Was just thinking about titrations (as you do), and was windering about the immediate colour change in the aliquot before the colour returns back to normal. Why does this happen?
Shouldnt the change in colour of the aliquot be proportional to the amount of solution added from the burette?
Thanks
There are actually three things happening.
For a titration in a controlled environment, it's a combination of mixing and reaction rates. In an uncontrolled environment, atmospheric contaminants will also alter the solution.
Before I get into that, let's look at the physical changes. For now, consider an acidic aliquot, a basic titrant and phenolphthalein indicator.
- The indicator (which are molecules like everything else) is evenly dispersed in the aliquot.
- A drop of titrant (basic, concentrated) is added to the aliquot (acidic, dilute). This forms a temporary region where the concentration of base is higher than acid.
- The indicator molecules in this region will react with base and become pink.
- As mixing takes place, the temporary region disperses. The concentration of base becomes even throughout the solution, and most of the base is neutralised by reaction with acid.
- As mixing/reaction takes place, deprotonated indicator (pink, basic) must find extra H+ in the solution to become clear again.
So, when you add a drop of base into acid, a small region of the liquid turns pink, but then quickly disappear. This is because the drop of base does not immediately mix with the liquid, so a small region of the liquid is more basic, and the indicator in that region takes on the purple basic form. This quickly disappear as the solution mixes and all the base are neutralised (indicator becomes clear again).
As you approach the equivalence point, the concentration of acid in the aliquot becomes very small. This drastically decrease the reaction rate. Even after adequate mixing has occurred, the solution can still remain pink, as the acid/base eventually neutralise each other, and the deprotonated indicator molecules (pink, basic) eventually find spare H+ to become protonated (clear, acidic). The temporary pink colour can remain for a few seconds at most.
However, a weird observation is that even after you've reached (or slightly passed) the equivalence point, sometimes the solution can go back to clear after 10 or 15 minutes. This is contrary to the belief that once you've reached the end point, it's 'permanent'. This is caused by atmospheric CO2 acidifying your nearly-neutral solution, via CO2(g) + 2H2O(l) --> HCO3-(aq) + H3O+(aq). This is what I mean by 'controlled' vs 'uncontrolled' environments: a totally controlled environment would have a totally inert atmosphere, such as pure N2.
Neat (pure, deionised) water equilibrated in normal atmosphere has a pH of 5.4~5.7. Any neutral/basic solution would tend towards this pH if left in open atmosphere for long enough: enough CO2 will eventually dissolve in the solution to turn it slightly acidic again. Because of CO2, we still don't quite understand the precise origin of water's surface tension and its surface composition. It's a bitch, really