Chemistry Letters 2000
987
(ppm))/(HCN inlet concn (ppm)) × 100. As shown in Figure
1(a), HCN decomposed into equivalent amounts of NH3 and
CO in the presence of H2O vapor. Evidently, hydrolysis
occurred according to the reaction:
HCN conversion increased with increasing temperature. Since
equivalent amounts of NH3 and CO were also produced under
O2 + H2O flow below 670 K (Figure 1(b)), it is clear that HCN
was preferentially hydrolyzed under these conditions. Above
670 K, small amounts of NO and CO2 were detected. Since the
decomposition of NH3 or CO was negligible under similar con-
ditions, we speculate the NO and CO2 to be formed by the oxi-
dation of HCN. Figures 1(c) and (d) show HCN decomposition
behavior in the presence of NO + O2 + H2O and NO2 + O2 +
H2O, respectively. HCN conversions increased, compared to
the results obtained in the absence of NO or NO2. However,
CO yields were almost equal to HCN conversions below 670 K.
On the other hand, NH3 was not formed at all; instead, N2 was
formed in amounts equal to the amount of HCN converted.
Moreover, NOx conversion in figure 1(c) was very close to N2
yield. These results strongly suggest that one NO molecule
reacts with one NH3 molecule produced by HCN hydrolysis to
give one N2 molecule. In figure 1(d), NOx conversion was
apparently higher than HCN conversion and N2 yield but it was
due to the formation of HNO3 and HNO2. In the presence of
NO2, HNCO was formed at high temperatures, probably due to
the oxidation of HCN by NO2, and N2O was formed with the
maximum yield at 623 K, presumably as a product of the reac-
tion between NO2 and NH3. The increase in the HCN conver-
sion in the presence of NOx is discussed below.
tion of NO2 (1000 ppm) with C2H4 (1000 ppm) in the presence
of O2 (5%) over the same H-ferrierite, and observed the produc-
tion of 76, 106, and 51 ppm HCN at 523, 623, and 723 K,
respectively. Taking account of the high reactivity toward
hydrolysis, HCN observed in the HC-SCR process may not be a
simple by-product but may be one of the intermediates toward
N2 and N2O. The mechanism of HCN formation in HC-SCR is
under investigation and will be reported elsewhere.
Figure 2 shows the selectivities of N2 and N2O in the NH3
+ NO + NO2 + O2 reaction at 623 K with a varying ratio of NO
and NO2 in the reactant gas (total NOx = 1000 ppm). Under all
conditions, NH3 was completely converted into N2 or N2O.
N2O formation was observed particularly in the presence of
much more NO2 than NO. It is evident from these results that
NH3 reacts rapidly on H-ferrierite with both NO and NO2 to
produce N2 and N2O. Also, it is strongly suggested that self-
poisoning by the NH3 formed was suppressed due to the reac-
tion between NH3 and NOx, so that HCN hydrolysis, occurring
most probably on acid sites, was enhanced in the presence of
NOx.
In conclusion, below 670 K the decomposition of HCN
over H-ferrierite proceeds preferentially through hydrolysis,
which results in the formation of NH3 and CO. In the presence
of NO or NO2, the NH3 formed reacts further with NOx to form
N2 and N2O, with N2O produced only in the presence of much
more NO2 than NO. We separately performed selective reduc-
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