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Yunusov et al.
deuterium content 14.9 at.% is formed from methaneꢀd0
and D2 in 20 h. The K2Ru4/H2 catalyst is substantially
more active than K2Os3/H2 and K2Os3/Ar but is inferior
in activity to the K2Ru4/Ar catalyst.
Thus, as a result of our work it has been shown for the
first time that the systems based on supported potassium
salts of transition metal carbonyl hydrides are capable of
activating C—H bonds of hydrocarbons and introducing
them into hydrogen—deuterium exchange reactions.
On an increase in temperature to 200 С, the rhenium
and iron samples, KRe/Ar and K2Fe2/Ar, start also to catꢀ
alyze the H/D exchange between methaneꢀd0 and D2,
although with a lower rate. The highest activity at this temꢀ
perature is manifested by the osmium and ruthenium catꢀ
alysts K2Os3/H2, K2Ru4/Ar, and K2Ru4/H2, in the presꢀ
ence of which the deuterium content in methane reaches
26—29 at.% in 20 h. The K2Os3/Ar catalyst is less active.
The deuteration of methane during its interaction with
D2 is accompanied by the formation of HD and H2 and, as
a consequence, by a decrease in the deuterium content in
the starting D2. To reveal whether the hydrogen atoms of
the "Sibunit" carbon are involved in this process along with
methane, the K2Os3/Ar catalyst (0.19 g) was heated with
D2 for 20 h in the absence of methane at 150 С. The
results of the experiment showed that the deuterium conꢀ
tent in D2 also decreases (from 99.5 to 88.1 at.%) under
such conditions due to the formation of a mixture of D2,
HD, and H2 in a ratio of 78.1 : 19.9 : 2.0. In a similar
experiment but in the presence of methane, the
D2 : HD : H2 ratio is 70 : 20 : 10 and the deuterium content
is 80 at.%. Thus, the hydrogen atoms of "Sibunit" can also
be involved, along with methane, in the hydrogen—deuteꢀ
rium exchange with D2. It can be thus inferred that the
aboveꢀmentioned violations of the isotope balance in the
experiments on the H/D exchange in trideuteromethane
can be due, at least partially, to the participation of the hyꢀ
drogen atoms of the carbon support in the isotope exchange.
The nature of active particles responsible for the ocꢀ
currence of the aboveꢀconsidered H/D exchange reactions
remains yet unclear. It has previously been shown16 by the
ꢀresonance spectroscopy that the thermal decomposition
of K2[Fe2(CO)8] on the SKT carbon or of K2[Fe2(CO)8]
without a support in an H2 flow at 200 С for 6 h results in
the formation of two ironꢀcontaining amorphous alloys
characterized by a diffuse hyperfine structure in the
ꢀresonance spectra and differed from each other by spectral
characteristics. If the thermal decomposition of the supꢀ
ported K2[Fe2(CO)8] is carried out under the same condiꢀ
tions but in a flow of Ar, only one of these alloys is formed.
It is important that on using argon at the step of the deꢀ
composition of the carbonylferrate only trace amounts of
ꢀiron are present in the thermolysis products, while no
ꢀiron is formed when H2 is used. Based on these data, it can
be assumed that similar amorphous alloys are those partiꢀ
cles that are responsible for the activity of the K2Fe2/H2
and K2Fe2/Ar catalysts in the isotope exchange of hydroꢀ
carbons. Further studies are necessary to establish the comꢀ
position and structure of these amorphous alloys.
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Received March 1, 2013;
in revised form April 4, 2013