Earth Science Chapter 4
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Brief Guide to the Nomenclature of Organic Chemistry
1 Brief Guide to the Nomenclature of Table 1: Components of the substitutive name Organic Chemistry (4S,5E)-4,6-dichlorohept-5-en-2-one for K.-H. Hellwich (Germany), R. M. Hartshorn (New Zealand), CH3 Cl O A. Yerin (Russia), T. Damhus (Denmark), A. T. Hutton (South 4 2 Africa). E-mail: [email protected] Sponsoring body: Cl 6 CH 5 3 IUPAC Division of Chemical Nomenclature and Structure suffix for principal hept(a) parent (heptane) one Representation. characteristic group en(e) unsaturation ending chloro substituent prefix 1 INTRODUCTION di multiplicative prefix S E stereodescriptors CHEMISTRY The universal adoption of an agreed nomenclature is a key tool for 2 4 5 6 locants ( ) enclosing marks efficient communication in the chemical sciences, in industry and Multiplicative prefixes (Table 2) are used when more than one for regulations associated with import/export or health and safety. fragment of a particular kind is present in a structure. Which kind of REPRESENTATION The International Union of Pure and Applied Chemistry (IUPAC) multiplicative prefix is used depends on the complexity of the provides recommendations on many aspects of nomenclature.1 The APPLIED corresponding fragment – e.g. trichloro, but tris(chloromethyl). basics of organic nomenclature are summarized here, and there are companion documents on the nomenclature of inorganic2 and Table 2: Multiplicative prefixes for simple/complicated entities polymer3 chemistry, with hyperlinks to original documents. An No. Simple Complicated No. Simple Complicated AND overall -
Introduction to NMR Spectroscopy of Proteins
A brief introduction to NMR spectroscopy of proteins By Flemming M. Poulsen 2002 1 Introduction Nuclear magnetic resonance, NMR, and X-ray crystallography are the only two methods that can be applied to the study of three-dimensional molecular structures of proteins at atomic resolution. NMR spectroscopy is the only method that allows the determination of three-dimensional structures of proteins molecules in the solution phase. In addition NMR spectroscopy is a very useful method for the study of kinetic reactions and properties of proteins at the atomic level. In contrast to most other methods NMR spectroscopy studies chemical properties by studying individual nuclei. This is the power of the methods but sometimes also the weakness. NMR spectroscopy can be applied to structure determination by routine NMR techniques for proteins in the size range between 5 and 25 kDa. For many proteins in this size range structure determination is relatively easy, however there are many examples of structure determinations of proteins, which have failed due to problems of aggregation and dynamics and reduced solubility. It is the purpose of these notes to introduce the reader to descriptions and applications of the methods of NMR spectroscopy most commonly applied in scientific studies of biological macromolecules, in particular proteins. The figures 1,2 and 11 are copied from “Multidímensional NMR in Liquids” by F.J.M de Ven (1995)Wiley-VCH The Figure13 and Table 1 have been copied from “NMR of Proteins and Nucleic acis” K. Wüthrich (1986) Wiley Interscience The Figures 20, 21 and 22 have been copied from J. -
The Bacteriohopanepolyol Inventory of Novel Aerobic Methane Oxidising Bacteria Reveals New Biomarker Signatures of Aerobic Methanotrophy in Marine Systems
Rush D, Osborne KA, Birgel D, Kappler A, Hirayama H, Peckmann J, Poulton SW, Nickel JC, Mangelsdorf K, Kalyuzhnaya M, Sidgwick FR, Talbot HM. The Bacteriohopanepolyol Inventory of Novel Aerobic Methane Oxidising Bacteria Reveals New Biomarker Signatures of Aerobic Methanotrophy in Marine Systems. PLoS One 2016, 11(11), e0165635. Copyright: © 2016 Rush et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. DOI link to article: http://dx.doi.org/10.1371/journal.pone.0165635 Date deposited: 20/12/2016 This work is licensed under a Creative Commons Attribution 4.0 International License Newcastle University ePrints - eprint.ncl.ac.uk RESEARCH ARTICLE The Bacteriohopanepolyol Inventory of Novel Aerobic Methane Oxidising Bacteria Reveals New Biomarker Signatures of Aerobic Methanotrophy in Marine Systems Darci Rush1☯*, Kate A. Osborne1☯, Daniel Birgel2, Andreas Kappler3,4, Hisako Hirayama5, JoÈ rn Peckmann2,6, Simon W. Poulton7, Julia C. Nickel8, Kai Mangelsdorf8, Marina Kalyuzhnaya9, Frances R. Sidgwick1, Helen M. Talbot1 1 School of Civil Engineering & Geosciences, Newcastle University, Drummond Building, Newcastle upon a11111 Tyne, NE1 7RU, Newcastle-upon-Tyne, United Kingdom, 2 Institute of Geology, University of Hamburg, Hamburg, Germany, 3 Center for Applied Geoscience, University of TuÈbingen, TuÈbingen, Germany, 4 Center for Geomicrobiology, Department -
Chapter 1: Atoms, Molecules and Ions
Previous Chapter Table of Contents Next Chapter Chapter 1: Atoms, Molecules and Ions Section 1.1: Introduction In this course, we will be studying matter, “the stuff things are made of”. There are many ways to classify matter. For instance, matter can be classified according to the phase, that is, the physical state a material is in. Depending on the pressure and the temperature, matter can exist in one of three phases (solid, liquid, or gas). The chemical structure of a material determines the range of temperatures and pressures under which this material is a solid, a liquid or a gas. Consider water for example. The principal differences between water in the solid, liquid and gas states are simply: 1) the average distance between the water molecules; small in the solid and the liquid and large in the gas and 2) whether the molecules are organized in an orderly three-dimensional array (solid) or not (liquid and gas). Another way to classify matter is to consider whether a substance is pure or not. So, matter can be classified as being either a pure substance or a mixture. A pure substance has unique composition and properties. For example, water is a pure substance (whether from Texas or Idaho, each water molecule always contains 2 atoms of hydrogen for 1 atom of oxygen). Under the same atmospheric pressure and at the same ambient temperature, water always has the same density. We can go a little further and classify mixtures are either homogeneous or heterogeneous. In a homogeneous mixture, for example, as a result of mixing a teaspoon of salt in a glass of water, the composition of the various components and their properties are the same throughout. -
Electron Paramagnetic Resonance of Radicals and Metal Complexes. 2. International Conference of the Polish EPR Association. Wars
! U t S - PL — voZ, PL9700944 Warsaw, 9-13 September 1996 ELECTRON PARAMAGNETIC RESONANCE OF RADICALS AND METAL COMPLEXES 2nd International Conference of the Polish EPR Association INSTITUTE OF NUCLEAR CHEMISTRY AND TECHNOLOGY UNIVERSITY OF WARSAW VGL 2 8 Hi 1 2 ORGANIZING COMMITTEE Institute of Nuclear Chemistry and Technology Prof. Andrzej G. Chmielewski, Ph.D., D.Sc. Assoc. Prof. Hanna B. Ambroz, Ph.D., D.Sc. Assoc. Prof. Jacek Michalik, Ph.D., D.Sc. Dr Zbigniew Zimek University of Warsaw Prof. Zbigniew Kqcki, Ph.D., D.Sc. ADDRESS OF ORGANIZING COMMITTEE Institute of Nuclear Chemistry and Technology, Dorodna 16,03-195 Warsaw, Poland phone: (0-4822) 11 23 47; telex: 813027 ichtj pi; fax: (0-4822) 11 15 32; e-mail: [email protected] .waw.pl Abstracts are published in the form as received from the Authors SPONSORS The organizers would like to thank the following sponsors for their financial support: » State Committee of Scientific Research » Stiftung fur Deutsch-Polnische Zusammenarbeit » National Atomic Energy Agency, Warsaw, Poland » Committee of Chemistry, Polish Academy of Sciences, Warsaw, Poland » Committee of Physics, Polish Academy of Sciences, Poznan, Poland » The British Council, Warsaw, Poland » CIECH S.A. » ELEKTRIM S.A. » Broker Analytische Messtechnik, Div. ESR/MINISPEC, Germany 3 CONTENTS CONFERENCE PROGRAM 9 LECTURES 15 RADICALS IN DNA AS SEEN BY ESR SPECTROSCOPY M.C.R. Symons 17 ELECTRON AND HOLE TRANSFER WITHIN DNA AND ITS HYDRATION LAYER M.D. Sevilla, D. Becker, Y. Razskazovskii 18 MODELS FOR PHOTOSYNTHETIC REACTION CENTER: STEADY STATE AND TIME RESOLVED EPR SPECTROSCOPY H. Kurreck, G. Eiger, M. Fuhs, A Wiehe, J. -
How to Read and Interpret FTIR Spectroscope of Organic Material
97| Indonesian JournalIndonesian of Science Journal & Technology of Science &,Volum Technologye 4 Issue 4 ( 11,) (20April19 )2019 97-1 18Page 97-118 Indonesian Journal of Science & Technology Journal homepage: http://ejournal.upi.edu/index.php/ijost/ How to Read and Interpret FTIR Spectroscope of Organic Material Asep Bayu Dani Nandiyanto, Rosi Oktiani, Risti Ragadhita Departemen Kimia, Universitas Pendidikan Indonesia, Jl. Dr. Setiabudi no 229 Bandung 40154, Indonesia Correspondence: E-mail: [email protected] A B S T R A C T S A R T I C L E I N F O Article History: Fourier Transform Infrared (FTIR) has been developed as a Received 10 Jan 2019 tool for the simultaneous determination of organic Revised 20 Jan 2019 components, including chemical bond, as well as organic Accepted 31 Aug 2019 Available online 09 Apr 2019 content (e.g., protein, carbohydrate, and lipid). However, ____________________ until now, there is no further documents for describing the Keywords: detailed information in the FTIR peaks. The objective of this FTIR, study was to demonstrate how to read and assess chemical infrared spectrum, organic material, bond and structure of organic material in the FTIR, in which chemical bond, the analysis results were then compared with the literatures. organic structure. The step-by-step method on how to read the FTIR data was also presented, including reviewing simple to the complex organic materials. This study is potential to be used as a standard information on how to read FTIR peaks in the biochemical and organic materials. © 2019Tim Pengembang Jurnal UPI 1. INTRODUCTION analysis is quite rapid, good in accuracy, and relatively sensitive (Jaggi and Vij, 2006). -
Numerical Methods in Electron Magnetic Resonance
NO0000039 NUMERICAL METHODS IN ELECTRON MAGNETIC RESONANCE ANALYSES AND SIMULATIONS IN QUEST OF STRUCTURAL AND DYNAMICAL PROPERTIES OF FREE RADICALS IN SOLIDS BY ANDERS RASMUS S0RNES Thesis submitted for the degree Doctor scientiarum Department of Physics, University of Oslo 1998 31-18 Preface This thesis encompasses a collection of six theoretical and experimental Electron Magnetic Resonance (EMR) studies of the structure and dynamics of free radicals in solids. Radicals are molecular systems having one or more unpaired electron. Due to their energetically unfavourable open shell configuration, they are highly reactive. Radicals are formed in different ways. They are believed to be present in many chemical reactions as short-lived intermediate products, and they are also produced in interactions of x-radiation with matter, in Compton and photoelectric processes and interactions of their secondary electrons. Longer-lived, quasistable radicals do also exist and these may be used as spin-labels or spin-probes and may be attached to larger molecules and surfaces as measurement probes to examine the environment in their immediate vicinity. EMR is a collective term for a group of spectroscopic techniques inducing and observing transitions between the Zeeman levels of a paramagnetic system, such as a radical situated in an external magnetic field. Whithin the broader concept of EMR, the particular experimental techniques of Electron Paramagnetic Resonance (EPR), ELectron Nuclear DOuble Resonance (ENDOR), Field Swept ENDOR (FSE) and Electron Spin Echo Envelope Modulation (ESEEM) are discussed in this thesis. The focal point of this thesis is the development and use of numerical methods in the analysis, simulation and interpretation of EMR experiments on radicals in solids to uncover the structure, the dynamics and the environment of the system. -
Fourier Transform Infrared (FTIR) Spectroscopy Analysis of Transformer Paper in Mineral Oil-Paper Composite Insulation Under Accelerated Thermal Aging
energies Article Fourier Transform Infrared (FTIR) Spectroscopy Analysis of Transformer Paper in Mineral Oil-Paper Composite Insulation under Accelerated Thermal Aging Abi Munajad * ID , Cahyo Subroto ID and Suwarno ID School of Electrical Engineering and Informatics, Institut Teknologi Bandung, Bandung 40132, Indonesia; [email protected] (C.S.); [email protected] (S.) * Correspondence: [email protected]; Tel.: +62-857-465-76059 Received: 26 December 2017; Accepted: 29 January 2018; Published: 4 February 2018 Abstract: Mineral oil is the most popular insulating liquid for high voltage transformers due to its function as a cooling liquid and an electrical insulator. Kraft paper has been widely used as transformer solid insulation for a long time already. The degradation process of transformer paper due to thermal aging in mineral oil can change the physical and chemical structure of the cellulose paper. Fourier transform infrared (FTIR) spectroscopy analysis was used to identify changes in the chemical structure of transformer paper aged in mineral oil. FTIR results show that the intensity of the peak absorbance of the O–H functional group decreased with aging but the intensity of the peak absorbance of the C–H and C=O functional groups increased with aging. Changes in the chemical structure of the cellulose paper during thermal aging in mineral oil can be analyzed by an oxidation process of the cellulose paper and the reaction process between the carboxylic acids in the mineral oil and the hydroxyl groups on the cellulose. The correlation between the functional groups and the average number of chain scissions of transformer paper gives initial information that the transformer paper performance can be identified by using a spectroscopic technique as a non-destructive diagnostic technique. -
Syllabus Chem 646
SYLLABUS CHEM 646 Course title and number Physical Organic Chemistry, CHEM 646 Term Fall 2019 Meeting times and location MWF 10:20 am – 11:10 am, Room: CHEM 2121 Course Description and Learning Outcomes Prerequisites: Organic Chemistry I and II or equivalent undergraduate organic chemistry courses. Physical Organic Chemistry (CHEM646) is a graduate/senior-undergrad level course of advanced organic chemistry. Physical organic chemistry refers to a discipline of organic chemistry that focuses on the relationship between chemical structure and property/reactivity, in particular, applying experimental and theoretical tools of physical chemistry to the study of organic molecules and reactions. Specific focal points of study include the bonding and molecular orbital theory of organic molecules, stability of organic species, transition states, and reaction intermediates, rates of organic reactions, and non-covalent aspects of solvation and intermolecular interactions. CHEM646 is designed to prepare students for graduate research on broadly defined organic chemistry. This course will provide the students with theoretical and practical frameworks to understand how organic structures impact the properties of organic molecules and the mechanism for organic reactions. By the end of this course, students should be able to: 1. Gain in-depth understanding of the nature of covalent bonds and non-covalent interactions 2. Use molecule orbital theory to interpret the property and reactivity of organic species. 3. Understand the correlation between the structure and physical/chemical properties of organic molecules, such as stability, acidity, and solubility. 4. Predict the reactivity of organic molecules using thermodynamic and kinetic analyses 5. Probe the mechanism of organic reactions using theoretical and experimental approaches. -
New Zealand Geothermal Association Presentation, 2013
The 1000 Project A microbial inventory of geothermal ecosystems New Zealand Geothermal Workshop 20 November 2012 Matthew Stott Craig Cary Melissa Climo Extremophile Research Group Dept. Biological Sciences Dept. Geothermal Sciences GNS Science University of Waikato GNS Science GNS Science Purpose of presentation • Microbiology: – The basics – A microbial world – Microbiology and geothermal systems • Geothermal microbiology – What little we know, and what we know we don’t know • The 1000 Project – A microbial bioinventory of NZ geothermal ecosystems GNS Science Microorganisms: single-celled organisms. Includes: Bacteria, Archaea and some eukaryotes ~ one billion (1 x 109) bacteria per gram of soil (1,000,000,000) ~ seven billion (7 x 109) humans on earth (7,051,000,000) ~ 4-6 x 1030 bacteria on the earth (4,000,000,000,000,000,000,000,000,000,000) This equals roughly half the world’s biomass GNS Science … into context …if we took 1 kg of soil: ~50 billion bacteria and arranged them end-to-end More than enough bacteria to stretch from Hamilton to and Tauranga (~100km) 2 μm (2/1000th of a millimetre) GNS Science …more fun with numbers In a standard Human: # cells in the human body: ~1 x 1013 (10,000,000,000,000) # bacteria in the human body: ~ 1 x 1014 (100,000,000,000,000) 10x more bacterial cells than human cells! (No matter whether you are the Prime Minister, the President, the Queen or the King!) GNS Science Bacteria=Germs=Bad!.... Really? • Bacteria are normally associated with disease But is this fair? • Microbes are EVERYWHERE and involved in practically EVERYTHING you can think of. -
OCN 401 Biogeochemical Systems
OCN 401 Biogeochemical Systems (Welcome!) Instructors: Brian Glazer Kathleen Ruttenberg Frank Sansone Chris Measures Textbook: Biogeochemistry, An analysis of Global Change by William H. Schlesinger & Emily S. Bernhardt Course Goals (SLOs) 1. Understand the underlying principles of biogeochemical cycling in aquatic and terrestrial Obj-1 systems. 2. Identify the major global pathways of bioactive elements and human perturbations of these pathways. 3. Develop / improve written and oral communication skills focused on biogeochemical processes. Obj-2 4. Achieve facility using electronic resources. Course Informational Resources 1. Syllabus with important due dates highlighted 2. Course Info Sheet – your ‘go to’ for ‘how to’ 3. Professor Office Hours (by appointment) 4. Writing Assistance. - Manoa Writing Center - Course hand-outs - Meet with professors LECTURES Lectures will generally be given using PowerPoint presentations. As a convenience to students, copies of the PowerPoint slides will generally be handed out in class. However, do not be fooled into thinking that the handouts are a substitute for careful note-taking in class. Much of the useful information in this class will be in the form of classroom discussion of the subject material. Thus, students are expected to attend all lectures and to actively participate in class discussions. GRADING Midterm Exam: 25% Final Exam: 25% Homework & Class Participation: 20% Term Paper & Presentation: 30% The Text Book Biogeochemistry, An analysis of Global Change by William H. Schlesinger & Emily S. Bernhardt • Read chapter before class • Subsections generally begin with an overview, and build from the general to the specific • Almost without exception, very specific examples are given from the literature. • Important to grasp the overview; understand but no need to memorize specific examples (with a few exceptions). -
Chapter 12. Decoding Organic Structures: the Functional Groups
CHAPTER 12. DECODING ORGANIC STRUCTURES: THE FUNCTIONAL GROUPS Functional Groups: The Key To Understanding Organic Molecules Since life on this planet is based on compounds of the element carbon, the study of these compounds, called organic chemistry, is an important area of chemistry.The ability of carbon to form single or multiple covalent bonds with itself to form chains of varying length, and even rings of varying size, leads to great versatility in the size and shape of carbon-based molecules. In this chapter we consider the bonds carbon forms with other elements, further expanding the number and types of possible compounds. The number of compounds formed by carbon is so great that it far exceeds the number of all the compounds formed by all the other elements. Some of these compounds contain thousands of atoms. How are we to begin to understand this myriad of complex molecules? The backbone of any organic compound is its carbon structure, whether in long chains, branched chains, rings, or some combination of these. In nature only a few elements other than carbon are found in most organic compounds: oxygen and nitrogen are the most common of these, along with sulfur and phosphorous. These tend to be found most commonly in only a few arrangements called functional groups. When the structure of an organic compound is drawn, frequently the carbon backbone is indicated only by a structural skeleton, with symbols for the carbon atoms left out. Usually hydrogen atoms attached to carbon atoms are left out, too. Only the atoms and bonds belonging to the functional groups are shown in detail.