Open Access Article
This Open Access Article is licensed under a Creative Commons Attribution-Non Commercial 3.0 Unported Licence

Free electron laser infrared action spectroscopy of nitrous oxide binding to platinum clusters, Ptn(N2O)+

Gabriele Meizyte a, Alice E. Green a, Alexander S. Gentleman a, Sascha Schaller b, Wieland Schöllkopf b, André Fielicke *bc and Stuart R Mackenzie *a
aDepartment of Chemistry, University of Oxford, Physical and Theoretical Chemistry Laboratory, South Parks Road, Oxford, OX1 3QZ, UK. E-mail: stuart.mackenzie@chem.ox.ac.uk
bFritz-Haber-Institut der Max-Planck-Gesellschaft, Faradayweg 4-6, 14195 Berlin, Germany. E-mail: fielicke@fhi-berlin.mpg.de
cInstitut für Optik und Atomare Physik, Technische Universität Berlin, Hardenbergstraße 36, 10623 Berlin, Germany

Received 23rd May 2020 , Accepted 27th July 2020

First published on 29th July 2020


Abstract

Infrared multiple-photon dissociation spectroscopy has been applied to study Ptn(N2O)+ (n = 1–8) clusters which represent entrance-channel complexes on the reactive potential energy surface for nitrous oxide decomposition on platinum. Comparison of spectra recorded in the spectral region 950 cm−1 to 2400 cm−1 with those simulated for energetically low-lying structures from density functional theory shows a clear preference for molecular binding via the terminal N atom, though evidence of O-binding is observed for some cluster sizes. Enhanced reactivity of Ptn+n ≥ 6 clusters towards N2O is reflected in the calculated reactive potential energy surfaces and, uniquely in the size range studied, Pt6(N2O)+ proved impossible to form in significant number density even with cryogenic cooling of the cluster source. Infrared-driven N2O decomposition, resulting in the formation of cluster oxides, PtnO+, is observed following vibrational excitation of several Ptn(N2O)+ complexes.


I. Introduction

Nitrous oxide (N2O) is a significant atmospheric pollutant both as a greenhouse gas (GHG) and for the role it plays in ozone depletion.1 As a result of its relatively high global warming potential (GWP) coefficient N2O is considered to be the third principal long-lived GHG after CO2 and CH42 and one of the most potent waste gases resulting from human activity that has a significant impact on both the future ozone layer and climate.3 N2O discharge is not covered by the Montreal Protocol4 but, given its harmful environmental impact, there is considerable interest in using heterogeneous catalysis to reduce anthropogenic emissions.5

The platinum group metals (Ru, Rh, Pd, Os, Ir & Pt) are well-known heterogeneous catalysts. Platinum metal itself shows versatile catalytic abilities and is frequently used in industrial as well as everyday applications. For example, the production of nitric acid for fertilizers involves ammonia oxidation using a platinum catalyst.6 However, platinum is probably best known for its role, along with palladium and rhodium, in promoting exhaust gas reactions in the automobile catalytic converter (design first developed by R. C. Stempel et al.7). Highly inert (noble even) in its bulk form, most catalytic applications of platinum make use of it in highly divided, often nanoscale form. In addition to maximizing surface area, this introduces defects into the metal which are not present in extended single crystal surfaces and it is these defect sites which often provide the sites for interesting chemistry.8,9

Transition metal clusters serve as tractable model systems for the study of heterogeneous nanocatalysts at the molecular level.10 In the gas phase, the fundamental interactions involved in reactive chemistry can be studied in the absence of complex interactions present in real catalysts, such as the influence of substrates, solvation, and aggregation effects, which are challenging to analyse and often obscure the fundamental interactions of interest.11 The subject of this study, isolated Ptn(N2O)+ clusters, represent model entrance-channel complexes for the initial chemisorption step in the metal-catalysed decomposition of N2O.

Reflecting the catalytic properties of platinum, the reactions of platinum clusters, Ptn+/0/−, have received considerable attention previously. A variety of experimental techniques, including flow reactor, molecular beam-gas cell studies, and Fourier-transform ion-cyclotron resonance (FT-ICR) mass spectrometry, have been employed to study the reactions of Ptn+/0/− with small molecules. These include dehydrogenation of small hydrocarbons,12–18 as well as H2, CO2, N2O etc.19–23 Pt4+ exhibits particularly low reactivity, also supported by a theoretical investigation,24 and a photofragmentation study of bare Ptn+ clusters by Janssens25 suggests the reason lies in the anomalously large HOMO–LUMO gap for tetrahedral Pt4+. Interestingly, Pt4 activates carbon dioxide26 and dehydrogenates methane very efficiently, perhaps because of its own planar structure.18,26

Of particular relevance here are the single collision studies of Ptn+/− reactions with N2O in which the cationic clusters exhibit dramatic size-dependent rate constants changing by several orders of magnitude upon the addition of a single metal atom.22 In this small cluster regime, every atom counts. In all cases the reaction proceeds exclusively via an O atom transfer generating sequential cluster oxides, PtnOm+. Additional collisions are required to stabilize the molecular adsorption of N2O.

Several studies have established catalytic abilities and even full cycles using platinum clusters. Water formation was observed in the catalytic oxidation of H2 on Ptn for n = 7–30 by Andersson and Rosén19 and Shi and Ervin27 found small Ptn (n = 3–6) cluster anions to be effective catalysts for CO oxidation under thermal conditions. A full catalytic cycle of CO oxidation/N2O reduction for Ptn+ (n = 6–8) was reported by Beyer, Bondybey, and coworkers.28

N2O represents an interesting adsorbate for infrared studies, with the possibility of both N- or O-binding reflected in the degree of activation. This is very clearly observed in infrared action spectroscopy of N2O binding at single metal centers, for example, M+(N2O)n (M = Cu, Ag, Au,29 Co, Rh, Ir,30 and Li, Al31) by Cunningham et al. These studies have revealed interesting binding motifs and structural isomers as well as the important role played by low-lying electronically excited states.

We have previously studied N2O adsorption on small gas-phase Rhn+ clusters (Rhn(N2O)+, n = 4–8)32,33 using the same methods to those employed in this work. Interesting IR-induced reactivity was observed in which excitation of infrared active modes results in N2O decomposition and cluster oxide formation. Rh5+ proved special in this regard with a single co-adsorbed oxygen atom changing the chemistry observed from N2O loss on Rh5(N2O)+ to Rh5O2+ formation from Rh5(ON2O)+.34 These results, along with those from related blackbody infrared35 and collisional excitation studies36 were explained in terms of relative reaction barriers and dissociation thresholds demonstrating how spectral characterization of entrance-channel complexes yields important information on the full reactive potential energy surface.

Here we report the first experimental investigation of cationic platinum clusters with adsorbed nitrous oxide, Ptn(N2O)+ (n = 1–8), using infrared multiple-photon dissociation spectroscopy. Cluster structures, along with relative cluster reactivities, are revealed with the help of complementary quantum chemical calculations.

II. Experimental methods

The infrared multiple-photon dissociation (IR-MPD) spectra presented in this report were recorded at the Fritz Haber Institute (FHI) in Berlin making use of the FHI free electron laser (FEL)37 facility. The experimental setup has been described in detail previously38,39 and only essential details are described here. Briefly, a rotating natural Pt target is ablated by a Nd:YAG laser (532 nm, 10 Hz). Ablated atoms cool and cluster by colliding with helium within a reaction channel, to which nitrous oxide is added by an additional late-mixing pulsed valve, downstream of the ablation point. The resulting gas mix, now entrained with a range of pure and decorated clusters, expands into the vacuum forming a molecular beam which is then skimmed before entering the extraction region of a reflectron time-of-flight (ToF) mass spectrometer used to detect the presence of cationic species. In an attempt to suppress direct oxidation and maximize the generation of molecularly bound Ptn(N2O)+ clusters, the cluster source was cooled with liquid nitrogen.

To record infrared multiple-photon dissociation (IR-MPD) spectra, the cluster beam is subjected to alternate pulses of output of the FHI FEL, operating for these purposes in the 950–2400 cm−1 range and corresponding parent ion depletion and fragment(s) channel enhancement are recorded as a function of wavenumber. In this way the spectra yield information on the infrared active modes of the parent cluster as well as dissociation branching ratios, which can be compared with the results of DFT simulations.

III. Computational methods

Energetically low-lying structures and relevant transition states connecting them have been calculated at the def2TZVP40/TPSSh41,42 level, using the Gaussian 16 software package.43 This functional reproduces the transition metal–ligand bond dissociation energies44 and showed similar energetic ordering of the PtnO2CO+ cluster geometries45 to using the TPSS42 functional that has previously proved to generate reliable IR-MPD experimental results.46,47 The GD3-BJ dispersion term48 was introduced to account for weak intramolecular interactions and a quasirelativistic Wood-Boring effective core potential (WB-ECP)49 was used to freeze 60 inner electrons and introduce relativistic corrections for Pt atoms. As starting structures, the coordinates of bare Ptn+ clusters for n = 3–5 were taken from earlier work by Harding et al.47 To provide a better match with experimental data, computed harmonic vibrational frequencies were scaled by a factor of 0.955, determined by calculating the vibrational frequency of the asymmetric free N2O band.50 All energies reported here include zero point energies. Potential energy profiles were generated by identifying plausible transition states between two minima and performing Intrinsic Reaction Coordinate (IRC)51,52 calculations in order to verify the correct path.

IV. Results and discussion

A. Time-of-flight spectra and analysis

Fig. 1(a) shows part of the time-of-flight spectrum for the species produced following ablation of a natural platinum target in the presence of helium with low pressure nitrous oxide introduced downstream via the late mixing valve. We have repeated the experiment at a range of N2O pressures and these results are representative. A range of PtnOx+ and Ptn(N2O)m+ clusters are observed. We have previously reported an IR-MPD study of platinum oxide clusters.53 Analysis of the time-of-flight spectrum is complicated by the fact that platinum has six stable isotopes, leading to a wide range of masses for the same chemical species. Nevertheless, deconvolution is possible and is illustrated in Fig. 1(b) for the Pt3+X species produced. PtnOx+ (x = 1, 2, 3) and Ptn(N2O)m+ (m = 1, 2, 3) dominate the mass spectrum but a trace of Pt3C+ and Pt3CO+ is also observed – the carbon assumed to originate from polishing the target rod.
image file: d0cp02800b-f1.tif
Fig. 1 (a) Time-of-flight mass spectrum; (b) (lower) experimental and (upper) simulated time-of-flight mass spectrum of Pt3+ clusters – both produced by laser ablation of a natural platinum rod in helium to which nitrous oxide is added downstream. The cluster source was cooled to −140 °C with liquid N2. The principal species produced are simple cluster oxides, Pt3Ox+, and Pt3(N2O)m+ with traces of Pt3C+ and Pt3CO+.

Quantitative analysis of the mass spectrum, including deconvolution for the isotopes of platinum, leads to the normalized product abundances shown in Fig. 2(a) which yield important information on the relative reactivity of different Ptn+ cluster sizes towards N2O. Reactivity pathways can be visualized as:

 
(encounter complex formation) Ptn+ + N2O → [PtnN2O+]*(1)


image file: d0cp02800b-f2.tif
Fig. 2 (a) Histogram with normalised ion abundances (to a unity within each n; Ptn+ not shown) for reaction products generated in the cluster source by the reaction of Ptn+ (n = 3–8) with N2O. The uncertainties shown reflect the fitting of overlapping isotope patterns for different species (see inset Fig. 1(b)); (b) fractional oxide production as a measure of Ptn+ + N2O reactivity. A step change in reactivity occurs between n = 5 and 6.

In the absence of additional collisions or radiative cooling, this complex must either dissociate or react, in all probability forming the simple cluster oxide for which evidence is observed in the mass spectrum:

 
(direct dissociation) [PtnN2O+]* → Ptn+ + N2O(2)
 
(oxidation) [PtnN2O+]* → PtnO+ + N2(3)

The multiple-collision conditions of the cluster source reaction channel permit stabilisation of the initial complex, trapping it in an entrance-channel minimum of the reactive potential energy surface:

 
(N2O adsorption) [PtnN2O+]* + M → Ptn(N2O)+ + M(4)

By measuring the charged products we are blind to process (2) but the relative branching ratios for the oxidation reaction (3) and molecular adsorption (4) can be quantified as a function of cluster size.

For the n = 3 cluster under these approximately thermal, multiple collision conditions, the branching ratios for processes (3) and (4) are similar. For n = 4, 5 clusters, however, minimal cluster oxide formation is observed, with PtnN2O+ being the dominant product. For n ≥ 6 the situation changes markedly and oxide production dominates. Indeed, for n = 6 itself, negligible Pt6N2O+ is observed. This change in reactivity is highlighted in Fig. 2(b) which shows the PtnO+ signal as a fraction of total primary products [PtnO+]/{[PtnO+] + [PtnN2O+]} as a function of cluster size. The reactions reported here occur under very different conditions to the single collision experiments performed by Balteanu et al.22 in which only the direct oxidation process (3) was observed due to the lack of stabilizing collisions required for process (4). Nevertheless, the same step increase in reactivity between n = 5 and 6 is observed.

In an attempt to better understand the reactivity data, IRC profiles for cluster sizes n = 4–6 were calculated, as shown in Fig. 3. In each case, the two minima towards the left hand side represent O- and N-bound entrance-channel complexes of the respective Ptn(N2O)+ species and TS1 – a transition state for N2O rotation connecting the two. These entrance channels are separated from the product channel by a potential barrier TS2, which involves significant N2O rearrangement, ultimately leading to the production of PtnO+ cluster and molecular nitrogen. In all cases the overall reaction is calculated to be exothermic by more than 1 eV.


image file: d0cp02800b-f3.tif
Fig. 3 Intrinsic reaction coordinate for (a) Pt4+, (b) Pt5+, and (c) Pt6+ + N2O entrance channels. Blue boxes highlight the predominant species observed in the mass spectrum for each n. The barrier to N2O dissociation on Ptn+ cluster is pronounced for n = 4 and submerged for n = 6. This is reflected in the observed reactivity (see Fig. 2); Pt4+ is the least reactive favouring N2O adsorption whereas Pt6+ does not form any adsorption products and mainly produces oxides. Only the lowest electronic states are shown. For n = 4, geometries of both doublet and quartet are virtually indistinguishable; for n = 5, they are not – higher in energy sextet structures are given in the ESI.

The difference in reactivity between Pt4+ and Pt6+ (reported by Balteanu et al.22 as more than three orders of magnitude) is readily attributed to the fact that whilst the former has a real barrier on the ground state surface, in the latter the barrier is submerged. Calculations also show no reactive barrier for either of the two energetically low-lying electronic states of the n = 5 cluster and thus it is harder to explain the apparent lack of reactivity of this cluster. We note, however, that Balteanu et al. found Pt5+ to have intermediate reactivity (a factor ca. 44 less than for n = 6). Caution should be applied when interpreting barrier heights from DFT calculations and we have not performed an exhaustive study with different functionals. The answer may lie in the apparent need for greater fluxionality of the Pt5+ cluster during the reaction pathway than the prism/tetrahedral structures of Pt6+ and Pt4+, respectively.

B. IR-MPD spectra

Fig. 4 shows the IR-MPD spectra recorded in depletion for Ptn(N2O)+ (n = 1–8) in the region 950–2400 cm−1 covering the nitrous oxide N[double bond, length as m-dash]N and N[double bond, length as m-dash]O stretches. In Fig. 4 these bands in the free N2O molecules are indicated with dashed lines at around 2224 cm−1 (N[double bond, length as m-dash]N stretch) and 1285 cm−1 (N[double bond, length as m-dash]O stretch), respectively. As discussed above, negligible Pt6(N2O)+ is produced and hence no spectrum could be recorded of this species.
image file: d0cp02800b-f4.tif
Fig. 4 IR-MPD spectra of Ptn(N2O)+ (n = 1–8) clusters recorded in depletion of the parent cluster ion. The dashed lines at 1285 cm−1 and 2224 cm−1 indicate the wavenumbers of the N[double bond, length as m-dash]O and N[double bond, length as m-dash]N stretches of free N2O, respectively.50

The spectra of each species n ≥ 3 exhibit clear features slightly blue-shifted from the free N2O band positions. The presence of these bands, close to those of free nitrous oxide, clearly indicates molecularly-bound N2O on the metal cluster. The blue-shift of both bands indicates preferential N-binding on n ≥ 3 clusters (supported by computational results below) and reflects the dominance of σ-donation from the nitrous oxide to the cationic Ptn+ cluster over π-back bonding. For the smallest species, n = 1–2, the observed vibrational bands are considerably broader and there is evidence of components both blue- and red-shifted with respect to the free N2O stretches. Red-shifted bands, especially around the N[double bond, length as m-dash]O stretch, are strong evidence for the presence of O-bound clusters, which have been seen before in similar, higher-resolution infrared studies of M+(N2O)n (M = Co, Rh, Ir, Cu, Ag, Au, Li and Al).29–31 The smallest clusters, with fewer degrees of freedom, are less efficiently annealed into lower energy (N-bound) structures, allowing the trapping of energetically higher-lying isomers, including O-bound structures.

The Pt8(N2O)+ cluster is intriguing amongst the larger clusters studied in that its spectrum exhibits both blue- and red-shifted bands in both spectral regions, possibly reflecting a mix of N- and O-bound structures. The O-bound structure has an N[double bond, length as m-dash]O stretch band, which is red-shifted by >100 cm−1, compared with the corresponding free N2O band, indicating marked molecular activation.

A clear trend is observed in the frequency of the N-bound N[double bond, length as m-dash]O stretching band with cluster size. This band moves smoothly from 1390 ± 5 cm−1 on n =1 to 1315 ± 5 cm−1 by n = 8 (shown in Fig. 4 with a red arrow). The same trend is observed in the calculated band positions which move from 1421 cm−1 for Pt(N2O)+ to 1287 cm−1 for Pt5(N2O)+. The broader nature of the band in the N[double bond, length as m-dash]N stretch region makes it harder to discern any such trend in this region.

Fig. 5 compares the experimental spectra of Pt3(N2O)+ and Pt4(N2O)+ with those predicted for energetically low-lying calculated structures. The lowest energy calculated structures are inserted (i.e., dissociative N2O adsorption), but given the low binding energy of N2 and the overall exothermicity of the dissociation, it is unlikely that such PtnO(N2)+ structures would remain bound. The IR-MPD spectra clearly indicate the presence of molecularly-bound structures suggesting a kinetic barrier to dissociation. For this reason we choose the lowest-energy molecularly-bound structure as our zero of energy. Low-lying doublet and quartet electronic states are found for both clusters but the N-bound isomers lie lower in energy than corresponding O-bound isomers by approximately 0.5 eV in each case, supporting the assignments of the IR-MPD spectra made above. All structures are bound at single atom rather than bridging sites and the agreement between the simulated spectra and those observed experimentally is so good that there is no need to invoke the presence of any other structures in the beam.


image file: d0cp02800b-f5.tif
Fig. 5 Comparison of experimental and simulated IR-MPD spectra for a range of low-lying isomers of (a) Pt3(N2O)+ and (b) Pt4(N2O)+ complexes. All molecularly-bound isomers within 1 eV of the lowest energy structure are presented. Blue spectra represent N-bound isomers and red spectra – O-bound variants. The dashed lines at 1285 cm−1 and 2224 cm−1 represent the fundamental bands in free N2O.50

In any infrared action spectrum the depletion of a parent ion signal must be matched by an enhancement in the signal for some daughter species. By tracking parent ion depletions and absolute signal enhancements in different daughter channels simultaneously, it is possible to determine the branching ratios for the two most likely possibilities:

 
(N2O loss) Ptn(N2O)+ + → Ptn+ + N2O,(5)
and
 
(infrared driven dissociation) Ptn(N2O)+ + → PtnO+ + N2.(6)

Such an analysis is shown in Fig. 6 for Ptn(N2O)+ (n = 3–5, 7, 8) in the region of the N[double bond, length as m-dash]O stretching mode (with very similar behaviour observed in the N[double bond, length as m-dash]N stretch). A quantitative comparison of product channel enhancements versus parent ion depletion is a real challenge due to multiple species with similar spectra yielding the same fragmentation products. This affects net lineshapes and relative enhancements/depletion signal size in each channel. Nevertheless some clear pictures do emerge. In terms of reactivity, the smaller cluster sizes, n = 3–5 behave qualitatively differently to the n = 7, 8 clusters. For Ptn(N2O)+ (n = 3–5), excitation of the N[double bond, length as m-dash]O stretch leads almost exclusively to N2O loss (process (5)), consistent with the idea that, from the entrance-channel minimum, the Ptn+ + N2O dissociation threshold is reached before the transition state leading to nitrous oxide decomposition. By contrast, for Ptn(N2O)+ (n = 7, 8), comparable enhancements in both the Ptn+ and PtnO+ daughter channels (processes (5) and (6)) imply that the reactive transition state lies below or at a comparable energy to the dissociation threshold. These observations are in good agreement with the reactivity data extracted from the time-of-flight spectra even down to the small Pt3O+ production following excitation of Pt3(N2O)+.


image file: d0cp02800b-f6.tif
Fig. 6 (black) IR-MPD spectra of Ptn(N2O)+ clusters in the N2O (N[double bond, length as m-dash]O) stretch region. Red and blue spectra show the simultaneous enhancements observed in the PtnO+ and Ptn+ mass channels representing IR driven reactive (N2 loss) and desorptive (N2O loss) processes.

Observation of efficient generation of the PtnO+ daughter is a signal of infrared-induced chemistry on the surface of the cluster, a process which we have documented in several previous studies of other systems including Rhn(N2O)+,32,33 RhnO(N2O)+,32,34 PtnO2(CO)+,45 and, recently, Aun(OCS)+.54 In several previous studies32,36 we have also demonstrated that the products observed following infrared excitation mirror those of collisional activation implying that we essentially “heat” the entrance-channel complexes until dissociation/reactive channels open. Previous studies have not revealed any mode-selective character to the chemistry induced and the current system is no exception. However, the ability to selectively increase the internal energy of a known cluster with spectral knowledge of its structure represents a unique feature in the exploration of these catalytically-relevant reactive potential energy surfaces.

V. Summary and conclusions

A combined experimental (IR-MPD) and computational study of nitrous oxide reacting with and binding to platinum cluster cations, Ptn+ (n = 3–8), has revealed key features on the potential energy surface of the Ptn+ + N2O → PtnO+ + N2 reaction. The laser ablation/molecular beam conditions employed in this study are shown, in most cases, to lead to the efficient formation of entrance-channel complexes on the reactive surface, the structures of which can be probed by multiple-photon dissociation action spectroscopy. One notable exception is the Pt6+ cluster, which reacts completely to generate the oxide with no evidence of Pt6(N2O)+ observed.

The observed reactivity can be well-understood in terms of potential energy surfaces calculated at the DFT level. Similarly, the simulated vibrational spectra for calculated low-energy entrance-channel complexes match well with the action spectra recorded. For several cluster sizes, clear evidence for infrared-driven cluster chemistry is observed in the loss of N2 following infrared excitation of the N[double bond, length as m-dash]O stretching mode of the parent Ptn(N2O)+. These results, too, are in quantitative agreement with calculated reactive barrier heights compared to N2O binding energies.

Conflicts of interest

There are no conflicts to declare. 

Acknowledgements

This work was funded in part by EPSRC under Programme Grant EP/L005913. The Oxford authors would like to acknowledge the use of the University of Oxford Advanced Research Computing (ARC) facility in carrying out this work: https://doi.org/10.5281/zenodo.22558. Financial support permitting research visits is also gratefully acknowledged from the Oxford-Berlin Research Partnership (Ref.: OXBER_STEM5, “A Collaborative Approach to Understanding Nitrogen Oxide Reduction at Metal Centres”). G. M. and A. E. G. thank Worcester and Magdalen Colleges, Oxford, respectively for their graduate studentships. A. F. thanks the Deutsche Forschungsgemeinschaft for his Heisenberg Grant (FI893/5). Open Access funding provided by the Oxford University Agreement.

References

  1. J. Pérez-Ramírez, F. Kapteijn, K. Schöffel and J. A. Moulijn, Appl. Catal., B, 2003, 44, 117–151 CrossRef.
  2. WMO (World Meteorological Organization), Scientific Assessment of Ozone Depletion: 2018, Global Ozone Research and Monitoring Project-Report No. 58, 588 pp., Geneva, Switzerland, 2018.
  3. A. R. Ravishankara, J. S. Daniel and R. W. Portmann, Science, 2009, 326, 123 CrossRef CAS PubMed.
  4. UNEP 2015, Synthesis of the 2014 Reports of the Scientific, Environmental Effects, and Technology & Economic Assessment Panels of the Montreal Protocol, United Nations Environment Programme (UNEP), Nairobi.
  5. V. Rosca, M. Duca, M. T. de Groot and M. T. M. Koper, Chem. Rev., 2009, 109, 2209–2244 CrossRef CAS PubMed.
  6. G. Chinchen, P. Davies and R. J. Sampson, in Catalysis: Science and Technology, ed. J. R. Anderson and M. Boudart, Springer, Berlin, Heidelberg, 1987, vol. 8, pp. 1–67 Search PubMed.
  7. R. C. Stempel and S. W. Martens, SAE Trans., 1974, 83, 2358–2372 Search PubMed.
  8. A. Cho, Science, 2003, 299, 1684–1685 CrossRef CAS PubMed.
  9. A. Ulvestad, A. Singer, J. N. Clark, H. M. Cho, J. W. Kim, R. Harder, J. Maser, Y. S. Meng and O. G. Shpyrko, Science, 2015, 348, 1344–1347 CrossRef CAS PubMed.
  10. M. B. Knickelbein, Annu. Rev. Phys. Chem., 1999, 50, 79–115 CrossRef CAS PubMed.
  11. D. K. Böhme and H. Schwarz, Angew. Chem., Int. Ed., 2005, 44, 2336–2354 CrossRef PubMed.
  12. D. J. Trevor, R. L. Whetten, D. M. Cox and A. Kaldor, J. Am. Chem. Soc., 1985, 107, 518–519 CrossRef CAS.
  13. D. J. Trevor, D. M. Cox and A. Kaldor, J. Am. Chem. Soc., 1990, 112, 3742–3749 CrossRef CAS.
  14. T. Hanmura, M. Ichihashi and T. Kondow, J. Phys. Chem. A, 2002, 106, 11465–11469 CrossRef CAS.
  15. G. S. Jackson, F. M. White, C. L. Hammill, R. J. Clark and A. G. Marshall, J. Am. Chem. Soc., 1997, 119, 7567–7572 CrossRef CAS.
  16. C. Adlhart and E. Uggerud, Chem. – Eur. J., 2007, 13, 6883–6890 CrossRef CAS PubMed.
  17. C. Adlhart and E. Uggerud, Chem. Commun., 2006, 2581–2582 RSC.
  18. U. Achatz, C. Berg, S. Joos, B. S. Fox, M. K. Beyer, G. Niedner-Schatteburg and V. E. Bondybey, Chem. Phys. Lett., 2000, 320, 53–58 CrossRef CAS.
  19. M. Andersson and A. Rosén, J. Chem. Phys., 2002, 117, 7051–7054 CrossRef CAS.
  20. H. Yamamoto, K. Miyajima, T. Yasuike and F. Mafuné, J. Phys. Chem. A, 2013, 117, 12175–12183 CrossRef CAS PubMed.
  21. K. Koszinowski, D. Schröder and H. Schwarz, J. Phys. Chem. A, 2003, 107, 4999–5006 CrossRef CAS.
  22. I. Balteanu, O. Petru Balaj, M. K. Beyer and V. E. Bondybey, Phys. Chem. Chem. Phys., 2004, 6, 2910–2913 RSC.
  23. P. A. Hintz and K. M. Ervin, J. Chem. Phys., 1995, 103, 7897–7906 CrossRef CAS.
  24. L. Lv, Y. Wang, Q. Wang and H. Liu, J. Phys. Chem. C, 2010, 114, 17610–17620 CrossRef CAS.
  25. P. Ferrari, K. Hansen, P. Lievens and E. Janssens, Phys. Chem. Chem. Phys., 2018, 20, 29085–29090 RSC.
  26. A. E. Green, J. Justen, W. Schöllkopf, A. S. Gentleman, A. Fielicke and S. R. Mackenzie, Angew. Chem., Int. Ed., 2018, 57, 14822–14826 CrossRef CAS PubMed.
  27. Y. Shi and K. M. Ervin, J. Chem. Phys., 1998, 108, 1757–1760 CrossRef CAS.
  28. O. P. Balaj, I. Balteanu, T. T. J. Roßteuscher, M. K. Beyer and V. E. Bondybey, Angew. Chem., Int. Ed., 2004, 43, 6519–6522 CrossRef CAS PubMed.
  29. E. M. Cunningham, A. S. Gentleman, P. W. Beardsmore, A. Iskra and S. R. Mackenzie, J. Phys. Chem. A, 2017, 121, 7565–7571 CrossRef CAS PubMed.
  30. E. M. Cunningham, A. S. Gentleman, P. W. Beardsmore and S. R. Mackenzie, Phys. Chem. Chem. Phys., 2019, 21, 13959–13967 RSC.
  31. E. M. Cunningham, A. S. Gentleman, P. W. Beardsmore and S. R. Mackenzie, Mol. Phys., 2019, 117, 2990–3000 CrossRef CAS.
  32. S. M. Hamilton, W. S. Hopkins, D. J. Harding, T. R. Walsh, M. Haertelt, C. Kerpal, P. Gruene, G. Meijer, A. Fielicke and S. R. Mackenzie, J. Phys. Chem. A, 2011, 115, 2489–2497 CrossRef CAS PubMed.
  33. S. M. Hamilton, W. S. Hopkins, D. J. Harding, T. R. Walsh, P. Gruene, M. Haertelt, A. Fielicke, G. Meijer and S. R. Mackenzie, J. Am. Chem. Soc., 2010, 132, 1448–1449 CrossRef CAS PubMed.
  34. A. C. Hermes, S. M. Hamilton, W. S. Hopkins, D. J. Harding, C. Kerpal, G. Meijer, A. Fielicke and S. R. Mackenzie, J. Phys. Chem. Lett., 2011, 2, 3053–3057 CrossRef CAS.
  35. I. S. Parry, A. Kartouzian, S. M. Hamilton, O. P. Balaj, M. K. Beyer and S. R. Mackenzie, Angew. Chem., Int. Ed., 2015, 54, 1357–1360 CrossRef CAS PubMed.
  36. I. S. Parry, A. Kartouzian, S. M. Hamilton, O. P. Balaj, M. K. Beyer and S. R. Mackenzie, J. Phys. Chem. A, 2013, 117, 8855–8863 CrossRef CAS PubMed.
  37. W. Schöllkopf, S. Gewinner, H. Junkes, A. Paarmann, G. von Helden, H. Bluem and A. M. Todd, Proc. SPIE, 2015, 9512, 95121L CrossRef.
  38. A. Yanagimachi, K. Koyasu, D. Y. Valdivielso, S. Gewinner, W. Schöllkopf, A. Fielicke and T. Tsukuda, J. Phys. Chem. C, 2016, 120, 14209–14215 CrossRef CAS.
  39. A. Fielicke, G. von Helden and G. Meijer, Eur. Phys. J. D, 2005, 34, 83–88 CrossRef CAS.
  40. F. Weigend and R. Ahlrichs, Phys. Chem. Chem. Phys., 2005, 7, 3297–3305 RSC.
  41. V. N. Staroverov, G. E. Scuseria, J. Tao and J. P. Perdew, J. Chem. Phys., 2003, 119, 12129–12137 CrossRef CAS.
  42. J. Tao, J. P. Perdew, V. N. Staroverov and G. E. Scuseria, Phys. Rev. Lett., 2003, 91, 146401 CrossRef PubMed.
  43. M. J. Frisch, G. W. Trucks, H. B. Schlegel, G. E. Scuseria, M. A. Robb, J. R. Cheeseman, G. Scalmani, V. Barone, G. A. Petersson, H. Nakatsuji, X. Li, M. Caricato, A. V. Marenich, J. Bloino, B. G. Janesko, R. Gomperts, B. Mennucci, H. P. Hratchian, J. V. Ortiz, A. F. Izmaylov, J. L. Sonnenberg, D. Williams-Young, F. Ding, F. Lipparini, F. Egidi, J. Goings, B. Peng, A. Petrone, T. Henderson, D. Ranasinghe, V. G. Zakrzewski, J. Gao, N. Rega, G. Zheng, W. Liang, M. Hada, M. Ehara, K. Toyota, R. Fukuda, J. Hasegawa, M. Ishida, T. Nakajima, Y. Honda, O. Kitao, H. Nakai, T. Vreven, K. Throssell, J. A. Montgomery Jr., J. E. Peralta, F. Ogliaro, M. J. Bearpark, J. J. Heyd, E. N. Brothers, K. N. Kudin, V. N. Staroverov, T. A. Keith, R. Kobayashi, J. Normand, K. Raghavachari, A. P. Rendell, J. C. Burant, S. S. Iyengar, J. Tomasi, M. Cossi, J. M. Millam, M. Klene, C. Adamo, R. Cammi, J. W. Ochterski, R. L. Martin, K. Morokuma, O. Farkas, J. B. Foresman and D. J. Fox, Gaussian 16 Revision C.01, Gaussian, Inc., Wallingford CT, 2016 Search PubMed.
  44. K. P. Jensen, J. Phys. Chem. A, 2009, 113, 10133–10141 CrossRef CAS PubMed.
  45. A. C. Hermes, S. M. Hamilton, G. A. Cooper, C. Kerpal, D. J. Harding, G. Meijer, A. Fielicke and S. R. Mackenzie, Faraday Discuss., 2012, 157, 213–225 RSC.
  46. A. Fielicke, P. Gruene, M. Haertelt, D. J. Harding and G. Meijer, J. Phys. Chem. A, 2010, 114, 9755–9761 CrossRef CAS PubMed.
  47. D. J. Harding, C. Kerpal, D. M. Rayner and A. Fielicke, J. Chem. Phys., 2012, 136, 211103 CrossRef PubMed.
  48. S. Grimme, S. Ehrlich and L. Goerigk, J. Comput. Chem., 2011, 32, 1456–1465 CrossRef CAS PubMed.
  49. D. Andrae, U. Häußermann, M. Dolg, H. Stoll and H. Preuß, Theor. Chim. Acta, 1990, 77, 123–141 CrossRef CAS.
  50. G. Herzberg, Molecular Spectra and Molecular Structure: II Infrared and Raman Spectra of Polyatomic Molecules, Krieger, Malabar, Florida, 1991 Search PubMed.
  51. K. Fukui, Acc. Chem. Res., 1981, 14, 363–368 CrossRef CAS.
  52. H. P. Hratchian and H. B. Schlegel, Theory and Applications of Computational Chemistry: The First 40 Years, Elsevier, Amsterdam, 2005 Search PubMed.
  53. C. Kerpal, D. J. Harding, A. C. Hermes, G. Meijer, S. R. Mackenzie and A. Fielicke, J. Phys. Chem. A, 2013, 117, 1233–1239 CrossRef CAS PubMed.
  54. A. E. Green, S. Schaller, G. Meizyte, B. J. Rhodes, S. P. Kealy, A. S. Gentleman, W. Schöllkopf, A. Fielicke and S. R. Mackenzie, J. Phys. Chem. A, 2020, 124, 5389–5401 CrossRef CAS PubMed.

Footnote

Electronic supplementary information (ESI) available: Containing calculated structures of important species observed experimentally, plus calculated N2O binding energies and bond lengths. See DOI: 10.1039/d0cp02800b

This journal is © the Owner Societies 2020
Click here to see how this site uses Cookies. View our privacy policy here.