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Analytical Chemistry Homework

Due Wednesday Week 6

Problems 6-26: 9-17,23,29: 7-7,8,11

6-26. A solution contains 0.0500 M Ca2+ and 0.0300 M Ag+. Can 99.00% of either ion be precipitated by addition of sulfate without precipitating the other metal ion? What will be the concentration of Ca2+ when Ag2SO4 begins to precipicate?

Physical – a solution with [Ca2+] = 0.0500 M and [Ag+] = 0.0300 M. “Can 99% of either ion be precipitated by addition of sulfate, without precipitating the other metal ion?” We are going to add sulfate until one precipitates until only 1% of it is left as ions in solution. Which one?

Ksp for silver sulfate is 1.5 x 10-5 Ag2SO4(s) <= => 2 Ag+ + SO42-

Ksp for calcium sulfate is 2.4 x 10-5 CaSO4(s) <= => Ca2+ + SO42-

Ksp for barium sulfate is 1.1 x 10-10 BaSO4(s) <= => Ba2+ + SO42-

Ksp = [Ca2+][SO42-] Ksp = [Ag+]2 [SO42-]

Calcium least soluble – will precipitate first. Final [Ca2+] = .000500 M (1% of initial)

At this point the equilibrium with sulfate will be

[SO42-] = Ksp / [Ca2+] = 2.4 x 10-5/0.000500 = 0.048 M

______

So [Ag+] =  Ksp/ [SO42-] =  1.5x10-5/0.048 = .0177 M

this is lower than .0300 M so some of the silver has already precipitated at this level of sulfate.

.0177/0.0300 x 100% = 59% so 59% of the original silver is left in solution and 41% has precipitated.

What can we learn from this? We can not use sulfate precipitation to remove a calcium ion interferent from a silver solution. Nor can we analyze calcium ion with this methos in the presence of silver ion.

What about the second half of the question? When does silver sulfate begin to precipitate?

[SO42-] = Ksp/ [Ag+]2 = 1.5 x 10-5/ (0.0300)2 = 0.01667 M

[Ca2+] = Ksp /[SO42-] = 2.4 x 10-5 / 0.01667 = 1.4 x 10-3 M

1.4 x 10-3 M/0.0500 M x 100% = 2.8%

When silver sulfate starts to precipitate, 97% of the calcium has precipitated. And when calcium from 97 to 99% precipitated, silver ion goes from 0 to 41% precipitated.

9-17 a) Why do many rivers in Box 9-1. lie on the line [HCO3-] = 2[Ca2+]?

According to Box 9-1, the source of calcium in the rivers is the mineral calcite, which dissolves by reacting with carbon dioxide in the river waver according to the equation:

CaCO3(s) + CO2(aq) + H2O < == > Ca2+ + 2 HCO3-

If the predominate product is bicarbonate and not carbonate or carbonic acid,then the mass balance of this reaction is [HCO3-] = 2[Ca2+]. Rivers on the line [HCO3-] = 2[Ca2+]

are saturated with calcite.

b) What is happening in rivers that lie above the line [HCO3-] = 2[Ca2+]?

Rivers above the line [HCO3-] = 2[Ca2+] contain more bicarbonate than Ca2+. These rivers are not saturated with calcite.

c) The Rio Grande lies below the line [HCO3-] = 2[Ca2+]. Propose a hypothesis for what might be happening in this river.

The Rio Grande has more Ca2+ than expected from dissolved calcite. Therefore there is probably another source of calcium ions than calcite. This source is likely to be more soluble than calcite. For example, CaSO4 found in anhydrite and gypsum is 104 times more soluble than calcite. Perhaps the Rio Grande flows over minerals like this that are more soluble than calcite.

9-23.a) Charge balance

[NH4+] + [H+] = 2 [SO42-] + [HSO4-] + [OH-]

b)mass balance

[NH3] + [NH4+] = 2 [SO42-] + 2 [HSO4-]

c) Want to determine ammonia concentration so we will aim to get everything solved for ammonia.

[H+] = 10-9.25 M = 5.62 x 10-10 so [OH-] = 1.00 x 10-14 / 5.62 x 10-10 = 1.78 x 10-5

Ka = [NH3][H+]/[NH4+] solving for ammonium ion gives

[NH4+] = [NH3][H+]/ Ka = 5.62 x 10-10/ 5.70 x 10-10 [NH3] = 0.986 [NH3]

Kb = [HSO4-][OH-]/[SO42-] solving for hydrogen sulfate gives

[HSO4-] = Kb [SO42-]/[OH-] = 9.80 x 10-13/1.78 x 10-5 [SO42-] = 5.51x10-8 [SO42-]

now let’s substitute what we know into the mass balance equation

[NH3] + [NH4+] = 2 [SO42-] + 2 [HSO4-]

[NH3] + 0.986 [NH3] = 2 [SO42-] + 2 x 5.51x10-8 [SO42-] = 2 + 1.10x10-7 [SO42-]

1.986 [NH3] = 2 [SO42-]  [SO42-] = 0.993 [NH3]

Now putting all of the ammonia terms into the Ksp gives

Ksp = [NH4+]2[SO42-] = {0.986 [NH3]}2 {0.993[NH3]} = 0.9654 [NH3]3

[NH3]3 = 276/0.9654 = 286

[NH3] = 6.59 M

7-7. How many milliliters of 0.100 M KI are needed to react with 40.0 mL of 0.0400 M Hg2(NO3)2 if the reaction is Hg22+ + 2 I- Hg2I2(s)?

40.0 mL x 0.0400 mmol Hg22+/mL x 2 mmol I-/1 mmol Hg22+ x 1 mL/0.100 mmol I- =

32.0 mL

7-8. For reaction 7-1, how many milliliters of 0.1650 M KMnO4 are needed to react with 108.0 mL of 0.1650 oxalic acid? How many milliliters of 0.1650 M oxalic acid are required to reaction with 108.0 mL of 0.1650 M KMnO4?

The chemical equation is (using C2O4H2 for oxalic acid)

5 C2O4H2 + 2 MnO4- + 6 H+  10 CO2 + 2 Mn2+ + 8 H2O

The long way to do this is through the stoichiometry

108.0 mL x 0.1650 mmol oxalic/mL x 2 mol MnO4-/5 mol oxalic x 1 mL/0.1650 mol MnO4-

= 43.20 mL MnO4- solution

An easy way is to note that the reagents have the same concentration. Therefore, the volume of permanganate needed is 2/5 of the volume of oxalic acid.

i.e. 108.0 mL x 2/5 = 43.0 mL

For the second part of the question

Volume of oxalic acid needed is = 5/2 volume of MnO4- = 108.0 x 5/2 = 270.0 mL

7-11. Limestone consists mainly of the mineral calcite, CaCO3. The carbonate content of 0.5413g of powdered limestone was measured by suspending the powder in water, adding 10.00 mL of 1.396 M HCl, and heating to dissolvethe solid and expel CO2.

CaCO3(s) + 2 H+ == > Ca2+ + CO2(g) + H2O

FW 100.087

The excess acid required 39.96 mL of 0.1004 M NaOH for complete titration to a phenolphthalein end point. Find the weight percent of calcite in the limestone.

This is like a back titration. Some of the acid reacts with carbonate in the above reaction and the rest reacts with the hydroxide. We get the amount that reacts with carbonate by knowing the total moles of acid and subtracting the amount that reacts with hydroxide in the titration.

Total HCl is 10.00 mL x 1.396 mmol/mL = 13.96 mmol H+

The hydroxide required is 39.96 mL x 0.1004 mmol/mL = 4.012 mmol OH-

Since 1 OH- reacts with one H+, the titration reacted with 4.012 mmol H+

Therefore, 13.96 – 4.012 = 9.948 mmol H+ were consumed in the reaction with carbonate.

9.948 mmol H+ x 1 mmol CaCO3/2 mmol H+ x 100.087 mg/mmol = 497.8 mg of CaCO3

Weight Percent in sample is

0.4978 CaCO3/ 0.5413 x 100% = 91.96 % = 92.0 wt %