A Deductive Approach to Biogenesis! Rob Hengeveld* Vrije Universiteit, Amsterdam, the Netherlands
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Course CHEM 3341, Inorganic Chemistry Professor Dr. Sheel Dodani Term Fall 2016 Meetings MWF 10:00-10:50 AM, MC 2.410
Course CHEM 3341, Inorganic Chemistry Professor Dr. Sheel Dodani Term Fall 2016 Meetings MWF 10:00-10:50 AM, MC 2.410 Professor’s Contact Information Office Phone 972-883-7283 Other Phone N/A Office Location Bioengineering Science Building (BSB) Email Address [email protected] Office Hours Wednesdays 11:30 AM – 12:30 PM, Thursdays 4 PM – 5 PM BSB 11.302 Other Information Please contact me for appointments outside of office hours General Course Information Pre-requisites, Co- requisites, & other Chem 2323 and Chem 2325 restrictions Survey of inorganic chemistry with emphasis on the modern concepts and theories of inorganic chemistry including electronic and geometric Course Description structure of inorganic compounds. Topics address contemporary physical and descriptive inorganic chemistry. Objectives The goal of this course is to provide students with a thorough foundation in atomic structure, periodicity, bonding and symmetry with subsequent extension of these basic principles to acid/base, solid state and coordination chemistry. Students will develop an understanding of the elements and the ability to predict the structures, certain properties and reactivities of a range of representative ionic and covalent compounds. Learning Expected Learning Outcomes Outcomes Upon successful completion of this course, students will therefore: 1. Be able to explain atomic structure and bonding using currently accepted theories. 2. Be able to use group theory to describe molecular orbital diagrams and molecular properties. 3. Be able to integrate knowledge of atomic structure with the structure and properties of ionic and molecular compounds. 4. Be able to explain the history, bonding and properties of representative main group elements, coordination and organometallic compounds Inorganic Chemistry, 5th Edition Required Texts & by Gary L. -
General Inorganic Chemistry
General Inorganic Chemistry Pre DP Chemistry Period 1 • Teacher: Annika Nyberg • [email protected] • Urgent messages via Wilma! Klicka här för att ändra format på underrubrik i bakgrunden • Course book: • CliffsNotes: Chemistry Quick Review http://www.chem1.com/acad/webtext/virtualtextbook.html Content • Introduction • The Structure of Matter (Chapter 1) • The Atom (Chapter 2 and 3) • Chemical bonding (Chapter 5) • The Mole (Chapter 2) • Solutions (Chapter 9) • Acids and bases (Chapter 10) • Quiz • Revision • EXAM 9.00-11.45 Assessment Exam: 80 % Quiz: 20% + practical work, activity and absences 1. Chemistry: a Science for the twenty-first century ● Chemistry has ancient roots, but is now a modern and active, evolving science. ● Chemistry is often called the central science, because a basic knowledge of chemistry is essential for students in biology, physics, geology and many other subjects. https://www.youtube.com/watch?v=tTlnrhiadnI ● Chemical research and development has provided us with new substances with specific properties. These substances have improved the quality of our lives. Health and medicine vaccines sanitation systems antibiotics anesthesia and all other drugs Energy new alternative energy sources (e.g. solar energy to electric energy, nuclear fission) electric cars with long lasting batteries Environment greenhouse gases acid rain and smog Materials and Technology ● polymers (rubber and nylon), ceramics (cookware), liquid crystals (electronic displays), adhesives (Post-It notes), coatings (latex-paint), silicon chips (computers) Food and Agriculture substances for biotechnology ● The purpose of this course is to make you understand how chemists see the world. ● In other words, if you see one thing (in the macroscopic world) you think another (visualize the particles and events in the microscopic world). -
Purification and Characterization of Bromocresol Purple for Spectrophotometric Seawater Alkalinity Titrations
University of Montana ScholarWorks at University of Montana Undergraduate Theses and Professional Papers 2016 PURIFICATION AND CHARACTERIZATION OF BROMOCRESOL PURPLE FOR SPECTROPHOTOMETRIC SEAWATER ALKALINITY TITRATIONS Taymee A. Brandon The University Of Montana, [email protected] Follow this and additional works at: https://scholarworks.umt.edu/utpp Part of the Analytical Chemistry Commons, and the Environmental Chemistry Commons Let us know how access to this document benefits ou.y Recommended Citation Brandon, Taymee A., "PURIFICATION AND CHARACTERIZATION OF BROMOCRESOL PURPLE FOR SPECTROPHOTOMETRIC SEAWATER ALKALINITY TITRATIONS" (2016). Undergraduate Theses and Professional Papers. 97. https://scholarworks.umt.edu/utpp/97 This Thesis is brought to you for free and open access by ScholarWorks at University of Montana. It has been accepted for inclusion in Undergraduate Theses and Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. PURIFICATION AND CHARACTERIZATION OF BROMOCRESOL PURPLE FOR SPECTROPHOTOMETRIC SEAWATER ALKALINITY TITRATIONS By TAYMEE ANN MARIE BRANDON Undergraduate Thesis presented in partial fulfillment of the requirements for the University Scholar distinction Davidson Honors College University of Montana Missoula, MT May 2016 Approved by: Dr. Michael DeGrandpre Department of Chemistry and Biochemistry ABSTRACT Brandon, Taymee, B.S., May 2016 Chemistry Purification and Characterization of Bromocresol Purple for Spectrophotometric Seawater Alkalinity Titrations Faculty Mentor: Dr. Michael DeGrandpre The topic of my research is the purification of the sulfonephthalein indicator bromocresol purple (BCP). BCP is used as an acid-base indicator in seawater alkalinity determinations. Impurities in sulfonephthalein indicator salts often result in significant errors in pH values3. -
Chemistry ‐ Student Learning Outcomes CHEM 100 Introduction to Chemistry 1.Analyze Chemical Reactions and Chemical Problems Through Stoichiometry
Chemistry ‐ Student Learning Outcomes CHEM 100 Introduction To Chemistry 1.analyze chemical reactions and chemical problems through stoichiometry. (ILO2) 2. predict properties of matter using atomic theory. (ILO2) 3. use the periodic table properly to determine trends in elements (atomic size, number of valence electrons, metallic character, electronegativity, etc.). (ILO2, ILO4) 4. perform chemical experiments in a safe, accurate, and scientific manner, using proper glasswares, graphs, and spreadsheets. (ILO2, ILO4) CHEM 160 Introduction to General, 1. calculate drug dosage using English and Metric unit interconversions and dimensional Organic & Biological analysis. (ILO4) Chemistry 2. identify different classes of organic compounds. (ILO2) 3. identify different functional groups in organic compounds. (ILO2) 4. write a research paper on biochemical disorders. (ILO4) 5. discuss the geographical/ethnic distribution of biochemical disorders. (ILO5) CHEM 200 General Inorganic Chemistry I 1. perform dimensional analysis calculations as they relate to problems involving percent composition and density. (ISLO2) 2. write chemical formulas, and name inorganic compounds. (ISLO2) 3. relate chemical equations and stoichiometry as they apply to the mole concept. (ISLO2) 4. identify the basic types of chemical reactions including precipitation, neutralization, and oxidation‐reduction. (ISLO4) 5. knowledge of atomic structure and quantum mechanics and apply these concepts to the study of periodic properties of the elements. (ISLO4) CHEM 202 General Inorganic Chemistry 1. examine and develop concepts of covalent bonding, orbital hybridization and II molecular orbital theory. (ISLO4) 2. identify and perform organic addition and elimination reactions. (ISLO2) 3. compare and analyze Thermodynamics properties and differentiate between spontaneity and maximum useful work heat and Free energy. (ISLO2) 4. -
CHEM 110 Week 1 Inorganic Chemistry I Atoms, Elements, and Compounds
CHEM 110 Week 1 Inorganic Chemistry I Atoms, Elements, and Compounds Week 1 Reading Assignment Your week 1 reading assignment has been selected from chapters 3 and 5 in your textbook. As part of your reading assignment, you are expected to work the sample problems and the selected “questions and problems” at the end of your book sections. The answers to the odd numbered “questions and problems” can be found at the end of your book chapters. You should use this key to check yourself. If you are having problems arriving at the correct answer as listed in the back of your book chapter, please email me. Read section 3.1 and answer the odd numbered “questions and problems” on page 85. Read section 3.2 and answer the odd numbered “questions and problems” on page 91. Read section 3.3 and answer “questions and problems” 3.15 and 3.17 on page 94. You do not have to know the experimental details used to determine the structure of an atom. Read section 3.4 and answer the odd numbered “questions and problems” on page 97. Read about isotopes and atomic mass in section 3.5 and answer “questions and problems” 3.29 and 3.31 on page 100. Skip the part on calculating atomic mass using isotopes. Read section 3.6. Read section 3.7. Read about “Group Number and Valence Electrons” and “Electron-Dot Symbols” in section 3.8. Answer “questions and problems” 3.57 and 3.59 on page 118. Read section 5.1 and answer the odd numbered “questions and problems” on page 163 and 164. -
Geochemistry of Corals: Proxies of Past Ocean Chemistry, Ocean Circulation, and Climate
Proc. Natl. Acad. Sci. USA Vol. 94, pp. 8354–8361, August 1997 Colloquium Paper This paper was presented at a colloquium entitled ‘‘Carbon Dioxide and Climate Change,’’ organized by Charles D. Keeling, held November 13–15, 1995, at the National Academy of Sciences, Irvine, CA. Geochemistry of corals: Proxies of past ocean chemistry, ocean circulation, and climate ELLEN R. M. DRUFFEL Department of Earth System Science, University of California, Irvine, CA 92697 ABSTRACT This paper presents a discussion of the status Second, a synthesis is presented of the available proxy of the field of coral geochemistry as it relates to the recovery of records from corals as they relate to past climate, ocean past records of ocean chemistry, ocean circulation, and climate. circulation changes, and anthropogenic input of excess CO2. The first part is a brief review of coral biology, density banding, For some databases, the anthropogenic CO2 appears clear and and other important factors involved in understanding corals as globally distributed. For other databases it appears that vari- proxies of environmental variables. The second part is a syn- ability on interannual to decadal time scales complicates a thesis of the information available to date on extracting records straightforward attempt to separate natural perturbations of the carbon cycle and climate change. It is clear from these from the anthropogenic CO2 signal on the Earth’s environ- proxy records that decade time-scale variability of mixing pro- ment. Shen (4) presents a review of the types of coral archives cesses in the oceans is a dominant signal. That Western and available from the perspective of historical El Nin˜o-Southern Eastern tropical Pacific El Nin˜o-Southern Oscillation (ENSO) Oscillation (ENSO) influences on the tropical Pacific Ocean. -
25Th Anniversary of Molecules—Recent Advances in Inorganic Chemistry
molecules Editorial 25th Anniversary of Molecules—Recent Advances in Inorganic Chemistry Burgert Blom 1,* , Erika Ferrari 2 , Vassilis Tangoulis 3 ,Cédric R. Mayer 4, Axel Klein 5 and Constantinos C. Stoumpos 6 1 Maastricht Science Programme, Assistant Professor of Inorganic Chemistry and Catalysis, Maastricht University, Kapoenstraat 2, P.O. Box 616, 6200 MD Maastricht, The Netherlands 2 Department of Chemical and Geological Sciences, University of Modena and Reggio Emilia, Via Campi 103, 41125 Modena, Italy; [email protected] 3 Department of Chemistry, University of Patras, 26504 Patras, Greece; [email protected] 4 Laboratoire LuMin, FRE CNRS 2036, CNRS, Université Paris-Sud, ENS Paris-Saclay, Centrale Supelec, Université Paris-Saclay, F-91405 Orsay CEDEX, France; [email protected] 5 Department für Chemie, Institut für Anorganische Chemie, Universität zu Köln, Greinstraße 6, 50939 Köln, Germany; [email protected] 6 Department of Chemistry, Northwestern University, Evanston, IL 60208, USA; [email protected] * Correspondence: [email protected] Celebrating the “25th Anniversary of Molecules” with a Special Issue dedicated to “Recent Advances in Inorganic Chemistry” strengthens the renewed role that inorganic chemistry, one of the oldest chemistry divisions, has lately earned thanks to cutting-edge perspectives and interdisciplinary applications, eventually receiving the veneration and respect which its age might require [1,2]. The last 25 years have seen staggering advances in both solid-state, molecular, catalytic Citation: Blom, B.; Ferrari, E.; Tangoulis, V.; Mayer, C.R.; Klein, A.; and bio-inorganic chemistry. Some notable highlights in molecular inorganic chemistry Stoumpos, C.C. 25th Anniversary of over the last 2.5 decades certainly must include the propensity of heavy p-block elements Molecules—Recent Advances in (those in period 3 or higher) to undergo multiple bonding with other heavy p-block Inorganic Chemistry. -
Ocean Acidification in the Geological Past
UK Ocean Acidification programme synopsis Ocean acidification in the geological past www.oceanacidification.org.uk Lessons from the past Global-scale ocean acidification is happening now, as a result of human activities adding CO2 to the atmosphere. But ocean acidity has increased previously in the Earth’s history, as a result of natural changes in atmospheric composition. Of particular interest are past releases of CO2 that have occurred relatively rapidly in geological terms, since they may provide natural analogues for the effects of current acidification on chemical processes and marine life. Calcifying organisms (that construct their shells out of calcium carbonate) provide an important research focus, since they are preserved in the fossil record and are also likely to be especially sensitive to changes in ocean chemistry. Most of the palaeo-oceanographic Specific aims of the consortium study were: work in UKOA was carried out by a consortium project Abrupt ocean l To produce new estimates of seawater acidity and atmospheric CO2 levels for acidification events and their effects the period 40-65 million years ago in the Earth’s past, led by Paul l To study the response of the carbon cycle during the onset of the Paleocene - Pearson at Cardiff University. Formal Eocene thermal maximum (PETM) using new data from Tanzania and elsewhere partners were at Southampton, and new computer models University College London and the l To compare the PETM with other known ocean acidification events in the Open University, with additional Earth’s past contributions by researchers at Bristol, l To quantify the biotic response to ocean acidification events both directly Oxford, Yale and elsewhere. -
The Physical and Chemical Characteristics of Marine Primary Open Access Organic Aerosol: a Review Biogeosciences Biogeosciences Discussions B
EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Natural Hazards Natural Hazards and Earth System and Earth System Sciences Sciences Discussions Open Access Open Access Atmos. Chem. Phys., 13, 3979–3996, 2013 Atmospheric Atmospheric www.atmos-chem-phys.net/13/3979/2013/ doi:10.5194/acp-13-3979-2013 Chemistry Chemistry © Author(s) 2013. CC Attribution 3.0 License. and Physics and Physics Discussions Open Access Open Access Atmospheric Atmospheric Measurement Measurement Techniques Techniques Discussions Open Access The physical and chemical characteristics of marine primary Open Access organic aerosol: a review Biogeosciences Biogeosciences Discussions B. Gantt and N. Meskhidze Department of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, North Carolina, USA Open Access Open Access Correspondence to: N. Meskhidze ([email protected]) Climate Climate Received: 19 July 2012 – Published in Atmos. Chem. Phys. Discuss.: 23 August 2012 of the Past of the Past Revised: 5 March 2013 – Accepted: 24 March 2013 – Published: 18 April 2013 Discussions Open Access Open Access Abstract. Knowledge of the physical characteristics and 1 Introduction Earth System chemical composition of marine organic aerosols is needed Earth System for the quantification of their effects on solar radiation trans- Dynamics Dynamics fer and cloud processes. This review examines research per- One of the largest uncertainties of the aerosol-cloud sys- Discussions tinent to the chemical composition, size distribution, mixing tem is the background concentration of natural aerosols, es- state, emission mechanism, photochemical oxidation and cli- pecially over clean marine regions where cloud condensa- Open Access Open Access matic impact of marine primary organic aerosol (POA) asso- tion nuclei (CCN) concentrationGeoscientific ranges from less than 100 Geoscientific −3 ciated with sea-spray. -
Ocean Acidification Due to Increasing Atmospheric Carbon Dioxide
Ocean acidification due to increasing atmospheric carbon dioxide Policy document 12/05 June 2005 ISBN 0 85403 617 2 This report can be found at www.royalsoc.ac.uk ISBN 0 85403 617 2 © The Royal Society 2005 Requests to reproduce all or part of this document should be submitted to: Science Policy Section The Royal Society 6-9 Carlton House Terrace London SW1Y 5AG email [email protected] Copy edited and typeset by The Clyvedon Press Ltd, Cardiff, UK ii | June 2005 | The Royal Society Ocean acidification due to increasing atmospheric carbon dioxide Ocean acidification due to increasing atmospheric carbon dioxide Contents Page Summary vi 1 Introduction 1 1.1 Background to the report 1 1.2 The oceans and carbon dioxide: acidification 1 1.3 Acidification and the surface oceans 2 1.4 Ocean life and acidification 2 1.5 Interaction with the Earth systems 2 1.6 Adaptation to and mitigation of ocean acidification 2 1.7 Artificial deep ocean storage of carbon dioxide 3 1.8 Conduct of the study 3 2 Effects of atmospheric CO2 enhancement on ocean chemistry 5 2.1 Introduction 5 2.2 The impact of increasing CO2 on the chemistry of ocean waters 5 2.2.1 The oceans and the carbon cycle 5 2.2.2 The oceans and carbon dioxide 6 2.2.3 The oceans as a carbonate buffer 6 2.3 Natural variation in pH of the oceans 6 2.4 Factors affecting CO2 uptake by the oceans 7 2.5 How oceans have responded to changes in atmospheric CO2 in the past 7 2.6 Change in ocean chemistry due to increases in atmospheric CO2 from human activities 9 2.6.1 Change to the oceans -
Analysis of Seawater a Guide for the Analytical and Environmental Chemist T.R
Analysis of Seawater A Guide for the Analytical and Environmental Chemist T.R. Crompton Analysis of Seawater A Guide for the Analytical and Environmental Chemist With 48 Figures and 45 Tables 123 T.R. Crompton Hill Cottage (Bwthyn Yr Allt) Anglesey, Gwynedd United Kingdom Library of Congress Control Number: 2005929412 ISBN-10 3-540-26762-X Springer Berlin Heidelberg New York ISBN-13 978-3-540-26762-1 Springer Berlin Heidelberg New York DOI 10.1007/b95901 This work is subject to copyright. All rights reserved, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilm or in any other way, and storage in data banks. Duplication of this publication or parts thereof is permitted only under the provisions of the German Copyright Law of September 9, 1965, in its current version, and permission for use must always be obtained from Springer. Violations are liable for prosecution under the German Copyright Law. Springer is a part of Springer Science+Business Media springer.com © Springer-Verlag Berlin Heidelberg 2006 Printed in Germany The use of general descriptive names, registered names, trademarks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. Product liability: The publishers cannot guarantee the accuracy of any information about dosage and application contained in this book. In every individual case the user must check such information by consulting the relevant literature. -
Chemistry and Biochemistry (CHBC) 1
Chemistry and Biochemistry (CHBC) 1 3. Each advanced degree candidate must present a suitable program Chemistry and of advanced courses and research. The specific courses needed to provide a basis for scholarly work beyond the B.S. level will vary with Biochemistry (CHBC) the student’s undergraduate preparation, area of concentration and the degree sought. Individual course enrollments must be approved initially by the graduate adviser and subsequently by the student’s Matt McIntosh advisory committee. Department Chair 119 Chemistry Building 4. Every student must register for a minimum of one credit hour of 479-575-4362 CHEM 600V or CHEM 700V in each term during which the student Email: [email protected] is present and doing thesis or dissertation research. Post-candidacy doctoral students are required to be enrolled in at least one hour Julie Stenken of dissertation credit (CHEM 700V) every semester (fall, spring, Director of Graduate Studies summer), until the degree is conferred. 119 Chemistry Building 479-575-7945 Additional Requirement for Master of Science Degree:The Master Email: [email protected] of Science degree in Chemistry requires a minimum 24 hours of course work plus six hours of thesis. A thesis reporting original research will be Department of Chemistry and Biochemistry Website (https:// required of all candidates for the Master of Science degree in chemistry. fulbright.uark.edu/departments/chemistry/) Students should also be aware of Graduate School requirements with Degrees Conferred: regard to master's degrees (http://catalog.uark.edu/graduatecatalog/ M.S., Ph.D. in Chemistry (CHEMMS, CHEMPH) degreerequirements/#mastersdegreestext). Areas of Study: Analytical, inorganic, organic, physical, biophysical, and Requirements for Ph.D.