Vibrational Spectroscopies for Adsorbed Species Alexis T. Bell, EDITOR University of California, Berkeley Michael L. Hair, EDITOR Xerox Research Center of Canada Based on a symposium sponsored by the Division of Colloid and Surface Chemistry at the 178th Meeting of the American Chemical Society, Washington, D.C., September 12-13, 1979. 137 ACS SYMPOSIUM SERIES AMERICAN CHEMICAL SOCIETY WASHINGTON, D. C. 1980 In Vibrational Spectroscopies for Adsorbed Species; Bell, A., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1980. Library of Congress CIP Data Vibrational spectroscopies for adsorbed species. (ACS symposium series; 137 ISSN 0097-6156) Includes bibliographies and index. 1. Vibrational spectra—Congresses. 2. Infrared spectrometry—Congresses. 3. Surface chemistry—Con gresses. I. Bell, Alexis T., 1942- . II. Hair, Michael L., 1934- . III. American Chemical Society. Division of Colloid and Surface Chemistry. IV. Title: Adsorbed species. V. Series: American Chemical Society. ACS symposium series; 137. QC454.V5V534 541.3'453 80-21181 ISBN 0-8412-0585-X ACSMC8 137 1-295 1980 Copyright © 1980 American Chemical Society All Rights Reserved. The appearance of the code at the bottom of the first page of each article in this volume indicates the copyright owner's consent that reprographic copies of the article may be made for personal or internal use or for the personal or internal use of specific clients. This consent is given on the condition, however, that the copier pay the stated per copy fee through the Copyright Clearance Center, Inc. for copying beyond that permitted by Sections 107 or 108 of the U.S. Copyright Law. This consent does not extend to copying or transmission by any means—graphic or electronic—for any other purpose, such as for general distribution, for advertising or promotional purposes, for creating new collective works, for resale, or for information storage and retrieval systems. 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Dollberg Leon Petrakis Robert E. Feeney F. Sherwood Rowland Jack Halpern Alan G Sartorelli Brian M. Harney Raymond B. Seymour Robert A. Hofstader Gunter Zweig In Vibrational Spectroscopies for Adsorbed Species; Bell, A., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1980. FOREWORD The ACS SYMPOSIUM SERIES was founded in 1974 to provide a medium for publishin format of the Serie parallel g IN CHEMISTRY SERIES except that in order to save time the papers are not typeset but are reproduced as they are sub mitted by the authors in camera-ready form. Papers are re viewed under the supervision of the Editors with the assistance of the Series Advisory Board and are selected to maintain the integrity of the symposia; however, verbatim reproductions of previously published papers are not accepted. Both reviews and reports of research are acceptable since symposia may embrace both types of presentation. In Vibrational Spectroscopies for Adsorbed Species; Bell, A., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1980. PREFACE The identification of species adsorbed on surfaces has preoccupied chem ists and physicists for many years. Of all the techniques used to deter mine the structure of molecules, interpretation of the vibrational spectrum probably occupies first place. This is also true for adsorbed molecules, and identification of the vibrational modes of chemisorbed and physisorbed species has contributed greatly to our understanding of both the underlying surface and the adsorbed molecules. The most common method for deter mining the vibrational modes of a molecule is by direct observation of adsorptions in the infrared region of the spectrum. Surface spectroscopy is no exception and by fa ture refer to the infrared time, the main approach has been the use of conventional transmission IR and work in this area up to 1967 has been summarized in three books. The first chapter in this volume, by Hair, presents a necessarily brief over view of this work with emphasis upon some of the developments that have occurred since 1967. One of the major advances in the past decade has been the maturation of the electronic revolution. This has had its effect on surface spectroscopy, with regard to instrumentation for transmission IR, but particularly for sensitivity gains that have made reflectance techniques the preferred alterna tive for fundamental studies. In the transmission mode, the commercial development of the Fourier transform IR spectrometer has led to signifi cant advantages in the determination of the vibrational spectra of adsorbed species. This is covered in the chapter by Bell. In the transmission mode, IR spectroscopy is limited by sensitivity requirements to the study of surfaces exhibiting relatively high surface area, i.e., porous oxides and supported metals. A major advance in the past decade has been achieved by using reflection techniques. Modulation of the incident beam or ellipsometry usually are employed and optimization of these techniques now enables the IR spectra of highly absorbing mole cules to be obtained on single crystal surfaces. As a result, it has become possible to compare vibrational data with data obtained from other surface diagnostic techniques (i.e., LEED and AES). Chapters describing the determination of these reflection absorption spectra are given by Allara, Pritchard, and Dignam. Surface wave spectroscopy provides yet another means for obtaining absorption spectra of species present on a single crystal surface. In this case, IR radiation is coupled to the sample in such a way that it propagates vii In Vibrational Spectroscopies for Adsorbed Species; Bell, A., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1980. laterally along the surface for a finite distance before it is decoupled and detected. Use of this technique permits a larger absorption to be achieved than normally is obtained by means of reflection techniques. The theory and practice of surface wave spectroscopy are discussed by Bell. Raman spectroscopy is a complementary technique that yields the same vibrational information as is obtained in conventional IR absorption spectroscopy. Here, however, the exciting radiation is in the visible region of the spectrum. Application of this technique to surfaces has been difficult because of practical problems associated with fluorescence. This problem now has been essentially resolved, and recent progress in the application of Raman spectroscopy to surfaces is reviewed by Morrow. Conventionally, in IR spectroscopy the measured absorptions are caused by the fundamental vibrations of the atoms within a molecule. In many cases, important information can be obtained by examining the overtones of these fundamental vibrations. This can be done in the trans mission mode, but elegan discussed by Klier. The final chapters of this book review the progress of three recently developed techniques that provide information about the vibrational states of adsorbed molecules. Perhaps the most important of these techniques is electron energy loss spectroscopy that, despite its inherent low resolution, gives valuable information on vibrational modes that are either inactive in the IR, or inaccessible because of experimental difficulties. The applica tions of this technique are discussed in two chapters by Somorjai and Weinberg. The review of new experimental techniques concludes with presentations on inelastic electron tunneling spectroscopy and neutron scattering by Kirtley and Taub. In assembling this collection of review/progress articles, the editors have tried to provide an update of all techniques used to determine the vibrational structure of molecules adsorbed on surfaces. The symposium itself provided a forum whereby the leading workers in the field could interact and rationalize their various approaches. No single technique will ever give all the information required to describe an adsorbed molecule and the recent developments relating the vibrational spectroscopies and the UHV techniques are, thus, particularly exciting. Further overlap between these techniques will undoubtedly occur and inevitably lead to a deeper understanding of the molcular structure of adsorbed species. Department of Chemical Engineering ALEXIS T. BELL Berkeley, California Xerox Research Center of Canada MICHAEL L. HAIR Mississauga, Ontario, Canada May 19, 1980 viii In Vibrational Spectroscopies for Adsorbed Species; Bell, A., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1980. 1 Transmission Infrared Spectroscopy for High Surface Area Oxides MICHAEL L. HAIR Xerox Research Centre of Canada, 2480 Dunwin Drive, Mississauga, Ontario, L5L 1J9, Canada Interest in the vibrational spectra of adsorbed molecules is at least 40 years old. The past ten years have seen the development of many novel techniques for determining the vibrationa brings together a state-of-the-ar ethusiasm for the recent advances made in any subject there is a tendency to forget the parent technique and its steady contribution to our knowledge. In this case, the parent is simple transmission infrared spectroscopy. This paper, therefore, is an attempt to briefly present an overview of some of the developments which have occurred in the application of transmission infrared spectroscopy to surface studies with emphasis upon results generated in the past 10 years. For more detailed information on work published prior to 1967 the reader is referred to three texts which have appeared on this subject (1-3). Because of the maturity of the method the advances in technique are incremental rather than revolutionary. Perhaps the major new developments have been in the instrumental area where the ready availability of the Fourier Transform instruments has led to its introduction to surface studies. The ease of obtaining spectra and the advantages associated with the direct computation of data will be discussed in a separate paper (4). Transmission IR still remains the best method for examining insulating oxide surfaces and over the past decade there has developed a considerable understanding of many surfaces, particularly those of silica, alumina, molecular sieves and complex catalysts. The objective of this paper, therefore, will be to demonstrate how some of the recent advances have been made. Clearly it is not possible to discuss all the materials studied by transmission IR and the author has chosen to use the surface properties of silica to illustrate the type of understanding that is now available. Some History The first application of transmission infrared spectroscopy to the study of adsorbed species appears to be the work of Buswelf et al in 1938 (5). Those authors pressed a montmorillonite clay into a disc which was then "dried" at various temperatures. The spectra they obtained bear a remarkable similarity to many others that have been produced in the literature over the next forty years: the authors were clearly able to resolve bands due to hydroxyl groups associated with the clay lattice and to adsorbed water which was slowly removed as a function of drying. 0-8412-0585-X/80/47-137-001$05.00/0 © 1980 American Chemical Society In Vibrational Spectroscopies for Adsorbed Species; Bell, A., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1980. 2 VIBRATIONAL SPECTROSCOPIES Almost twenty years elapsed before the next advances. In the 1950's the Russian School (Terenin, Yaroslavski, Kiselev) (6) studied the structure of porous glass and made the first assignments for hydroxyl groups on such surfaces; the Cambridge School (Shephard, Little, Yates) (7) investigated the process of physical adsorbtion and the rotational motion of physcially adsorbed molecules; and the American workers (Eischens, Francis, Pliskin) (8) applied the technique to supported metal catalysts and initiated the application of this technique to the study of catalysts. The work of Eischens and co-workers on CO/Ni is remarkable in that the spectra obtained (and the interpretation) have stood the test of time and are confirmed most elegantly by some of the studies on single crystal surfaces which will be presented in later chapters. Experimental In the application of transmission infrared spectroscopy to the study of surfaces it is important that high surface area materials be used in order that the resultant spectrum contains a considerable contribution from the surface as distinct from the bulk of th pressed into thin self-supportin the infrared radiation in the spectrometer. Developments in this area in the past decade have been aimed mainly at quantifying the infrared data and two basic types of vacuum cell have emerged: those in which the sample is moved in and out of the beam into a furnace above the spectrometer, and those in which the furnace is built around a static sample holder which is permantly held in the beam. The latter is clearly a more desirable system but suffers from the experimental disadvantages that the furnace must be constructed within the confines of the infrared spectrometer, thus giving rise to problems associated with the cooling of the infrared transmitting windows. An excellent cell capable of temperatures up to 600°C under UHV conditions has been described (9). Silica A classical paper on the adsorption of water on silica surfaces appeared from* the General Electric Laboratories in 1958 (10). One set of spectra from this paper are redrawn in Fig. 1. The results clearly demonstrate the difference between the two forms of high surface area silica commonly found in the laboratory: the silica which is precipitated from solution and is widely used as a dessicant and the finely divided silica (Cabosil, Aerosil, etc.) which is prepared by flame oxidation of SiCI at elevated temperatures. Experimentally, 4 MacDonald made pressed discs of each of the forms of silica, placed them in a simple IR cell in the beam of a spectrometer as described earlier and recorded the spectra. The solid black lines (a) are the spectra recorded at room temperature and the difference between the two silicas is readily apparent. The Cabosil spectrum shows distinct structure with bands being readily observed at 3747, 3660 and 3520 cm*1. In the case of the precipitated silica there is complete absorption between 3750 and 3000 cm"1. On evacuating the samples at room temperature changes are seen in the spectra which can be related to the removal of physically adsorbed water from the surface. This is done by comparing (a) and (b). A broad band (d) centered around 3400 cm"1 has been removed by the evacuation and this is coincident with the removal (not shown) of a band at 1625 cm*1. These are clearly due to the stretching and bending In Vibrational Spectroscopies for Adsorbed Species; Bell, A., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1980. HAIR Transmission IR Spectroscopy CABOSIL BULKY SILICA 0.0 I I I I I I I tfTTT" I I I I III I 0.1 0.2 0.3 0.4 0.5 10 1.5 0.0 0.1 0.2 7--} (X3 degassed 1/2 hr at 500°C 0.4 0.5 1.0 1.5 8 8 8 8 8 3 s 8 S § (cm-1) Journal of Physical Chemistry Figure 1. The IR spectra of Cab-O-Sil and bulky silica: (a) before degassing; (b) after degassing for 3 h at 30°C in vacuo; (c) difference between (a) and (b); (d) de gassed 30 min at 500°C in vacuo; (e) degassed 8.5 h at 940° C in vacuo (10) 3747 cm-1 H V 150°C. + H0 2 _\ Sis— O—H''' NH / 3660 cm-1 3500 cm-1 1630 cm-1 11 <400°C REVERSIBLE 800°C IRREVERSIBLE ~7S,S\ ^H20 Ο +H20 Figure 2. Schematic of hydration-dehydration on a silica surface In Vibrational Spectroscopies for Adsorbed Species; Bell, A., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1980. 4 VIBRATIONAL SPECTROSCOPIES motions of molecular water. On heating the sample to higher temperatures further changes can be observed. In both samples the band at 3660 cm*1 becomes more distinct as the heating temperature is raised until it eventually is seen as a shoulder on the 3747 cm*1 band. After the sample has been degassed at 940°C in vacuum, both the precipitated silica and the Cabosil exhibit identical spectra which consist of one very narrow, sharp band at 3747 cm*1. One important observation which can be drawn from these spectra is the fact that, at least at low coverages, the removal of molecular water from the surface of the silica does not particularly affect the intensity of the band at 3747 cm"1. Thus, it can be concluded that the water is not specifically interacting with this group during the adsorption at low coverages and is therefore sitting on other parts of the surface. (This view is widely held, but definitive evidence is not available. Interaction certainly occurs at higher partial pressure but this would be expected in a random rather than a specific adsorption process.) The interpretation of th universally accepted althoug and fine structure. Thus, the band at 3747 cm*1 is assigned to a hydroxl group attached to a silicon atom on the surface. The OH group is situtated so that it is vibrating freely and is unperturbed by its neighbours. The band at 3660 cm*1 is attributed to surface hydroxyl groups which are sufficiently close together that they are hydrogen bonded to each other and are thus perturbed from the 3747 cm"1 position. It is usually accepted that the frequency shift is related to the strength of the Η-bonding interaction, the larger shifts corresponding to stronger interaction and it is noted that dehydration proceeds from the lower frequency end. Other absorptions in this region are attributed to molecular water adsorbed on the surface. The dehydration which occurs as the temperature of the sample is raised clearly proceeds by a mechanism in which the Η-bonded SiOH groups are removed from the surface, the more strongly Η-bonded groups being removed initially. Rehydration of the surface is found to be reversible only if the pretreatement temperature is kept below about 400°C. Above that temperature a restructuring of the surface apparently occurs. The removal of the H-bonded groups removes the adsorption site for water thus giving rise to a surface which does not adsorb water very readily at low pressure (Fig. 2). Sample Preparation One of the major experimental problems in studying surfaces by the transmission techniques has always been the sample preparation. Indeed, the quality of the spectra was limited by the quality of the pressed disc and good transmission below 1300 cm"1 was not possible. This precluded observation of the region where many bending modes would be expected and prevented complete assignment of surface structures. After much experience it is now possible to prepare very thin, high quality discs of Cabosil and other oxides (10 mg/cm2) and the resultant increase in available information is illustrated by the work of Morrow and his co-workers on Cabosil (11-14). Thus, Morrow and Cody were able to obtain the spectra shown in Fig. 3 in the region between 800 and 1000 cm*1. The effect of heating the sample is clearly shown and can be In Vibrational Spectroscopies for Adsorbed Species; Bell, A., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1980.
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