10 mL aliquots of a natural water sample were pipetted into 50 mL volumetric
flasks. Exactly 0, 5, 10, 15 and 20mL of a standard solution containing 11.1ppm
of Fe
3+ were added to each flask, followed by an excess of thiocynate ion to give
the red complex Fe(SCN)
2+
. After dilution to volume, the instrument response for
each of the five solutions, measured with a colorimeter, was found to be 0.240, 0.437, 0.621, 0.809 and 1.009 respectively. Determine the original concentration
of Fe
3+
in the water sample. (2 points)