The Surface Structure and Growth of Natural Zeolites

Total Page:16

File Type:pdf, Size:1020Kb

The Surface Structure and Growth of Natural Zeolites A thesis submitted for the degree of Doctor of Philosophy The Surface Structure and Growth of Natural Zeolites by Manisha Mistry University College London 2005 Davy Faraday Research Laboratory, The Royal Institution of Great Britain. Centre for Theoretical and Computational Chemistry, Department of Chemistry, University College London 1 UMI Number: U592160 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. Dissertation Publishing UMI U592160 Published by ProQuest LLC 2013. Copyright in the Dissertation held by the Author. Microform Edition © ProQuest LLC. All rights reserved. This work is protected against unauthorized copying under Title 17, United States Code. ProQuest LLC 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106-1346 A b s t r a c t A systematic study has been carried out in order to investigate two aspects o f zeolite chemistry: to determine the external surface structure and to establish the mechanism of crystal growth. The natural zeolite edingtonite (EDI) was chosen as a model material and the surface structures were studied by finding the most stable termination for each face. For each of the four morphologically important faces the surface structure was found to minimise the number of broken bonds created upon cleaving the surface. In the absence of experimental data, the crystal morphologies were used as a proxy indicator of relative growth rate of different faces. Qualitative inspection indicates that only the equilibrium morphology is able to reproduce the habit of the natural crystal. However, quantitative analysis with the crystal habit observed in SEM images reveals a discrepancy in aspect ratios. By predicting the crystal morphology by using a newly proposed, less demanding method of calculating the number of broken bonds upon cleaving the surface per surface area (Nbb/S A ), one is able to accurately reproduce the crystal morphology with the correct aspect ratio. The utility of the NBb/S A method has been tested for a sample of zeolites, results show the Nbb/S A technique has correctly predicted the growth rate and crystal habit of merlinoite, analcime, natrolite, and zeolite A. The test on thomsonite was able to reproduce the correct order o f stability for each face, however the aspect ratios were not precisely predicted. By the use o f atomistic and ab-initio methods, this research has also investigated the growth mechanism of EDI. The total and condensation energies of a range o f possible solution fragments have been calculated and the most stable cluster along with the mechanism of formation has been suggested. The energetics of clusters along with the surface structural analysis has shown strong evidence that characteristic building units control the growth and aggregation o f EDI, which dictates the extended crystalstructure and the rate at which these building units condense onto the surface determines the crystal shape. 2 To Sandip an exceptional person who has inspired me to believe that goals can be achieved by reaching beyond material concepts 3 A cknowledgements I would firstly like to thank my supervisor Ben Slater for his encouragement, enthusiasm and guidance throughout my PhD. I would also like to acknowledge my secondary supervisors: Dewi Lewis for useful conversations, and C. Richard. A. Catlow for the opportunity to work at The Royal Institution o f Great Britain. I am also grateful to Matt Johnson for his help with SEM experiments. Personal thanks to my parents, Ramanbhai and Laxmiben Mistry, for their endless support, and giving me the opportunity to always achieve my goals. I am very grateful to my sister Mala Mistry, for her assistance with exhausting tasks. I would also like to thank my fiance Sandip Vekaria, who has always given me unparalleled strength and encouragement throughout the past four years. Finally I would like to thank my friends Iman Saadoune, Dinah Parker, Ilona Franklin, Naseem Ramsahye, Donna Arnold, Dave Plant, David Coombes, Martin Foster, Dan Wilson and Misbah Sarwar, who have made working at the RI an unforgettable experience; and other close friends Sarah Harper, Lin Yan Liu and Sarah Choudhury. 4 Ta b l e o f C o n t e n t s LIST OF FIGURES.................................................................................................................................................... 9 LIST OF TABLES.................................................................................................................................................... 13 CONVENTION.........................................................................................................................................................16 C h a p t e r O n e INTRODUCTION.................................................................................................................................................... 17 1.0 OBJECTIVES.................................................................................................................................................... 17 1.1 Zeolites................................................................................................................................................... 19 1.1.1 The geochemistry of natural zeolites ............................................................................................19 1.1.2 Classification of zeolites................................................................................................................. 20 1.1.3 Structure and composition..............................................................................................................20 1.2 Applications of zeolites .......................................................................................................................26 1.2.1 Ion exchange in zeolites .................................................................................................................. 26 1.2.2 Bulk catalysis................................................................................................................................... 28 1.2.3 Surface catalytic processes.............................................................................................................30 1.2.3.1 Pore mouth catalysis ............................................................................................................ 31 1.2.3.2 Key-lock catalysis .................................................................................................................32 1.2.3.3 Nest effect.............................................................................................................................. 33 REFERENCES......................................................................................................................................................... 34 C h a p t e r T w o CRYSTAL GROWTH: AN OVERVIEW OF THEORY AND EXPERIMENTAL TECHNIQUES 38 2.0 UNDERSTANDING THE CONCEPTS OF CRYSTAL GROWTH........................................................38 2.1 Crystal nucleation and growth ............................................................................................................ 39 2.1.1 Homogenous nucleation................................................................................................................. 39 2.1.2 Heterogeneous nucleation...............................................................................................................42 2.2 Models of a crystal surface................................................................................................................. 43 2.2.1 Surface point defects........................................................................................................................48 2.3 Atomistic nature of crystal growth .....................................................................................................50 2.4 Spiral growth model ............................................................................................................................. 52 2.5 Experimental surface analytical techniques .......................................................................................55 2.5.1 Scanning tunnel microscope...........................................................................................................55 2.5.2 Atomic force microscope................................................................................................................ 56 2.5.3 Transmission electron microscopy ................................................................................................58 2.5.4 Scanning Electron Microscopy.......................................................................................................59 2.5.5 Energy Dispersive X-ray Analysis ................................................................................................60 REFERENCES......................................................................................................................................................... 60 C h a p t e r T h r e e METHODOLOGY...................................................................................................................................................64 3.0 COMPUTATIONAL TECHNIQUES..........................................................................................................
Recommended publications
  • Observation of Quadrupole Helix Chirality and Its Domain Structure in Dyfe3(BO3)4
    ARTICLES PUBLISHED ONLINE: 6 APRIL 2014 | DOI: 10.1038/NMAT3942 Observation of quadrupole helix chirality and its domain structure in DyFe3(BO3)4 T. Usui1, Y. Tanaka2, H. Nakajima1, M. Taguchi2, A. Chainani2, M. Oura2, S. Shin2, N. Katayama3, H. Sawa3, Y. Wakabayashi1 and T. Kimura1* Resonant X-ray diraction (RXD) uses X-rays in the vicinity of a specific atomic absorption edge and is a powerful technique for studying symmetry breaking by motifs of various multipole moments, such as electric monopoles (charge), magnetic dipoles (spin) and electric quadrupoles (orbital). Using circularly polarized X-rays, this technique has been developed to verify symmetry breaking eects arising from chirality, the asymmetry of an object upon its mirroring. Chirality plays a crucial role in the emergence of functionalities such as optical rotatory power and multiferroicity. Here we apply spatially resolved RXD to reveal the helix chirality of Dy 4f electric quadrupole orientations and its domain structure in DyFe3(BO3)4, which shows a reversible phase transition into an enantiomorphic space-group pair. The present study provides evidence for a helix chiral motif of quadrupole moments developed in crystallographic helix chirality. t is well known that chirality often plays a critical role in various detect not only crystallographic helix handedness but also the disciplines, such as biology, organic chemistry and particle chirality ascribed to the periodic motif of multipole moments, such Iphysics1,2. In contrast, chirality in solid-state physics, which as magnetic dipoles and electric quadrupoles12–14. In the case of is largely concerned with crystals possessing periodic arrays of magnetic dipoles, the handedness of a `helical magnetic structure' atoms, has attracted less attention.
    [Show full text]
  • Washington State Minerals Checklist
    Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite
    [Show full text]
  • Mineral Processing
    Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19
    [Show full text]
  • Key to Rocks & Minerals Collections
    STATE OF MICHIGAN MINERALS DEPARTMENT OF NATURAL RESOURCES GEOLOGICAL SURVEY DIVISION A mineral is a rock substance occurring in nature that has a definite chemical composition, crystal form, and KEY TO ROCKS & MINERALS COLLECTIONS other distinct physical properties. A few of the minerals, such as gold and silver, occur as "free" elements, but by most minerals are chemical combinations of two or Harry O. Sorensen several elements just as plants and animals are Reprinted 1968 chemical combinations. Nearly all of the 90 or more Lansing, Michigan known elements are found in the earth's crust, but only 8 are present in proportions greater than one percent. In order of abundance the 8 most important elements Contents are: INTRODUCTION............................................................... 1 Percent composition Element Symbol MINERALS........................................................................ 1 of the earth’s crust ROCKS ............................................................................. 1 Oxygen O 46.46 IGNEOUS ROCKS ........................................................ 2 Silicon Si 27.61 SEDIMENTARY ROCKS............................................... 2 Aluminum Al 8.07 METAMORPHIC ROCKS.............................................. 2 Iron Fe 5.06 IDENTIFICATION ............................................................. 2 Calcium Ca 3.64 COLOR AND STREAK.................................................. 2 Sodium Na 2.75 LUSTER......................................................................... 2 Potassium
    [Show full text]
  • Mineralogy and Geochemistry of Ocelli in the Damtjernite Dykes and Sills, Chadobets Uplift, Siberian Craton: Evidence of the Fluid–Lamprophyric Magma Interaction
    minerals Article Mineralogy and Geochemistry of Ocelli in the Damtjernite Dykes and Sills, Chadobets Uplift, Siberian Craton: Evidence of the Fluid–Lamprophyric Magma Interaction Anna A. Nosova 1,*, Ludmila V. Sazonova 1,2, Alexey V. Kargin 1 , Elena O. Dubinina 1 and Elena A. Minervina 1 1 Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry, Russian Academy of Sciences (IGEM RAS), 119017 Moscow, Russia; [email protected] (L.V.S.); [email protected] (A.V.K.); [email protected] (E.O.D.); [email protected] (E.A.M.) 2 Geology Department, Lomonosov Moscow State University, 119991 Moscow, Russia * Correspondence: [email protected]; Tel.:+7-499-230-8414 Abstract: The study reports petrography, mineralogy and carbonate geochemistry and stable iso- topy of various types of ocelli (silicate-carbonate globules) observed in the lamprophyres from the Chadobets Uplift, southwestern Siberian craton. The Chadobets lamprophyres are related to the REE-bearing Chuktukon carbonatites. On the basis of their morphology, mineralogy and relation with the surrounding groundmass, we distinguish three types of ocelli: carbonate-silicate, containing carbonate, scapolite, sodalite, potassium feldspar, albite, apatite and minor quartz ocelli (K-Na-CSO); carbonate–silicate ocelli, containing natrolite and sodalite (Na-CSO); and silicate-carbonate, con- taining potassium feldspar and phlogopite (K-SCO). The K-Na-CSO present in the most evolved Citation: Nosova, A.A.; Sazonova, damtjernite with irregular and polygonal patches was distributed within the groundmass; the patches L.V.; Kargin, A.V.; Dubinina, E.O.; consist of minerals identical to minerals in ocelli. Carbonate in the K-Na-CSO are calcite, Fe-dolomite Minervina, E.A.
    [Show full text]
  • Studies of the Zeolites Composition of Zeolites of the Natrolite Group and Compositional Relations Among Thomsonites Gonnardites, and Natrolites
    r-'1 ~ Q I ~ c lt') ~ r-'1 'JJ ~ Q.) < ~ ~ ......-~ ..,.;;j ~ <z 0 0 Q.) 1-4 rJ:J rJ:J N r-'1 ~ Q.) 0 ~ ..c ~ ~ ~ I r-'1 ~ > ~ 0 I ~ rJ:J 'JJ ..,.;;j Q.) < .....-~ 0 . 1-4 ~ C"-' 0 ~ ..,.;;j ~ 0 r-'1 00 C"-' Foster-STUDIES•. OF THE ZEOLITES-Geological Survey Professional Paper 504-D, E Studies of the Zeolites Composition of Zeolites of the Natrolite Group and Compositional Relations among Thomsonites Gonnardites, and Natrolites By MARGARET D. FOSTER SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 504-D, E UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1965 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretory GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication as follows: Foster, Margaret Dorothy, 1895- Studies of the zeolites. D. Composition of zeolites of the natrolite group. E. Compositional relations among thom­ sonites, gonnardites, and natrolites. Washington, U.S. Govt. Print. Off., 1965. v, 7; iii, 10 p. diagrs., tables. 30 em. (U.S. Geological Survey. Professional paper 504-D, E) Shorter contributions to general geology. Each part also has separate title page. Includes bibliographies. (Continued on next card) Foster, Margaret Dorothy, 1895- Studies of the zeolites. 1965. (Card 2) 1. Zeolites. I. Title. II. Title: Composition of zeolites of the natro­ lite group. III. Title: Compositional relations among thomsonites, gonnardites, and natrolites. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 25 cents (paper cover) Studies of the Zeolites Composition of Zeolites of the N atrolite Group By MARGARET D.
    [Show full text]
  • The Thermal Dehydration of Natural Zeolites
    549.67:536.4 MEDEDELINGEN LANDBOUWHOGESCHOOL WAGENINGEN • NEDERLAND • 74-9 (1974) THE THERMAL DEHYDRATION OF NATURAL ZEOLITES (with a summary in Dutch) L. P. VAN REEUWIJK Department of Soil Science and Geology, Agricultural University, Wageningen, The Netherlands (Received 11-11-1974) H. VEENMAN & ZONEN B.V. - WAGENINGEN - 1974 Ml Mededelingen Landbouwhogeschool Wageningen 74-9 (1974) (Communications Agricultural University) is also published as a thesis CONTENTS 1. INTRODUCTION 1 1.1. History 1 1.2. Genesis and occurrence of natural zeolites 2 1.3. Structural classification 4 1.4. Practical applications of zeolites 8 2. THE DEHYDRATION OF ZEOLITES - A CRITICAL REVIEW 11 2.1. Introduction 11 2.2. DTA and TG 12 2.3. High temperature X-ray analysis 13 2.4. Vapour pressure 14 2.5. The reaction mechanism 15 2.6. Rehydration 16 3. THE COMPLEXITY OF THE DEHYDRATION PROCESS 17 3.1. Types of dehydration 17 3.2. Examples 18 3.3. Effect of pressure on dehydration 22 3.3.1. Qualitative aspect 22 3.3.2. Quantitative aspect - Calibration of pressure 25 3.4. Dehydration equilibrium and hysteresis 26 3.5. Internal and external adsorption 28 4. DEHYDRATION OF ZEOLITES OF THE NATROLITE GROUP 30 4.1. Materials and procedures 30 4.2. Results and discussion 31 4.2.1. Natrolite 31 4.2.2. Mesolite 33 4.2.3. Scolecite 36 4.2.4. Thomsonite 37 4.2.5. Gonnardite 37 4.2.6. Edingtonite 38 4.3. Conclusions 39 5. PRESSURE-TEMPERATURE RELATIONS 40 5.1. The Clausius-Clapeyron equation 41 5.2. Experimental 43 5.3.
    [Show full text]
  • Adamsite-(Y), a New Sodium–Yttrium Carbonate Mineral
    1457 The Canadian Mineralogist Vol. 38, pp. 1457-1466 (2000) ADAMSITE-(Y), A NEW SODIUM–YTTRIUM CARBONATE MINERAL SPECIES FROM MONT SAINT-HILAIRE, QUEBEC JOEL D. GRICE§ and ROBERT A. GAULT Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada ANDREW C. ROBERTS Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario K1A 0E8, Canada MARK A. COOPER Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada ABSTRACT Adamsite-(Y), ideally NaY(CO3)2•6H2O, is a newly identified mineral from the Poudrette quarry, Mont Saint-Hilaire, Quebec. It occurs as groups of colorless to white and pale pink, rarely pale purple, flat, acicular to fibrous crystals. These crystals are up to 2.5 cm in length and form spherical radiating aggregates. Associated minerals include aegirine, albite, analcime, ancylite-(Ce), calcite, catapleiite, dawsonite, donnayite-(Y), elpidite, epididymite, eudialyte, eudidymite, fluorite, franconite, gaidonnayite, galena, genthelvite, gmelinite, gonnardite, horváthite-(Y), kupletskite, leifite, microcline, molybdenite, narsarsukite, natrolite, nenadkevichite, petersenite-(Ce), polylithionite, pyrochlore, quartz, rhodochrosite, rutile, sabinaite, sérandite, siderite, sphalerite, thomasclarkite-(Y), zircon and an unidentified Na–REE carbonate (UK 91). The transparent to translucent mineral has a vitreous to pearly luster and a white streak. It is soft (Mohs hardness 3) and brittle with perfect {001} and good {100} and {010} cleav- ␣ ␤ ␥ ° ° ages. Adamsite-(Y) is biaxial positive, = V 1.480(4), = 1.498(2), = 1.571(4), 2Vmeas. = 53(3) , 2Vcalc. = 55 and is nonpleochroic. Optical orientation: X = [001], Y = b, Z a = 14° (in ␤ obtuse). It is triclinic, space group P1,¯ with unit-cell parameters refined from powder data: a 6.262(2), b 13.047(6), c 13.220(5) Å, ␣ 91.17(4), ␤ 103.70(4), ␥ 89.99(4)°, V 1049.1(5) Å3 and Z = 4.
    [Show full text]
  • Gonnardite Na2caal4si6o20 ² 7H2O C 2001 Mineral Data Publishing, Version 1.2 ° Crystal Data: Tetragonal
    Gonnardite Na2CaAl4Si6O20 ² 7H2O c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Tetragonal. Point Group: 42m: Fibrous crystals, at the centers of radiating spherulites, to 3 cm; massive. Physical Properties: Hardness = 5 D(meas.) = 2.25{2.36 D(calc.) = 2.33 Optical Properties: Translucent. Color: White, yellowish to salmon-red. Luster: Silky. Optical Class: Biaxial (+) or ({); commonly zoned. Orientation: X = c. ® = 1.497{1.508 ¯ = 1.498{1.510 ° = 1.499{1.513 2V(meas.) = 50± Cell Data: Space Group: I42d: a = 13.21(1) c = 6.622(4) Z = 2 X-ray Powder Pattern: Chaux de Bergonne, France; may be confused with natrolite and tetranatrolite. 2.92 (100), 5.93 (80), 6.70 (60), 4.44 (60), 4.74 (50), 3.23 (50), 3.12 (40) Chemistry: (1) (2) (3) SiO2 43.45 43.20 44.58 Al2O3 27.91 27.90 25.22 CaO 6.95 3.61 6.94 Na2O 8.69 13.16 7.66 H2O [13.00] 11.74 15.60 Total [100.00] 99.61 100.00 (1) Chaux de Bergonne, France; by electron microprobe, H2O by di®erence; corresponding to Na2:22Ca0:98Al4:32Si5:71O20 ² 5:70H2O: (2) Aci Trezza, Sicily, Italy; corresponds to Na3:5Ca0:5Al4:5 Si5:9O20:8 ² 5:35H2O: (3) Na2CaAl4Si6O20 ² 7H2O: Mineral Group: Zeolite group. Occurrence: In cavities in basalt, leucite tephrite, and altered skarn. Association: Zeolites, calcite. Distribution: Well characterized material from: in France, at Chaux de Bergonne, Gignat, Puy de D^ome. In Italy, from Capo di Bove, near Rome, Lazio; and at Aci Castello, Aci Trezza, Osilo, and other places on Sardinia.
    [Show full text]
  • THE CRYSTAL STRUCTURE of CAHNITE, Cabaso4 (OH)4
    THE CRYSTAL STRUCTURE OF CAHNITE, CaBAsO4 (OH)4 by Charles T. Prewitt S.B., M.I.T.AAT.rc (1955) SUBMITTED IN PARTIAL YULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY (1960) Signature of Author .,. ..... .. ... .... Department of>Geolgy nd Geophysics, May 20, 1960 Certified by . t -.. 4-w.Vi 4 ... .. ... , . Thesis Supervisor Accepted by . .* . .... ... Chairman, Departmental Committee on Graduate Students THE CRYSTAL STRUCTURE OF CAHNITE, Ca2 BAs04 (OH)4 Charles T. Prewitt Submitted to the Department of Geology on May 20, 1960 in partial fulfillment of the requirements for the degree of Master of Science. Cahnite is one of the few crystals which had been assigned to crystal class 4. A precession study showed that its diffraction sphol is 4/m I-/-, which contains space groups I4, I4E, and14/. Because of the known 4 morphology, it must be assigned to space group I4. The unit cell, whose dimensions are a = 7.11A, o = 6.201, contains two formula weights of Ca BAsO (OH)L. The structure was studied with the aid of in ensity medsurements made with a single-crystal diffractometer. Patterson s ntheses were first made for projections along the c, a, and 110 directions. The atomic numbers of the atoms are in the ratio As:Ca.0:B = 33:20:8:5, so that the Patterson peaks are dominated by the atom pairs containing arsenic as one member of the pair. Since there are only two arsenic atoms in a body-centered cell, one As can be arbitrarily assigned to the origin.
    [Show full text]
  • Energetic Characterization of Faujasite Zeolites Using a Sensor Gas Calorimeter
    catalysts Article Energetic Characterization of Faujasite Zeolites Using a Sensor Gas Calorimeter Volker Mauer 1,* , Christian Bläker 1, Christoph Pasel 1 and Dieter Bathen 1,2 1 Chair of Thermal Process Engineering, University of Duisburg-Essen, Lotharstraße 1, 47057 Duisburg, Germany; [email protected] (C.B.); [email protected] (C.P.); [email protected] (D.B.) 2 Institute of Energy and Environmental Technology e.V. (IUTA), Bliersheimer Straße 60, 47229 Duisburg, Germany * Correspondence: [email protected]; Tel.: +49-203-3792176 Abstract: In addition to the adsorption mechanism, the heat released during exothermic adsorption influences the chemical reactions that follow during heterogeneous catalysis. Both steps depend on the structure and surface chemistry of the catalyst. An example of a typical catalyst is the faujasite zeolite. For faujasite zeolites, the influence of the Si/Al ratio and the number of Na+ and Ca2+ cations on the heat of adsorption was therefore investigated in a systematic study. A comparison between a NaX (Sodium type X faujasite) and a NaY (Sodium type Y faujasite) zeolite reveals that a higher Si/Al ratio and therefore a smaller number of the cations in faujasite zeolites leads to lower loadings and heats. The exchange of Na+ cations for Ca2+ cations also has an influence on the adsorption process. Loadings and heats first decrease slightly at a low degree of exchange and increase significantly with higher calcium contents. If stronger interactions are required for heterogeneous catalysis, then the CaNaX zeolites must have a degree of exchange above 53%. The energetic contributions show that the highest-quality adsorption sites III and III’ make a contribution to the load-dependent heat of adsorption, which is about 1.4 times (site III) and about 1.8 times (site III’) larger than that of adsorption site II.
    [Show full text]
  • Origin of Analcime in the Neogene Arikli Tuff, Biga Peninsula, NW Turkey
    N. Jb. Miner. Abh. 189/1, 21 –34 Article Published online November 2011 Origin of analcime in the Neogene Arikli Tuff, Biga Peninsula, NW Turkey Sevgi Ozen and M. Cemal Goncuoglu With 8 fi gures and 3 tables Abstract: The Arikli Tuff in the Behram Volcanics, NW Anatolia, is characterized by its dominance of authigenic analcime. It was studied by optical microscopy, XRD, SEM/EDX, and ICP for a better understanding of the analcime formation, which occurs as coarse-grained euhedral to subhedral crystals in pores and pumice fragments as well as in clusters or fi ne-grained single crystals embedded in the matrix. Besides analcime, K-feldspar, dolomite, and smectite are found as further authigenic minerals. Based on the dominance of these authigenic minerals, the tuffs are petrographically separated into phyllosilicate-bearing vitric tuff, dolomite- rich vitric tuff, and K-feldspar-dominated vitric tuff. No precursor of zeolites other than analcime was detected. Petrographical and SEM investigations indicate that euhedral to subhedral analcime crystals found as a coarse-grained fi lling cement in voids and pumice fragments are precipitated from pore water, whereas fi ne-grained disseminated crystals are formed by the dissolution- precipitation of glassy material. Hydrolysis of glassy material that is similar in composition to analcime provides the additional Na, Al, Si, and K elements which are necessary for the formation of analcime. Key words: Alteration, analcime, Neogene tuff, NW Turkey, volcanic glass. Introduction (Kopenez), Kirka (Karaoren), Urla, Bahcecik-Golpazari- Goynuk, Nallihan-Cayirhan-Beypazari-Mihaliccik, Ka- Tuffs deposited in lacustrine conditions present a unique lecik-Hasayaz-Sabanozu-Candir, Polatli-Mülk-Oglakci- opportunity to study the zeolite-forming processes.
    [Show full text]