Water Mediated Growth of Oriented Single Crystalline Srco3 Nanorod
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Download PDF About Minerals Sorted by Mineral Name
MINERALS SORTED BY NAME Here is an alphabetical list of minerals discussed on this site. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). APATITE Crystal system: hexagonal. Fracture: conchoidal. Color: red, brown, white. Hardness: 5.0. Luster: opaque or semitransparent. Specific gravity: 3.1. Apatite, also called cellophane, occurs in peridotites in eastern and western Kentucky. A microcrystalline variety of collophane found in northern Woodford County is dark reddish brown, porous, and occurs in phosphatic beds, lenses, and nodules in the Tanglewood Member of the Lexington Limestone. Some fossils in the Tanglewood Member are coated with phosphate. Beds are generally very thin, but occasionally several feet thick. The Woodford County phosphate beds were mined during the early 1900s near Wallace, Ky. BARITE Crystal system: orthorhombic. Cleavage: often in groups of platy or tabular crystals. Color: usually white, but may be light shades of blue, brown, yellow, or red. Hardness: 3.0 to 3.5. Streak: white. Luster: vitreous to pearly. Specific gravity: 4.5. Tenacity: brittle. Uses: in heavy muds in oil-well drilling, to increase brilliance in the glass-making industry, as filler for paper, cosmetics, textiles, linoleum, rubber goods, paints. Barite generally occurs in a white massive variety (often appearing earthy when weathered), although some clear to bluish, bladed barite crystals have been observed in several vein deposits in central Kentucky, and commonly occurs as a solid solution series with celestite where barium and strontium can substitute for each other. Various nodular zones have been observed in Silurian–Devonian rocks in east-central Kentucky. -
Adsorption of RNA on Mineral Surfaces and Mineral Precipitates
Adsorption of RNA on mineral surfaces and mineral precipitates Elisa Biondi1,2, Yoshihiro Furukawa3, Jun Kawai4 and Steven A. Benner*1,2,5 Full Research Paper Open Access Address: Beilstein J. Org. Chem. 2017, 13, 393–404. 1Foundation for Applied Molecular Evolution, 13709 Progress doi:10.3762/bjoc.13.42 Boulevard, Alachua, FL, 32615, USA, 2Firebird Biomolecular Sciences LLC, 13709 Progress Boulevard, Alachua, FL, 32615, USA, Received: 23 November 2016 3Department of Earth Science, Tohoku University, 2 Chome-1-1 Accepted: 15 February 2017 Katahira, Aoba Ward, Sendai, Miyagi Prefecture 980-8577, Japan, Published: 01 March 2017 4Department of Material Science and Engineering, Yokohama National University, 79-5 Tokiwadai, Hodogaya-ku, Yokohama This article is part of the Thematic Series "From prebiotic chemistry to 240-8501, Japan and 5The Westheimer Institute for Science and molecular evolution". Technology, 13709 Progress Boulevard, Alachua, FL, 32615, USA Guest Editor: L. Cronin Email: Steven A. Benner* - [email protected] © 2017 Biondi et al.; licensee Beilstein-Institut. License and terms: see end of document. * Corresponding author Keywords: carbonates; natural minerals; origins of life; RNA adsorption; synthetic minerals Abstract The prebiotic significance of laboratory experiments that study the interactions between oligomeric RNA and mineral species is difficult to know. Natural exemplars of specific minerals can differ widely depending on their provenance. While laboratory-gener- ated samples of synthetic minerals can have controlled compositions, they are often viewed as "unnatural". Here, we show how trends in the interaction of RNA with natural mineral specimens, synthetic mineral specimens, and co-precipitated pairs of synthe- tic minerals, can make a persuasive case that the observed interactions reflect the composition of the minerals themselves, rather than their being simply examples of large molecules associating nonspecifically with large surfaces. -
Strontium Chromate from Austria and France
Strontium Chromate from Austria and France Investigation Nos. 731-TA-1422-1423 (Preliminary) Publication 4836 October 2018 U.S. International Trade Commission Washington, DC 20436 U.S. International Trade Commission COMMISSIONERS David S. Johanson, Chairman Irving A. Williamson Meredith M. Broadbent Rhonda K. Schmidtlein Jason E. Kearns Catherine DeFilippo Director of Operations Staff assigned Kristina Lara, Investigator Samantha DeCarlo, Industry Analyst Tana von Kessler Economist Jennifer Brinckhaus, Accountant KaDeadra McNealy, Statistician David Goldfine, Attorney Douglas Corkran, Supervisory Investigator Address all communications to Secretary to the Commission United States International Trade Commission Washington, DC 20436 U.S. International Trade Commission Washington, DC 20436 www.usitc.gov Strontium Chromate from Austria and France Investigation Nos. 731-TA-1422-1423 (Preliminary) Publication 4836 October 2018 CONTENTS Page ....................................................................................................................... 1 ........................................................................................................ 3 Introduction ................................................................................................................ I‐1 Background ................................................................................................................................ I‐1 Statutory criteria and organization of the report .................................................................... -
4. CHEMICAL, PHYSICAL, and RADIOLOGICAL INFORMATION
STRONTIUM 189 4. CHEMICAL, PHYSICAL, and RADIOLOGICAL INFORMATION 4.1 CHEMICAL IDENTITY Strontium is an alkaline earth element in Group IIA of the periodic table. Because of its high reactivity, elemental (or metallic) strontium is not found in nature; it exists only as molecular compounds with other elements. The chemical information for elemental strontium and some of its compounds is listed in Table 4-1. Radioactive isotopes of strontium (e.g., 89Sr and 90Sr, see Section 4.2) are the primary cause of concern with regard to human health (see Chapter 3). 4.2 PHYSICAL, CHEMICAL, AND RADIOLOGICAL PROPERTIES The physical properties of strontium metal and selected strontium compounds are listed in Table 4-2. The percent occurrence of strontium isotopes and the radiologic properties of strontium isotopes are listed in Table 4-3. Strontium can exist in two oxidation states: 0 and +2. Under normal environmental conditions, only the +2 oxidation state is stable enough to be of practical importance since it readily reacts with both water and oxygen (Cotton and Wilkenson 1980; Hibbins 1997). There are 26 isotopes of strontium, 4 of which occur naturally. The four stable isotopes, 84Sr, 86Sr, 87Sr, and 88Sr, are sometimes referred to as stable strontium. The most important radioactive isotopes, 89Sr and 90Sr, are formed during nuclear reactor operations and during nuclear explosions by the nuclear fission of 235U, 238U, or 239Pu. For example, 235U is split into smaller atomic mass fragments such as 90Sr by a nuclear chain reaction initiated by high energy neutrons of approximately 1 million electron volts (or 1 MeV). -
Strontium-90 and Strontium-89: a Review of Measurement Techniques in Environmental Media
STRONTIUM-90 AND STRONTIUM-89: A REVIEW OF MEASUREMENT TECHNIQUES IN ENVIRONMENTAL MEDIA Robert J. Budnitz Lawrence Berkeley Laboratory University of California Berkeley, CA 91*720 1. IntroiUiction 2. Sources of Enivronmental Radiostrontium 3. Measurement Considerations a. Introduction b. Counting c. •»Sr/"Sr Separation 4. Chemical Techniques a. Air b. Water c. Milk d. Other Media e. Yttrium Recovery after Ingrowth f. Interferences S- Calibration Techniques h. Quality Control 5. Summary and Conclusions 6. Acknowli'J.jnent 7. References -NOTICE- This report was prepared as an account of worK sponsored by the United States Government. Neither the United States nor the United Slates Atomic Energy Commission, nor any of their employees, nor any of their contractors, subcontractors, or their employees, makes any wananty, express or implied, or asjumes any legal liabili:y or responsibility for the accuracy, com pleteness or usefulness of any Information, apparatus, J product or process disclosed, or represents that its use I would not infringe privately owned rights. Mmh li\ -1- 1. INTRODUCTION There are only two radioactive isotopes SrflO of strontium of significance in radiological measurements in the environment: strontium-89 Avg.jS energy 196-1 k«V and strontium-90. 100 Strontium-90 is the more significant from the point of view of environmental impact. 80 Energy keV 644 This is due mostly to its long half-life % Emission 100 (28.1 years). It is a pure beta emitter with 60 Typ* of only one decay mode, leading to yttrium-90 •mission by emission of a negative beta with HUBX * 40 h S46 keV. -
PUBLIC HEALTH STATEMENT Strontium CAS#: 7440-24-6
PUBLIC HEALTH STATEMENT Strontium CAS#: 7440-24-6 Division of Toxicology April 2004 This Public Health Statement is the summary External exposure to radiation may occur from chapter from the Toxicological Profile for natural or man-made sources. Naturally occurring strontium. It is one in a series of Public Health sources of radiation are cosmic radiation from space Statements about hazardous substances and their or radioactive materials in soil or building materials. health effects. A shorter version, the ToxFAQs™, is Man-made sources of radioactive materials are also available. This information is important found in consumer products, industrial equipment, because this substance may harm you. The effects atom bomb fallout, and to a smaller extent from of exposure to any hazardous substance depend on hospital waste and nuclear reactors. the dose, the duration, how you are exposed, personal traits and habits, and whether other If you are exposed to strontium, many factors chemicals are present. For more information, call determine whether you’ll be harmed. These factors the ATSDR Information Center at 1-888-422-8737. include the dose (how much), the duration (how _____________________________________ long), and how you come in contact with it. You must also consider the other chemicals you’re This public health statement tells you about exposed to and your age, sex, diet, family traits, strontium and the effects of exposure. lifestyle, and state of health. The Environmental Protection Agency (EPA) identifies the most serious hazardous waste sites in 1.1 WHAT IS STRONTIUM? the nation. These sites make up the National Priorities List (NPL) and are the sites targeted for Strontium is a natural and commonly occurring long-term federal cleanup activities. -
Electrochemical Separation and Purification of Yttrium-86
Radiochim. Acta 90, 225–228 (2002) by Oldenbourg Wissenschaftsverlag, München Electrochemical separation and purification of yttrium-86 By G. Reischl1,F.Rösch2 and H.-J. Machulla1 ,∗ 1 PET-Center, Division of Radiopharmacy, University Hospital Tübingen, D-72076 Tübingen, Germany 2 Institute of Nuclear Chemistry, University of Mainz, D-55099 Mainz, Germany (Received July 5, 2001; accepted in revised form October 24, 2001) Yttrium-86 / Electrolytic purification / radioactive rare earth nuclides onto a small tungsten cath- Electrochemical separation / Y-86 labeling ode was described in 1974 [6]. Recently, the electrochemical deposition of radionuclides of superheavy elements in de- pendence on electrode material and deposition potential was Summary. For quantitative determination of in vivo dosime- investigated [7]. An electrochemical method, based on a pro- try of 90Y-labeled radiotherapeuticals by means of PET, the cedure developed at Mainz [8, 9] to isolate 90Sr from a mix- positron emitting analogue yttrium-86 was produced at a low ture of 90Yand90Sr (c.a.) electrochemically, appeared very 86 86 energy (“medical”) cyclotron via the known Sr(p, n) Y 86 86 promising for isolating and purifying Y. reaction. Using 200 mg of SrCO3 (enrichment 95.6%) and protons of 15.1 MeV energy, average yields of 86Y of 48 ± 8MBq/µA h were produced. After dissolution of 86 86 Experimental SrCO3 in 3 ml of 0.6 N HNO3, Y was deposited in a simple and highly efficient electrochemical two-step procedure onto Materials a platinum cathode at 450 mA (= 20 mA/cm2). The isotope was finally removed from the electrode by 100–300 µlof Strontium-86 was supplied by Chemotrade, Germany, with . -
Strontium Minerals from Wise County, Virginia - an Update 1 2 D
Vol. 29 May 1983 No. 2 STRONTIUM MINERALS FROM WISE COUNTY, VIRGINIA - AN UPDATE 1 2 D. Allen Penick and Lynn D. Haynes The two principal minerals containing Strontianite crystallizes in the ortho- strontium, celestite and strontianite, have rhcanbic crystal system, and in Wise Funty been found in relative abundance in the area usually forms dull globular msses terrmnat- around East Stone Gap in Wise County, Vir- ed by acicular crystals. Crystals are gen- @ ginia. Celestite is strontium sulfate erally white and often can be seen as small (SrS04) and contains 56.4 percent strontium sprays attached to the celestite crystals. oxide. The name celestite is derived fm The mineral has a specific gravity of 3.7, the Latin mrd caelistis "of the sky" in hardness of 3.5 to 4, and good primtic reference to the typical blue color. Crys- cleavage. tals are predminantly blue and zoned in According to R. V. Dietrich (1970) and J. color but can also be red, green, or brown. A. Speer (1977) , strontium minerals have The mineral crystallizes in the ortho- been reported frcm seven different areas in rhcmbic crystal system and can fom thin to Virginia. These localities, all in the Val- thick heavy tabular crystals elongated along ley and Ridge Province, extend frcm Wise the b-axis; prismatic crystals elongated County in Southwest Virginia to Frederick along the a-axis; or equant crystals elon- County in the northwestern corner of the gated on the c-axis. Crystals can also have State (Figure 1). All exposures except two pyramidal faces with good terminations. -
Strontium Carbonate Solubility Data in Aqueous Mixtures of Monoethyleneglycol Under a Carbon Dioxide Atmosphere
Brazilian Journal ISSN 0104-6632 of Chemical Printed in Brazil www.scielo.br/bjce Engineering Vol. 35, No. 02, pp. 395 - 402, April - June, 2018 dx.doi.org/10.1590/0104-6632.20180352s20160355 STRONTIUM CARBONATE SOLUBILITY DATA IN AQUEOUS MIXTURES OF MONOETHYLENEGLYCOL UNDER A CARBON DIOXIDE ATMOSPHERE Deborah C. de Andrade1,*, Naíra S. de A. Maniçoba1, Rony O. Sant'ana1, Fedra A.V. Ferreira1, Camila S. Figueiredo2, Jailton F. Nascimento2, Leonardo S. Pereira2 and Osvaldo Chiavone-Filho1 1UFRN. Campus Universitário. Departamento de Engenharia Química. Lagoa Nova. Natal – RN – Brazil, ZIP 59066-800. 2PETROBRAS/CENPES/PDEP/TPP. Av. Horácio Macedo, 950 – Cidade Universitária - Ilha do Fundão. Rio de Janeiro – RJ – Brazil, ZIP 219141-915. (Submitted: June 1, 2016; Revised: March 20, 2017; Accepted: April 5, 2017) Abstract - In order to inhibit natural gas hydrate formation, monoethyleneglycol (MEG) is usually injected into producing well heads. The MEG regeneration process is continuously performed at the platform. Scaling problems usually occur due to the presence of chlorides and carbonates. This work presents salt solubility data for the aqueous system with strontium carbonate, MEG and carbon dioxide. A specific analytical method was developed. Thus, experimental data for strontium carbonate (SrCO3) solubility at various carbon dioxide pressures are reported. Solubilities of SrCO3 in water were measured from 760 to 1610 mmHg at 278.15. 288.15. 298.15 and 323.15 K. For the mixed solvent (ms) conditions, solubilities were measured at 298.15 K and four isobars, i.e., 760, 1210, 1410 and 1520 mmHg. Experimental data were correlated and demonstrated to be accurate for thermodynamic modeling and process simulation. -
Appendix a of Final Environmental Impact Statement for a Geologic Repository for the Disposal of Spent Nuclear Fuel and High-Lev
Appendix A Inventory and Characteristics of Spent Nuclear Fuel, High-Level Radioactive Waste, and Other Materials Inventory and Characteristics of Spent Nuclear Fuel, High-Level Radioactive Waste, and Other Materials TABLE OF CONTENTS Section Page A. Inventory and Characteristics of Spent Nuclear Fuel, High-Level Radioactive Waste, and Other Materials ................................................................................................................................. A-1 A.1 Introduction .............................................................................................................................. A-1 A.1.1 Inventory Data Summary .................................................................................................... A-2 A.1.1.1 Sources ......................................................................................................................... A-2 A.1.1.2 Present Storage and Generation Status ........................................................................ A-4 A.1.1.3 Final Waste Form ......................................................................................................... A-6 A.1.1.4 Waste Characteristics ................................................................................................... A-6 A.1.1.4.1 Mass and Volume ................................................................................................. A-6 A.1.1.4.2 Radionuclide Inventories ...................................................................................... A-8 A.1.1.4.3 -
Ferricerite-(La) (La, Ce, Ca)9Fe (Sio4)3(Sio3oh)4(OH)3
3+ Ferricerite-(La) (La, Ce, Ca)9Fe (SiO4)3(SiO3OH)4(OH)3 Crystal Data: Hexagonal. Point Group: 3m. Forms boxwork-like aggregates of equant to tabular crystals flattened on [00*1] to 2 mm with dominant rhombohedral and pinacoidal faces, as pseudomorphs after an unidentified hexagonal prismatic mineral. Physical Properties: Cleavage: None. Tenacity: Brittle. Fracture: Conchoidal. Hardness = 5 D(meas.) = 4.7(1) D(calc.) = 4.74 Optical Properties: Translucent. Color: Light yellow to pinkish brown. Streak: White. Luster: Vitreous. Optical Class: Uniaxial (+). ω = 1.810(5) ε = 1.820(5) Cell Data: Space Group: R3c. a = 10.7493(6) c = 38.318(3) Z = 6 X-ray Powder Pattern: Mt. Yuksporr, Khibina massif, Kola Peninsula, Russia. 2.958 (100), 3.47 (40), 3.31(38), 2.833 (37), 2.689 (34), 1.949 (34), 3.53 (26) Chemistry: (1) (2) La2O3 37.57 CaO 5.09 Ce2O3 23.67 Fe2O3 1.40 Pr2O3 0.61 MgO 0.51 Nd2O3 1.48 SiO2 22.38 Sm2O3 0.10 P2O5 0.63 Gd2O3 0.24 H2O 3.20 SrO 1.97 Total 98.85 (1) Mt. Yuksporr, Khibina massif, Kola Peninsula, Russia; average electron microprobe analysis supplemented by IR spectroscopy, H2O by Penfield method; corresponds to (La4.23Ce2.65Ca1.37Sr0.35 Nd0.16Pr0.07Gd0.02Sm0.01)Σ=8.86(Fe0.32Ca0.30Mg0.23)Σ=0.85[SiO4]3[(Si0.84P0.16)Σ=1.00O3(OH)]4(OH)2.78. Mineral Group: Cerite supergroup, cerite group. Occurrence: A late-stage, low-temperature secondary phase in a symmetrically zoned, aegirine- natrolite-microcline vein in gneissose foyaite. -
The Role of Calcium and Strontium As the Most Dominant Elements During
crystals Article The Role of Calcium and Strontium as the Most Dominant Elements during Combinations of Different Alkaline Earth Metals in the Synthesis of Crystalline Silica-Carbonate Biomorphs Mayra Cuéllar-Cruz 1,2,* and Abel Moreno 2,* 1 Departamento de Biología, División de Ciencias Naturales y Exactas, Campus Guanajuato, Universidad de Guanajuato, Noria Alta S/N, Col. Noria Alta, Guanajuato C.P. 36050, Mexico 2 Instituto de Química, Universidad Nacional Autónoma de México, Av. Universidad 3000, Ciudad Universitaria, Ciudad de México 04510, Mexico * Correspondence: [email protected] (M.C.-C.); [email protected] (A.M.) Received: 22 June 2019; Accepted: 22 July 2019; Published: 24 July 2019 Abstract: The origin of life from the chemical point of view is an intriguing and fascinating topic, and is of continuous interest. Currently, the chemical elements that are part of the different cellular types from microorganisms to higher organisms have been described. However, although science has advanced in this context, it has not been elucidated yet which were the first chemical elements that gave origin to the first primitive cells, nor how evolution eliminated or incorporated other chemical elements to give origin to other types of cells through evolution. Calcium, barium, and strontium silica-carbonates have been obtained in vitro and named biomorphs, because they mimic living organism structures. Therefore, it is considered that these forms can resemble the first structures that were part of primitive organisms. Hence, the objective of this work was to synthesize biomorphs starting with different mixtures of alkaline earth metals—beryllium (Be2+), magnesium (Mg2+), calcium (Ca2+), barium (Ba2+), and strontium (Sr2+)—in the presence of nucleic acids, RNA and genomic DNA (gDNA).