Acid-base, or H+ transfer, reactions are crucial to
organic chemistry for both practical and theoretical reasons.
At a simple, practical level: many reaction rates
can be influenced by adding acids and bases. An acid can make a
substrate into a better electron acceptor (more electrophilic),
while a base can make a substrate into a better electron donor (more
nucleophilic). Therefore, acids and bases are used to promote, and
even catalyze, chemical reactions.
Equally important, H+ transfer changes a molecule's
ionization state. Organic ions are often more water-soluble than
their neutral counterparts, so acid-base chemistry may offer a way
to separate organic compounds (the ions dissolve in any water that
is present and leave the neutrals behind).
Water solubility also determines how a substance will
migrate through our bodies and penetrate our cells. Water solubility
also determines how a compound moves through the natural environment.
Therefore, the acid-base reactivity of organic molecules plays an
important role in medicinal and environmental chemistry.
Finally, the theory of acid-base reactivity guides our thinking about most other kinds of reactivity. Most organic reactions involve charge transfer and bond breaking and/or bond making. Acid-base reactions are the simplest kind
of reaction of this type. Therefore, chemists have expended considerable effort in trying to understand what structural factors make a molecule a strong acid or base.
pKa tables
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