A nucleophile such as CN⁻ dissolved in water cannot reach an organic-soluble alkyl halide sitting in a second, immiscible solvent layer — the two never meet. A quaternary ammonium salt Q⁺X⁻ (e.g. a tetrabutylammonium salt) fixes this by ferrying the anion across the interface. This is Starks' extraction mechanism (C. Starks, 1971), the founding model of phase-transfer catalysis:
(aq) Q+Br- + Na+X- ⇌ Q+X- + Na+Br- ion exchange
(aq→org) Q+X-(aq) → Q+X-(org) extraction, Kex
(org) Q+X- + R-Br → R-X + Q+Br- SN2, rate = k2[QX][RBr]
(org→aq) Q+Br-(org) → Q+Br-(aq) back-extraction, closes cycle
The catalyst is never consumed — each Q⁺ cation completes the cycle over and over, each pass converting one substrate molecule. Turnover number (TON) counts how many product molecules one average catalyst particle has produced.
- Catalyst loading — sets how many Q⁺ shuttles exist per fixed amount of substrate; more shuttles move more anions per second, up to a stirring-limited ceiling.
- Stirring rate — raises interfacial contact area and diffusion, the real-world lever for phase-transfer reaction rate; too little stirring starves the cycle even with excess catalyst.
- Anion lipophilicity — models the extraction constant Kex: soft, polarizable anions (I⁻, SCN⁻) partition into the organic phase far more readily than hard, small ones (F⁻, OH⁻), which is why PTC works well for some nucleophiles and poorly for others.
- Temperature — scales the SN2 rate constant k₂ through an Arrhenius-like factor, speeding the organic-phase step once the anion has actually arrived.
Real-world relevance: this exact catalytic cycle underlies industrial nitrile, ether and ester syntheses that avoid expensive anhydrous or dipolar-aprotic solvents — the catalyst does the solvent's job of "dissolving" the ionic reagent into the organic layer.