Beneficial Uses of Production of Isotopes
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Stable Isotopes of Cobalt Properties of Cobalt
Stable Isotopes of Cobalt Isotope Z(p) N(n) Atomic Mass Natural Abundance Nuclear Spin Co-59 27 32 58.93320 100.00% 7/2- Cobalt was discovered in 1735 by Georg Brandt. Its name derives from the German word kobald, meaning "goblin" or "evil spirit." Minerals containing cobalt were used by the early civilizations of Egypt and Mesopotamia for coloring glass deep blue. Cobalt oxide is used today to add a pink or blue color to glass. It is also an important trace element in soils and necessary for animal nutrition. The most important modern use of cobalt is in the manufacture of various wear-resistant and superalloys. Its alloys have shown high resistance to corrosion and oxidation at high temperatures. Radioactive Cobalt-60 is used in radiography and in the sterilization of food. A silvery-white, shining, hard, ductile, somewhat malleable metal, cobalt is also ferromagnetic, with permeability two-thirds that of iron. It has exceptional magnetic properties in alloys. It is attached by dilute hydrochloric and sulfuric acids. It corrodes readily in air, and it has unusual coordinating properties, especially the trivalent ion. It is noncombustible except in powder form. Cobalt occurs in two allotropic modifications over a wide range of temperatures: the crystalline close-packed- hexagonal form is known as the alpha form, which turns into the beta (or gamma) form above 417 ºC. In finely powdered form, cobalt ignites spontaneously in air. Reactions with acetylene and bromine pentafluoride proceed to incandescence and can become violent. The metal is moderately toxic by ingestion. Inhalation of dusts can damage lungs. -
Annual Report 1951 National Bureau of Standards
Annual Report 1951 National Bureau of Standards Miscellaneous Publication 204 UNITED STATES DEPARTMENT OF COMMERCE Charles Sawyer, Secretary NATIONAL BUREAU OF STANDARDS A. V. Astint, Director Annual Report 1951 National Bureau of Standards For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 2 5, D. C. Price 50 cents CONTENTS Page 1. General Review 1 2. Electricity 16 Beam intensification in a high-voltage oscillograph 17, Low-temperature dry cells 17, High-rate batteries 17, Battery additives 18. 3. Optics and Metrology 18 The kinorama 19, Measurement of visibility for aircraft 20, Antisubmarine aircraft searchlights 20, Resolving power chart 20, Refractivity 21, Thermal expansivity of aluminum alloys 21. 4. Heat and Power . 21 Thermodynamic properties of materials 22, Synthetic rubber and other high polymers 23, Combustors for jet engines 24, Temperature and composition of flames 25, Engine "knock" 25, Low-temperature physics 26, Medical physics instrumentation 28. 5. Atomic and Radiation Physics 28 Atomic standard of length 29, Magnetic moment of the proton 29, Spectra of artificial elements 31, Photoconductivity of semiconductors 31, Radiation detecting instruments 32, Protection against radiation 32, X-ray equipment 33, Atomic and molecular ions 35, Electron physics 35, Tables of nuclear data 35, Atomic energy levels 36. 6. Chemistry 36 Radioactive carbohydrates 36, Dextran as a substitute for blood plasma 37, Acidity and basicity in organic solvents 37, Interchangeability of fuel gases 38, Los Angeles "smog" 39, Infrared spectra of alcohols 39, Electrodeposi- tion 39, Development of analytical methods 40, Physical constants 42. 7. Mechanics 42 Turbulent flow 43, Turbulence at supersonic speeds 43, Dynamic properties of materials 43, High-frequency vibrations 44, Hearing loss 44, Physical properties by sonic methods 44, Water waves 46, Density currents 46, Precision weighing 46, Viscosity of gases 46, Evaporated thin films 47. -
The Dole Effect and Its Variations During the Last 130,000 Years As Measured in the Vostok Ice Core
GLOBAL BIOGEOCHEMICAL CYCLES, VOL. 8, NO. 3, PAGES 363-376, SEPTEMBER 1994 The Dole effect and its variations during the last 130,000 years as measured in the Vostok ice core Michael Bender • and Todd Sowers 2 GraduateSchool of Oceanography,University of RhodeIsland, Kingston Laurent Labeyrie Centredes Faibles Radioactivites, Centre National de la RechercheScientifique, Commissariat a L'EnergieAtomique, Gif-sur- Yvette, France Abstract. We review the currentunderstanding of the Dole effect (the observeddifference between the •5180of atmospheric0 2 andthat of seawater)and its causes, extend the record of variationsin theDole effectback to 130kyr before present using data on the •5180 of 0 2obtained from studying the Vostok ice core(Sowers et al., 1993), anddiscuss the significanceof temporalvariations. The Dole effectreflects oxygenisotope fractionation during photosynthesis, respiration, and hydrologic processes (evaporation, precipitation,and evapotranspiration). Our bestprediction of the present-dayDole effect,+20.8 %0,is considerablylower thanthe observedvalue, + 23.5 %0,and we discusspossible causes of this discrepancy. During the past 130 kyr, the Dole effecthas been 0.05 %0lower thanthe present value, on average.The standarddeviation of the Dole effect from the meanhas been only _+0.2 %0,and the Dole effect is nearly unchangedbetween glacial maxima and interglacial periods. The smallvariability in theDole effect suggeststhat relative rates of primaryproduction in theland and marine realms have been relatively constant.Most periodicvariability in the Dole effectis in the precessionband, suggesting that changes in thisglobal biogeochemical term reflects variations in low-latitudeland hydrology and productivity or possiblyvariability in low-latitudeoceanic productivity. Introduction they can potentially be made to do so. Ice core reconstructionsof the concentrationsof bioactivegases in air Our understanding of the response of the biosphere to provide an integratedglobal signal which complementsthe Pleistoceneclimate change is actually quite limited. -
Chapter 2 Atoms, Molecules and Ions
Chapter 2 Atoms, Molecules and Ions PRACTICING SKILLS Atoms:Their Composition and Structure 1. Fundamental Particles Protons Electrons Neutrons Electrical Charges +1 -1 0 Present in nucleus Yes No Yes Least Massive 1.007 u 0.00055 u 1.007 u 3. Isotopic symbol for: 27 (a) Mg (at. no. 12) with 15 neutrons : 27 12 Mg 48 (b) Ti (at. no. 22) with 26 neutrons : 48 22 Ti 62 (c) Zn (at. no. 30) with 32 neutrons : 62 30 Zn The mass number represents the SUM of the protons + neutrons in the nucleus of an atom. The atomic number represents the # of protons, so (atomic no. + # neutrons)=mass number 5. substance protons neutrons electrons (a) magnesium-24 12 12 12 (b) tin-119 50 69 50 (c) thorium-232 90 142 90 (d) carbon-13 6 7 6 (e) copper-63 29 34 29 (f) bismuth-205 83 122 83 Note that the number of protons and electrons are equal for any neutral atom. The number of protons is always equal to the atomic number. The mass number equals the sum of the numbers of protons and neutrons. Isotopes 7. Isotopes of cobalt (atomic number 27) with 30, 31, and 33 neutrons: 57 58 60 would have symbols of 27 Co , 27 Co , and 27 Co respectively. Chapter 2 Atoms, Molecules and Ions Isotope Abundance and Atomic Mass 9. Thallium has two stable isotopes 203 Tl and 205 Tl. The more abundant isotope is:___?___ The atomic weight of thallium is 204.4 u. The fact that this weight is closer to 205 than 203 indicates that the 205 isotope is the more abundant isotope. -
Compilation of Minimum and Maximum Isotope Ratios of Selected Elements in Naturally Occurring Terrestrial Materials and Reagents by T
U.S. Department of the Interior U.S. Geological Survey Compilation of Minimum and Maximum Isotope Ratios of Selected Elements in Naturally Occurring Terrestrial Materials and Reagents by T. B. Coplen', J. A. Hopple', J. K. Bohlke', H. S. Reiser', S. E. Rieder', H. R. o *< A R 1 fi Krouse , K. J. R. Rosman , T. Ding , R. D. Vocke, Jr., K. M. Revesz, A. Lamberty, P. Taylor, and P. De Bievre6 'U.S. Geological Survey, 431 National Center, Reston, Virginia 20192, USA 2The University of Calgary, Calgary, Alberta T2N 1N4, Canada 3Curtin University of Technology, Perth, Western Australia, 6001, Australia Institute of Mineral Deposits, Chinese Academy of Geological Sciences, Beijing, 100037, China National Institute of Standards and Technology, 100 Bureau Drive, Stop 8391, Gaithersburg, Maryland 20899 "institute for Reference Materials and Measurements, Commission of the European Communities Joint Research Centre, B-2440 Geel, Belgium Water-Resources Investigations Report 01-4222 Reston, Virginia 2002 U.S. Department of the Interior GALE A. NORTON, Secretary U.S. Geological Survey Charles G. Groat, Director The use of trade, brand, or product names in this report is for identification purposes only and does not imply endorsement by the U.S. Government. For additional information contact: Chief, Isotope Fractionation Project U.S. Geological Survey Mail Stop 431 - National Center Reston, Virginia 20192 Copies of this report can be purchased from: U.S. Geological Survey Branch of Information Services Box 25286 Denver, CO 80225-0286 CONTENTS Abstract...................................................... -
Boron and Oxygen in Cometary Particles: O. J
79th Annual Meeting ofBORON the Meteoritical AND OXYGEN Society IN COMETARY (2016) PARTICLES: O. J. Stenzel and J. Paquette 6380.pdf BORON AND OXYGEN IN COMETARY PARTICLES. Oliver J. Stenzel and J. Paquette and the COSIMA Team, Max Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, D-37077 Göttingen, Germany, [email protected]. Introduction: The cometary dust experiment COSIMA is a time of flight secondary ion mass spectrometer (ToF-SIMS) on board the Rosetta space craft. Since August 2014, COSIMA has been collecting dust from the inner coma of 67P/Churyumov-Gerasimenko [1], [2]. The particles have been analyzed for their size distribution, particle flux and morphology [3], [4]. [5] as well as [1] found high amounts of sodium in the particles using the high resolution ToF-SIMS. In this work we present some of our results for boron and oxygen and compare with meteorite samples analyzed in the lab with the COSIMA reference model (RM). Varying degrees of oxygen isotopic fractionation have long been known in solar system solids such as the terrestrial planets, chondrules, and CAIs (calcium-aluminum-rich inclusions) [6] and, more recently, in the sun [7]. A value has also been measured for the cometary gas from comet 67P [8]. Evidence for the presence of CAIs (which can have quite different oxygen isotopic content than the terrestrial value) has already been seen in this comet [9]. Thus a comparison of the isotopic ratio of a cometary dust particle may shed light on the history of Churyumov-Gerasimenko. Data and Methods: COSIMA produces high resolution mass spectra (1400 at 100 u). -
Investigation of Nitrogen Cycling Using Stable Nitrogen and Oxygen Isotopes in Narragansett Bay, Ri
University of Rhode Island DigitalCommons@URI Open Access Dissertations 2014 INVESTIGATION OF NITROGEN CYCLING USING STABLE NITROGEN AND OXYGEN ISOTOPES IN NARRAGANSETT BAY, RI Courtney Elizabeth Schmidt University of Rhode Island, [email protected] Follow this and additional works at: https://digitalcommons.uri.edu/oa_diss Recommended Citation Schmidt, Courtney Elizabeth, "INVESTIGATION OF NITROGEN CYCLING USING STABLE NITROGEN AND OXYGEN ISOTOPES IN NARRAGANSETT BAY, RI" (2014). Open Access Dissertations. Paper 209. https://digitalcommons.uri.edu/oa_diss/209 This Dissertation is brought to you for free and open access by DigitalCommons@URI. It has been accepted for inclusion in Open Access Dissertations by an authorized administrator of DigitalCommons@URI. For more information, please contact [email protected]. INVESTIGATION OF NITROGEN CYCLING USING STABLE NITROGEN AND OXYGEN ISOTOPES IN NARRAGANSETT BAY, RI BY COURTNEY ELIZABETH SCHMIDT A DISSERTATION SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN OCEANOGRAPHY UNIVERSITY OF RHODE ISLAND 2014 DOCTOR OF PHILOSOPHY DISSERTATION OF COURTNEY ELIZABETH SCHMIDT APPROVED: Thesis Committee: Major Professor Rebecca Robinson Candace Oviatt Arthur Gold Nassar H. Zawia DEAN OF THE GRADUATE SCHOOL UNIVERSITY OF RHODE ISLAND 2014 ABSTRACT Estuaries regulate nitrogen (N) fluxes transported from land to the open ocean through uptake and denitrification. In Narragansett Bay, anthropogenic N loading has increased over the last century with evidence for eutrophication in some regions of Narragansett Bay. Increased concerns over eutrophication prompted upgrades at wastewater treatment facilities (WWTFs) to decrease the amount of nitrogen discharged. The upgrade to tertiary treatment – where bioavailable nitrogen is reduced and removed through denitrification – has occurred at multiple facilities throughout Narragansett Bay’s watershed. -
Załącznik Nr 3 Do Wniosku O Przeprowadzenie Postępowania Habilitacyjnego
Załącznik nr 3 do wniosku o przeprowadzenie postępowania habilitacyjnego Author's review of his own writings 1. Jan Kurpeta 2. Posiadane dyplomy, stopnie naukowe Degree of Doctor of Philosophy in physics, University of Warsaw, Faculty of Physics, year 1999, title of dissertation: „Properties of the neutron-rich nuclei at the edge of known nuclei area.” Master of Science and Engineering, Warsaw University of Technology, Faculty of Technical Physics and Applied Mathematics, year 1993, title of master's thesis: „Influence of nucleon effective mass on single particle motion in the deformed nuclei.” 3. Informacje o dotychczasowym zatrudnieniu w jednostkach naukowych University of Warsaw, Faculty of Physics, Institute of Experimental Physics, Nuclear Spectroscopy Division, assistant professor since15 February 2001 University of Leuven (Belgium), Instituut voor Kern- en Stralingsfysica, post-doc position from 1 September 1998 to 31 October 1999 University of Jyväskylä (Finland), Faculty of Physics, scholarship from Center for International Mobility, PhD studies from 3 February to 15 December 1995 University of Warsaw, Faculty of Physics, Institute of Experimental Physics, Nuclear Spectroscopy Division, PhD studies from October 1993 to September 1998 Space Research Center Polish Academy of Sciences in Warsaw, Department of Planetary Geodesy, part time job for 6 months in 1993 1 4. Wskazanie osiągnięcia* wynikającego z art. 16 ust. 2 ustawy z dnia 14 marca 2003 r. o stopniach naukowych i tytule naukowym oraz o stopniach i tytule w zakresie sztuki (Dz. U. nr 65, poz. 595 ze zm.): a) tytuł osiągnięcia naukowego Structure of exotic, neutron-rich fission fragments of mass around A = 110. b) Jednotematyczny cykl publikacji przedstawiających osiągnięcie naukowe [A1] J. -
Analytical Developments in the Measurements of Boron, Nitrate
XA9848324 ANALYTICAL DEVELOPMENTS IN THE MEASUREMENTS OF BORON, NITRATE, PHOSPHATE AND SULPHATE ISOTOPES AND CASE EXAMPLES OF DISCRIMINATION OF NITROGEN AND SULPHUR SOURCES IN POLLUTION STUDIES J. AGGARWAL, D.S. SHEPPARD Institute of Geological & Nuclear Sciences, Lower Hutt B.W. ROBINSON Wairakei Research Centre, Institute of Geological & Nuclear Sciences, Taupo New Zealand Abstract - Methods are documented for the analysis of B isotopes, O and N isotopes in nitrates. B isotopes can be measured by negative ion thermal ionisation mass spectrometry. Nitrate is recovered from groundwaters by ion exchange and the resulting silver nitrate combusted for stable isotope gas analysis. Oxygen isotope analysis of phosphates can be determined by generating and analysing CO2 gas from the combustion of silver phosphate produced from aqueous samples. Sulphate in ground and surface waters can be separated and concentrated by ion exchange and precipitated as barium sulphate. This is reacted with graphite to yield CO2 and CO, the latter being spark discharged to CO2 and the total CO2 measured for oxygen isotope analysis. Barium sulphide from this reaction is converted to silver sulphide which is reacted with cuprous oxide to give SO2 gas for sulphur isotope measurements. A case study of the semi-rural Manakau area in New Zealand was conducted to see if nitrate isotopes could be used to detect the source of nitrate contamination (groundwater nitrate <0.5 to 11.3 mg/L NO'3-N). Nitrogen isotope (+4 to +12%o) coupled with oxygen isotope measurements (+5 to +9%o) demonstrated that the nitrogen is not sourced from fertilisers but from some combination of septic tank and animal waste. -
High Specific Radioactivities of Cobalt, Platinum and Iridium From
Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1951 High specific ar dioactivities of cobalt, platinum and iridium from photonuclear reactions Darleane Christian Iowa State College Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Physical Chemistry Commons Recommended Citation Christian, Darleane, "High specific ar dioactivities of cobalt, platinum and iridium from photonuclear reactions " (1951). Retrospective Theses and Dissertations. 13387. https://lib.dr.iastate.edu/rtd/13387 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. NOTE TO USERS This reproduction is the best copy available. UMI HIGH SPECIFIC MDIOACTIVITI OF COBALT, PLATIirOl-I Mm IRIDIUIl FROM PHOTOirUCL:mR R3ACTI0KS by Darloana Christian A Dissertation S-ubmitted to the Graduate Faculty in Partial Fulfillmant of The Requiramants for the Degrea of DOCTOR OP PHILOflOPIir Major Subject: Physical Chamistry Approveds Signature was redacted for privacy. In Cha3?i¥ of tlay6r' Worls: Signature was redacted for privacy. Heaa of tiajor Departraent ^ Signature was redacted for privacy. Daan of Graduate Collage loi/a State College 1951 UMI Number: DP12638 INFORMATION TO USERS The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleed-through, substandard margins, and improper alignment can adversely affect reproduction. -
Isotopes Are Atoms with the Same # of Protons (Making Them the SAME ELEMENT), but Have a Different # of Neutrons
Each element has a unique # of protons. So…EVERY SINGLE ATOM of that element MUST HAVE the SAME number of protons, ALWAYS! This is the reason why each element has a unique Atomic Number that never changes! Isotopes are atoms with the same # of protons (making them the SAME ELEMENT), but have a different # of neutrons. Having different # of neutrons for the same element means that the isotopes will have different mass numbers, too! There are 3 isotopes of oxygen: 8 8 8 O8 O9 O10 neutronsOxygen neutronsOxygen neutronsOxygen ALL oxygen16 isotopes 17have an atomic 18# of 8, so they all have 8 protons! How many protons does each isotope have? How many neutrons does each isotope have? There are 3 isotopes of carbon: 6 6 6 C6 C7 C8 neutronsCarbon neutronsCarbon neutronsCarbon ALL carbon12 isotopes 13have an atomic #14 of 6, so they all have 6 protons! How many protons does each isotope have? How many neutrons does each isotope have? Atomic Masses on the periodic table are normally decimals. WHY?? Atomic Masses are decimals because it is an AVERAGE mass of all of the element’s isotopes. Some isotopes are more common than others, so this is a weighted average. 5 So the Mass # from the periodic table is B always closest to the most common Boron isotope’s mass. 10.81 In the universe, there are MUCH more carbon-12 atoms that exist than carbon-13 and carbon-14 atoms. 6 C Carbon- 12 Carbon 12.01 When you find the weighted average of the masses of the carbon isotopes, the average will be closest to 12! The Atomic Mass of calcium is 40.08. -
Oxygen Isotopes in Nature and in the Laboratory Author(S): Harold C
Oxygen Isotopes in Nature and in the Laboratory Author(s): Harold C. Urey Source: Science, New Series, Vol. 108, No. 2810 (Nov. 5, 1948), pp. 489-496 Published by: American Association for the Advancement of Science Stable URL: http://www.jstor.org/stable/1677444 Accessed: 22/10/2008 09:24 Your use of the JSTOR archive indicates your acceptance of JSTOR's Terms and Conditions of Use, available at http://www.jstor.org/page/info/about/policies/terms.jsp. JSTOR's Terms and Conditions of Use provides, in part, that unless you have obtained prior permission, you may not download an entire issue of a journal or multiple copies of articles, and you may use content in the JSTOR archive only for your personal, non-commercial use. Please contact the publisher regarding any further use of this work. Publisher contact information may be obtained at http://www.jstor.org/action/showPublisher?publisherCode=aaas. Each copy of any part of a JSTOR transmission must contain the same copyright notice that appears on the screen or printed page of such transmission. JSTOR is a not-for-profit organization founded in 1995 to build trusted digital archives for scholarship. We work with the scholarly community to preserve their work and the materials they rely upon, and to build a common research platform that promotes the discovery and use of these resources. For more information about JSTOR, please contact [email protected]. American Association for the Advancement of Science is collaborating with JSTOR to digitize, preserve and extend access to Science. http://www.jstor.org Oxygen Isotopes in Nature and in the Laboratory Harold C.