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Let me ask a different sort of question. If you have a reef tank with a total alkalinity of 7 dKH at a pH of 8.5, does your method give exactly the same result (7 dKH, within the claimed error) as when the alkalinity is 7 dKH and the pH starts at pH 7.7?
The total amount of CO2 is obviously very different, and that is known to impact the proper pH endpoint of aa total alkalinity titration, making any particular pH endpoint not exactly right for both cases.
But I'm wondering how it impacts your method which is not simply a pH titration.
TIA.
The method should be expected to perform similarly to the titration to a single set endpoint (that is, the more CO2 in the sample, the lower the alkalinity measured). The Hanna alkalinity reagents contain both an acid and an indicator which changes in intensity based on the pH. The best way to think of it is by putting a quantitative color measurement to the intensity of the indicator in a titration. Of course, in this method, we cannot compensate for changes in endpoint.
EPA 310.1 states that the titration goes to pH 4.5 (except for in rare cases). Standard Methods 2320B (AWWA, APHA, WEF) suggests changes based on alkalinity values. You are right - the pH value at which the equivalence point occurs changes based on the amount of CO2 in the solution. In the cases of typical instrumentation though, it’s challenging to pick a set pH value for all samples. The “best” way to determine alkalinity would be to determine the equivalence point directly, by way of an automatic (or manual) derivative plot of the pH over volume. This way, we can choose the inflection point regardless of the effect of CO2 on our samples.





