the ionic equation for the dissolution and the solubility product for each of the following slightly soluble compounds:

  1. BaSO4
  2. Ag2SO4
  3. Al(OH)3
  4. Pb(OH)Cl

Check Your Answer[1]

Now we will extend the discussion of Ksp and show how the solubility product constant is determined from the solubility of its ions, as well as how Ksp can be used to determine the molar solubility of a substance.

Ksp and Solubility

Recall that the definition of solubility is the maximum possible concentration of a solute in a solution at a given temperature and pressure. We can determine the solubility product of a slightly soluble solid from that measure of its solubility at a given temperature and pressure, provided that the only significant reaction that occurs when the solid dissolves is its dissociation into solvated ions, that is, the only equilibrium involved is:

[latex]\text{M}_p\text{X}_q(s)\;{\rightleftharpoons}\;p\text{M}^{\text{m+}}(aq)\;+\;q\text{X}^{\text{n-}}(aq)[/latex]

In this case, we calculate the solubility product by taking the solid’s solubility expressed in units of moles per litre (mol/L), known as its molar solubility.

Example 17.6b

Calculation of Ksp from Equilibrium Concentrations

Fluorite, CaF2, is a slightly soluble solid that dissolves according to the equation:

[latex]\text{CaF}_2(s)\;{\rightleftharpoons}\;\text{Ca}^{2+}(aq)\;+\;2\text{F}^{-}(aq)[/latex]

The concentration of Ca2+ in a saturated solution of CaF2 is 2.15 × 10–4M; therefore, that of F– is 4.30 × 10–4M, that is, twice the concentration of Ca2+. What is the solubility product of fluorite?

Solution

First, write out the Ksp expression, then substitute in concentrations and solve for Ksp:

[latex]\text{CaF}_2(s)\;{\rightleftharpoons}\;\text{Ca}^{2+}(aq)\;+\;2\text{F}^{-}(aq)[/latex]

A saturated solution is a solution at equilibrium with the solid. Thus:

[latex]K_{\text{sp}} = [\text{Ca}^{2+}][\text{F}^{-}]^2 = (2.1\;\times\;10^{-4})(4.2\;\times\;10^{-4})^2 = 3.7\;\times\;10^{-11}[/latex]

As with other equilibrium constants, we do not include units with Ksp.

Exercise 17.6b

Check Your Learning Exercise (Text Version)

In a saturated solution that is in contact with solid Mg(OH)2, the concentration of Mg2+ is 1.31 × 10–4M. What is the solubility product for Mg(OH)2?

MgOH2(s) ↔ Mg2+(aq) + 2OH–(aq)

  1. 1.31
  2. 4.99 x 10-6
  3. 1.31 x 10-4
  4. 8.99 x 10-12

Check Your Answer[2]

Source: “Exercise 17.6b” is adapted from “Example 15.1-2” in General Chemistry 1 & 2, a derivative of Chemistry (Open Stax) by Paul Flowers, Klaus Theopold, Richard Langley & William R. Robinson, licensed under CC BY 4.0.

Example 17.6c

Determination of Molar Solubility from Ksp

The Ksp of copper(I) bromide, CuBr, is 6.3 × 10–9. Calculate the molar solubility of copper bromide.

Solution

The solubility product constant of copper(I) bromide is 6.3 × 10–9.

The reaction is:

[latex]\text{CuBr}(s)\;{\rightleftharpoons}\;\text{Cu}^{+}(aq)\;+\;\text{Br}^{-}(aq)[/latex]

First, write out the solubility product equilibrium constant expression:

[latex]K_{\text{sp}} = [\text{Cu}^{+}][\text{Br}^{-}][/latex]

Create an ICE table (as introduced in the chapter on fundamental equilibrium concepts), leaving the CuBr column empty as it is a solid and does not contribute to the Ksp:
This table has two main columns and four rows. The first row for the first column does not have a heading and then has the following in the first column: Initial concentration ( M ), Change ( M ), and Equilibrium concentration ( M ). The second column has the header of, “C u B r equilibrium arrow C u superscript positive sign plus B r superscript negative sign.” Under the second column is a subgroup of three rows and three columns. The first column is blank. The second column has the following: 0, x, 0 plus x equals x. The third column has the following 0, x, 0 plus x equals x.

At equilibrium:

[latex]K_{\text{sp}} = [\text{Cu}^{+}][\text{Br}^{-}][/latex]
[latex]6.3\;\times\;10^{-9} = (x)(x) = x^2[/latex]
[latex]x = \sqrt{(6.3\;\times\;10^{-9})} = 7.9\;\times\;10^{-5}[/latex]

Therefore, the molar solubility of CuBr is 7.9 × 10–5M.

Exercise 17.6c

The Ksp of AgI is 1.5 × 10–16. Calculate the molar solubility of silver iodide.

Check Your Answer[3]

Example 17.6d

Determination of Molar Solubility from Ksp, Part II

The Ksp of calcium hydroxide, Ca(OH)2, is 1.3 × 10–6. Calculate the molar solubility of calcium hydroxide.

Solution

The solubility product constant of calcium hydroxide is 1.3 × 10–6.

The reaction is:

[latex]\text{Ca(OH)}_2(s)\;{\rightleftharpoons}\;\text{Ca}^{2+}(aq)\;+\;2\text{OH}^{-}(aq)[/latex]

First, write out the solubility product equilibrium constant expression:

[latex]K_{\text{sp}} = [\text{Ca}^{2+}][\text{OH}^{-}]^2[/latex]

Create an ICE table, leaving the Ca(OH)2 column empty as it is a solid and does not contribute to the Ksp:
This table has two main columns and four rows. The first row for the first column does not have a heading and then has the following in the first column: Initial concentration ( M ), Change ( M ), and Equilibrium concentration ( M ). The second column has the header of, “C a ( O H ) subscript 2 equilibrium arrow C a superscript 2 positive sign plus 2 O H superscript negative sign.” Under the second column is a subgroup of three rows and three columns. The first column is blank. The second column has the following: 0, x, and 0 plus x equals x. The third column has the following 0, 2 x, and 0 plus 2 x equals 2 x.

At equilibrium:

[latex]K_{\text{sp}} = [\text{Ca}^{2+}][\text{OH}^{-}]^2[/latex]
[latex]1.3\;\times\;10^{-6} = (x)(2x)^2 = (x)(4x^2) = 4x^3[/latex]
[latex]x = \sqrt[3]{\frac{1.3\;\times\;10^{-6}}{4}} = 6.9\;\times\;10^{-3}[/latex]

Therefore, the molar solubility of Ca(OH)2 is 1.3 × 10–2 M.

 

Using Barium Sulfate for Medical Imaging

Various types of medical imaging techniques are used to aid diagnoses of illnesses in a noninvasive manner. One such technique utilizes the ingestion of a barium compound before taking an X-ray image. A suspension of barium sulfate, a chalky powder, is ingested by the patient. Since the Ksp of barium sulfate is 1.1 × 10–10, very little of it dissolves as it coats the lining of the patient’s intestinal tract. Barium-coated areas of the digestive tract then appear on an X-ray as white, allowing for greater visual detail than a traditional X-ray (Figure 17.6b).

This figure contains one image. A black and white abdominal x-ray image is shown in which the intestinal tract of a person is clearly visible in white.
Figure 17.6b The suspension of barium sulfate coats the intestinal tract, which allows for greater visual detail than a traditional X-ray. (credit modification of work by glitzy queen00, PD)

Further diagnostic testing can be done using barium sulfate and fluoroscopy. In fluoroscopy, a continuous X-ray is passed through the body so the doctor can monitor, on a TV or computer screen, the barium sulfate’s movement as it passes through the digestive tract. Medical imaging using barium sulfate can be used to diagnose acid reflux disease, Crohn’s disease, and ulcers in addition to other conditions.

Visit Barium X-Rays (Upper and Lower GI) at Johns Hopkins Medicine for more information on how barium is used in medical diagnoses and which conditions it is used to diagnose.

Predicting Precipitation

The equation that describes the equilibrium between solid calcium carbonate and its solvated ions is:

[latex]\text{CaCO}_3(s)\;{\rightleftharpoons}\;\text{Ca}^{2+}(aq)\;+\;\text{CO}_3^{\;\;2-}(aq)[/latex]

We can establish this equilibrium either by adding solid calcium carbonate to water or by mixing a solution that contains calcium ions with a solution that contains carbonate ions. If we add calcium carbonate to water, the solid will dissolve until the concentrations are such that the value of the reaction quotient (Q = [Ca2+][CO32-]) is equal to the solubility product (Ksp = 8.7 × 10–9). If we mix a solution of calcium nitrate, which contains Ca2+ ions, with a solution of sodium carbonate, which contains CO32- ions, the slightly soluble ionic solid CaCO3 will precipitate, provided that the concentrations of Ca2+ and CO32- ions are such that Q is greater than Ksp for the mixture. The reaction shifts to the left and the concentrations of the ions are reduced by formation of the solid until the value of Q equals Ksp. A saturated solution in equilibrium with the undissolved solid will result. If the concentrations are such that Q is less than Ksp, then the solution is not saturated and no precipitate will form.

We can compare numerical values of Q with Ksp to predict whether precipitation will occur, as Example 5 shows. (Note: Since all forms of equilibrium constants are temperature dependent, we will assume a room temperature environment going forward in this chapter unless a different temperature value is explicitly specified.)

Example 17.6e

Precipitation of Mg(OH)2

The first step in the preparation of magnesium metal is the precipitation of Mg(OH)2 from sea water by the addition of lime, Ca(OH)2, a readily available inexpensive source of OH– ion:

[latex]\text{Mg(OH)}_2(s)\;{\rightleftharpoons}\;\text{Mg}^{2+}(aq)\;+\;2\text{OH}^{-}(aq)\;\;\;\;\;\;\;K_{\text{sp}} = 8.9\;\times\;10^{-12}[/latex]

The concentration of Mg2+(aq) in sea water is 0.0537 M. Will Mg(OH)2 precipitate when enough Ca(OH)2 is added to give a [OH–] of 0.0010 M?

Solution

This problem asks whether the reaction:

[latex]\text{Mg(OH)}_2(s)\;{\leftrightharpoons}\;\text{Mg}^{2+}(aq)\;+\;2\text{OH}^{-}(aq)[/latex]

shifts to the left and forms solid Mg(OH)2 when [Mg2+] = 0.0537 M and [OH–] = 0.0010 M. The reaction shifts to the left if Q is greater than Ksp. Calculation of the reaction quotient under these conditions is shown here:

[latex]Q = [\text{Mg}^{2+}][\text{OH}^{-}]^2 = (0.0537)(0.0010)^2 = 5.4\;\times\;10^{-8}[/latex]

Because Q is greater than Ksp (Q = 5.4 × 10–8 is larger than Ksp = 8.9 × 10–12), we can expect the reaction to shift to the left and form solid magnesium hydroxide. Mg(OH)2(s) forms until the concentrations of magnesium ion and hydroxide ion are reduced sufficiently so that the value of Q is equal to Ksp.

 

Example 17.6f

Precipitation of AgCl upon Mixing Solutions

Does silver chloride precipitate when equal volumes of a 2.0 × 10–4–M solution of AgNO3 and a 2.0 × 10–4–M solution of NaCl are mixed?

(Note: The solution also contains Na+ and NO3– ions, but when referring to solubility rules, one can see that sodium nitrate is very soluble and cannot form a precipitate.)

Solution

The equation for the equilibrium between solid silver chloride, silver ion, and chloride ion is:

[latex]\text{AgCl}(s)\;{\rightleftharpoons}\;\text{Ag}^{+}(aq)\;+\;\text{Cl}^{-}(aq)[/latex]

The solubility product is 1.6 × 10–10 (see Appendix K).

AgCl will precipitate if the reaction quotient calculated from the concentrations in the mixture of AgNO3 and NaCl is greater than Ksp. The volume doubles when we mix equal volumes of AgNO3 and NaCl solutions, so each concentration is reduced to half its initial value. Consequently, immediately upon mixing, [Ag+] and [Cl–] are both equal to:

[latex]\frac{1}{2}(2.0\;\times\;10^{-4})\;M = 1.0\;\times\;10^{-4}\;M[/latex]

The reaction quotient, Q, is momentarily greater than Ksp for AgCl, so a supersaturated solution is formed:

[latex]Q = [\text{Ag}^{+}][\text{Cl}^{-}] = (1.0\;\times\;10^{-4})(1.0\;\times\;10^{-4}) = 1.0\;\times\;10^{-8}\;{\geq}\;K_{\text{sp}}[/latex]

Since supersaturated solutions are unstable, AgCl will precipitate from the mixture until the solution returns to equilibrium, with Q equal to Ksp.

Exercise 17.6d

Will KClO4 precipitate when 20 mL of a 0.050-M solution of K+ is added to 80 mL of a 0.50-M solution of ClO4–? (Remember to calculate the new concentration of each ion after mixing the solutions before plugging into the reaction quotient expression.)

Check Your Answer[4]

In the previous two examples, we have seen that Mg(OH)2 or AgCl precipitate when Q is greater than Ksp. In general, when a solution of a soluble salt of the Mm+ ion is mixed with a solution of a soluble salt of the Xn– ion, the solid, MpXq precipitates if the value of Q for the mixture of Mm+ and Xn– is greater than Ksp for MpXq. Thus, if we know the concentration of one of the ions of a slightly soluble ionic solid and the value for the solubility product of the solid, then we can calculate the concentration that the other ion must exceed for precipitation to begin. To simplify the calculation, we will assume that precipitation begins when the reaction quotient becomes equal to the solubility product constant.

Example 17.6g

Precipitation of Calcium Oxalate

Blood will not clot if calcium ions are removed from its plasma. Some blood collection tubes contain salts of the oxalate ion, C2O42-, for this purpose (Figure 17.6c). At sufficiently high concentrations, the calcium and oxalate ions form solid, CaC2O4·H2O (which also contains water bound in the solid). The concentration of Ca2+ in a sample of blood serum is 2.2 × 10–3M. What concentration of C2O42- ion must be established before CaC2O4·H2O begins to precipitate?

A photograph is shown of 6 vials of blood resting on and near a black and white document. Two of the vials have purple caps, three have tan caps, and one has a red cap. Each has a label and the vials with tan caps have a small amount of an off-white material present in a layer at the base of the vial.
Figure 17.6c Anticoagulants can be added to blood that will combine with the Ca2+ ions in blood serum and prevent the blood from clotting. (credit: modification of work by Neeta Lind, CC BY 2.0)

Solution

The equilibrium expression is:

[latex]\text{CaC}_2\text{O}_4(s)\;{\rightleftharpoons}\;\text{Ca}^{2+}(aq)\;+\;\text{C}_2\text{O}_4^{\;\;2-}(aq)[/latex]

For this reaction:

[latex]K_{\text{sp}} = [\text{Ca}^{2+}][\text{C}_2\text{O}_4^{\;\;2-}] = 1.96\;\times\;10^{-8}[/latex]

(see Appendix K)

CaC2O4 does not appear in this expression because it is a solid. Water does not appear because it is the solvent.

Solid CaC2O4 does not begin to form until Q equals Ksp. Because we know Ksp and [Ca2+], we can solve for the concentration of C2O42- that is necessary to produce the first trace of solid:

[latex]Q = K_{\text{sp}} = [\text{Ca}^{2+}][\text{C}_2\text{O}_4^{\;\;2-}] = 1.96\;\times\;10^{-8}[/latex]
[latex](2.2\;\times\;10^{-3})[\text{C}_2\text{O}_4^{\;\;2-}] = 1.96\;\times\;10^{-8}[/latex]
[latex][\text{C}_2\text{O}_4^{\;\;2-}] = \frac{1.96\;\times\;10^{-8}}{2.2\;\times\;10^{-3}} = 8.9\;\times\;10^{-6}[/latex]

A concentration of C2O42- = 8.9 × 10–6 M is necessary to initiate the precipitation of CaC2O4 under these conditions.

Exercise 17.6e

If a solution contains 0.0020 mol of CrO42– per litre, what concentration of Ag+ ion must be reached by adding solid AgNO3 before Ag2CrO4 begins to precipitate? Neglect any increase in volume upon adding the solid silver nitrate.

Check Your Answer[5]

It is sometimes useful to know the concentration of an ion that remains in solution after precipitation. We can use the solubility product for this calculation too: If we know the value of Ksp and the concentration of one ion in solution, we can calculate the concentration of the second ion remaining in solution. The calculation is of the same type as that in Example 17.6g—calculation of the concentration of a species in an equilibrium mixture from the concentrations of the other species and the equilibrium constant. However, the concentrations are different; we are calculating concentrations after precipitation is complete, rather than at the start of precipitation.

Example 17.6h

Concentrations Following Precipitation

Clothing washed in water that has a manganese [Mn2+(aq)] concentration exceeding 0.1 mg/L (1.8 × 10–6M) may be stained by the manganese upon oxidation, but the amount of Mn2+ in the water can be reduced by adding a base. If a person doing laundry wishes to add a buffer to keep the pH high enough to precipitate the manganese as the hydroxide, Mn(OH)2, what pH is required to keep [Mn2+] equal to 1.8 × 10–6M?

Solution

The dissolution of Mn(OH)2 is described by the equation:

[latex]\text{Mn(OH)}_2(s)\;{\rightleftharpoons}\;\text{Mn}^{2+}(aq)\;+\;2\text{OH}^{-}(aq)\;\;\;\;\;\;\;K_{\text{sp}} = 2\;\times\;10^{-3}[/latex]

We need to calculate the concentration of OH– when the concentration of Mn2+ is 1.8 × 10–6M. From that, we calculate the pH. At equilibrium:

[latex]K_{\text{sp}} = [\text{Mn}^{2+}][\text{OH}^{-}]^2[/latex]

or

[latex](1.8\;\times\;10^{-6})[\text{OH}^{-}]^2 = 2\;\times\;10^{-3}[/latex]

so

[latex][\text{OH}^{-}] = 3.3\;\times\;10^{-4}\;M[/latex]

Now we calculate the pH from the pOH:

[latex]\text{pOH} = -\text{log}[\text{OH}^{-}] = -\text{log}(3.3\;\times\;10\;-\;4) = 3.48[/latex]
[latex]\text{pH} = 14.00\;-\;\text{pOH} = 14.00\;-\;3.80 = 10.52[/latex]

If the person doing laundry adds a base, such as the sodium silicate (Na4SiO4) in some detergents, to the wash water until the pH is raised to 10.52, the manganese ion will be reduced to a concentration of 1.8 × 10–6M; at that concentration or less, the ion will not stain clothing.

Exercise 17.6f

The first step in the preparation of magnesium metal is the precipitation of Mg(OH)2 from sea water by the addition of Ca(OH)2. The concentration of Mg2+(aq) in sea water is 5.37 × 10–2M. Calculate the pH at which [Mg2+] is diminished to 1.0 × 10–5M by the addition of Ca(OH)2.

Check Your Answer[6]

Due to their light sensitivity, mixtures of silver halides are used in fibre optics for medical lasers, in photochromic eyeglass lenses (glass lenses that automatically darken when exposed to sunlight), and—before the advent of digital photography—in photographic film. Even though AgCl (Ksp = 1.6 × 10–10), AgBr (Ksp = 5.0 × 10–13), and AgI (Ksp = 1.5 × 10–16) are each quite insoluble, we cannot prepare a homogeneous solid mixture of them by adding Ag+ to a solution of Cl–, Br–, and I–; essentially all of the AgI will precipitate before any of the other solid halides form because of its smaller value for Ksp. However, we can prepare a homogeneous mixture of the solids by slowly adding a solution of Cl–, Br–, and I– to a solution of Ag+.

When two anions form slightly soluble compounds with the same cation, or when two cations form slightly soluble compounds with the same anion, the less soluble compound (usually, the compound with the smaller Ksp) generally precipitates first when we add a precipitating agent to a solution containing both anions (or both cations). When the Ksp values of the two compounds differ by two orders of magnitude or more (e.g., 10–2 vs. 10–4), almost all of the less soluble compound precipitates before any of the more soluble one does. This is an example of selective precipitation, where a reagent is added to a solution of dissolved ions causing one of the ions to precipitate out before the rest.

The Role of Precipitation in Wastewater Treatment

Solubility equilibria are useful tools in the treatment of wastewater carried out in facilities that may treat the municipal water in your city or town (Figure 17.6d). Specifically, selective precipitation is used to remove contaminants from wastewater before it is released back into natural bodies of water. For example, phosphate ions (PO42-) are often present in the water discharged from manufacturing facilities. An abundance of phosphate causes excess algae to grow, which impacts the amount of oxygen available for marine life as well as making water unsuitable for human consumption.

A color photograph is shown of a high volume wastewater treatment facility. Nineteen large circular pools of water undergoing treatment are visible across the center of the photograph. A building and parking lot are visible in the foreground.
Figure 17.6d Wastewater treatment facilities, such as this one, remove contaminants from wastewater before the water is released back into the natural environment. (credit: work by eutrophication&hypoxia, CC BY 2.0)

One common way to remove phosphates from water is by the addition of calcium hydroxide, known as lime, Ca(OH)2. The lime is converted into calcium carbonate, a strong base, in the water. As the water is made more basic, the calcium ions react with phosphate ions to produce hydroxylapatite, Ca5(PO4)3(OH), which then precipitates out of the solution:

[latex]5\text{Ca}^{2+}\;+\;3\text{PO}_4^{\;\;3-}\;+\;\text{OH}^{-}\;{\leftrightharpoons}\;\text{Ca}_{10}(\text{PO}_4)_6{\cdot}(\text{OH})_2(s)[/latex]

The precipitate is then removed by filtration and the water is brought back to a neutral pH by the addition of CO2 in a recarbonation process. Other chemicals can also be used for the removal of phosphates by precipitation, including iron(III) chloride and aluminum sulfate.

View Phosphorus Removal – Wastewater for more information on how phosphorus is removed from wastewater.

Common Ion Effect

As we saw when we discussed buffer solutions, the hydronium ion concentration of an aqueous solution of acetic acid decreases when the strong electrolyte sodium acetate, NaCH3CO2, is added. We can explain this effect using Le Châtelier’s principle. The addition of acetate ions causes the equilibrium to shift to the left, decreasing the concentration of H3O+ to compensate for the increased acetate ion concentration. This increases the concentration of CH3CO2H:

[latex]\text{CH}_3\text{CO}_2\text{H}\;+\;\text{H}_2\text{O}\;{\rightleftharpoons}\;\text{H}_3\text{O}^{+}\;+\;\text{CH}_3\text{CO}_2^{\;\;-}[/latex]

Because sodium acetate and acetic acid have the acetate ion in common, the influence on the equilibrium is called the common ion effect.

The common ion effect can also have a direct effect on solubility equilibria. Suppose we are looking at the reaction where silver iodide is dissolved:

[latex]\text{AgI}(s)\;{\rightleftharpoons}\;\text{Ag}^{+}(aq)\;+\;\text{I}^{-}(aq)[/latex]

If we were to add potassium iodide (KI) to this solution, we would be adding a substance that shares a common ion with silver iodide. Le Châtelier’s principle tells us that when a change is made to a system at equilibrium, the reaction will shift to counteract that change. In this example, there would be an excess of iodide ions, so the reaction would shift toward the left, causing more silver iodide to precipitate out of solution.

Example 17.6i

Common Ion Effect

Calculate the molar solubility of cadmium sulfide (CdS) in a 0.010-M solution of cadmium bromide (CdBr2). The Ksp of CdS is 1.0 × 10–28.

Solution

The first thing you should notice is that the cadmium sulfide is dissolved in a solution that contains cadmium ions. We need to use an ICE table to set up this problem and include the CdBr2 concentration as a contributor of cadmium ions:

[latex]\text{CdS}(s)\;{\leftrightharpoons}\;\text{Cd}^{2+}(aq)\;+\;\text{S}^{2-}(aq)[/latex]


This table has two main columns and four rows. The first row for the first column does not have a heading and then has the following in the first column: Initial concentration ( M ), Change ( M ), and Equilibrium concentration ( M ). The second column has the header, “C d S equilibrium arrow C d to the second power plus S to the second power superscript negative sign.” Under the second column is a subgroup of three rows and three columns. The first column is blank. The second column has the following: 0.010, x, 0.010 plus x. The third column has the following: 0, x, 0 plus x equals x.

[latex]K_{\text{sp}} = [\text{Cd}^{2+}][\text{S}^{2-}] = 1.0\;\times\;10^{-28}[/latex]
[latex](0.010\;+\;x)(x) = 1.0\;\times\;10^{-28}[/latex]
[latex]x^2\;+\;0.010x\;-\;1.0\;\times\;10^{-28} = 0[/latex]

We can solve this equation using the quadratic formula, but we can also make an assumption to make this calculation much simpler. Since the Ksp value is so small compared with the cadmium concentration, we can assume that the change between the initial concentration and the equilibrium concentration is negligible, so that 0.010 + x ~ 0.010. Going back to our Ksp expression, we would now get:

[latex]K_{\text{sp}} = [\text{Cd}^{2+}][\text{S}^{2-}] = 1.0\;\times\;10^{-28}[/latex]
[latex](0.010)(x) = 1.0\;\times\;10^{-28}[/latex]
[latex]x = 1.0\;\times\;10^{-26}[/latex]

Therefore, the molar solubility of CdS in this solution is 1.0 × 10–26M.

Exercise 17.6g

Calculate the molar solubility of aluminum hydroxide, Al(OH)3, in a 0.015-M solution of aluminum nitrate, Al(NO3)3. The Ksp of Al(OH)3 is 2 × 10–32.

Check Your Answer[7]

Key Equations

  • [latex]\text{M}_p\text{X}_q(s)\;{\leftrightharpoons}\;p\text{M}^{\text{m}+}(aq)\;+\;q\text{X}^{\text{n}-}(aq)\;\;\;\;\;\;\;K_{\text{sp}} = [\text{M}^{\text{m}+}]^p[\text{X}^{\text{n}-}]^q[/latex]

Attribution & References

Except where otherwise noted, this page is adapted by David Wegman from “15.1 Precipitation and Dissolution” In General Chemistry 1 & 2 by Rice University, a derivative of Chemistry (Open Stax) by Paul Flowers, Klaus Theopold, Richard Langley & William R. Robinson and is licensed under CC BY 4.0. ​Access for free at Chemistry (OpenStax)
    1. [latex]\text{BaSO}_4(s)\;{\rightleftharpoons}\;\text{Ba}^{2+}(aq)\;+\;\text{SO}_4^{\;\;2-}(aq)\;\;\;\;\;\;\;K_{\text{sp}} = [\text{Ba}^{2+}][\text{SO}_4^{\;\;2-}][/latex];
    2. [latex]\text{Ag}_2\text{SO}_4(s)\;{\rightleftharpoons}\;2\text{Ag}^{+}(aq)\;+\;\text{SO}_4^{\;\;2-}(aq)\;\;\;\;\;\;\;K_{\text{sp}} = [\text{Ag}^{+}]^2[\text{SO}_4^{\;\;2-}][/latex];
    3. [latex]\text{Al(OH)}_3(s)\;{\rightleftharpoons}\;\text{Al}^{2+}(aq)\;+\;3\text{OH}^{-}(aq)\;\;\;\;\;\;\;K_{\text{sp}} = [\text{Al}^{3+}][\text{OH}^{-}]^3[/latex];
    4. [latex]\text{Pb(OH)Cl}(s)\;{\rightleftharpoons}\;\text{Pb}^{2+}(aq)\;+\;\text{OH}^{-}(aq)\;+\;\text{Cl}^{-}(aq)\;\;\;\;\;\;\;K_{\text{sp}} = [\text{Pb}^{2+}][\text{OH}^{-}][\text{Cl}^{-}][/latex]
    ↵
  2. d) 8.99 x 10-12 ↵
  3. 1.2 × 10–8 M ↵
  4. No, Q = 4.0 × 10–3, which is less than Ksp = 1.05 × 10–2 ↵
  5. 4.5 × 10–9M ↵
  6. 10.97 ↵
  7. 1 × 10–10M ↵
definition

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Chemistry v. 1 backup Copyright © 2023 by Gregory Anderson; Caryn Fahey; Jackie MacDonald; Adrienne Richards; Samantha Sullivan Sauer; J.R. van Haarlem; and David Wegman is licensed under a Creative Commons Attribution 4.0 International License, except where otherwise noted.

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