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Article

A Simple Angle-Resolved Thermal Molecular Beam Reactor: Applied to CO Oxidation on Pt{110}

1
Cardiff Catalysis Institute, School of Chemistry, Cardiff University, Cardiff CF10 3AT, UK
2
Catalysis Hub, RCAH, Rutherford Appleton Laboratory, Harwell, Oxfordshire OX11 0FA, UK
3
Department of Chemistry, University of Reading, Reading RG6 6DX, UK
4
Department of Structural Biochemistry, Max Planck Institute of Molecular Physiology, Otto-Hahn-Str. 11, 44227 Dortmund, Germany
5
Forensic Scientific Institute, State Criminal Police Office of Schleswig-Holstein, 24146 Kiel, Germany
*
Authors to whom correspondence should be addressed.
Catalysts 2020, 10(11), 1229; https://doi.org/10.3390/catal10111229
Submission received: 23 September 2020 / Revised: 20 October 2020 / Accepted: 21 October 2020 / Published: 23 October 2020
(This article belongs to the Special Issue Surface Chemistry in Catalysis)

Abstract

:
We developed a simple form of thermal molecular beam catalytic reactor system which is capable of measuring sticking probabilities and reaction probabilities, together with angle-resolved scattering of molecules and products during catalytic reactions at the surface. This includes very fast determination of the angle dependence of the reaction product flux at steady-state. It was employed to determine the oxidation of CO on Pt{110}-(1 × 2), including individual molecular sticking and scattering. The initial sticking probability of oxygen on Pt{110} shows a small variation between 140 and 750 K surface temperature, from 0.45 to 0.28. The saturation uptake drops from 1.5 ± 0.2 ML at 140 K to 0.6 ML at 300 K and to 0.23 ± 0.02 ML at 750 K. The initial sticking probability of CO at 300 K is 0.80 and decreases to 0.62 at 470 K. Beyond that temperature, it descends steeply down to near zero at 570 K, due to the high desorption rate of CO at that temperature. Kisliuk precursor mobility parameters K were calculated from shape of the sticking curves. For 300 K, a value of 0.11 ± 0.01 was found, which increases to 0.76 ± 0.01 at 470 K, indicating a change from considerable mobility in the precursor state, to more limited mobility before desorption at high temperature. In temperature-programmed CO-O2 reaction experiments, CO2 production was observed to initiate in the temperature region 460–510 K. Using isothermal angle-resolved experiments, the CO2 flux was determined in the [ 1 1 ¯ 0 ] plane at temperatures of 470–620 K. Two sharp scattering lobes at positions of ±16° off the surface normal were found, with a high cosine power angle dependence, which were attributed to desorption from the {111}-like microfacets of the 1 × 2 reconstructed surface, with products evolving over a high barrier.

Graphical Abstract

1. Introduction

Molecular beam methods are important means of analyzing the surface reactivity and structure of single crystal surfaces. By using a molecular beam to supply the crystal continuously with new reaction mixture, it is possible to measure reactions under steady-state conditions, which is not possible by ARTPD (angle-resolved temperature programmed desorption), since, due to the temperature ramping, it is essentially a non-steady-state kind of experiment. Recent, elegant work on CO oxidation on Pt{111} for example has shown two channels for reaction, on terrace and step edges, which may be distinguished by the desorption characteristics of CO2 [1]. In this paper, we report data for the adsorption, desorption and reaction of CO and oxygen on the {110} surface of platinum using a new design of a molecular beam apparatus. The CO oxidation was measured in angle-resolved mode under steady-state conditions.
The reconstructed clean Pt{110}-(1 × 2) surface has a missing-row type structure [2,3,4]. The Pt atoms build close-packed rows along the [ 1 1 ¯ 0 ] direction with every second row missing. Due to these missing rows, there is a series of troughs between the close packed rows. The walls of the troughs can be described as {111} microfacets.
Adsorption of CO is known to lift the reconstruction of the missing-row structure. Above an exposure of 1 L, single Pt atoms of the first layer diffuse out of the [ 1 1 ¯ 0 ] atomic rows and occupy lattice sites being out of phase with regard to the (1 × 2) periodicity [5]. This happens even at temperatures as low as 250 K [6]. The lifting of the reconstruction leads to a (1 × 1) low energy electron diffraction (LEED) pattern at CO coverages of about 0.6 ML [7]. This is not due to a bulk-truncated structure but because of a random distribution of top layer Pt atoms on the bulk layer underneath which has a (1 × 1) periodicity [8]. Oertzen et al. mentioned that the phase transition starts at a CO coverage of 0.2 ML and is completed at 0.5 ML [9]. At 300 K, CO adsorbs exclusively at on-top sites up to a coverage of 0.5 ML. Above this coverage, a small amount of CO also adsorbs on bridge sites [10]. The room-temperature saturation coverage of CO is 0.88 ML (1 ML = 9.22 × 1014 molecules cm−2) [11].
In contrast, the adsorption of O2 does not lift the Pt{110}-(1 × 2) missing-row structure [12]. Performing quantitative X-ray photoelectron spectroscopy (XPS) and work function studies, Freyer et al. found a saturation coverage for room temperature adsorption onto the (1 × 2) reconstructed surface of 0.35 ML [7]. This value is quite low in comparison to other authors. Walker et al. measured a saturation coverage of close to 1 ML for room temperature adsorption [13]. Below 0.25 ML, oxygen is adsorbed in a state where it fluctuates across ridge bridge sites. Between 0.25 and 0.5 ML, oxygen is pinned at fcc sites on the walls of the {111} microfacets. Due to lateral interactions, only every other site along the row can be occupied at these coverages. As shown by Walker et al., above 0.5 ML, oxygen produces a coverage-dependent variable unit mesh structure [13], and this results in a change from second- to first-order behavior for the oxygen desorption above this coverage.
The activation energy for diffusion of CO on a Pt{110}-(1 × 2) surface was measured by Oertzen et al. to be about 9–13 kcal/mol, while the activation energy of diffusion for O2 is 30 kcal/mol for low coverages and 40 kcal/mol for high coverages [9]. This means that the diffusion of O2 is negligible in comparison to the CO diffusion. The CO oxidation will therefore take place nearly exclusively on the surface sites that are occupied by oxygen, with CO diffusing to these sites for reaction. Oertzen et al. also found a great anisotropy for O2 diffusion, with diffusion occurring only parallel to the crystallographic [ 1 1 ¯ 0 ] direction. This is consistent with the observation that O2 forms rows in the troughs of the Pt{110}-(1 × 2) surface [9].
Using an ultrathin Pt{110} single crystal, Wartnaby et al. measured the excess energy of desorbing CO2 molecules in comparison to thermally accommodated molecules [14]. They found that, when CO is dosed onto a saturated oxygen overlayer, the excess energy is 9 ± 17 kJ/mol, while the excess energy was 52 ± 21 kJ/mol for oxygen dosed onto a CO overlayer. They explained this behavior by a drop of the reaction activation energy with increasing oxygen coverage and the formation of “hot” oxygen atoms. The “hot” oxygen atoms could react with CO before thermal accommodation to the surface and therefore carry their excess energy over to the product CO2.
The reaction mechanism of the CO oxidation reaction was found to be mainly of Langmuir–Hinshelwood type on Pt surfaces, excluding any reaction via the direct collision of gas phase CO with oxygen adatoms [15,16]. On the other hand, Bonzel and Ku predicted that the reaction on a Pt{110}-(1 × 2) surface takes place via a Langmuir–Hinshelwood mechanism at conditions where CO was pre-adsorbed on the surface while with O2 pre-adsorbed on the surface, it shifts to an Eley–Rideal mechanism [17].
Using a cross-correlation time-of-flight method combined with non-steady-state angle-resolved thermal desorption (ARTPD), Matsushima et al. measured the angular and velocity distributions of CO2 desorbing from a Pt{110}-(1 × 2) surface [18,19,20]. They found that the CO2 desorption is collimated at angles of ±25° off the surface normal. At these angles, the translational temperature of desorbing CO2 also reaches a maximum. The difference between the facet angles of the {111} facet normals of about ±35.2°, and the measured values have been explained by the “smoothing effect” of conducting electrons and surface distortions, the latter reducing the facet angle to about ±30° as found by LEED and TOF-SARS (time of flight scattering and recoiling spectrometry) investigations [21,22].
Relatively few angle-resolved measurements under steady-state conditions have been performed on the CO oxidation reaction on Pt surfaces. Cao et al. performed such an investigation on a Pt{113} surface, finding two desorption peaks at angles of −20 ± 2° and at +22 ± 2° off the surface normal [23]. They assigned these results to reactions to the {001} and the {111} facets of this surface, with facet normals of −25.2° and +29.5°, respectively. On Pt{110}-(1 × 2), CO2 formation dynamics was probed with angular and velocity resolution at relatively high O2 pressures of 1 × 10−7–1 × 10−4 Torr and found that reactions are dominated by the (1 × 2) regions of the surface giving hyperthermal desorption directed at 25° from the surface normal [24]. These were attributed to reactions occurring on the facets.
There has been a great deal of work on the kinetics, light-off and the spatiotemporal oscillations of CO oxidation [25,26,27,28,29,30] including Ertl’s Nobel Prize-winning work [31,32], and the work described above [18,19,20]. To the best of our knowledge, there have been no continuous angle-resolved measurements under steady-state conditions combining the advantages of molecular beams to access sticking, trapping, uptake and desorption in the CO oxidation reaction on a Pt{110}-(1 × 2) surface. Mullins et al. did this for the reaction at 90 K surface temperature on Pt{111} and found a cos12 dependence of the scattered flux. However, they used non-thermal and separate sources of O2 (from a microwave source) and supersonic CO [33]. Similarly, in the ground-breaking work of Neugebohren et al., discussed below, high source pressure beams were used [1]. Near ambient pressure XPS experiments have shown how local structure and oxide formation on Pt{110} influence CO oxidation and provide motivation to continue to develop in-situ tools to probe catalytic reactivity in response to surface nanostructural changes [34].
The aim of this study was to gain a further understanding of the oxidation of CO on a Pt{110}-(1 × 2) surface, with continuous thermal beams. By performing the experiments under steady-state conditions, we were able to observe the reaction at much higher temperatures than possible with ARTPD. We used a recently-designed molecular beam machine that can perform fast angle-resolved measurements even in steady-state mode in a continuous manner.

2. Results and Discussion

2.1. Inert Gas Scattering

To investigate the scattering behavior of Pt{110}-(1 × 2), experiments with helium and argon were carried out. The results are shown in Figure 1. For helium, an intense sharp peak was observed at an angle of 101 ± 3° and a small peak at 37 ± 3° (the beam enters the chamber at 45° and the angle-resolved MS is at 90°). In contrast, the scattering curve for argon shows a rather broad and featureless distribution, although the signal maximum is also positioned at around 101°. A specularly reflected He beam from a flat Pd{111} surface shows a sharp maximum at 67.5° (see Figure S2). For a sample with facets a specularly reflected beam should arise when the facet normal is held at 67.5° and thus specular peaks are expected at ± the facet angle which is ±35° for {111} micro facets on {110} yielding peaks expected at 32.5 and 102.5° in our geometry. The experimentally measured angles suggest the facets are slightly less steep than ±35°.
For comparison with the experiment, we simulated the scattering at the surface. The Pt{110}-(1 × 2) surface was modeled by assuming a cosine-shaped hard surface potential (Figure 2). The size of the scattered atoms has been neglected, and only fully elastic scattering has been assumed (“billiard ball model”). Double scattering on both facets was considered and was of minor influence in the idealized simulation. As the facet angle deviates from the geometrical value of 35.2° for an undistorted surface, an angle of 30° was used, as this value was reported from LEED [21] and TOF-SARS experiments [22]. The angle between incident beam and detector was set to 45°, with a detector acceptance angle of ±5°. The result of the simulation is shown in Figure 2. It exhibits two sharp peaks at angles of 40° and 95°.
For helium, the simulation fits the experimental result quite well except for the lack of intensity of the peak at 37°. The reason for this lies in shadowing effect of the facets in a non-ideal surface which is underestimated in the simulation due to the assumption of dimensionless atoms and a hard surface potential (facet bunches due to local miscuts can shadow the outgoing atoms). Each facet also receives a different proportion of the flux so at ~102° the facet oriented for specular reflection sees the vast majority of the flux, whereas the other facet is at grazing incidence and hence this orientation generates a large signal. At 37°, the beam is at near normal incidence and both facets see similar fluxes so only approximately half of the beam hits the facet aligned for specular reflection, resulting in a smaller signal.
There is some decrease in the transmission function of the system, particularly at high angles where the beam grazes the crystal surface (the mass spectrometer apertures are designed to accept scattered gas from the full width of the sample, but at grazing some beam spill over from the sample edges). Otherwise, the well-reproduced Helium peak positions indicate that the assumed model is adequate for the performed scattering experiment.
In contrast to the simulated scattering, the experimental result for Argon shows no separated peaks, and is due to the fact that Ar scattering is not elastic due to its higher accommodation and a much higher enthalpy of physisorption (~1–2 kJ/mol for He and about 10× that figure for Ar [35]). A more detailed discussion of these data and fitting of the Ar data is given in the Supplementary Materials.

2.2. Oxygen Interaction with Pt{110}

The results for the sticking experiments with oxygen are shown in Figure 3.
The initial sticking probability s0 shows a gradual decrease with increasing surface temperature above 400 K, from 0.34 to 0.27 at 750 K. At lower temperatures, there is a larger decrease from ~0.45 at 130 K to 0.36 at 350 K.
The high uptake at low temperatures, and big decrease up to 350 K, coincides with a low-temperature oxygen desorption peak found by Wilf and Dawson at a temperature of 250 K that extends to 350 K [12]. A similar observation was made by Walker et al. [13], although they also found a very sharp peak at approximately 220 K. They attributed this peak to the presence of molecularly chemisorbed oxygen O2. Sticking probability versus uptake curves at several temperatures are given in the Supplementary Materials (Figure S3).
The TPD spectra of oxygen are extremely sensitive to the surface structure of a Pt{110} surface. Even a different cooling rate of the crystal after the usual annealing at 970 K results in significantly altered spectra, possibly due to a change in the step density [22]. O2 TPD is therefore a good test for the quality of the surface structure.
Desorption traces for oxygen TPD as a function of heating rate and coverage are shown in Figure 4 and Figure 5, respectively. For heating rate dependent TPD (Figure 4), the crystal was dosed with 22.5 L (3 × 10−5 mbar.s) of oxygen at 420 K.
The relationship between the peak maximum temperature Tmax and the heating rate β for a first-order desorption is described by the following equation [12]:
l n ( T m a x 2 β ) = l n ( E d ν 1 R ) + E d R T m a x
where ν1 is the preexponential factor of desorption, Ed is the desorption energy and R is the molar gas constant. Using this approach, we calculated a desorption energy of Ed = 218.6 ± 5.7 kJ/mol and a preexponential factor of ν1 = 3.6 × 1015±0.4 s−1. These values are high in comparison to literature. Wilf and Dawson found a desorption energy for the β1 state of 134 kJ/mol, with a preexponential factor of 1.7 × 109 s−1 [12], while Walker et al. measured the adsorption heat of O2 using microcalorimetry [13] and found a value of 170 kJ/mol for the β1 oxygen state. They also calculated the desorption energy using the Redhead formula [36] (Equation (2)):
E d = R T m a x ( l n ( ν 1 T m a x β ) 3.64 )
They assumed a preexponential factor of ν1 = 1 × 1013 s−1 and found a value of Ed = 198 kJ/mol.
From the coverage-dependent TPD spectra (Figure 5), we also calculated the desorption energy of the first-order peak using the Redhead equation. With the preexponential factor of ν1 = 3.6 × 1015±0.4 s−1 from the heating rate dependent measurements and the averaged value of the peak maximum temperature of Tmax = 706.4 ± 0.6 K, we found a desorption energy of Ed = 219.4 ± 6.6 kJ/mol, in close agreement with the value obtained by our heating rate dependent measurement. Assuming a preexponential factor of 1 × 1013 s−1, as used by Walker et al., gives a desorption energy of 184.8 kJ/mol, in good agreement with their value. Finally, assuming a preexponential factor of 1.7 × 109 s−1, as found by Wilf and Dawson, the desorption energy would be 133.8 kJ/mol, in agreement with their value.
For the second-order desorption peak, the data at lowest coverage were analyzed following Equation (3), where the subscript max indicates values recorded at the maximum in the second-order TPD peak.
l n [ 2 R T m a x 2 θ m a x β ] = E d R T m a x + l n [ E d υ 2 ]
We found from the gradient and intercept of the inset in Figure 5 that the activation energy for desorption is Ed = 103.2 ± 4.4 kJ/mol and the second-order prefactor υ 2 is 4.2 × 10−9±0.3 cm2 molecule−1 s−1. Wilf and Dawson found an average desorption energy of this β2 state of 123 kJ/mol, with a preexponential factor of 6.5 × 10−7 cm2 molecule−1 s−1 [12].
Although the values for desorption energy and the preexponential factor differ significantly from author to author, the measurements are consistent with each other, as assuming a particular preexponential factor gives consistent values for the desorption energy for all measurements. The large scatter in the values for ν can be explained by the extreme sensitivity to slightly different peak maximum temperatures that result in a large uncertainty for this parameter. Simulations of the spectra are given in the Supplementary Materials, using a two-state model, and give reasonable fits to the experimental curves (Figure S4).

2.3. CO Interaction with Pt{110}

Figure 6 shows a high-temperature first-order desorption peak (β1) at 490 K for all coverages, with a second peak evolving at 398 K (β2). This behavior is consistent with literature [37,38,39]. Using the Redhead equation assuming a frequency prefactor of ν = (4.5 ± 1.5) × 1014 s−1 (averaged from values of ν = 6 × 1014 s−1 found by Fair and Madix [39] and ν = 3 × 1014 s−1 found by Engstrom and Weinberg [16]), a value of Ed = 143 (±4) kJ/mol for the desorption activation energy for the β1 desorption peak in the high-coverage region was obtained. This is in reasonable agreement with their values of Ed = 148 kJ/mol [39] and Ed = 151 (±6) kJ/mol [16], but is rather different from the value of Ed = 129 kJ/mol found by Comrie and Lambert [37] who assumed a frequency prefactor of ν = 1013 s−1. Again, recalculating their experimental results with ν = 4.5 × 1014 s−1 gives a value of Ed = 144 kJ/mol, which is in perfect agreement with our result. For the low-temperature β2 desorption peak, a desorption activation energy of Ed = 102 (±3) kJ/mol was calculated assuming a frequency prefactor of ν = 1013 s−1. This value is in agreement with the values of Ed = 108 kJ/mol found by Bonzel and Ku [38] and Ed = 105 kJ/mol found by Comrie and Lambert [37].
Our results for the initial sticking probability of CO, and its saturation coverage, as a function of crystal temperature, on Pt{110} are shown in Figure 7.
At 300 K, we found a value of 0.80 ± 0.04, which is in good agreement with the values of 0.8 found by Fair and Madix [39] and 0.83 found by Wartnaby et al. [11]. Between 330 and 480 K, the initial sticking probability (s0) stays almost constant at 0.62 ± 0.04. This is consistent with the conclusion of Fair and Madix [39] that the initial sticking probability is temperature independent over a wide region, although our values show an earlier decline in s0 at temperatures above 480 K and the onset of a rise below 320 K. Above 480 K, the initial sticking probability falls steeply to 0 at 570 K, due to entering the tail of the β1 TPD desorption peak with a peak maximum temperature of 490 K. The behavior of the initial sticking probability confirms the similarity in the s0 values found for several different noble metal surfaces (Rh{110}, Pd{110}, Rh{111} and Pd{111} have values in the range 0.4–0.7, as seen in [40] and references therein).
The saturation coverage values of the crystal for different temperatures were obtained from the total CO uptake by normalizing to a saturation coverage of 0.88 ML at 300 K. Saturation coverage declines with increasing temperature up to 490 K, the CO TPD peak maximum temperature. For higher temperatures, it shows a slight drop to very low values, finally reaching zero coverage at 570 K.
The sticking probability curves of CO (an example is shown in Figure 8) show precursor-mediated adsorption behavior [11]. CO is trapped into a weakly held mobile precursor state, which can be described as a two-dimensional gas [39]. This mobility gives the possibility of finding sites for adsorption on the surface even if the arrival site is blocked. Some of our sticking curves have been fitted by the Kisliuk expression [41], Equation (4).
s s 0 = 1 θ 1 + ( K 1 ) θ
where s is the instantaneous sticking probability, s0 is the initial (zero coverage) sticking probability and θ is the relative coverage of the crystal surface for a particular temperature, normalized to saturation coverage. The parameter K describes the mobility of the precursor state with small values for a highly mobile precursor and a value of K = 1 for an immobile precursor, which gives rise to the Langmuir adsorption isotherm.
The results for the temperature dependence of K are shown in Figure 9:
It shows a strong tendency towards higher values and thus less mobile precursors with increasing temperature, due to a shorter lifetime of the precursor state and a reduced number of site visits. The value of K = 0.11 (±0.01) found for 300 K is low compared to the value of 0.25 found by Wartnaby et al. [11]. In contrast, a value of 0.13 at 327 K for CO adsorption on Pd{110} found by Jones et al. [38] fits well to our values, again indicating similarity of these surfaces regarding CO adsorption.

2.4. CO Oxidation

Steady-state Temperature Programmed Reaction (TPR) experiments were carried out with different CO/O2 ratios in the beam. Initially, when introduced to the clean surface at 373 K, the mixed beam produces CO2 until the surface is covered with CO (Figure 10). With a high CO/O2 ratio, the CO2 evolution stops quickly (after ~25 s of reaction) due to surface poisoning with CO, whereas at a low ratio it seems to reach near steady-state CO2 evolution.
If the CO poisoned surface is taken to higher temperatures when the CO desorption becomes appreciable, oxygen can adsorb and thus CO oxidation is made possible (Figure 11). This “light-off” of the steady-state reaction takes place in the temperature region between 460 and 510 K (which is also the β1 CO desorption temperature range). At low CO/O2 ratios, the surface is not initially poisoned with CO. The CO2 production shows therefore a steady decrease with temperature as the coverage of CO decreases with increasing temperature. The highest rate is achieved with the ratio nearest to 1.
Angle-resolved CO oxidation measurements were performed at temperatures of 470–620 K, slightly above the CO desorption temperature to avoid surface poisoning and to keep a steady state of reaction. A high temperature was also necessary to keep the CO equilibrium coverage low, as at temperatures above 250 K and CO coverages of more than 0.2 ML, the phase transition (1 × 2) → (1 × 1) takes place [9,42]. Steady-state experiments that were performed at room temperature or below, even at CO/O2 ratios that should ensure that no surface poisoning occurred, showed too low a signal to noise ratio and therefore could not be evaluated. For the angle-resolved measurements, the CO2 flux was measured in the [ 1 1 ¯ 0 ] plane. To achieve a high CO2 signal, a pressure ratio 1:1 of CO/O2 was used in the beam.
The resulting curves showed a broad distribution over the measured angular range, but, for temperatures above 470 K, three components are clearly visible. The curves were deconvoluted into cosine power functions using a numerical least-square fit (Simplex and Levenberg–Marquardt algorithms) to the function given in Equation (5).
I ( θ )   =   I 0 + I 1 cos α 1 ( θ x 1 ) + I 2 cos α 2 ( θ x 2 ) + I 3 cos α 3 ( θ x 3 )
with I(θ) the signal intensity for the crystal polar angle θ, I0 the baseline height, I1I3 the peak heights, α1α3 their exponents and x1x3 their angular positions. The two extreme temperatures are shown in Figure 12 and Figure 13, while the other scattering distributions at 523 and 573 K are given in the Supplementary Materials (Figure S5a,b). The low temperature distribution is quite different from the other three, which are all fairly similar in shape. The computed best fit parameters for the different temperatures are listed in Table 1.
In all four cases two lobes were evident at angles of about ±16° from the Pt{110} surface normal, appearing at approximately 74° and 106°. We could not discriminate a crystal surface normal peak in our data. The inclined angles for product evolution may be attributed to CO2 desorption normal to the reaction sites on the {111} microfacets, and therefore shows sensitivity to the local structure in the reaction, rather than average surface plane dependence. That is, the CO2 is generated at such sites and desorbs directly over the lowest barrier directly into the gas phase in a direction perpendicular to the local potential energy surface.
At the transition state of the reaction, the O-CO complex forms on a highly repulsive potential energy surface with respect to the local facet and the formation of CO2 leads to ejection of the molecule with excess kinetic energy (in comparison to thermal). This kinetic energy leads to a high velocity perpendicular to the reaction site in comparison to lateral thermal motion and hence is characterized by a high exponent in the cosine fits (typically α is 10–20).
The third peak in CO2 evolution that appears with the crystal oriented at ~44° does not correspond to a facet or a surface normal. We believe that this peak is likely to be due to the angle dependence of the absolute amount of produced CO2. The angle integrated mass spectrometer showed a maximum in the CO2 production at the facing beam position, so the third peak can be attributed to this maximum.
In an angle-resolved TPD study, Matsushima et al. found desorption angles of ±25° for a CO2 formation peak at 310 K and ±23° for a CO2 formation peak at 410 K [20]. They explained the difference between facet angles and desorption angles with effects of conducting electrons and surface distortions (see Introduction). Their method to deconvolute the measured curves in single peaks was to fit two peaks to the outer parts of the curves assuming symmetrical behavior and to subtract these two peaks from the measured curve to get a third peak centered at the surface normal. For several reasons, this approach is inappropriate for our data: at very grazing angles between surface and beam, the beam is spread across the face of the crystal and will overspill the edges leading to a dramatic drop in apparent reaction products until at an angle of 135° the beam will only hit the side of the crystal. The steep decrease at high angles is therefore an artificial effect, as described in Figure S1. This inherent asymmetry in our experimental geometry therefore dictates our analysis approach.
Despite these difficulties, the achieved angles for the lobes are only slightly below the values obtained by Matsushima et al. [20,24], but, importantly, we ran a continuous angle-resolved experiment under low coverage steady-state reaction conditions. At 470 K, there are no obvious peaks in the curve, although the computed best fit also showed two peaks at ~±17° from the surface normal. It may well be that at 470 K the surface coverage of CO is sufficient to initiate a partial (1 × 2) → (1 × 1) phase transition. This would be expected to decrease the amount of CO2 that desorbs from the {111} microfacets of the Pt{110}-(1 × 2) surface. The newly formed (1 × 1) surface has lower corrugation and so will not show such distinct facet desorption.
Note that Neugebohren et al. [1] mapped velocity-resolved rates of carbon monoxide at stepped platinum surfaces and found two distinct channels for reaction, being dominated at low temperatures by the more active step sites and at high temperatures by the more abundant terrace sites. The temperature switch between channels is at ~700 K under their supersonic conditions. Our work is in the temperature regime below this, where step sites on an otherwise flat surface might be most active. Of course, in the work here, effectively all sites are step sites on Pt{110}, but the {111}-facetted (1 × 2) surface dominates the distribution of evolving, activated CO2 molecules.

3. Experimental

The experiments were carried out in an ultra-high vacuum chamber(VG Scientific, East Grinstead, UK) (Figure 14) pumped by a diffusion pump (Edwards Ltd, Burgess Hill, UK) and an additional titanium sublimation pump (VG) to give a base pressure below 10−10 mbar.
The Pt{110} crystal was mounted centrally in the chamber on a manipulator capable of moving in the X, Y and Z directions as well as rotating the crystal around its polar and azimuthal axes (Figure 14). Both axes were equipped with stepper motors (VG) to allow automated angle-resolved experiments by preprograming sequences of temperature ramps and angular movements. The crystal was held by two tungsten wires spot-welded to its side, which were also used for conductive heating. For low-temperature experiments, the crystal could be cooled down to 120 K by liquid nitrogen cooling. The temperature of the crystal was measured by a K-type thermocouple (Goodfellow, Cambridge, UK) spot-welded to the rear face.
Gases could be dosed onto the crystal surface either via leak valves (VG) (background dosing) or using a thermal molecular beam attached to the chamber, normally operated at ~40 mbar source pressure. The beam could be shut off using a computer-controllable shutter inside the beam system and a gold flag in the chamber right between beam nozzle and crystal. The beam was sharply collimated to give a spot of 3-mm diameter. The resulting beam flux was calculated from the sticking measurements with O2 to be F = 1.2 (±0.4) × 1018 molecules m−2 s−1 for a source pressure of 40 mbar. For this calculation, an O2 “saturation” coverage of 0.6 was assumed in the temperature range of 300–400 K.
Angle-integrated experiments could be performed using a quadrupole mass spectrometer (MS, Hiden Analytical, Warrington, UK) built into the main chamber without line of sight of the sample to analyze the background gas. A second quadrupole mass analyzer was situated in a differentially pumped side chamber at an angle of 45° to the molecular beam behind two collimator apertures to allow angle-resolved observations. Both spectrometers ran concurrently and analog inputs on both instruments were used to record sample temperature, orientation and molecular beam pressure synchronized with the MS data.
The chamber was further equipped with an argon ion sputter gun and a LEED/AES unit for crystal cleaning and confirming surface order and cleanliness, respectively. The crystal was cleaned by sputtering with argon ions, followed by heating in oxygen at 700 K and 5 × 10−8 mbar for 30 min. Finally, the crystal was annealed at 970 K for 10 min. Cleanliness of the surface was checked by LEED (VG) and oxygen TPD measurements. The sample was aligned by hand while viewing the LEED to give datums for azimuth and polar angle motors.
Temperature programmed desorption, and sticking experiments using the King and Wells technique [25] could be performed in the machine. Temperature programmed reaction (TPR) experiments could also be made on a pseudo-steady-state basis by beaming gases at the crystal surface while ramping surface temperature [26]. Angle-resolved experiments could be performed under steady-state conditions by beaming gas at the crystal surface while automatically turning the crystal around the polar axis and recording the angle-dependent flux of molecules with the mass spectrometer in the side chamber. Typically, this could be achieve in 200 s. The yield curves were normalized by baseline subtraction and division by the beam source pressure (there is a linear dependency of the beam flux on the source pressure for P < 70 mbar) to obtain comparable values. They were averaged over several experiments for noise reduction. Calibration of the sticking measurements is described in the Supplementary Materials.

4. Conclusions

We constructed a simple thermal molecular beam reactor which can determine the angular distribution of products from surface reactions under in-situ steady-state reaction conditions in a fast, efficient manner. It can also be done in a pseudo-steady state, temperature-programmed manner. Product scattering during CO oxidation could be achieved in about 200 s. The products are resolved into two components at high temperature which desorb at ~±16°, close to the normal to the {111} microfacets of the Pt{110}-(1 × 2) surface. We determined the sticking probabilities and desorption energies of oxygen and CO and show that reaction between them only occurs at steady state at low CO:O2 ratios at low temperature, but can occur at high CO:O2 ratios at elevated temperature.

Supplementary Materials

The following are available online at https://www.mdpi.com/2073-4344/10/11/1229/s1, Figure S1: Apparent initial sticking probability s0,app of oxygen at 420 K, Figure S2: He, Ar and O2 scattering from Pd(111) at 373, 573 and 873 K, respectively, Figure S3: Sticking probability of oxygen as a function of uptake for different sample temperatures, Figure S4: Simulated oxygen TPD spectra, Figure S5: Angle-resolved CO oxidation at 523 and 573 K surface temperature.

Author Contributions

Conceptualization, M.B. and R.A.B.; methodology, B.U.K. and K.L.; software, R.A.B., B.U.K. and K.L.; formal analysis, M.B., B.U.K., K.L. and R.A.B.; investigation, B.U.K., K.L. and R.A.B.; resources, M.B.; writing—original draft preparation, B.U.K. and K.L.; writing—review and editing, R.A.B. and M.B.; visualization, R.A.B.; supervision, M.B. and R.A.B.; project administration, M.B.; and funding acquisition, M.B. All authors have read and agreed to the published version of the manuscript.

Funding

This research was funded by EPSRC, grant numbers EP/R026939/1 and EP/R026815/1.

Acknowledgments

K.L. and B.U.K are grateful for student mobility grants within the ERASMUS program of the EU.

Conflicts of Interest

The authors declare no conflict of interest. The funders had no role in the design of the study; in the collection, analyses, or interpretation of data; in the writing of the manuscript, or in the decision to publish the results.

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Figure 1. (a) Polar representation of the scattering of He and Ar from Pt(110), clearly showing the differences between the light and heavy inert gases. The latter has a much longer residence time on the surface and so becomes largely thermalized to the surface temperature. (b) The signal intensity is plotted as a function of crystal polar angle (Cartesian plot).
Figure 1. (a) Polar representation of the scattering of He and Ar from Pt(110), clearly showing the differences between the light and heavy inert gases. The latter has a much longer residence time on the surface and so becomes largely thermalized to the surface temperature. (b) The signal intensity is plotted as a function of crystal polar angle (Cartesian plot).
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Figure 2. (a) Simulated signal intensity of a scattering simulation for Pt{110}-(1 × 2). Pictograms of the {110} crystal orientation at key specular positions: (b) pseudo-specular reflection from the surface plane ignoring microfacets; (c) specular reflection from first facet ~102°; and (d) specular reflection from second facet at ~33°.
Figure 2. (a) Simulated signal intensity of a scattering simulation for Pt{110}-(1 × 2). Pictograms of the {110} crystal orientation at key specular positions: (b) pseudo-specular reflection from the surface plane ignoring microfacets; (c) specular reflection from first facet ~102°; and (d) specular reflection from second facet at ~33°.
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Figure 3. Initial sticking probability of oxygen and saturation coverage (in atoms), as a function of crystal temperature.
Figure 3. Initial sticking probability of oxygen and saturation coverage (in atoms), as a function of crystal temperature.
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Figure 4. TPD spectra of oxygen for heating rates of 0.5, 1, 2, 3 and 4 K/s in the order of increasing peak maximum. The clean Pt{110} sample was dosed with 22.5 L of oxygen at 420 K with TPD recorded angle integrated from the main chamber MS. The insert shows a plot of the peak maximum points linearised according to Equation (1).
Figure 4. TPD spectra of oxygen for heating rates of 0.5, 1, 2, 3 and 4 K/s in the order of increasing peak maximum. The clean Pt{110} sample was dosed with 22.5 L of oxygen at 420 K with TPD recorded angle integrated from the main chamber MS. The insert shows a plot of the peak maximum points linearised according to Equation (1).
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Figure 5. TPD-spectra of oxygen on Pt{110} for different exposures. The sample was dosed at 420 K with a pressure of 1 × 10−8 mbar O2. The measurements were performed on two different days (indicated by n.d. for next day’s results). Due to the extreme sensitivity of oxygen TPD to the surface structure, the TPD spectra of each day differ slightly from each other. The heating rate was 4 K/s. The insert shows a plot of the TPD peak maximum at low coverage according to equation (3) for exposures up to 5 min.
Figure 5. TPD-spectra of oxygen on Pt{110} for different exposures. The sample was dosed at 420 K with a pressure of 1 × 10−8 mbar O2. The measurements were performed on two different days (indicated by n.d. for next day’s results). Due to the extreme sensitivity of oxygen TPD to the surface structure, the TPD spectra of each day differ slightly from each other. The heating rate was 4 K/s. The insert shows a plot of the TPD peak maximum at low coverage according to equation (3) for exposures up to 5 min.
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Figure 6. TPD-spectra of CO on Pt{110} for different exposures, as indicated in the figure. The sample was dosed at 200 K with a CO pressure of 5 × 10−8 mbar. The heating rate was 3 K/s.
Figure 6. TPD-spectra of CO on Pt{110} for different exposures, as indicated in the figure. The sample was dosed at 200 K with a CO pressure of 5 × 10−8 mbar. The heating rate was 3 K/s.
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Figure 7. Initial sticking probability and saturation uptake of CO as a function of crystal temperature.
Figure 7. Initial sticking probability and saturation uptake of CO as a function of crystal temperature.
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Figure 8. Plot of relative sticking probability s/s0 versus relative coverage θ for CO sticking at 450 K (solid line). The corresponding Kisliuk fit is shown as a red line.
Figure 8. Plot of relative sticking probability s/s0 versus relative coverage θ for CO sticking at 450 K (solid line). The corresponding Kisliuk fit is shown as a red line.
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Figure 9. The dependence of the Kisliuk precursor mobility parameters for CO adsorption on Pt{110} with temperature.
Figure 9. The dependence of the Kisliuk precursor mobility parameters for CO adsorption on Pt{110} with temperature.
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Figure 10. CO2 evolution during the introduction of a mixture of CO and oxygen on a clean Pt{110} surface with a molecular beam at a constant temperature of 370 K. CO/O2 ratios are 0.3 (blue curve), 1.3 (red curve) and 3.3 (green curve).
Figure 10. CO2 evolution during the introduction of a mixture of CO and oxygen on a clean Pt{110} surface with a molecular beam at a constant temperature of 370 K. CO/O2 ratios are 0.3 (blue curve), 1.3 (red curve) and 3.3 (green curve).
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Figure 11. Pseudo-steady-state CO2 evolution while ramping the surface temperature at 4 K/s. The crystal was supplied with a constant flux of CO and oxygen from the molecular beam. CO/O2 ratios as in Figure 10.
Figure 11. Pseudo-steady-state CO2 evolution while ramping the surface temperature at 4 K/s. The crystal was supplied with a constant flux of CO and oxygen from the molecular beam. CO/O2 ratios as in Figure 10.
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Figure 12. Angle-resolved CO oxidation experiment at T = 473 K. The CO2 signal intensity is plotted as a function of the crystal polar angle. Three cosineα-shaped peaks are fitted simultaneously, and their sum are shown as solid lines.
Figure 12. Angle-resolved CO oxidation experiment at T = 473 K. The CO2 signal intensity is plotted as a function of the crystal polar angle. Three cosineα-shaped peaks are fitted simultaneously, and their sum are shown as solid lines.
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Figure 13. As in Figure 12, but at 623 K surface temperature.
Figure 13. As in Figure 12, but at 623 K surface temperature.
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Figure 14. Schematic diagram of the molecular beam apparatus. The small insert illustrates the angle-resolved experimental facility.
Figure 14. Schematic diagram of the molecular beam apparatus. The small insert illustrates the angle-resolved experimental facility.
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Table 1. CO2 angular desorption parameters from fitting of profiles in steady-state CO oxidation from Pt{110}-(1 × 2) at four surface temperatures. Angles x1x3 are highlighted and R2, the coefficient of determination, for each fit is given. Data at 523 and 573 K are shown in Figure S5a,b.
Table 1. CO2 angular desorption parameters from fitting of profiles in steady-state CO oxidation from Pt{110}-(1 × 2) at four surface temperatures. Angles x1x3 are highlighted and R2, the coefficient of determination, for each fit is given. Data at 523 and 573 K are shown in Figure S5a,b.
Temperature/K473523573623
I01.68 ± 0.861.14 ± 0.460.99 ± 0.512.44 ± 0.24
I10.64 ± 0.305.77 ± 0.606.78 ± 0.664.97 ± 0.42
x165.4 ± 1.643.2 ± 2.043.6 ± 2.144.0 ± 1.7
α1130.6 ± 129.214.6 ± 3.712.2 ± 2.917.0 ± 3.0
I26.09 ± 0.987.06 ± 0.427.70 ± 0.667.70 ± 0.20
x273.9 ± 7.374.3 ± 1.474.2 ± 1.377.0 ± 1.1
α22.74 ± 0.9419.1 ± 2.719.2 ± 2.215.0 ± 2.1
I33.32 ± 1.6910.6 ± 0.511.9 ± 0.59.35 ± 0.33
x3107.3 ± 0.1105.8 ± 0.1105.6 ± 0.1107.2 ± 0.1
α310.9 ± 4.915.8 ± 1.614.5 ± 1.221.9 ± 1.3
R20.9680.9930.9860.988
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Bowker, M.; Klink, B.U.; Lass, K.; Bennett, R.A. A Simple Angle-Resolved Thermal Molecular Beam Reactor: Applied to CO Oxidation on Pt{110}. Catalysts 2020, 10, 1229. https://doi.org/10.3390/catal10111229

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Bowker M, Klink BU, Lass K, Bennett RA. A Simple Angle-Resolved Thermal Molecular Beam Reactor: Applied to CO Oxidation on Pt{110}. Catalysts. 2020; 10(11):1229. https://doi.org/10.3390/catal10111229

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Bowker, Michael, Björn Udo Klink, Kristian Lass, and Roger A. Bennett. 2020. "A Simple Angle-Resolved Thermal Molecular Beam Reactor: Applied to CO Oxidation on Pt{110}" Catalysts 10, no. 11: 1229. https://doi.org/10.3390/catal10111229

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