“…Most previous reports (19)(20)(21)(22) described essentially synthetic investigations of 1, including a valuable study (21) of the formation of betaines by reaction with tertiary amines in glacial acetic acid and certain other media. Two kinetic studies have been reported (8b, 23); the former concluded that the cation CH2=CHSO2' was 'Complete set of tables giving observed first-order rate constants, product composition, and reaction conditions (5 -" k , and k, , are the exper~mental first-and second-order rate constants for reactlon wlth H 2 0 and OH-, respect~vely, kls and klc are calculated from kl = kls + klc and kls/klc = the ratlo of 4 to 5 (or of 6 to 7) In the product at pH 4 0, slmllarly k,,,,, and k,,,,, are from bH = k,,,,,, + k,,,,, and k,oHls/k,oHlc = the ratlo of 4 to 5 (or of 6 to 7) In the product at pH 10 5 to 12.7 (see d~s c u s s~o n In text) 0 1 M aqueous KC1 (plus 0 2% 1.2-d~methoxyethane) for 1 and 3, 0 05 M KC1 for CaHsS02CI and p-MeC6H4SO2C1 ' Values of k, for 1 at other temperatures are 8 86 X 10-'at I 0, 5 14 X lo-' at 17 3, 2 91 X W ' a t 35 0 , 7 18 X 10-'at 45 0, and 3 47 x lo-' s-I at 60 0°C (see also Table S1); these, after conversion to second-order rate constants (by dlvldlng by 55 5 M ) , gave AH' = 17 5 t 2 kcal mol-' and AS' = -21 t 8 cal K-' mol-I (maxlmum errors as estimated by Wlberg's method (24)) "At I 0°C kt for 3 IS 8 1 x 10-ss-l, AH' = 17.5 f 3 kcal mol-I and AS' = -21 f 10 cal K-' mol-I (also from second-order rate constants). …”