Coupling of Geochemical Reactions and Geophysical Properties of Clay Minerals in Energy- Related Subsurface Engineered Systems Lijie Zhang Washington University in St

Total Page:16

File Type:pdf, Size:1020Kb

Coupling of Geochemical Reactions and Geophysical Properties of Clay Minerals in Energy- Related Subsurface Engineered Systems Lijie Zhang Washington University in St Washington University in St. Louis Washington University Open Scholarship Engineering and Applied Science Theses & McKelvey School of Engineering Dissertations Spring 5-15-2018 Coupling of Geochemical Reactions and Geophysical Properties of Clay Minerals in Energy- related Subsurface Engineered Systems Lijie Zhang Washington University in St. Louis Follow this and additional works at: https://openscholarship.wustl.edu/eng_etds Part of the Environmental Engineering Commons Recommended Citation Zhang, Lijie, "Coupling of Geochemical Reactions and Geophysical Properties of Clay Minerals in Energy-related Subsurface Engineered Systems" (2018). Engineering and Applied Science Theses & Dissertations. 337. https://openscholarship.wustl.edu/eng_etds/337 This Dissertation is brought to you for free and open access by the McKelvey School of Engineering at Washington University Open Scholarship. It has been accepted for inclusion in Engineering and Applied Science Theses & Dissertations by an authorized administrator of Washington University Open Scholarship. For more information, please contact [email protected]. WASHINGTON UNIVERSITY IN ST. LOUIS Department of Energy, Environmental and Chemical Engineering Dissertation Examination Committee: Young-Shin Jun, Chair Richard L. Axelbaum Randall T. Cygan John D. Fortner Daniel E. Giammar Coupling of Geochemical Reactions and Geophysical Properties of Clay Minerals in Energy- related Subsurface Engineered Systems by Lijie Zhang A dissertation presented to The Graduate School of Washington University in partial fulfillment of the requirements for the degree of Doctor of Philosophy May 2018 St. Louis, Missouri © 2018, Lijie Zhang Table of Contents List of Figures .............................................................................................................................. vii List of Tables ............................................................................................................................... xii Acknowledgments ...................................................................................................................... xiii Abstract of the Dissertation ....................................................................................................... xv Chapter 1. Introduction ............................................................................................................... 1 1.1 Background ........................................................................................................................... 1 1.1.1 Geologic CO2 Sequestration (GCS) and CO2-enhanced Unconventional Oil/Gas Recovery .................................................................................................................................. 1 1.1.2 Brine–mineral Interactions under Conditions Relevant to Subsurface Operations ........ 2 1.1.3 Importance of Coupling Geochemical Reactions and the Geophysical Properties of Minerals ................................................................................................................................... 5 1.2 Research Objectives and Tasks ............................................................................................. 7 1.2.1 Current Knowledge Gaps ............................................................................................... 7 1.2.2 Specific Objectives and Tasks ........................................................................................ 9 1.3 Dissertation Overview ......................................................................................................... 11 Chapter 2. Effects of Salinity-Induced Chemical Reactions on Biotite Wettability Changes under Geologic CO2 Sequestration Conditions ........................................................................ 15 Abstract ..................................................................................................................................... 15 2.1 Introduction ......................................................................................................................... 16 2.2 Experimental Section .......................................................................................................... 17 2.2.1 Minerals and Chemicals ............................................................................................... 17 2.2.2 High Temperature and High Pressure Batch Experiments ........................................... 18 2.2.3 Contact Angle Measurements ....................................................................................... 20 2.2.4 Characterization of Reacted Biotite .............................................................................. 21 2.3 Results and Discussion ........................................................................................................ 22 2.3.1 Higher Salinity Enhances Biotite Dissolution .............................................................. 22 2.3.2 Chemical Reactions Make Biotite Surfaces More Hydrophilic ................................... 25 2.3.3 Reacted Biotite Surfaces Exhibit a Lower CO2 Adhesion and Contact Angle Hysteresis ............................................................................................................................................... 28 2.4 Environmental Implications ................................................................................................ 31 Acknowledgments ..................................................................................................................... 33 ii Supporting Information for Chapter 2 ....................................................................................... 34 Chapter 3. Distinctive Reactivities at Biotite Edge and Basal Planes in the Presence of Organic Ligands: Implications for Organic-Rich Geologic CO2 Sequestration ................... 42 Abstract ..................................................................................................................................... 42 3.1 Introduction ......................................................................................................................... 43 3.2 Experimental Section .......................................................................................................... 47 3.2.1 Chemicals and Mineral Sample Preparation ................................................................ 47 3.2.2 High Temperature and High Pressure Dissolution Experiments .................................. 48 3.2.3 Analyses of Surface Morphological Changes .............................................................. 50 3.2.4 Identification of Secondary Mineral Phases ................................................................. 50 3.2.5 Fourier Transform Infrared (FTIR) Spectroscopy Analyses ........................................ 51 3.3 Results ................................................................................................................................. 52 3.3.1 Enhanced Biotite Dissolution by Oxalate and Inhibited Dissolution by Acetate ......... 52 3.3.2 Effects of Acetate and Oxalate on Biotite’s Surface Morphological Changes ............. 54 3.3.3 Biotite Anisotropic Dissolution .................................................................................... 57 3.3.4 Precipitation of Secondary Minerals on Basal surfaces and Edge Surfaces................. 59 3.4 Discussion ........................................................................................................................... 60 3.4.1 Interactions between Acetate and Biotite: pH-induced Mechanisms ........................... 60 3.4.2 Interactions between Oxalate and Biotite: Surface Complexation ............................... 62 3.4.3 Distinctive Reactivities at Biotite Edge and Basal Surfaces ........................................ 65 3.5 Environmental Implications ................................................................................................ 66 Acknowledgments ..................................................................................................................... 67 Supporting Information for Chapter 3 ....................................................................................... 68 Chapter 4. Effects of Phosphate on Biotite Dissolution and Secondary Precipitation under Conditions Relevant to Engineered Subsurface Systems ........................................................ 80 Abstract ..................................................................................................................................... 80 4.1 Introduction ......................................................................................................................... 81 4.2 Experimental Section .......................................................................................................... 85 4.2.1 Minerals and Chemicals ............................................................................................... 85 4.2.2 High Temperature and High Pressure Reactions .......................................................... 86 4.2.3 Characterization of Reacted Biotite Samples ............................................................... 87 4.2.4 Fourier Transform Infrared (FTIR) Spectroscopy Analyses of Phosphate Complexation ............................................................................................................................................... 90 4.3 Results and Discussion .......................................................................................................
Recommended publications
  • Diaspore Alo(OH) C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Orthorhombic
    Diaspore AlO(OH) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 2/m 2/m 2/m. As crystals, platy on {010} and elongated to acicular along [001], to 40 cm; stalactitic, foliated, scaly; disseminated, massive. Twinning: On {021}, to form heart-shaped twins or pseudohexagonal aggregates; on {061}, uncommon. Physical Properties: Cleavage: {010} perfect, {110} distinct, {100} in traces. Fracture: Conchoidal. Tenacity: Very brittle. Hardness = 6.5–7 D(meas.) = 3.2–3.5 D(calc.) = 3.380 Optical Properties: Transparent to translucent. Color: White, pale gray, colorless, greenish gray, brown, pale yellow, pink, lilac; color may vary with viewing direction in the same specimen, may show a color change from brownish green in daylight to raspberry pink in artificial light; colorless in thin section. Luster: Adamantine, vitreous, pearly on cleavage faces. Optical Class: Biaxial (+). Pleochroism: In thick plates, may be reddish brown to reddish violet; grayish green to green. Orientation: X = c; Y = b; Z = a. Dispersion: r< v,weak. Absorption: Z > Y > X, seen on strongly colored specimens. α = 1.682–1.706 β = 1.705–1.725 γ = 1.730–1.752 2V(meas.) = 84◦–86◦ Cell Data: Space Group: P bnm. a = 4.4007(6) b = 9.4253(13) c = 2.8452(3) Z = 4 X-ray Powder Pattern: Springfield, Massachusetts, USA. 3.99 (100), 2.317 (56), 2.131 (52), 2.077 (49), 1.633 (43), 2.558 (30), 1.480 (20) Chemistry: (1) (2) (1) (2) SiO2 0.42 Fe2O3 0.18 Al2O3 84.44 84.98 H2O 14.99 15.02 Total 100.03 100.00 (1) Kossoi Brod, Russia.
    [Show full text]
  • The Structure and Vibrational Spectroscopy of Cryolite, Na3alf6 Cite This: RSC Adv., 2020, 10, 25856 Stewart F
    RSC Advances PAPER View Article Online View Journal | View Issue The structure and vibrational spectroscopy of cryolite, Na3AlF6 Cite this: RSC Adv., 2020, 10, 25856 Stewart F. Parker, *a Anibal J. Ramirez-Cuesta b and Luke L. Daemenb Cryolite, Na3[AlF6], is essential to commercial aluminium production because alumina is readily soluble in molten cryolite. While the liquid state has been extensively investigated, the spectroscopy of the solid state has been largely ignored. In this paper, we show that the structure at 5 K is the same as that at Received 31st May 2020 room temperature. We use a combination of infrared and Raman spectroscopies together with inelastic Accepted 1st July 2020 neutron scattering (INS) spectroscopy. The use of INS enables access to all of the modes of Na3[AlF6], DOI: 10.1039/d0ra04804f including those that are forbidden to the optical spectroscopies. Our spectral assignments are supported rsc.li/rsc-advances by density functional theory calculations of the complete unit cell. Introduction In view of the technological importance of cryolite, we have Creative Commons Attribution 3.0 Unported Licence. carried out a comprehensive spectroscopic investigation and 1 Cryolite, Na3[AlF6], occurs naturally as a rare mineral. Histori- report new infrared and Raman spectra over extended temper- cally, it was used as a source of aluminium but this has been ature and spectral ranges and the inelastic neutron scattering superseded by bauxite (a mixture of the Al2O3 containing (INS) spectrum. The last of these is observed for the rst time minerals boehmite, diaspore and gibbsite), largely because of and enables access to all of the modes of Na3[AlF6].
    [Show full text]
  • Minerals of the San Luis Valley and Adjacent Areas of Colorado Charles F
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/22 Minerals of the San Luis Valley and adjacent areas of Colorado Charles F. Bauer, 1971, pp. 231-234 in: San Luis Basin (Colorado), James, H. L.; [ed.], New Mexico Geological Society 22nd Annual Fall Field Conference Guidebook, 340 p. This is one of many related papers that were included in the 1971 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States.
    [Show full text]
  • Iidentilica2tion and Occurrence of Uranium and Vanadium Identification and Occurrence of Uranium and Vanadium Minerals from the Colorado Plateaus
    IIdentilica2tion and occurrence of uranium and Vanadium Identification and Occurrence of Uranium and Vanadium Minerals From the Colorado Plateaus c By A. D. WEEKS and M. E. THOMPSON A CONTRIBUTION TO THE GEOLOGY OF URANIUM GEOLOGICAL S U R V E Y BULL E TIN 1009-B For jeld geologists and others having few laboratory facilities.- This report concerns work done on behalf of the U. S. Atomic Energy Commission and is published with the permission of the Commission. UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1954 UNITED STATES DEPARTMENT OF THE- INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan. Director Reprint, 1957 For sale by the Superintendent of Documents, U. S. Government Printing Ofice Washington 25, D. C. - Price 25 cents (paper cover) CONTENTS Page 13 13 13 14 14 14 15 15 15 15 16 16 17 17 17 18 18 19 20 21 21 22 23 24 25 25 26 27 28 29 29 30 30 31 32 33 33 34 35 36 37 38 39 , 40 41 42 42 1v CONTENTS Page 46 47 48 49 50 50 51 52 53 54 54 55 56 56 57 58 58 59 62 TABLES TABLE1. Optical properties of uranium minerals ______________________ 44 2. List of mine and mining district names showing county and State________________________________________---------- 60 IDENTIFICATION AND OCCURRENCE OF URANIUM AND VANADIUM MINERALS FROM THE COLORADO PLATEAUS By A. D. WEEKSand M. E. THOMPSON ABSTRACT This report, designed to make available to field geologists and others informa- tion obtained in recent investigations by the Geological Survey on identification and occurrence of uranium minerals of the Colorado Plateaus, contains descrip- tions of the physical properties, X-ray data, and in some instances results of chem- ical and spectrographic analysis of 48 uranium arid vanadium minerals.
    [Show full text]
  • THE COLOR ORIGIN of GEM DIASPORE: CORRELATION to CORUNDUM Che Shen and Ren Lu
    FEATURE AR ICLES THE COLOR ORIGIN OF GEM DIASPORE: CORRELATION TO CORUNDUM Che Shen and Ren Lu Color-change diaspore, known commercially as Zultanite, is sought by designers and consumers for its special optical characteristics, namely its color and color change. Understanding the color origin of gem-grade diaspore could provide a scientific basis to guide its gemological testing, cutting, and valuation. This study uses ultravio- let-visible (UV-Vis) spectra and laser ablation–inductively coupled plasma–mass spectrometry (LA-ICP-MS) to examine the color origin of color-change diaspore and to compare it with corundum. As Raman spectra vibration intensities are closely related to crystal direction for diaspore, crystal orientation was determined through Raman spectroscopy. The color correlation between color-change diaspore and corundum confirmed the identity of 3+ 3+ 2+ 4+ each chromophore. In addition, the effectiveness of different chromophores such as Cr , Fe , Fe -Ti pairs, 3+ and V between gem-quality diaspore and corundum is compared quantitatively. em-quality diaspore occupies an important structure consists of AlO octahedra (Hill, 1979; Lewis 6 position in the gem market due to its rarity, et al., 1982). Both types of crystals are composed solely Gstriking pleochroism, and color-change phe- of octahedral units. In addition, the diaspore structure nomenon (figure 1). The material’s value depends on is able to convert to corundum structure through de- these factors. A clear understanding of color origin hydration (Iwai et al., 1973). Due to their closely related offers considerable benefits for gemological testing, crystallographic structure and chemical composition, cutting, and even valuation of gem diaspore.
    [Show full text]
  • Part 629 – Glossary of Landform and Geologic Terms
    Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition.
    [Show full text]
  • From Monovalent Ions to Complex Organic Molecules Udo Becker*†, Subhashis Biswas*, Treavor Kendall**, Peter Risthaus***, Christine V
    [American Journal of Science, Vol. 305, June, September, October, 2005,P.791–825] INTERACTIONS BETWEEN MINERAL SURFACES AND DISSOLVED SPECIES: FROM MONOVALENT IONS TO COMPLEX ORGANIC MOLECULES UDO BECKER*†, SUBHASHIS BISWAS*, TREAVOR KENDALL**, PETER RISTHAUS***, CHRISTINE V. PUTNIS****, and CARLOS M. PINA***** ABSTRACT. In order to understand the interactions of inorganic and organic species from solution with mineral surfaces, and more specifically, with the growth and dissolution behavior of minerals, we start by reviewing the most basic level of interaction. This is the influence of single monovalent ions on the growth and dissolution rate of minerals consisting of divalent ions. Monovalent ions as back- ground electrolyte can change the morphology of growth features such as growth islands and spirals. These morphology changes can be similar to the؉ ones caused by organic molecules and are, therefore, easily mixed up. Both Na and Cl- promote growth and dissolution of some divalent crystals such as barite and celestite. In addition, morphology changes and the stability of polar steps on sulfates are explained using atomistic principles. Subsequently, we will increase the level of complexity by investigating the interac- tion between organic molecules and mineral surfaces. As an example, we describe the influence of different organic growth inhibitors on the growth velocity of barite and use molecular simulations to identify where these organic molecules attack the surface to inhibit growth. Nature provides a number of complex organic molecules, so-called siderophores that are secreted by plants to selectively extract Fe ions from the surrounding soil. The molecular simulations on siderophores are complemented by atomic force-distance measurements to mimic the interaction of these molecules with Fe and Al oxide surfaces.
    [Show full text]
  • Leaching Behavior of Lithium-Bearing Bauxite with High-Temperature Bayer Digestion Process in K2O-Al2o3-H2O System
    metals Article Leaching Behavior of Lithium-Bearing Bauxite with High-Temperature Bayer Digestion Process in K2O-Al2O3-H2O System Dongzhan Han 1,2 , Zhihong Peng 1,*, Erwei Song 2 and Leiting Shen 1 1 School of Metallurgy and Environment, Central South University, Changsha 410083, China; [email protected] (D.H.); [email protected] (L.S.) 2 Zhengzhou Non-Ferrous Metals Research Institute Co. Ltd. of CHALCO, Zhengzhou 450041, China; [email protected] * Correspondence: [email protected] Abstract: Lithium is one of the secondary mineral elements occurring in bauxite. The behavior of lithium-bearing bauxite in the digestion process was investigated, and the effect of digestion conditions on the extraction rates of lithium was studied. The results demonstrate that the mass ratio of the added CaO to bauxite, the KOH concentration, and the digestion temperature had a significant effect on the lithium extraction efficiency. An L9(34) orthogonal experiment demonstrated that the order of each factor for lithium extraction from primary to secondary is lime dosage, caustic concentration, and reaction temperature. Under the optimal conditions (t = 60 min, T = 260 ◦C, r(K2O) = 280 g/L, and 16% lime dosage), the leaching efficiencies of lithium and alumina are 85.6% and 80.09%, respectively, with about 15% of lithium entering into red mud. The findings of this study maybe useful for controlling lithium content in alumina products and lithium recovery from the Citation: Han, D.; Peng, Z.; Song, E.; Bayer process. Shen, L. Leaching Behavior of Lithium-Bearing Bauxite Keywords: lithium-bearing bauxite; digestion; K2O-Al2O3-H2O system withHigh-Temperature Bayer Digestion Process in K2O-Al2O3-H2O System.
    [Show full text]
  • Investigation of Lime Usage Impacts on Bauxite Processability at ETI Aluminyum Plant
    International Journal of Industrial Chemistry (2019) 10:57–66 https://doi.org/10.1007/s40090-019-0171-x RESEARCH Investigation of lime usage impacts on bauxite processability at ETI Aluminyum Plant Hüseyin Arıkan1 · Gökhan K. Demir2 · Sema Vural3 Received: 29 March 2018 / Accepted: 3 February 2019 / Published online: 11 February 2019 © The Author(s) 2019 Abstract ETI Aluminyum A.Ş., the primary aluminium manufacturer of Turkey, is also one of the major integrated plants of the world capable of performing production from mining until end product. The alumina refnery was designed on a certain boehmitic bauxite quality basis. However, bauxite properties have changed over the years, resulting in the urgent need for process opti- mization to not only keep the refnery cost efcient, but also prevent serious bottlenecks in the near future. Lime can be used to overcome problems when using bauxites with specifc and variable chemical and mineralogical characteristics. Although lime is extensively used when processing diasporic bauxites, the studies on boehmitic bauxites and the overall efects on the process are limited. In this paper, lime impact was investigated at all stages of the Bayer process including the efect on alumina quality, energy and raw material consumptions. The results showed signifcant improvements in the product quality as well as recordable savings on consumptions. Keywords Bayer process · Lime usage · Caustic consumption · Digestion · Alumina quality · Boehmitic bauxite Introduction crystalline structure to boehmite. Diferences in ore compo- sition and presence of iron, silicon and titanium impurities The Bayer process is used for producing alumina (Al2O3) infuence their subsequent processing [3, 4]. Thus, it is nec- from bauxite ore.
    [Show full text]
  • CURRICULUM VITAE Robert Michael Williams, Ph.D
    CURRICULUM VITAE Robert Michael Williams, Ph.D. University Distinguished Professor of Chemistry Department of Chemistry, Colorado State University, Fort Collins, CO 80523 Phone (970) 491-6747; FAX (970)-491-3944 e-mail: [email protected] Webpage: http://rwindigo1.chm.colostate.edu/ Personal Information: Date of birth: February 8, 1953 Married: Jill Janssen Williams Children: Ridge Janssen Williams (born February 23, 2001) Rainier Valentine Williams (born August 20, 2005) Education: B.A., Chemistry (with highest distinction), May, 1975. Syracuse University, Syracuse, NY. Thesis under Professor Ei-ichi Negishi on "A Stereoselective Synthesis of Partially Substituted 1,2,3-Butatriene Derivatives via Hydroboration". Ph.D., Organic Chemistry, June, 1979. Massachusetts Institute of Technology, Cambridge, MA. Thesis advisor, Dr. W. H. Rastetter. Thesis title: "Epidithiapiperazinedione Syntheses". Postdoctoral Fellow, September 1979-September 1980, Harvard University, Cambridge, MA. The late Professor R. B. Woodward group (Y. Kishi, principal investigator). Total synthesis of erythromycin A. Honors and Awards: Organic Synthesis Award, Local Rocky Mountain ACS Section, Reaching New Heights (2012) JSPS Invitation Fellowship Program for Research in Japan (Long-Term) 2012-2013 Ernest Guenther Award in the Chemistry of Natural Products, American Chemical Society (2011) Multiple Myeloma Research Foundation Senior Award (2009-2011) University Distinguished Professor, Colorado State University (2002) Arthur C. Cope Scholar Award, American
    [Show full text]
  • Curriculum Vitae
    V. Gouverneur – University of Oxford – Curriculum Vitae Véronique GOUVERNEUR FRS Professor of Chemistry University of Oxford, Department of Chemistry (Mathematical, Physical and Life Sciences Division) Born November 8, 1964 in Geel (Belgium) Chemistry Research Laboratory - 12 Mansfield Road- Oxford - OX1 3TA (United Kingdom) Phone and Fax: 44 (1865) 275 644 E-mail: [email protected] http://www.chem.ox.ac.uk/researchguide/vgouverneur.html EMPLOYMENT 2008- Oxford University, Department of Chemistry (UK), Professor in Chemistry 2006-2008 Oxford University, Department of Chemistry (UK), Reader in Organic Chemistry 1998-2006 Oxford University, Department of Chemistry (UK), University Lecturer in Organic Chemistry 1998- Merton College, Oxford (UK), Tutorial Fellowship 1994-1998 Université Louis Pasteur Strasbourg (France), Maître de Conférence (Dr C. Mioskowski) & Associate Member of the Institut de Science et d’Ingénierie Supramoleculaires (Prof. J.-M. Lehn) 1992-1994 The Scripps Research Institute (CA, USA), Postdoctoral Research Fellow, Advisor: Prof. R. A. Lerner EDUCATION 1985-1991: Université Catholique de Louvain, Louvain-la-Neuve (Belgium), Ph.D., Advisor: Prof. L. Ghosez 1981-1985: Université Catholique de Louvain, Louvain-la-Neuve (Belgium) B.Sc & M.Sc in Chemistry AWARDS, HONORS, NAMED LECTURES 2020, Organic Reactions Lecture, University of Alberta (Canada) 2019, Nankai Organic Lecture, Nankai University (China) 2019, Prof. H.J. Backer lecture 2019, University of Groningen (The Netherlands) 2019, Prelog Medal, ETH
    [Show full text]
  • V. Gouverneur – University of Oxford – Curriculum Vitae
    V. Gouverneur – University of Oxford – Curriculum Vitae Véronique GOUVERNEUR Professor of Chemistry - University of Oxford Department of Chemistry (Mathematical, Physical and Life Sciences Division) Born November 8, 1964 in Geel (Belgium) Chemistry Research Laboratory - 12 Mansfield Road- Oxford - OX1 3TA (United Kingdom) Phone and Fax: 44 (1865) 275 644 E-mail: [email protected] http://www.chem.ox.ac.uk/researchguide/vgouverneur.html EMPLOYMENT 2008- Oxford University, Department of Chemistry (UK), Professor in Chemistry 2006-2008 Oxford University, Department of Chemistry (UK), Reader in Organic Chemistry 1998-2006 Oxford University, Department of Chemistry (UK), University Lecturer in Organic Chemistry 1998- Merton College, Oxford (UK), Tutorial Fellowship 1994-1998 Université Louis Pasteur Strasbourg (France), Maître de Conférence (Dr C. Mioskowski) & Associate Member of the Institut de Science et d’Ingénierie Supramoleculaires (Prof. J.-M. Lehn) 1992-1994 The Scripps Research Institute (CA, USA), Postdoctoral Research Fellow, Advisor: Prof. R. A. Lerner EDUCATION 1985-1991: Université Catholique de Louvain, Louvain-la-Neuve (Belgium), Ph.D., Advisor: Prof. L. Ghosez 1981-1985: Université Catholique de Louvain, Louvain-la-Neuve (Belgium) B.Sc & M.Sc in Chemistry AWARDS, HONORS, NAMED LECTURES 2019, Prelog Medal, ETH Zurich (Switzerland) 2019, Frontiers in Chemical Research Lecture Series 2019, Texas A&M University (USA) 2018, Dorothy Hodgkin Memorial Lecture, Somerville College, Oxford (UK) 2018, Organic Reactions
    [Show full text]