The Michaelis–Arbuzov reaction is initiated with the
SN2 attack of the
nucleophilic phosphorus species (
1 - A phosphite) with the
electrophilic alkyl halide (
2) to give a
phosphonium salt as an intermediate (
3). These intermediates are occasionally stable enough to be isolated, such as for triaryl phosphites which do not react to form the phosphonate without thermal cleavage of the intermediate (200 °C), or cleavage by alcohols or bases. The displaced
halide anion then usually reacts via another SN2 reaction on one of the R1 carbons, displacing the oxygen atom to give the desired phosphonate (
4) and another alkyl halide (
5). This has been supported by the observation that chiral R1 groups experience inversion of configuration at the carbon center attacked by the halide anion. This is what is expected of an SN2 reaction. Evidence also exists for a
carbocation based mechanism of dealkylation similar to an
SN1 reaction, where the R1 group initially dissociates from the phosphonium salt followed by attack of the anion. Stereochemical experiments on cyclic phosphites have revealed the presence of both pentavalent
phosphoranes and tetravalent phosphonium intermediates in
chemical equilibrium being involved in the dealkylation step of the reaction using
31P NMR. The decomposition of these intermediates is driven primarily by the
nucleophilicity of the anion. There exists many instances of the intermediate phosphonium salts being sufficiently stable that they can be isolated when the anion is weakly nucleophilic, such as with
tetrafluoroborate or
triflate anions. == Scope ==