Natural and synthetic SnO₂ samples were studied using scanning tunneling microscopy (STM). The SnO₂ surface flattens considerably following high temperature treatments up to 1500 K. The conductivity of the synthetic SnO₂ surface is significantly reduced following annealing at temperatures of approximately 1200-1500 K, making tunneling impossible. A decrease in conductivity was not observed for the natural SnO₂ sample following similar high temperature treatments, most likely due to impurities which act as dopants. No atomic scale images were collected on the SnO₂ surface which provided information regarding atomic positions and point defects on the surface. Water adsorption was studied on the stoichiometric Cr₂O₃ (101̲2) surface, using thermal desorption spectroscopy (TDS). Water was the only desorption product observed during TDS. Adsorption is primarily dissociative following exposure to water at 163 K. Approximately, 0.12 monolayers of water dissociate on the clean, nearly stoichiometric Cr₂O₃ (101̲2) surface. The first order kinetics observed for the recombination of dissociated water are not well understood. One possible explanation is that the rate limiting step for desorption involves the breaking of a Cr-O bond resulting in a freely diffusing OH species. The exchange of halogen and oxygen was studied on Cr₂O₃ (101̲2) using Auger electron spectroscopy (AES) and TDS. The exchange of chlorine and oxygen is completely reversible. Chlorine is removed from the Cr₂O₃ (101̲2) surface following exposure to oxygen. Exposure of CFCl₂CH₂Cl reduces the surface oxygen concentration to that of the clean, nearly stoichiometric Cr₂O₃ (101̲2) surface. The exchange of chlorine with oxygen appears to involve only chemisorbed surface oxygen, not bulk lattice oxygen. / Master of Science

Diese Arbeit ist eine umfassende und systematische Untersuchung der Adsorption von Wasser auf der Fe2O3(0001)-Oberfläche. Sie deckt eine Vielzahl der Probleme auf, die während des Anfangs der Wasseradsorption auf den Übergangsmetalloxidoberflächen auftreten. Dazu gehören die Stabilität der reinen Oberfläche, die Rolle der Oberflächendefekte, der Einfluss der kristallographischen und elektronischen Strukturen, die elementare Kinetik der adsorbierten Arten von Wasser auf der Oberfläche, die Eigenschaften bei niedrigem und hohem Bedeckungsgrad und die Auswirkungen der Wasserstoffbrückenbindung auf die Adsorption und das XPS-Spektrum. Niedrige und hohe Bedeckungsgrade von 0.25 bis 1 Monolage werden untersucht, um die Grundlage für die folgende Erhöhung der Wasserbedeckung, die normalerweise in Experimenten beobachtet wird, zu ermitteln. Das Einzeladsorptionsregime wurde erweitert, um eine echte Wasserdampfumgebung mittels der Gibbs-Energie zu berücksichtigen. Die Ensemblemethode wurde benutzt, um die durchschnittlichen Werte der energisch entarteten Adsorptionskonfigurationen zu interpretieren. Der Abstandsmatrixansatz wurde entwickelt, um die statistische Analyse zu ermöglichen. Die Methode reduziert mithilfe der Oberflächensymmetrie die Gesamtzahl der Adsorptionskonfigurationen, die zu berücksichtigen sind. Das XPS-Spektrum wird für verschiedene Wasserdampftemperaturen und Drücke simuliert. Es wird eine gute Übereinstimmung zwischen theoretischen und experimentellen Spektren erreicht und die geringen Unterschiede werden erklärt. Die Hauptmerkmale des XPS-Spektrums beim Anstieg von relativer Feuchtigkeit des Wasserdampfs werden beschrieben. Die Ähnlichkeiten und Unterschiede der Wasseradsorption auf Fe2O3 und Al2O3 werden betont und die wichtigsten Tendenzen werden abgeleitet. Auf Grund dieser Arbeit kann der Anfangsprozess der Fe2O3(0001)-Oberflächenbenetzung erklärt werden. / The present study is a comprehensive systematic theoretical investigation of the water adsorption on the Fe2O3(0001) surface. It covers a broad number of problems inherent to the initial stage of the water adsorption on the transition metal oxide surface: clean surface stability, the influence of surface oxygen defects, the role of the crystallographic and electronic structures on the adsorption configuration, elementary kinetics, the particular qualities of the low and high adsorption coverage regimes and the effect of the hydrogen bonding on adsorption and on the XPS spectra simulation. The low and high coverage regimes from 0.25 up to 1 monolayer water coverage were considered to form a basis for the following increase of water loading mainly observed in experiments. A single adsorption energy picture was expanded to take into account the water vapour environment through the Gibbs free energy. The statistical ensemble was employed to classify and interpret the averaged values of the adsorption configurations set rather than the ``invisible'' in experiment quantities intrinsic to the particular single adsorption configuration. In order to make the statistical analysis feasible an effective distance matrix scheme was developed. It helped to reduce the total number of structures to consider without loss of generality by virtue of the surface space symmetry. Based on the statistical contribution of each individual adsorption configuration, the O-1s XPS was simulated for the various water vapour environments. A good agreement between the simulated and experimental spectra was found. Wherever it was important, the similarities and differences between water adsorption on the Fe2O3, Al2O3 and Fe3O4 surfaces were stressed and the main tendencies were deduced. Based on the present study, the whole picture of the initial stage of the Fe2O3(0001) surface wetting process was established.