“…Since v. e > 1, one might anticipate that SOLs would be in the neoclassical Pfirsch-Schliiter (P-S, collisional) [479] regime and that the P-S drifts resulting from toroidal geometry would be important in the SOL. Some modelling of the SOL has been carried out on this basis [7,[148][149][150][151][152], but it generally leads to underestimates of the measured cross-field transport rates and of the SOL thickness X s , i.e., transport is anomalous. Thus, the more usual procedure is to ignore toroidal and neoclassical effects altogether in the SOL and to invoke anomalous cross-field transport rates for particles and heat, which are adjusted to give agreement with the measured SOL widths for particle and energy density (see Section 3.4).…”