In: Chemistry
The alkalinity of natural waters is usually controlled by OH- , CO3 2- , and HCO3 - , which may be present alone or in combination. Titrating a 100.0 mL sample to a pH of 8.3 requires 18.70 mL of a 0.0281 M solution of HCl. A second 100.0 mL aliquot requires 48.20 mL of the same titrant to reach a pH of 4.5. Calculate the concentrations of CO3 2- and HCO3 - in ppm.
As mentioned there is no hydroxide ion concentration in the solution
the 100mL sample required 18.70mL of HCl solution to reach the pH =8.3
Hence, The first equivalence point is due to half neutralization of carbonate
CO3-2 + H+ ---> HCO3-
concentration of bicarbonate = concentration of acid used X volume of acid used / total volume
concentration of bicarbonate = 0.0281 x 18.70 / 100 = 0.0053 Moles / Litre
Second equivalence point is due to complete neutralization of HCO3- and bicarbonate, the pH = 4.5
CO3-2 + H+ ---> HCO3-
HCO3- + H+ --> H2O + CO2
so total concentration of carbonate and bicarbonate ions will be
volume of natural water X concentration = volume of HCl used X concentration of HCl
Concentration of natural water = 48.20 x 0.0281 / 100 = 0.0135
[CO3-2] = 0.0053 moles / Litres = 0.0053 X molecular weight (g / L) = 0.318 g/L = 318 mg / L = 318ppm
2X [CO3-2] + [HCO3-] = 0.0135
[HCO3-] = 0.0029 moles / Litres = 0.0029 X 61 g /L = 0.177 g /L = 177 mg / L = 177ppm