Aldehydes & Ketones: Carbonyl Addition

hydrate

If you drop an aldehyde or ketone into water, a little of it quietly reacts with the water itself. The water molecule adds across the C=O bond, and the product is a hydrate, a carbon bearing two -OH groups on the same carbon. Chemists call this arrangement a geminal diol (gem-diol), 'geminal' meaning the two like groups are twins on one atom.

Mechanistically it is plain nucleophilic addition: water's oxygen (the nucleophile) attacks the carbonyl carbon, the C=O electrons go onto the oxygen, and after proton shuffling you have HO-C-OH. The reaction is an equilibrium, and for most ordinary aldehydes and ketones it lies far to the carbonyl side, so only a tiny fraction is hydrated at any moment. But the position of the equilibrium depends strongly on the carbonyl: formaldehyde is almost completely hydrated in water, and trichloroacetaldehyde forms a stable, isolable hydrate (chloral hydrate) because the electron-withdrawing chlorines make the carbonyl extra hungry for the nucleophile.

Hydrates are usually a side note rather than a synthetic goal, because gem-diols are typically unstable and revert to the carbonyl plus water. But they are an honest, simple template for the whole nucleophilic-addition family: hemiacetals (with an alcohol instead of water) and the rest are just the same dance with a different partner.

Formaldehyde (H2C=O) in water exists overwhelmingly as its hydrate, methylene glycol, H2C(OH)2; this is why 'formalin' solutions behave the way they do.

A hydrate is one carbon carrying two OH groups (a gem-diol), made by adding water across C=O.

Do not confuse this organic gem-diol 'hydrate' with the everyday meaning of 'hydrate' in inorganic chemistry (e.g. CuSO4 5H2O), where water of crystallization is just held in the crystal, not bonded across a C=O.

Also called
gem-diolgeminal diol碳水合物偕二醇