Open Access Article
Ester Perez-Pencoa,
Jonathon Cottomab,
Emilia Olssonab and
Roland Bliem
*ac
aAdvanced Research Center for Nanolithography, Science Park 106, 1098 XG Amsterdam, The Netherlands. E-mail: r.bliem@arcnl.nl
bInstitute for Theoretical Physics, Institute of Physics, University of Amsterdam, Science Park 904, 1098 XH Amsterdam, The Netherlands
cvan der Waals–Zeeman Institute, Institute of Physics, University of Amsterdam, Science Park 904, 1098 XH Amsterdam, The Netherlands
First published on 16th June 2026
In chemical vapor deposition, the interaction of the precursor molecule with the substrate can crucially influence the deposition process and provide pathways to tailor the growth. Here, we report mechanistic differences of Si growth from silane (SiH4) at pristine and oxidized surfaces of Ru(0001) in a combined in situ X-ray photoelectron spectroscopy (XPS) and density functional theory (DFT) study. Silane decomposition is essentially barrierless and thus very efficient on Ru(0001), where it saturates at approximately a monolayer of silicon. Similarly, silane readily decomposes on a thin intermediate phase of Ru oxide, which is structurally different from thicker RuO2 layers, and induces a transformation to a compound with oxidized Si and reduced Ru. In contrast, the bulk-like RuO2 phase is observed to be fully inert towards the decomposition of SiH4 at room temperature. This difference between the two oxides is suggested to originate from disorder and the availability of active sites in the thin Ru oxide layer. The surface-assisted deposition of silicon on Ru can thus be modified and inhibited using oxidation, depending on the nature of the oxide layer.
The oxidation of Ru(0001) has been studied in substantial detail and provides a well-defined system for correlating structure and reactivity. The oxidation of the Ru(0001) surface is generally agreed to proceed via three regimes: (i) ordered chemisorbed O adlayers, (ii) thin surface-oxide structures, and (iii) bulk rutile RuO2 film.9–13 At low oxygen exposures, the surface exhibits a sequence of well-ordered chemisorbed O phases with coverages up to one monolayer, including p(2 × 2)-O, p(2 × 1)-O, (2 × 2)-3O and the dense (1 × 1)-O overlayer.14–16 These adlayers are now quantitatively characterized both experimentally and theoretically and constitute a robust reference for a metallic Ru(0001) surface decorated by on-surface oxygen. At intermediate oxygen coverages and higher oxygen chemical potentials, the picture is less clear: oxygen incorporation below the top Ru layer leads to subsurface O islands and the formation of oxide-like surface structures, but the detailed atomistic structure of this intermediate oxide remains an open question. Density-functional theory (DFT) predicts that an O–Ru–O trilayer is a low-energy metastable precursor and that stacking of such units provides a pathway towards a rutile-like RuO2 film once a critical thickness is exceeded.11 Subsequent real-space microscopy and diffraction have shown that oxygen-rich Ru(0001) is better described in terms of RuO2-derived domains, in particular RuO2(100)-(1 × 1) and RuO2(110) facets, rather than a single trilayer structure.10,12,13,16,17 Within this intermediate regime, disorder appears in two ways: as explicitly disordered or defect-rich oxide regions, and as structural disorder within otherwise RuO2-like domains, both of which have been implicated as catalytically active phases.17,18 At sufficiently high temperatures and oxygen pressures, the oxidation terminates in continuous RuO2(110) films with bulk-like rutile structure of well-defined stoichiometry.10,12,13
These distinct oxidation regimes of Ru(0001) are known to exhibit markedly different chemical reactivity. Chemisorbed O adlayers modulate the adsorption energies and activation barriers for small molecules, but retain many features of a metallic surface.11,14,15 In contrast, the formation of RuO2-like surface oxides introduces a transition to oxide-like electronic structure and coordinatively unsaturated cation sites, which profoundly change the kinetics and selectivity of oxidation reactions such as CO oxidation and NO2 activation.10,12,13,18 Subtle changes in oxide thickness, orientation and defect density can thus lead to large changes in reaction rates and preferred pathways on Ru-based catalysts.10,12,13 From the perspective of interconnect processing, this implies that small variations in surface preparation—ranging from a clean metal surface through thin defective oxides to thick RuO2—may qualitatively alter the interaction with reactive precursor molecules, even if the nominal substrate is “Ru(0001)” in all cases.
Silane (SiH4) and related SiHx species are ubiquitous precursors for silicon-containing films in chemical vapor deposition (CVD), plasma-enhanced CVD, and plasma-assisted processes for amorphous and microcrystalline Si, dielectrics, and barrier layers.19–24 In the gas phase, silane decomposes only at comparatively high temperatures, with significant pyrolysis typically occurring above ∼420 °C.25,26 On high-surface-energy metal substrates, silane and its fragments can decompose at far lower temperatures than in the gas phase, frequently at or below room temperature, yielding Si adlayers or surface silicides along with chemisorbed hydrogen.27–31 For example, on Cu(111) silane adsorption at cryogenic temperatures leads to SiH3 fragments that decompose upon modest heating to give elemental Si and bridging H,27,28 while on Ni(111) and Pd(100) silane CVD produces surface alloys and silicide-like phases.29,32 These studies establish that reactive late transition-metal surfaces can strongly catalyze Si–H bond activation, enabling Si deposition at temperatures relevant for interconnect processing.
In contrast, the microscopic interaction of silane with Ru(0001) and its oxides is still only partially understood, despite its relevance to both contamination control and purposeful Si incorporation. An early UHV study of disilane (Si2H6) adsorption on Ru(0001) using LEED, AES and RAIRS showed that Si2H6 dissociates via SiH fragments to elemental Si and, upon annealing, to an ordered Ru silicide overlayer,33 demonstrating efficient Si–H bond activation on the clean Ru(0001) surface. Plasma-based experiments have shown that volatile Si hydrides generated by hydrogen radicals can undergo self-limiting chemisorption on Ru thin films, yielding approximately one monolayer of chemisorbed Si under near-equilibrium conditions.7 Together these studies suggest a strong tendency of Ru surfaces to activate Si–H bonds and accommodate Si at the surface. However, they do not resolve how the detailed oxidation state and structure of the Ru substrate—clean metal, thin defective oxide, or thick RuO2—control the elementary adsorption and decomposition steps of silane itself. Moreover, apart from the disilane study on Ru(0001),33 most prior work either relies on polycrystalline Ru, complex multi-component plasma environments,7 or focuses on the growth of fully oxidized SiO2-like films on Ru(0001),34 leaving a gap in mechanistic understanding of the earliest stages of SiHx adsorption and decomposition on structurally well-defined Ru(0001) and RuOx surfaces.
Here, we follow the deposition of Si from silane in situ, comparing the adsorption mechanisms and kinetics at the pristine Ru(0001) surface and oxidized Ru(0001) with different oxide thicknesses. We observe a stark contrast between the highly reactive surfaces at low oxide thicknesses and a fully inert layer of the bulk-like phase of rutile RuO2. While increasing oxygen coverages on Ru(0001) are predicted to block silane adsorption, high sticking and changes in the deposited Si species indicate that different adsorption mechanisms prevail in the presence of oxygen. The complex role of oxygen in the site selection and Si chemistry illustrates the profound implications of seemingly subtle surface modifications on reactive deposition and contamination control.
The as-prepared Ru surfaces were exposed to a mixed gas containing 1 vol% SiH4 (≈0.92 mol%) in Ar gas at a starting total pressure of 4 × 10−6 mbar and increased until a maximum total pressure of 4.0 × 10−4 mbar. The pressure increases are indicated by gray dashed lines in all datasets except for the thick oxide (r-RuO2), for which the last increase occurred at a later point in time and would have extended the x-axis excessively. This step is not represented within the plotted range, as it caused no observable effect on the surface. In the experiment on the effect of X-rays on the activation of silane, the gas supply was closed and allowed to reach UHV again before starting the X-ray source for each data point and re-opened only after switching off the X-ray source. The surface composition during SiH4 exposure was investigated using near-ambient pressure XPS with a Scienta Omicron HiPP-3 spectrometer and a monochromatic Al Kα X-ray source (1486.6 eV). The HiPP-3 analyzer was used with a 0.8 mm cone and a slit setting of 1.0 mm. Survey spectra were acquired at a pass energy of 300 eV, Ru 3d, Si 2p and O 1s spectra at 300 eV, and high-resolution spectra at 100 eV. For each pass energy, the measured XPS binding energies were shifted using the Ru metal peak as a reference. XPS peak fitting was performed using KolXPD applying Shirley backgrounds for all peaks. To ensure reproducible and comparable fitting results, constraints based on fundamental physical principles, literature values, and reference samples were systematically applied. Specifically, Ru reference spectra for the main and satellite peaks were obtained from oxygen-free and fully oxidized Ru reference samples to determine the Lorentzian and Gaussian components and, where applicable, the asymmetry parameters of the peak shapes (Voigt, Doniach-Sunjic convoluted with Gaussian). The peak shapes of all regions as well as the energy difference and area ratio (Ru 3d5/2
:
Ru 3d3/2 = 1.5) of the spin–orbit-split components of Ru 3d were kept constant for all fits. The binding energies were fixed with respect to the Ru 3d metal peak, allowing for no relative variation of the individual species but small (<100 meV) changes of the reference energy between different sets of measurements. For both O 1s and Si 2p spectra, the focus was the determination of the total area of peaks emerging at a priori unknown binding energies and peak shapes. No constraints were applied to those peaks.
All DFT calculations were performed spin-polarized at the Γ-point using CP2K (v2023.1)37 with DZVP-SR-MOLOPT basis sets38 and GTH pseudopotentials.39,40 Plane-wave cutoffs of 850 Ry (CUTOFF) and 60 Ry (REL_CUTOFF) ensured convergence to ∼0.1 meV per atom. Bulk hcp Ru was modeled using a 6 × 6 × 5 hexagonal supercell and an equivalent 6 × 3 × 5 orthohexagonal representation of the same optimized hcp lattice. The nine-layer Ru(0001) slabs used in the surface calculations were constructed from the optimized orthohexagonal representation and separated by a minimum 20 Å of vacuum. The PBE functional41,42 and D3(BJ) dispersion43–45 were used, with energy and force thresholds of 10−7 eV and 0.005 eV Å−1. Oxygen coverages θ were referenced to Ru(0001) hcp sites, where θ = 1 corresponds to a (1 × 1)O overlayer. Ordered phases were denoted using Wood's notation (A × B).46 A symmetry-adapted enumeration generated 174 unique O configurations from (6 × 6) (θ ≈ 0.03) to (1 × 1) (1.0 ML). Adsorption energetics and coverages were post-processed using ASE47 and NumPy,48 with automated Ru-layer detection and normalized O-counts following the methodology in ref. 8.
![]() | (1) |
from gas-phase calculations at the same level of theory.
For each O/Ru(0001) surface, SiH4 was positioned above candidate adsorption O-sites, Ru-sites, and mixed O–Ru—sites identified within 3.0 Å of the surface and filtered by local fingerprint uniqueness (radius 4.0 Å, z-window 3.0 Å). A minimum-image clustering scheme (link radius 3.0 Å) selected unique SiH4 configuration per connected region. The SiH4 molecules were placed 2.0 Å above the reference atom (Hbase/Hdown/Si) and shifted outward to maintain a 2.0 Å H–surface clearance.
SiH4 interaction energies were evaluated as
| EInteraction(SiH4) = Efinal − Eslab − ESiH4, | (2) |
The evolution of the surface composition of the metallic and oxidized Ru(0001) was followed during exposure to SiH4, starting at equivalent pressures of approximately 4 × 10−8 mbar and increasing to 4 × 10−6 mbar after changes at low pressure had saturated. Fig. 2 shows the atomic percentage of Si 2p, O 1s and the Ru4+ content of the Ru 3d region as a function of exposure time to SiH4, with insets (e–g) in the right column zooming in on the changes in the initial phase of exposure. The times, at which the pressures were increased by a factor of 10, are indicated by grey lines. The respective initial and final compositions are summarized in Table 1. For pristine Ru (0 nm RuO2, Fig. 2(a) and (e)), the Si signal increases rapidly but the growth saturates quickly after less than ten minutes. The oxygen content increases gradually, but no signal of oxidized Ru or Si is observed, indicating the slow accumulation of adsorbed oxygen. When starting from the thin oxide (0.4 nm RuO2, Fig. 2(b) and (f)), Si deposition also occurs within the first ten minutes, similar to the metallic surface. At the same time, the Ru4+ content drops to zero, while the oxygen content is maintained and even slightly increases. The mixed oxide (1.2 nm RuO2, Fig. 2(c) and (g)) exhibits similar behavior, with fast growth of the Si signal but it saturates at a lower total Si coverage and exhibits a finite Ru4+ content after the deposition. For both oxides, the change in the Si content is more pronounced than the decrease of the Ru4+ content. In contrast to the metallic and mildly oxidized cases, the thick RuO2 layer (4.2 nm RuO2, Fig. 2(d)), does not present any discernible change upon SiH4 exposure in the in situ measurement despite a longer exposure than for the thin oxide. The second pressure increase performed after 190 minutes is not plotted but did not lead to any further change. Detailed Si 2p scans after the in situ experiment reveal a small fraction of Si (∼1% relative intensity), which we attribute to a small residual content of the intermediate oxide or extended defects such as step edges.
| Initial | Final | Initial | Final | Initial | Final | |
|---|---|---|---|---|---|---|
| Ru4+ % | Ru4+ % | O % | O % | Si % | Si % | |
| Pristine Ru | — | — | — | 2 | — | 12 |
| Thin oxide | 10 | — | 11 | 16 | — | 13 |
| Mixed oxide | 17 | 13 | 35 | 36 | — | 8 |
| Thick oxide | 33 | 32 | 58 | 57 | — | 1 |
To gain insights into the underlying deposition process and the nature of the deposited species, the Si 2p and O 1s spectra taken after the silane exposure are examined in detail. Fig. 3(a) shows that on Ru metal, Si deposits as a single species, illustrated by a single Si 2p peak at 99.6 eV. The precise identification of the deposited Si species is not straightforward, as the characteristic XPS peaks, Ru 3d and Si 2p, show only subtle changes in peak position between the elemental materials and their compounds. In the XPS literature, the 2p binding energy of elemental Si0 ranges from 98.3 eV54 to a range of values above 99 eV,55–58 and even up to 100 eV for high doping levels.59 Next to elemental Si, the binding energies of Ru silicides have been reported to match the observed values, with Si 2p core levels ranging from 99.3 to 99.8 eV.56,60,61 A key limitation in comparing our system with previous studies is that they investigate Ru on Si, while we investigate Si on Ru, which presents different intermixing behaviors and possibly different Ru/Si ratios, which can be reflected in different surface chemistry. Work by van Vliet et al.62 showed shifts in the 2p binding energy with the Si content of thin layers, ranging from 99.4 eV for Si on Si to 99.7 eV for Ru2Si3 and 100.0 eV for RuSi films. These results were related to the plasmon peak of the silicides for their identification, but the weak signal and the overlap with stronger features from metallic Ru (3d and 4p), prevent us from using this method of assigning the Si species. Reports of intermixing upon deposition of Si on Ru at room temperature63,64 indicate that silicide formation is likely to occur also on the surfaces presented here.
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| Fig. 3 Si 2p and O 1s core level XPS spectra acquired after silane exposure for pristine Ru, thin oxide, and mixed oxide. | ||
The cases of the oxides are equally intriguing, but more complex. While there is clear contrast between the absence of Si deposition for the bulk-like rutile RuO2 and its rapid growth on the thin oxide, resolving the individual species is challenging. Two components are required to fit the Si 2p peak of the thin oxide in Fig. 3(b), which has distinct features at 100.4 eV and 103.2 eV. The respective O 1s peak after exposure in Fig. 3(e) is in agreement with a single species centered at 532.2 eV. The mixed oxide with elements of the thin oxide and the inert rutile RuO2 seems to behave like a superposition of the two in the time-dependent results shown previously, with deposition only occurring on the thin oxide. The detailed analysis of the spectrum in Fig. 3(c), however, presents three Si 2p peaks. In addition to the two peaks at 100.4 eV and 103.2 eV, an additional one is observed at 101.8 eV. Fitting the respective O 1s peak, shown in Fig. 3(f), also requires three components at 531.8 eV, 529.9 eV, and 529.3 eV.
For the identification of the post-exposure species, it is essential to establish a link between the formation of the oxygen and silicon species and the modification of the Ru species at the surface, specifically the extinction of Ru4+ during the deposition of Si at the surface can clearly be resolved. To better understand the RuO2 compositional transformation upon Si deposition in the thin oxide, the in situ evolution of the oxygen species during silane exposure is analyzed in Fig. 4. Prior to silane exposure, iteration 1 finds the O 1s peak at 529.8 eV, as expected for Ru oxide.52 During iteration 2 silane gas is leaked in, which is reflected immediately in the O 1s signal by a lower intensity for the peak at 529.8 eV and the growth of a shoulder at 532.2 eV. Already in the next iteration approximately 2 minutes later, the feature at 532.2 eV becomes the dominant component of the O 1s peak. This broad peak remains unchanged within measurement error for the remaining 65 iterations. The difference in the O 1s peak binding energy showcases a complete change to a different surface species, while the time resolution establishes a causal link to the interaction with silane. The binding energy position after silane exposure is characteristic for Si oxides rather than Ru oxides, indicating that the main bonding partner of the oxygen changed to become Si. Exposure of the thin Ru oxide to silane thus not only leads to Si deposition, but triggers a full transformation of the thin oxide layer into an oxidized Si compound.
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| Fig. 4 XPS spectra of the O 1s region of the thin oxide (0.4 nm) during iteration 1 (before SiH4), and 2, 3 and 68 of exposure to SiH4. | ||
From the oxygen spectra and the high-binding energy component of Si, it seems straightforward to assign the new surface species as SiO2. Typical Si 2p binding energies for SiO2 ranging from 103.2 eV54 and 103.3 eV65,66 to 103.9 eV57 allow the conclusion that the nominal oxidation state of the high-binding energy species is closest to Si4+. The Si peaks at lower binding energies, however, correspond neither to Si4+ nor to silicides. They are found in the range of silicon's sub-oxides, reported at binding energies of 101 eV54 or 101.3 eV56 for Si1+ and 101.8 eV for Si2+.67 The coexistence of multiple Si 2p components may reflect different Si–O–Ru bonding environments, similar to the configurations suggested for ultrathin Si oxide on Ru(0001) by Kremer et al.68 The characteristic features of the ultrathin oxide layer, SiO4 tetrahedra, are also a common motif in silicates. While no XPS studies of Ru silicates were found, Si binding energies in other silicates have been reported in a range of 101.3–102.7 eV,55,69–71 which is consistent with the intermediate binding energies observed upon silane exposure. This binding energy range agrees with the additional peak observed for the mixed oxide, possibly indicating the coexistence of silicates with different Ru contents. This is plausible since we expect the mixed oxide to consist of patches of intermediate oxide and RuO2 in rutile structure, providing reactive boundary sites of the two different oxides, in addition to the active sites on the pure thin oxide. In the absence of spectroscopic literature on ruthenium silicate, assigning the sub-oxides of Si to silicate-like structures, however, remains a speculation.
For SiH4 adsorption (Fig. 5b), close-packed O overlayers—locally nearest-neighbour (NN) complete structures such as the (1 × 1) phase—block Ru sites and enforce physisorption. When the O layer is more open or irregular (striped or patch-like domains), SiH4 dehydrogenates to SiHx fragments (x = 1–3). Intermediate states (SiH4/SiH3/SiH2) appear where O crowding or surface rumpling limits access to multiple Ru neighbours—more strongly bound than physisorbed molecules but short of full Si–H scission. The energetic ordering is dictated by H termination: at low θ, H remains bound as Ru–H on top/bridge sites; at higher θ, nearby O accepts H to form surface OH, which markedly deepens the adsorption well. Because θ includes both surface and sub-surface O, dissociation can persist near θ ≈ 1 ML whenever a fraction of O resides below the surface, leaving Ru surface sites.
Dissociative adsorption progressively consumes the remaining reactive Ru sites. Initial SiH4 molecules dissociate at exposed Ru hollows, depositing Si at hcp positions and passivating adjacent top or bridge sites through Ru–H or, where O is present, OH formation. Each dissociation therefore reduces the local density of available Ru sites, and once the nearest-neighbour ring around an adsorption site becomes filled (NN-complete), subsequent SiH4 adsorption is frustrated. Sub-surface O remains energetically unfavourable and does not influence this process. The reaction thus becomes self-limiting: SiH4 dissociation ceases as the surface approaches O-, Si- and H-induced site saturation, providing the atomistic origin of the rapid saturation of Si observed in the experiment.
The highly efficient dissociation predicted by DFT together with the quick saturation observed in experiment call for a quantification of the deposited amount and the experimental sticking coefficient. To relate the saturation density to a surface coverage, we approximate the coverage of the Si-containing layer by monolayers (ML) of constant thickness, calculated from the relative XPS intensities of the Si 2p and Ru 3d. Since the estimated coverage will vary with the deposited compound, we compare two different configurations of Si-containing layers at the surface as thin and thick approximation of the grown layer. In the thin limit, all Si is concentrated in a monolayer of Si atoms adsorbed at the surface with an estimated thickness of 0.17 nm, derived from the layer spacing reported from DFT.8 In the thicker approximation, the Si forms a compound with Ru and spreads over a larger thickness, selected to be a layer of the stable silicide Ru2Si3. For this case the thickness of 1 ML is taken as 0.28 nm, corresponding to one fourth of the unit cell's c-axis. This value reflects the thinnest layer that preserves the stoichiometry of the silicide.72 The comparison of the two cases is displayed in Fig. 6 and shows that the saturation coverage of Si on pristine Ru is between 0.55 ML (pure Si) and 0.86 ML of Ru2Si3. In the context of the DFT results, this coverage is high, demonstrating that hydrogen does not block sites adjacent to SiH4 dissociation permanently, but is mobile at the conditions of the experiment. This mobility keeps sites for dissociation available until a saturation coverage of Si is reached. The blocking of Ru sites by oxygen predicted by DFT suggests a different possible pathway, in which oxygen also competes for adsorption sites with silane to lower the total Si coverage.
Since SiH4 decomposes readily in the presence of Ru sites, the initial sticking coefficient of the molecule is expected to be reflected in the rate of Si deposition. The sticking coefficient can thus be directly approximated from the time-dependent growth curves of the Si-containing layer. For an impingement rate of silane of Γ(SiH4) = 1.1 × 1013 molecules cm−2 s−1 and a site density of 1.75 × 1015atoms per cm2, we expect the molecules to have interacted with each surface atom after approximately 159 seconds. Only if all these interactions lead to the dissociation of silane and deposition of silicon, a full monolayer will grow within this short time. For a layer of Ru2Si3, the number of Si atoms per surface area is 1.2 × 1015atoms per cm2 (in the coarse approximation of a 2.8 Å thick slice of an orthorhombic Ru2Si3 unit cell cut perpendicular to the c-axis). The experimental observation of a saturation coverage close to a full layer after less than five minutes of exposure thus demonstrates that the probability of dissociative sticking of silane is higher than 36%. Within the experimental time resolution, it can not be excluded that the coefficient is even closer to unity. After this initial phase of fast deposition, no further growth is observed within experimental accuracy, reflecting the self-limiting character of the deposition and the consumption of the active Ru sites in the process. This saturation behavior suggests the growth of a complete layer of electronically different material, which would be consistent with the growth of a silicide approaching a coverage close to a monolayer. However, the observations could also be explained by other models of growth and site blocking, for example the case of Si atoms covering Ru, which is shown to inhibit further reactivity towards Si deposition from silane by our calculations. The presence of adsorbed oxygen or hydrogen could present an explanation why the growth terminates at sub-monolayer coverages.
On the surface covered with a thin or mixed oxide, the deposition kinetics is similar, whereas no deposition occurs on the rutile RuO2 layer beyond a very small content that is likely caused by reactive surface defects or gas-phase activation by electrons. The fast initial growth on the thin oxide is followed by saturation at comparable coverages and time scales to the metal surface. The average sticking coefficient on the thin oxide is thus similar to that of the metal surface, indicating a comparable density of active sites. According to the DFT calculations, however, dissociative adsorption is not expected to occur on Ru sites with oxygen adsorbates. This would only leave a small number of potential active sites on an ordered oxidized surface and would significantly alter the Si growth kinetics. Moreover, the total amount of deposited Si would decrease drastically, which is in contrast to the experimental results. Alternative explanations, such as the coexistence of oxide patches with large areas of Ru metal are not consistent with the different Si 2p binding energies for silane decomposition over Ru metal and thin Ru oxide. The peak positions of Si at the oxidized Ru surfaces demonstrate that all the observable Si interacts with oxygen, likely forming Si–O–Ru bonds and potentially also binary silicon oxides. The strong interaction of the deposited Si across the entire oxidized surface is further highlighted by the observation that all Ru in the thin oxide layer is reduced after silane exposure. However, according to the DFT calculations, oxygen adsorption on an ordered Ru surface deactivates the metal sites for silane decomposition, leading to the conclusion that the thin oxide layer deviates from a Ru surface with adsorbed and incorporated oxygen. While the simulation of layers with entirely different structural and electronic properties is beyond the scope of this study, the observed behavior could also be explained by a high level of disorder, in agreement with literature reports of the intermediate oxide.73 The high density of defect sites on a strongly disordered surface could provide ample opportunity for the adsorption and decomposition of silane, leaving behind Si and hydrogen, which readily bond to surface oxygen.
The proposed role of disorder and defects also prompts the question whether the sample preparation, in particular roughening by sputtering, influences the observed result. While the observation of sharp diffraction spots in LEED patterns after preparation of the pristine metal surface (see Supporting Information) demonstrates that large patches of the surface are ordered, a remaining increase in the density of defects and steps cannot be excluded. A more defective metal surface would likely also translate to more defects in the thin oxide layer prepared by annealing in oxygen. The observation of rapid deposition of Si up to a saturation coverage close to a full layer, however, highlights that also the defect-free Ru(0001) surface efficiently splits SiH4, in agreement with the DFT results. Similarly, the deposition on the thin oxide layer is rapid with a high sticking coefficient, indicating a very high defect density that is more likely intrinsic to the initial oxide formed before converting to the stable rutile structure. This interpretation agrees well with the absence of Si deposition on the thick oxide layer, suggesting that defects do not play a role in silane decomposition after this structural change.
In addition to the deposition of Si described above, the decomposition of SiH4 also liberates four hydrogen atoms per molecule. At the pristine Ru(0001) surface, the Ru metal lattice provides adsorption sites for hydrogen atoms, yielding Ru–SiH(4−n) + nRu–H. While hydrogen atoms are predicted to block sites for further silane adsorption according to the DFT calculation, reflecting the energy at 0 K, this effect is likely negligible thanks to the high mobility of adsorbed hydrogen at room temperature. Moreover, the rate of recombination and desorption of hydrogen is expected to be significant at the time scale and temperature of the experiment, based on temperature programmed desorption studies74 whereas solubility in bulk Ru has been reported to be low.75 Second order desorption peaks reaching close to 300 K for high coverages indicate a finite desorption rate should be expected at room temperature. High-coverage regions of hydrogen would thus result in efficient recombinative desorption from Ru metal, leaving only a low density of hydrogen atoms with long residence time. Upon dissociation of silane over thin Ru oxide, on the other hand, the released hydrogen likely forms hydroxyl groups, which are stable at room temperature. Accordingly, we considered the presence of an O 1s component at binding energies previously attributed to OH species on Ru surfaces.76 Indeed, the two spectra acquired during the main increase of Si intensity (iterations 2 and 3 in Fig. 4) exhibit additional intensity within this energy range. However, the transient nature of this feature, combined with the ambiguous composition and structure of the Ru–Si–O phase, precludes assigning definitive significance to its observation. Our results do not allow for assigning the detailed reaction steps with certainty, and pathways beyond adsorption and dissociation remain speculative. Adsorption on undercoordinated Ru sites, yielding Ru–SiH4−n + nRu–O–OH is considered a likely first step. Among multiple potential options with comparable experimental signature, the formation of SiRu2O4 + 2Ru(OH)2 would for example fulfil mass and charge balance of the entire layer and result in reduced Ru. Nevertheless, important uncertainties remain, for example whether the layer would remain intact at this high hydrogen concentration and whether hydroxyl groups would be stable at room temperature in the Si–Ru–O compound.
The observation of the high sticking coefficient of silane prompted an experimental test of the interference of the in situ measurement with its outcome by activating the silane molecules. Fig. 7 shows a comparison between the silane exposure to pristine Ru with (green) and without (lilac) simultaneous exposure to the Al Kα X-rays used by the spectroscopy tool. For the two data sets a comparable growth trend and the same final Si atomic percentage were observed, regardless of X-ray exposure during the experiment. Most importantly, the fast deposition within the first minutes of exposure was also observed without simultaneous exposure to X-rays. These results demonstrate that additional activation by the X-rays does not contribute decisively to the high sticking coefficient or the resulting Si deposition.
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| Fig. 7 Evolution of silicon atomic percentage throughout the exposure of Ru (0 nm RuO2) to SiH4 in Ar with (green) and without (lilac) simultaneous irradiation by X-rays at the same silane pressure. | ||
Supplementary information (SI) is available. See DOI: https://doi.org/10.1039/d6cp01417h.
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