Originally posted by Marvin
This is actually more simple than it looks. Reactions which produce pH changes have redox potentials which alter in a big way depending on the pH.
In essenance, certain oxidising agents are really powerful, or really whimpy in strong acid or strong base.
Alter the pH enough, and you can do tricks, molten hydroxides are about as extreme a pH change as you can get without resorting to some highly obscure
solvents/systems.
In this way permanganate is not possible becuase the ion that uses up the most base is manganate(VI), so on fusing manganese dioxide with a alkali
hydroxide atmospheric oxygen (which isnt affected by the pH changes) is a strong enough oxidising agent to produce this. Fortunatly, when you add
acid the reverse happens, manganate(VI) becomes strong enough to oxidise itself, and it disproportionates to manganese dioxide and permanganate.
Oxidising chloride, or chlorate to perchlorate doesnt use up base, so I would doubt this redox potential changes enough to be useful.
This is, it in a nutshell, my understanding of it. Ive skipped the [H+], [OH-] redox theory maths, partially because we dont need it to see how
altering the equilibrium affects the redox potential, and mainly because when it was explained to me I was busy daydreaming about nitrogen compounds
and white phosphorous manufacture. |