Coadsorption of sodium and water on MgO„100…/Mo„100… studied by ultraviolet photoelectron and metastable impact electron spectroscopies J. Günster, G. Liu, V. Kempter,a) and D. W. Goodmanb) Department of Chemistry, Texas A&M University, P. O. Box 300012, College Station, Texas 77842-3012 ~Received 4 October 1997; accepted 2 March 1998! The coadsorption of D2 O and Na on the MgO~100!/Mo~100! surface has been studied by metastable impact electron spectroscopy and ultraviolet photoelectron spectroscopy ~He I!. The initial layer of D2 O adsorbed on the MgO~100! surface at 100 K ‘‘wets’’ the surface. For multilayer adsorption, the outermost water molecules exhibit an electronic structure which is very similar to gas phase water. Na dosed onto a D2 O- precovered MgO surface leads to the formation of a hydroxide species, most likely NaOH. This hydroxide species is stable to 530 K. © 1998 American Vacuum Society. @S0734-2101~98!06103-X# I. INTRODUCTION II. EXPERIMENT The adsorption of water has been the subject of numerous experimental and theoretical investigations. In particular, the adsorption of water on the model basic oxide—magnesium oxide—has attracted considerable attention recently ~see Refs. 1–3 for a review!. This system has been studied utilizing techniques such as reflection adsorption infrared spectroscopy ~RAIRS!, temperature programmed desorption ~TPD!, helium atom scattering ~HAS!, high-resolution electron energy-loss spectroscopy ~HREELS! and low energy electron diffraction ~LEED!. From these investigations emerges a rather complete picture of the adsorption dynamics; however, very little information exists regarding the electronic structure of the valence band region of water adsorbed onto solid surfaces. Recently, surface sensitive spectroscopic techniques such as metastable impact electron spectroscopy ~MIES! and ultraviolet photoelectron spectroscopy ~UPS! have proved to be very useful in monitoring the electronic structure of molecular species adsorbed on insulating films.4–8 For an introduction to MIES and its various applications in molecular and surface spectroscopies, see the recent review by Harada et al.9 In the present article MIES and UPS have been used to characterize the adsorption of water on the MgO~100! surface at 100 K. In addition the effect of Na coadsorption has been investigated. In order to avoid charging of the surface during the measurements, ultrathin MgO films were grown on a Mo~100! substrate. As shown in previous investigations,10–13 thin MgO films grow epitaxially on a Mo~100! surface. In addition, these surfaces reproduce the adsorption behavior of a MgO~100! single crystal surface with respect to the adsorption of water.3 The experiments were carried out in an ultrahigh vacuum ~UHV! system ~base pressure ,2310210 Torr! consisting of two interconnected chambers: one for sample treatment and TPD and the other for electron spectroscopy. In the latter chamber, there exist facilities for x-ray photoelectron spectroscopy ~XPS!, Auger electron spectroscopy ~AES!, UPS and MIES measurements. MIES and UPS spectra were measured simultaneously using a cold-cathode discharge source which has been described previously.13,14 Briefly, a helium cold-cathode gas discharge provides both ultraviolet photons ~He I! and metastable He* 2 3 S/21 S (E * 519.8/20.6 eV! atoms with thermal kinetic energies. The triplet-to-singlet ratio has been measured by He* –Ar impact as 7:1, but very efficient conversion into He* 23 S has been observed on metallic and semiconducting surfaces.15–17 Metastable and photon contributions within the beam were separated by means of a time-of-flight method using a mechanical chopper. The collection of a MIES/UPS spectrum requires approximately 180 s. The AES, MIES and UPS spectra were acquired with incident photon/metastable beams 45° with respect to the surface normal in a constant pass energy mode using a double pass cylindrical mirror analyzer ~CMA!, PHI Model 15-255G. It is worth noting that the MIES spectra in the present study were acquired with a CMA which integrates over a relatively wide angular distribution. These results are very similar to those measured previously on MgO surfaces7 using a hemispherical analyzer with a relatively small acceptance angle. The energies denoted by E F in the spectra correspond to electrons emitted from the Fermi level of the Mo~100! substrate. In the following spectra all binding energies are referenced to E F . Since the metallic Mo substrate and the analyzer are in electrical contact, the Fermi energy appears at a constant position. Biasing of the sample ~245 V! permits the work function change of the surface to be measured directly from the high binding-energy cutoff of the spectra. MgO films were grown by depositing Mg in 1310 26 Torr O2 ambient on the Mo~100! surface at 550 K. The Mg a! Also with: Physikalisches Institut, Technischen Universität Clausthal, Leibnizstrasse 4, D-38678 Clausthal-Zellerfeld, Germany. b! Author to whom correspondence should be addressed; electronic mail: [email protected] 996 J. Vac. Sci. Technol. A 16„3…, May/Jun 1998 0734-2101/98/16„3…/996/4/$15.00 ©1998 American Vacuum Society 996 997 Günster et al. : Coadsorption of sodium and water on MgO„100…/Mo„100… 997 source was made from a high-purity Mg ribbon wrapped around a tantalum filament. In order to ensure a stoichiometric MgO layer, the as-prepared surface was further annealed to 700 K in a 1310 27 Torr O2 background for 20 min. As shown in previous investigations, MgO films prepared under these conditions grow epitaxially on the Mo~100! substrate.10,12,18 Water was dosed following the previously described procedure.3 D2O ~CIL, 99.9%! was used after further purification in the vacuum manifold via several freeze–pump– thaw cycles ~vacuum distillation!. In order to minimize H–D exchange, the manifold was baked repeatedly for several hours in an D2O background. Na was deposited onto the surface using a SAES Getters source. III. RESULTS The MIES and UPS spectra of a MgO-covered Mo~100! surface acquired during D2O exposure are presented in Fig. 1. As determined by AES, the thickness of the MgO layer is approximately 5 monolayers ~ML!. D2O was dosed ~0.6 L per minute! onto the substrate which was held at 100 K. MIES and UPS spectra were recorded continuously during the exposure. Due to the insulating character of the clean MgO~100! surface no intensity between E F and 3.8 eV binding energy is apparent in the bottom spectra of Fig. 1. These data show that there are no occupied states in resonance with the impinging He 2s electrons which could lead to MIES spectra dominated by an Auger capture process. Therefore, contributions from the Auger capture process need not be considered, and a direct comparison between the MIES and UPS data is possible.19 The MIES and UPS spectra of the clean MgO~100! surface are in good agreement with those reported previously.7 The structure in the bottom spectrum of Fig. 1, denoted by O(2p), corresponds to emission from the O 2p valence band of the MgO~100! substrate.7,20 During D2O dosing a continuous change from a spectrum typical for a MgO surface ~bottom spectrum! to a spectrum typical for water in the gas phase21 ~uppermost spectrum! is observed in the sequence of MIES data of Fig. 1. Binding energies and molecular orbital assignments for the three water induced structures 1b 1 , 3a 1 and 1b 2 , based on gas-phase photoelectron spectra22,23 and Penning ionization electron spectra ~PIES!24, are also presented in Fig. 1. After an exposure of 12 L D2O ~dotted MIES spectrum!, the MIES spectra are dominated by the water-induced features. We attribute this 12 L exposure to the completion of the first water monolayer ~ML! and the onset of second layer adsorption. After a 15 L exposure the water background pressure was increased by a factor of 2 as indicated in Fig. 1, from 5310 29 Torr to 1310 28 Torr. After a 33 L exposure the water pressure was increased yet again by a factor of 5 ~5310 28 Torr!. At an exposure between 15 and 33 L, the intensities of the water-induced features level off. At 33 L, a shift of the MIES and UPS spectra indicates charging of the surface. On the other hand, the sequence of UPS spectra in Fig. 1 shows a transition from a spectrum typical for a MgO surface JVST A - Vacuum, Surfaces, and Films FIG. 1. MIES and UPS spectra from a 100 K MgO~100!/Mo~100! substrate as a function of D2O exposure. The bottom spectrum shows the clean MgO~100! surface, and the uppermost spectrum shows the water-covered surface. The dashed spectrum corresponds to 1 ML of adsorbed D2O. ~bottom spectrum! to a spectrum typical for condensed water. In the exposure regime between 15 and 33 L, the spectral features corresponding to 1b 1 and 1b 2 are well developed. However, 3a 1 appears to be broadened considerably, which is typical for a condensed water layer.25 The MIES results obtained during exposure of Na to the water-covered MgO surface held at a substrate temperature of 100 K are presented in Fig. 2. The Na exposure and the direction of data collection are noted in the figure. The spectra are displayed with the Na-free, water-covered MgO/Mo spectrum at the top, followed by various Na coverages. In the binding energy range between 6 and 18 eV a spectral change occurs, from that dominated by the three waterinduced features, 1b 1 , 3a 1 and 1b 2 , to that with two additional peaks denoted by A 1 and A 2 . During the Na exposure an attenuation of the water-induced features and their shift to 998 Günster et al. : Coadsorption of sodium and water on MgO„100…/Mo„100… 998 comparison with UPS ~He I! data acquired for sodium hydroxide28 and water adsorbed onto a sodium-doped Cu~111!27 suggests that features A 1 and A 2 at 7 and 11.1 eV binding energy, respectively, correspond to the ionization of the first and third orbitals, respectively, of the Na-bound OH. As shown in Fig. 3, the hydroxide-induced features are stable on the surface up to 530 K. After flashing the substrate to 710 K, the MIES and UPS spectra ~bottom spectra in Fig. 3! are similar to those acquired for a clean MgO~100! surface. IV. DISCUSSION FIG. 2. MIES spectra from a D2O-covered surface as a function of Na exposure where the uppermost spectrum shows the water-covered MgO~100! surface without Na. The direction of the data collection and the relative Na exposure are indicated by the arrow. It is noted that the dotted spectrum shows the same structure between 6 and 18 eV as the substrate shown in Fig. 3 which has been flashed to 150 K. higher binding energies is apparent. The respective UPS measurements, which are not shown here, exhibit the same spectral features but are less well pronounced. The appearance of the feature near E F at the highest Na exposures, denoted by AU, and its satellite at 2.5 eV higher binding energy, likely corresponds to the Na coverage at which the formation of islands with metallic character begins to occur.8,26 Flashing the substrate to 190 K ~as shown in Fig. 3! results in a MIES spectrum that is dominated by A 1 and A 2 and is very similar to the UPS spectrum acquired from water adsorbed on Cu~111! covered by a multilayer Na.27 A FIG. 3. MIES spectra from a D2O-covered MgO surface following the addition of Na ~uppermost spectrum! as a function of the anneal temperature. J. Vac. Sci. Technol. A, Vol. 16, No. 3, May/Jun 1998 The adsorption of water on the clean MgO~100! surface ~Fig. 1!, in the coverage regime up to 1 ML ~dotted spectrum!, yields only weakly developed features with MIES and UPS. This is consistent with the formation of a strong interaction ~chemisorption! between the adsorbed molecules and the MgO surface.3 For coverages higher than 1 ML three distinct features, corresponding to the ionization of the outermost water molecules, are apparent in MIES. According to previous MIES and UPS investigations of condensed water on Cu21 and gas phase measurements,22,23 the features at binding energies of 7.2, 9.2 and 13.6 eV are assigned to 1b 1 , 3a 1 and 1b 2 , respectively. These binding energies correspond to ionization potentials @IP5~excitation energy! 2~electron kinetic energy!# of 11.2, 13.2 and 17.6 eV, respectively. These values are in agreement with those measured for water adsorbed on MoS2 by Yu et al.25 but are approximately 1 eV lower compared to the results of Campbell et al.29 Since no MgO substrate intensity is apparent in MIES after dosing 12 L water, it is assumed that the initial layer of water adsorbed at 100 K ‘‘wets’’ the surface. Due to the very high surface sensitivity of MIES it is not possible to distinguish one layer of condensed water from the uppermost water layer at higher coverages. Therefore, it cannot be excluded that three-dimensional island growth of water, subsequent to the formation of the first uniform layer, has occurred. The most significant difference between the UPS and MIES measurements on condensed water is the appearance of a narrow 3a 1 peak in MIES. This feature is only seen in the UPS measurements for gas phase water. A broadening of the 3a 1 feature in the UPS measurements for condensed water is most likely due to the overlap of the 3a 1 water molecular orbitals forming hydrogen bonds.30 The close agreement between the UPS gas phase 3a 1 spectral feature and the MIES spectra suggests a binding geometry of the outermost water molecules, which minimizes the overlap of the 3a 1 molecule orbitals. However, a determination of the precise geometry for this structure is beyond the scope of this investigation. Na adsorption on the water-precovered MgO~100! surface ~Fig. 2! leads to the formation of a sodium hydroxide species which is stable on the surface to 530 K ~see Fig. 3!. After dosing Na, two groups of features in the binding energy ranging between 6 and 18 eV are apparent in MIES ~bottom spectrum in Fig. 2!. One group (1b 1 , 3a 1 and 1b 2 ) corresponds to intact water molecules, and one (A 1 and A 2 ) corresponds to a hydroxide species . The appearance of both 999 Günster et al. : Coadsorption of sodium and water on MgO„100…/Mo„100… species on the surface subsequent to a saturation exposure of Na indicates that even at high Na coverages intact water molecules survive on the surface. After flashing the substrate to 190 K, which is the typical desorption temperature for multilayer water,3 the MIES spectrum ~see Fig. 3! is dominated by the hydroxide features. The similarity of these spectra with those acquired for solid NaOH suggests, in accordance with Ref. 27, that a three-dimensional D2O derived species is formed on the substrate. A detailed discussion and a comparison to measurements on a Na-precovered MgO surface will be published elsewhere. V. CONCLUSIONS Because of the enhanced surface sensitivity of MIES, it is superior to UPS for monitoring chemisorption phenomena at low adsorbate coverages. It is found that the initial layer of D2O adsorbed on the MgO~100! surface at 100 K wets the surface. 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