Angewandte
Communications
Chemie
Sulfur
The First Step of the Oxidation of Elemental Sulfur: Crystal Structure
of the Homopolyatomic Sulfur Radical Cation [S8]C+
Dedicated to Professor Jack Passmore
Abstract: The oxidation of elemental sulfur in superacidic
solutions and melts is one of the oldest topics in inorganic main
group chemistry. Thus far, only three homopolyatomic sulfur
cations ([S4]2+, [S8]2+, and [S19]2+) have been characterized
crystallographically although ESR investigations have given
evidence for the presence of at least two additional homopo-
lyatomic sulfur radical cations in solution. Herein, the crystal
structure of the hitherto unknown homopolyatomic sulfur
this intense color and that of similar solutions of other p-block
elements in oleum was one of the driving forces for
investigations of such systems in superacidic media.[7]
A
large number of homopolyatomic cations of sulfur and the
other p-block elements were discovered and structurally
characterized in the solid state, and have been reviewed
numerous times.[1,4b,8] Especially the impressive work by
Gillespie, Passmore, and co-workers led to the discovery of
the three presently known and crystallographically charac-
terized homopolyatomic sulfur cations [S4]2+,[9] [S8]2+,[9a,d,10]
+
+
radical cation [S8]C is presented. The radical cation [S8]C
represents the first step of the oxidation of the S8 molecule
present in elemental sulfur. It has a structure similar to the
known structure of [S8]2+, but the transannular sulfur···sulfur
contact is significantly elongated. Quantum-chemical calcula-
tions help in understanding its structure and support its
presence in solution as a stable compound. The existence of
and [S19]2+ [9d,11]
All known structurally characterized homo-
.
polyatomic sulfur cations are dications and were crystallized
with [AsF6]ꢀ or [SbF6]ꢀ counteranions.
In superacidic solutions, the situation is much more
complicated. As early as 1957, Symons and Ingram reported
evidence for the presence of paramagnetic compounds in the
blue solutions of sulfur in oleum.[12] In the 1970s, Gillespie and
co-workers thoroughly investigated sulfur cations in super-
acidic solutions (e.g., oleum, HSO3F).[10a,11,13] In contrast to
other main group elements such as phosphorus[2b,14] and
selenium,[15] studies of sulfur and its cations are severely
hindered by the absence of a useful nucleus for NMR
spectroscopic investigations. Therefore, the characterization
is limited to the interpretation of UV/Vis, IR, and electron
spin resonance (ESR) spectra of mixtures in solution or the
determination of crystal structures from isolated solids. The
oxidation of sulfur in liquid sulfur dioxide or superacidic
media with strong oxidizing agents gives colored solutions.
ESR spectra of these solutions show three different ESR
signals, namely a minor signal at g = 2.008 and two main
signals at g = 2.027 and 2.014, which change in intensity during
the addition of AsF5.[11] These signals obviously originate
from different sulfur radical cations in different oxidation
states, and these sulfur radicals have been discussed contro-
+
[S8]C is also in accord with previous ESR investigations.
H
omopolyatomic cations of the main group elements have
been one of the main themes in p-block chemistry in the
second half of the last century. These often very simple
compounds with unusual structures forced the development
of new models in chemical bonding.[1] Lately, the synthetic
strategies and methods that were very successful in the past
did not allow for further progress. Nevertheless, by using new
methods and techniques, spectacular results were still
obtained even recently. For instance, evidence for the first
homopolyatomic phosphorus cation [P9]+ was obtained by
using modern weakly coordinating anions instead of classical
hexafluorometallates such as [AsF6]ꢀ.[2] The first homopolya-
tomic antimony cation [Sb8]2+ was stabilized even by the
simple chloro anion [GaCl4]ꢀ.[3] Recently, ionic liquids as
reaction media[4] and electrochemical syntheses[5] were intro-
duced as new strategies for the field of homopolyatomic
cations of the heavier chalcogen elements.
+
+
+
+
The first generation of a homopolyatomic cation of the
main group element sulfur was reported already in 1804,
when Buchholz observed an intense blue color upon dissolv-
ing elemental sulfur in oleum.[6] The quest for the origin of
versially. The sulfur radicals [S12]C , [S8]C , [S7]C , [S5]C , and
+
[S4]C were suggested to be the origin of these resonan-
ces.[10a,11,13,16] Eventually, the ESR signal at g = 2.014, which
appears at high concentrations of an added oxidizing agent,
+
was unambiguously assigned to [S5]C by ESR experiments
using 33S-enriched sulfur.[17] Further evidence for the presence
of additional currently unidentified sulfur cations comes from
the color of these superacidic solutions. Typically, solutions of
sulfur in a superacidic medium containing a large excess of an
oxidizing agent are blue. However, Gillespie and co-workers
discovered that solutions with a formal composition of
[S16][AsF6]2 are red and turn blue only after addition of
more oxidizing agent.[11,13] Conversely, a blue solution of
[S8][AsF6]2 takes up sulfur up to an approximate composition
[*] J. Derendorf, Prof. Dr. C. Jenne, Dr. M. Keßler
Anorganische Chemie
Fakultꢀt fꢁr Mathematik und Naturwissenschaften
Bergische Universitꢀt Wuppertal
Gaußstr. 20, 42119 Wuppertal (Germany)
E-mail: carsten.jenne@uni-wuppertal.de
Supporting information and the ORCID identification number(s) for
the author(s) of this article can be found under:
Angew. Chem. Int. Ed. 2017, 56, 1 – 5
ꢀ 2017 Wiley-VCH Verlag GmbH & Co. KGaA, Weinheim
1
These are not the final page numbers!