Question

Chloride in a water sample can be determined indirectly by atomic absorption spectrometry by precipitating chloride as AgCl(s) with a measured amount of AgNO3 that is excess of the chloride content of the sample. The AgNO3 is added and the sample is centrifuged. The remaining Ag+ in the solution (supernatant) is quantified and the chloride is measured by assuming that chloride was quantitatively precipitated.

Chloride in a water sample can be determined indirectly by atomic absorption spectrometry by precipitating chloride as AgCl(s

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Answer #1

In the exercise we must consider the following factors:

  • The relation between the absorbance and the concentration is directly proportional.
  • The stoichiometric ratio in the AgCl is 1:1.
  • The chloride was quantitatively precipitated (all the chloride are precipitated adding a know concentration of the precipitating agent).

Adding Ag(NO3)(ac) to a recipient with Cl- (ac), will form AgCl(s).

Measuring the three samples supernatant, will give us the absorbance in response of the Ag+ excess, the measure of the blank will give us the maximum absorbance value (the Ag+ didn't reaccionate there).

Doing a difference between the blank and the standard & sample, will give us the value of the Ag+ that reaccionate to form AgCl(s).

For the standard: 12,8-5,7 = 7,1.

For the sample: 12,8-6,8 = 6.

With that, we must expect that sample concentration in Cl- is smaller than 100.00ppm.

Doing a relationship knowing the Cl- concentration of the standard:

7,1 - 100.00ppm Cl-

6 -> 84.5 ppm Cl- approximately.

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