Calibration and Titration of a Santa Ana River water sample
Calibration Titration
These variations can be linearized, using the Nernst function, by determining the concentration of protons in the solution as a result of the addition of the acid, in this case no bases are titrated. Lets plot the change in potential as a function of the logarithm of the proton concentration. One obtains a linear relationship from which one can determine, by standard statistical methods the slope (kT) and the intercept (EGo):
Titration of a water sample from the Santa Ana River
In a second step, one replaces the KCl solution by a filtered water sample. The titration curve becomes:
![]()
On the figure above are plotted the two Gran's functions F1 and F2. These functions serve to determine the volume equivalent, using F2 to compute the titration alkalinity in this case, and the protonation constant KHA of the acid/base system being titrated before the equivalent volume, using F1
Conclusions