Chemical Processes on Solid Surfaces
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From Real World Catalysis to Surface Science and Back
FROM REAL WORLD CATALYSIS TO SURFACESCIENCE AND BACK: CAN NANOSCIENCEHELP TO BRIDGEmE GAP? H.-J. FREUND,G~ RUPPRECHTER,M. BAUMER, TH. RISSE, N. ERNST, J. LInUDA Fritz-Haber-Institutder Max-P/anck-Gesel/schaft Faradayweg4-6, D-14195 Ber/in, Germany Abstract We review the possibilities in using model s~tems to explore~eterogeneous catalytic reactions under ultrahigh-vacuumand in-situ conditions. We discuss metal nano particles deposited on thin oxide films allowing to study hydrogenation and dehydrogenationreactions, while applyinga variety of surfacesensitive techniques. A secondclass of systems,where homogeneouscatalysts were heterogenized,has been studiedunder in-situ conditionsusing ESR spectroscopy. Introduction One prominentexample where heterogeneous catalysis affects our daily life is pollution control via exhaustcatalysis in everybody'scar. Figure 1 shows a schematicdiagram with a typical exhaustcatalyst in its housing[1]. The catalystconsists of a monolithic backbonecovered internally with a wash coat made of mainly alumina but also ceria and zirconia, which itself is mesoporousand holds the small metal particles, often platinum or rhodium. An electronmicroscope allows us to take a close look at the morphology of the catalyst at the nanometerscale. In order to be active, the metal particles have to be of a few nanometerin diameterand also the support has to be treated in the right way. To a certainextent the preparationis an art, some call it even "black magic". A full understandingof the microscopic processesoccurring at the surface of the particles or at the interface betweenparticle and support, however, is unfortunatelylacking. We have to realize that catalysis in connectionwith pollution control -the specific example chosenhere -does only utilize a small fraction of the world market for solid catalysts. -
Surface Crystallography
Modern Methods in Heterogeneous Catalysis Research Surface crystallography Dirk Rosenthal Department of Inorganic Chemistry Fritz-Haber-Institut der MPG Faradayweg 4-6, DE 14195 Berlin Part of the lecture is taken from Wolfgang Rankes LEED-Script Literature: G. Ertl, J. Küppers, Low Energy Electrons and Surface Chemistry, VCH, Weinheim (1985). M. Henzler, W. Göpel, Oberflächenphysik des Festkörpers, Teubner, Stuttgart (1991). M.A. Van Hove, W.H. Weinberg, C.-M. Chan, Low-Energy Electron Diffraction, Experiment, Theory and Surface Structure Determination, Springer Series in Surface Sciences 6, G. Ertl, R. Gomer eds., Springer, Berlin (1986). M. Horn-von Hoegen, Zeitschrift für Kristallographie 214 (1999) 1-75. FHI-Berlin, 21.11..2008 Dirk Rosenthal, Dept. AC, Fritz Haber Institute der MPG, Faradayweg 4-6, 14195 Berlin, Germany Content 1. Bravais lattices 2. Structure examples: Overlayers 3. Method: LEED, low energy electron diffraction 4. LEED principle in one and two dimensions 5. Reciprocal lattice 6. Ewald sphere construction 7. LEED and symmetry: glide lines 8. Astonishing example 9. LEED and defects 10. Comparison with other methods 11. LEED I-V measurement 12. Reality – an example from heterogeneous catalysis Bravais lattices or International Tables for X-Ray Crystallography, N. F. M. Henry and K. Lonsdale, Eds. (The Kynoch Press, Birmingham, 1969) ,chap. 1. Bravais lattices Structure examples: Overlayers Overlayer structures Ertl/Küppers fig. 9.2, p.204 p(2x2) c(2x2) (√3x√3)R30° on square lattice on hex. lattice Superstructure nomenclature Wood: Simplest in most cases Matrix notation (Park and Madden) p or c(n×m)Rϑ° more general unit cell vector lengths m11 m12 b1 = m11 a1 + m12 a2 b1 = n a1 b2 = m a2 m21 m22 b2 = m21 a1 + m22 a2 rotation ϑ p=primitive, c=centered Wood (2×2) [ϑ=0 is omitted] (√3×√3)R30° Matrix 2 0 1 1 0 2 2 -1 Three possible arrangements yielding c(2x2) structures. -
The Kinetics of Elementary Thermal Reactions in Heterogene- Ous Catalysis
1 The kinetics of elementary thermal reactions in heterogene- 2 ous catalysis 3 G. Barratt Park1,2, Theofanis Kitsopoulos2,5,6, Dmitriy Borodin1, Kai Golibrzuch2, Jannis 4 Neugebohren1, Daniel J. Auerbach2, Charles T. Campbell4 & Alec M. Wodtke1,2,3* 5 1Institute for Physical Chemistry, Georg-August University of Goettingen, Tammannstraße 6, 6 37077 Göttingen, Germany. 7 2Department of Dynamics at Surfaces, Max Planck Institute for Biophysical Chemistry, Am 8 Faßberg 11, 37077 Göttingen, Germany. 9 3International Center for Advanced Studies of Energy Conversion, Georg-August University 10 of Goettingen, Tammannstraße 6, 37077 Göttingen, Germany. 11 4 Department of Chemistry, University of Washington, Seattle, WA 98195-1700, USA 12 5 Department of Chemistry, University of Crete, Heraklion, Greece 13 6 Institute of Electronic Structure and Laser – FORTH, Heraklion, Greece 14 15 *email: [email protected] 16 17 KEYWORDS: Ion-imaging, velocity-resolved kinetics, CO oxidation, heterogeneous catalysis, 18 slice ion-imaging, molecular beams, surface chemistry. 19 20 1 21 Abstract 22 The kinetics of elementary reactions is fundamental to our understanding of catalysis. Just as 23 micro-kinetic models of atmospheric chemistry provided the predictive power that led to the 24 Montreal protocol reversing loss of stratospheric ozone, pursuing a micro-kinetic approach to 25 heterogeneous catalysis has tremendous potential for societal impact. However, developing this 26 approach for catalysis faces great challenges. Methods for measuring rate constants are quite 27 limited and present predictive theoretical methods remain largely un-validated. This paper pre- 28 sents a short perspective on recent experimental advances in our ability to measure the rates of 29 elementary reactions at surfaces that rely on a stroboscopic pump-probe concept for neutral 30 matter. -
Nanostructure of Biogenic Versus Abiogenic Calcium Carbonate Crystals
Nanostructure of biogenic versus abiogenic calcium carbonate crystals JAROSŁAW STOLARSKI and MACIEJ MAZUR Stolarski, J. and Mazur, M. 2005. Nanostructure of biogenic versus abiogenic calcium carbonate crystals. Acta Palae− ontologica Polonica 50 (4): 847–865. The mineral phase of the aragonite skeletal fibers of extant scleractinians (Favia, Goniastrea) examined with Atomic Force Microscope (AFM) consists entirely of grains ca. 50–100 nm in diameter separated from each other by spaces of a few nanometers. A similar pattern of nanograin arrangement was observed in basal calcite skeleton of extant calcareous sponges (Petrobiona) and aragonitic extant stylasterid coralla (Adelopora). Aragonite fibers of the fossil scleractinians: Neogene Paracyathus (Korytnica, Poland), Cretaceous Rennensismilia (Gosau, Austria), Trochocyathus (Black Hills, South Dakota, USA), Jurassic Isastraea (Ostromice, Poland), and unidentified Triassic tropiastraeid (Alpe di Specie, It− aly) are also nanogranular, though boundaries between individual grains occasionally are not well resolved. On the other hand, in diagenetically altered coralla (fibrous skeleton beside aragonite bears distinct calcite signals) of the Triassic cor− als from Alakir Cay, Turkey (Pachysolenia), a typical nanogranular pattern is not recognizable. Also aragonite crystals produced synthetically in sterile environment did not exhibit a nanogranular pattern. Unexpectedly, nanograins were rec− ognized in some crystals of sparry calcite regarded as abiotically precipitated. Our findings support the idea that nanogranular organization of calcium carbonate fibers is not, per se, evidence of their biogenic versus abiogenic origin or their aragonitic versus calcitic composition but rather, a feature of CaCO3 formed in an aqueous solution in the presence of organic molecules that control nanograin formation. Consistent orientation of crystalographic axes of polycrystalline skeletal fibers in extant or fossil coralla, suggests that nanograins are monocrystalline and crystallographically ordered (at least after deposition). -
Integration of Surface Science, Nanoscience, and Catalysis*
Pure Appl. Chem., Vol. 83, No. 1, pp. 243–252, 2011. doi:10.1351/PAC-CON-10-11-04 © 2010 IUPAC, Publication date (Web): 6 December 2010 Integration of surface science, nanoscience, and catalysis* Cun Wen, Yi Liu, and Franklin (Feng) Tao‡ Department of Chemistry and Biochemistry, University of Notre Dame, Notre Dame, IN 46556, USA Abstract: This article briefly reviews the development of surface science and its close rele- vance to nanoscience and heterogeneous catalysis. The focus of this article is to highlight the importance of nanoscale surface science for understanding heterogeneous catalysis perform- ing at solid–gas and solid–liquid interfaces. Surface science has built a foundation for the understanding of catalysis based on the studies of well-defined single-crystal catalysts in the past several decades. Studies of catalysis on well-defined nanoparticles (NPs) significantly promoted the understanding of catalytic mechanisms to an unprecedented level in the last decade. To understand reactions performed on catalytic active sites at nano or atomic scales and thus reach the goal of catalysis by design, studies of the surface of nanocatalysts are cru- cial. The challenges in such studies are discussed. Keywords: heterogeneous catalysis; interfaces; nanoparticles; nanoscience; surface science. INTRODUCTION Heterogeneous catalysis is in fact the foundation of industrial production [1–3]. More than one-third of the production processes in all industries involve heterogeneous catalysis in their production chains [4,5]. Particularly, it has been the core technology of the chemical industry, oil refineries, conversion of sustainable energy sources, and environmental remediation for several decades. The application of heterogeneous catalysis to industrial production was realized without under- standing of catalytic mechanisms at the microscopic level several decades ago. -
The Contribution of Surface Analysis and Surface Science to Technology*
Aust. J. Phys., 1982,35,769-75 The Contribution of Surface Analysis and Surface Science to Technology* C. J. Powell Surface Science Division, National Bureau of Standards, Washington, DC 20234, U.S.A. Abstract Surface science is a rapidly growing field offering many scientific and technological challenges. New experimental and theoretical tools have been developed which can be used to probe, at a fundamental atomic and molecular level, the physics and chemistry of complex processes at solid surfaces. Surface characterization, particularly surface analysis, is now an integral part of many technologies and industries (e.g., catalysis, coatings, corrosion, semiconductor devices, computer, automobile and communications) for many different applications (e.g., failure analysis, quality control, process and device development). Characterization of surface properties and processes is similarly important in many areas of public concern (e.g., energy and environment). The concepts apd techniques found useful for surface characterization are currently being extended to the character ization of solid-solid, solid-liquid and solid-gas interfaces. It is therefore expected that there will be significant developments in interface science and additional opportunities for technological applications in the coming decade. 1. Introduction Over the past two decades there has been considerable growth in surface science and in the application of surface-characterization methods, particularly surface analysis, to a wide range of problems of technological interest (Powell 1978). This growth is evident in the large number of local, national and international meetings sponsored by major professional societies and many other groups; the growth is also evident in journal and book publications. The purpose of this paper is to summarize key features of recent developments and to point out the impact of surface science and surface analysis in technological developments and problems. -
Decline of Giant Impacts on Mars by 4.48 Billion Years Ago and an Early Opportunity for Habitability
ARTICLES https://doi.org/10.1038/s41561-019-0380-0 Decline of giant impacts on Mars by 4.48 billion years ago and an early opportunity for habitability D. E. Moser 1*, G. A. Arcuri1, D. A. Reinhard2, L. F. White 3, J. R. Darling 4, I. R. Barker1, D. J. Larson2, A. J. Irving5, F. M. McCubbin6, K. T. Tait3, J. Roszjar7, A. Wittmann8 and C. Davis1 The timing of the wane in heavy meteorite bombardment of the inner planets is debated. Its timing determines the onset of crustal conditions consistently below the thermal and shock pressure limits for microbiota survival, and so bounds the occur- rence of conditions that allow planets to be habitable. Here we determine this timing for Mars by examining the metamor- phic histories of the oldest known Martian minerals, 4.476–4.429-Gyr-old zircon and baddeleyite grains in meteorites derived from the southern highlands. We use electron microscopy and atom probe tomography to show that none of these grains were exposed to the life-limiting shock pressure of 78 GPa. 97% of the grains exhibit weak-to-no shock metamorphic features and no thermal overprints from shock-induced melting. By contrast, about 80% of the studied grains from bombarded crust on Earth and the Moon show such features. The giant impact proposed to have created Mars’ hemispheric dichotomy must, therefore, have taken place more than 4.48 Gyr ago, with no later cataclysmic bombardments. Considering thermal habitability models, we conclude that portions of Mars’ crust reached habitable pressures and temperatures by 4.2 Gyr ago, the onset of the Martian ‘wet’ period, about 0.5 Gyr earlier than the earliest known record of life on Earth. -
I IMPROVING PALLADIUM CATALYSIS with SELF
IMPROVING PALLADIUM CATALYSIS WITH SELF-ASSEMBLED MONOLAYERS by STEPHEN T. MARSHALL B.S., Carnegie Mellon University, 2005 A thesis submitted to the Faculty of the Graduate School of the University of Colorado in partial fulfillment of the requirement for the degree of Doctor of Philosophy Department of Chemical and Biological Engineering 2010 i This thesis entitled: Improving Palladium Catalysis with Self-Assembled Monolayers written by Stephen T. Marshall has been approved for the Department of Chemical and Biological Engineering J. William Medlin John L. Falconer Date The final copy of this thesis has been examined by the signatories, and we Find that both the content and the form meet acceptable presentation standards Of scholarly work in the above mentioned discipline. ii ABSTRACT Marshall, Stephen T. (Ph.D., Chemical and Biological Engineering) Improving Palladium Catalysis with Self-Assembled Monolayers Thesis directed by Associate Professor J. William Medlin Improving selectivity in catalytic systems is of primary interest to a number of fields. One means of achieving selectivity is through the use of promoters, or deposited materials that improve catalytic properties. Here, we present the modification of palladium surfaces with self- assembled monolayers (SAMs) formed from thiols. SAM coatings are employed in two systems: metal-insulator-semiconductor (MIS) sensors and supported palladium catalysts. On MIS sensors, modification with alkanethiol SAMs results in enhanced sensitivity to acetylene. Excellent selectivity for acetylene over ethylene is also observed. The functionalized sensors would serve as excellent acetylene detectors in a variety of applications including the detection of fault gases in transformers and detecting trace acetylene in ethylene production plants. -
Biological Surface Science
Surface Science 500 (2002) 656–677 www.elsevier.com/locate/susc Biological surface science Bengt Kasemo * Department of Applied Physics, Chalmers University of Technology and Go€teborg University, S-41296 G o€teborg, Sweden Received 13 December 2000; accepted for publication 5 July 2001 Abstract Biological surface science (BioSS), as defined here is the broad interdisciplinary area where properties and processes at interfaces between synthetic materials and biological environments are investigated and biofunctional surfaces are fabricated. Six examples are used to introduce and discuss the subject: Medical implants in the human body, biosensors and biochips for diagnostics, tissue engineering, bioelectronics, artificial photosynthesis, and biomimetic materials. They are areas of varying maturity, together constituting a strong driving force for the current rapid development of BioSS. The second driving force is the purely scientific challenges and opportunities to explore the mutual interaction between biological components and surfaces. Model systems range from the unique water structures at solid surfaces and water shells around proteins and biomembranes, via amino and nucleic acids, proteins, DNA, phospholipid membranes, to cells and living tissue at surfaces. At one end of the spectrum the scientific challenge is to map out the structures, bonding, dynamics and ki- netics of biomolecules at surfaces in a similar way as has been done for simple molecules during the past three decades in surface science. At the other end of the complexity spectrum one addresses how biofunctional surfaces participate in and can be designed to constructively participate in the total communication system of cells and tissue. Biofunctional surfaces call for advanced design and preparation in order to match the sophisticated (bio) recognition ability of biological systems. -
Introduction to Surface Chemistry and Catalysis
INTRODUCTION TO SURFACE CHEMISTRY AND CATALYSIS GABOR A. SOMORJAI Department of Chemistry University of California Berkeley, California A Wiley-Interscience Publication JOHN WILEY & SONS, INC. New York • Chichester • Brisbane • Toronto • Singapore CONTENTS Preface xiii General Introduction xv Lists of Constants xvii List of Symbols xix 1 Surfaces—An Introduction 1 1.1 Historical Perspective, 1 1.2 Surfaces and Interfaces—Classification of Properties, 3 1.3 External Surfaces, 5 1.3.1 Surface Concentration, 5 1.3.1.1 Clusters and Small Particles, 6 1.3.1.2 Thin Films, 8 1.3.2 Internal Surfaces—Microporous Solids, 10 1.4 Clean Surfaces, 12 1.5 Interfaces, 13 1.5.1 Adsorption, 13 1.5.2 Thickness of Surface Layers, 15 1.6 The Techniques of Surface Science, 15 1.7 Summary and Concepts, 17 1.8 Problems, 17 References, 18 2 The Structure of Surfaces 36 2.1 Introduction, 36 2.2 Surface Diffraction, 42 2.3 Notation of Surface Structures, 43 2.3.1 Abbreviated Notation of Simple Surface Structures, 45 2.3.2 Notation of High-Miller-Index, Stepped Surfaces, 47 VII viii CONTENTS 2.4 The Structure of Clean Surfaces, 48 2.4.1 Bond-Length Contraction or Relaxation, 48 2.5 Reconstruction, 50 2.5.1 Atomic Steps and Kinks, 52 2.6 The Structure of Adsorbed Monolayers, 54 2.6.1 Ordered Monolayers and the Reasons for Ordering, 54 2.6.2 Adsorbate-Induced Restructuring, 55 2.6.3 Atomic Adsorption and Penetration into Substrates, 58 2.6.4 Metals on Metals: Epitaxial Growth, 60 2.6.5 Growth Modes at Metal Surfaces, 60 2.6.6 Molecular Adsorption, 60 2.6.6.1 Ethylene, -
N76-21508 Introduction
PHOTOCATALYTIC GENERATION OF HYDROGEN FROM WATER W.R. Bottoms and R.B. Miles Princeton University N76-21508 INTRODUCTION The dissociation of simple molecules provides a potentially efficient method of storing energy in a transportable form. Among the numerous chemical systems that have been proposed for energy conversion are the following: hv 2NOC1 ™ C\2 + 2NO hi> 2H20 ^ 2H2 + 02 2CO2 ^ 2CO + O2 Hydrogen offers the advantages of being a clean burning fuel, easily stored in gas, liquid, or hydride form, and efficiently transferable. It may be used as a fuel for a variety of energy conversion processes including fuel cells and rocket engines as well as conventional heat engines. In conjunction with a water dissociation process, it holds forth the promise of providing a closed cycle, photon powered, energy system where photon energy may be efficiently stored for future use and converted to thermal or electrical energy on demand. In this paper we will discuss a new concept which is designed to overcome the problems encountered when using photodissociation for the generation of hydrogen. Two fundamental problems limiting the efficiency of photodissociation of water are the separation of the photolysis products and the high energy photons necessary for the reaction. Although there has not been a great deal of work with metal-water systems, it has been shown that the dissociation energy of a large number of molecules is catalytically reduced when these molecules are in intimate contact with a surface of certain metals (ref. 1). The spontaneous dissociation of water has been demonstrated for Cu (ref. 2), Fe (ref. -
Urea-Assisted Synthesis and Characterization of Saponite with Different Octahedral (Mg, Zn, Ni, Co) and Tetrahedral Metals (Al, Ga, B), a Review
life Review Urea-Assisted Synthesis and Characterization of Saponite with Different Octahedral (Mg, Zn, Ni, Co) and Tetrahedral Metals (Al, Ga, B), a Review Concepcion P. Ponce 1 and J. Theo Kloprogge 1,2,* 1 Department of Chemistry, College of Arts and Sciences, University of the Philippines, Miag-ao, Iloilo 5023, Philippines; [email protected] 2 School of Earth and Environmental Sciences, The University of Queensland, Brisbane, Queensland 4072, Australia * Correspondence: [email protected] Received: 10 August 2020; Accepted: 26 August 2020; Published: 28 August 2020 Abstract: Clay minerals surfaces potentially play a role in prebiotic synthesis through adsorption of organic monomers that give rise to highly concentrated systems; facilitate condensation and polymerization reactions, protection of early biomolecules from hydrolysis and photolysis, and surface-templating for specific adsorption and synthesis of organic molecules. This review presents processes of clay formation using saponite as a model clay mineral, since it has been shown to catalyze organic reactions, is easy to synthesize in large and pure form, and has tunable properties. In particular, a method involving urea is presented as a reasonable analog of natural processes. The method involves a two-step process: (1) formation of the precursor aluminosilicate gel and (2) hydrolysis of a divalent metal (Mg, Ni, Co, and Zn) by the slow release of ammonia from urea decomposition. The aluminosilicate gels in the first step forms a 4-fold-coordinated Al3+ similar to what is found in nature such as in volcanic glass. The use of urea, a compound figuring in many prebiotic model reactions, circumvents the formation of undesirable brucite, Mg(OH)2, in the final product, by slowly releasing ammonia thereby controlling the hydrolysis of magnesium.