Ig. Dance et al., REACTIONS OF 29 TRANSITION-METAL CATIONS, IN THE SAME OXIDATION-STATEAND UNDER THE SAME GAS-PHASE CONDITIONS, WITH SULFUR, Inorganic chemistry, 35(14), 1996, pp. 4177-4184
A total of 29 transition metals (all except Tc), all as ions M(+), hav
e been reacted with gaseous S-8. The reactivities and reaction product
s provide a unique set of comparative data on a fundamental reaction o
f the elements. The results underlie the interpretation of many other
processes and compounds in condensed phases. Series of product ions [M
S(y)](+) are formed, with y generally starting at 4, and increasing wi
th time through 8 up to 10, 12, 16, or 21 (for La+). A general mechani
sm is proposed, in which the first {MS(8)}(+) encounter complex is rea
ctive and undergoes S-S bond scission and rearrangement around the met
al, such that [MS(8)](+) is not an early product. The early transition
metals react faster than later members of the series, and third row m
etals react about twice as fast as first row metals. The metals which
are more chalcophilic in condensed-phase chemistry are apparently less
so as M(+); Hg+ does not form observable [HgSy](+) (except for a very
low yield of [HgS3](+)) and is remarkably less reactive with sulfur t
han most of the other metal ions. Simple electron transfer between M() and S-8 does not occur except possibly for Ir+, but S-8(+) is someti
mes observed and is believed to be formed by electron transfer from S-
8 to some [MS(y)](+) complexes. Interpretation of the rates of reactio
n of the ions of groups 3, 4, and 5 with S-8 is complicated because th
ey react with adventitious water in the cell forming ore-species. The
results are discussed in the context of condensed-phase metal polysulf
ide chemistry.