. The concentration of chloride ions can be determined indirectly using atomic absorption spectroscopy. An excess of silver ions is added to each standard and sample and a silver chloride precipitate forms. The samples are centrifuged and the supernatant is aspirated into the instrument. A silver hollow cathode lamp is used as the source. For this analysis, 5 mL of 0.1 M AgNO3 was added to each standard and sample. a. Use the following data to determine the concentration of chloride ions in a water sample. chloride, ppm Absorbance 0 0.728 250 0.554 500 0.386 750 0.214 water sample 0.327 b. Explain the behavior of the calibration curve.
Ksp of AgCl = 1.8 x 10-10
[Ag+] [Cl-] = 1.8 x 10-10
Initial mMoles of Ag+ = 5 mL * 0.1 M = 0.5
Since Ag+ is in excess,
[Ag+] after precipitation on 250 mL addition = 0.5 / (5 + 250)
= 0.00196
[Cl-] = Ksp / [Ag+] = 9.18 x 10-8 M
Similarly for other volumes, concentrations can be obtained as shown below:
Volume, mL |
Absorbance |
[Ag+] |
[Cl-] |
0 |
0.728 |
0.1 |
1.80E-09 |
250 |
0.554 |
0.001961 |
9.18E-08 |
500 |
0.386 |
0.00099 |
1.82E-07 |
750 |
0.214 |
0.000662 |
2.72E-07 |
a)
A = 241.59 [Ag+] + 0.0937
0.327 = 241.59 [Ag+] + 0.0937
[Ag+] = 0.000966 M
[Cl-] = Ksp / [Ag+]
= 1.86 x 10-7 M
b)
On addition of more water, Ag+ concentration will decrease because 1) more Ag+ ions are utilized for precipitation and 2) dilution effect. As the [Ag+] decreases the absorption coefficient also decreases.
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