Ferromagnetic Minerals
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Podiform Chromite Deposits—Database and Grade and Tonnage Models
Podiform Chromite Deposits—Database and Grade and Tonnage Models Scientific Investigations Report 2012–5157 U.S. Department of the Interior U.S. Geological Survey COVER View of the abandoned Chrome Concentrating Company mill, opened in 1917, near the No. 5 chromite mine in Del Puerto Canyon, Stanislaus County, California (USGS photograph by Dan Mosier, 1972). Insets show (upper right) specimen of massive chromite ore from the Pillikin mine, El Dorado County, California, and (lower left) specimen showing disseminated layers of chromite in dunite from the No. 5 mine, Stanislaus County, California (USGS photographs by Dan Mosier, 2012). Podiform Chromite Deposits—Database and Grade and Tonnage Models By Dan L. Mosier, Donald A. Singer, Barry C. Moring, and John P. Galloway Scientific Investigations Report 2012-5157 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 This report and any updates to it are available online at: http://pubs.usgs.gov/sir/2012/5157/ For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Suggested citation: Mosier, D.L., Singer, D.A., Moring, B.C., and Galloway, J.P., 2012, Podiform chromite deposits—database and grade and tonnage models: U.S. -
The Sedimentology and Mineralogy of the River Uranium Deposit Near Phuthaditjhaba, Qwa-Qwa
PER-74 THE SEDIMENTOLOGY AND MINERALOGY OF THE RIVER URANIUM DEPOSIT NEAR PHUTHADITJHABA, QWA-QWA by J. P. le Roux NUCLEAR DEVELOPMENT CORPORATION OF SOUTH AFRICA (PTY) LTD NUCOR PRIVATE MO X2M PRETORIA 0001 m•v OCTOBER 1982 PER-74- THE SEDIMENTOLOGY AND MINERALOGY OF THE RIVER URANIUM DEPOSIT NEAR PHUTHADITJHABA, QWA-QWA b/ H.J. Brynard * J.P. le Roux * * Geology Department POSTAL ADDRESS: Private Bag X256 PRETORIA 0001 PELINDABA August 1982 ISBN 0-86960-747-2 CONTENTS SAMEVATTING ABSTRACT 1. INTRODUCTION 1 2. SEDIMENTOLOGY 1 2.1 Introduction 1 2.2 Depositional Environment 2 2.2.1 Palaeocurrents 2 2.2.2 Sedimentary structures and vertical profiles 5 2.2.3 Borehole analysis 15 2.3 Uranium Mineralisation 24 2.4 Conclusions and Recommendations 31 3. MINERALOGY 33 3.1 Introduction 33 3.2 Procedure 33 3.3 Terminology Relating to Carbon Content 34 3.4 Petrographic Description of the Sediments 34 3.5 Uranium Distribution 39 3.6 Minor and Trace Elements 42 3.7 Petrogenesis 43 3.8 Extraction Metallurgy 43 4. REFERENCES 44 PER-74-ii SAMEVATTING 'n Sedimentologiese en mineralogiese ondersoek is van die River-af setting uittigevoer wat deur Mynboukorporasie (Edms) Bpk in Qwa-Qwa, 15 km suaidwes van Phu triad it jnaba, ontdek is. Die ertsliggaam is in íluviale sand-steen van die boonste Elliot- formasie geleë. Palleostroomrigtings dui op 'n riviersisteem met 'n lae tot baie lae 3d.nuositeit en met "h vektor-gemiddelde aanvoer- rigting van 062°. 'n Studie van sedimentere strukture en korrelgroottes in kranssnitte is deuir to ontleding van boorgatlogs aangevul wat die sedimentêre afsettingsoragewing as h gevlegte stroom van die Donjek-tipe onthul. -
Canted Ferrimagnetism and Giant Coercivity in the Non-Stoichiometric
Canted ferrimagnetism and giant coercivity in the non-stoichiometric double perovskite La2Ni1.19Os0.81O6 Hai L. Feng1, Manfred Reehuis2, Peter Adler1, Zhiwei Hu1, Michael Nicklas1, Andreas Hoser2, Shih-Chang Weng3, Claudia Felser1, Martin Jansen1 1Max Planck Institute for Chemical Physics of Solids, Dresden, D-01187, Germany 2Helmholtz-Zentrum Berlin für Materialien und Energie, Berlin, D-14109, Germany 3National Synchrotron Radiation Research Center (NSRRC), Hsinchu, 30076, Taiwan Abstract: The non-stoichiometric double perovskite oxide La2Ni1.19Os0.81O6 was synthesized by solid state reaction and its crystal and magnetic structures were investigated by powder x-ray and neutron diffraction. La2Ni1.19Os0.81O6 crystallizes in the monoclinic double perovskite structure (general formula A2BB’O6) with space group P21/n, where the B site is fully occupied by Ni and the B’ site by 19 % Ni and 81 % Os atoms. Using x-ray absorption spectroscopy an Os4.5+ oxidation state was established, suggesting presence of about 50 % 5+ 3 4+ 4 paramagnetic Os (5d , S = 3/2) and 50 % non-magnetic Os (5d , Jeff = 0) ions at the B’ sites. Magnetization and neutron diffraction measurements on La2Ni1.19Os0.81O6 provide evidence for a ferrimagnetic transition at 125 K. The analysis of the neutron data suggests a canted ferrimagnetic spin structure with collinear Ni2+ spin chains extending along the c axis but a non-collinear spin alignment within the ab plane. The magnetization curve of La2Ni1.19Os0.81O6 features a hysteresis with a very high coercive field, HC = 41 kOe, at T = 5 K, which is explained in terms of large magnetocrystalline anisotropy due to the presence of Os ions together with atomic disorder. -
CERI 7022/8022 Global Geophysics Spring 2016
FerrimagnetismI I Recall three types of magnetic properties of materials I Diamagnetism I Paramagnetism I Ferromagnetism I Anti-ferromagnetism I Parasitic ferromagnetism I Ferrimagnetism I Ferrimagnetism I Spinel structure is one of the common crystal structure of rock-forming minerals. I Tetrahedral and octahedral sites form two sublattices. 2+ 3+ I Fe in 1/8 of tetrahedral sites, Fe in 1/2 of octahedral sites. FerrimagnetismII I xmujpkc.xmu.edu.cn/jghx/source/chapter9.pdf Ferrimagnetism III I www.tf.uni-kiel.de/matwis/amat/def_en/kap_2/basics/b2_1_6.html I Anti-spinel structure of the most common iron oxides 3+ 3+ 2+ I Fe in 1/8 tetrahedral sites, (Fe , Fe ) in 1/2 of octahedral sites. FerrimagnetismIV I Indirect exchange involves antiparallel and unequal magnetization of the sublattices, a net spontaneous magnetization appears. This phenomenon is called ferrimagnetism. I Ferrimagnetic materials are called ferrites. I Ferrites exhibit magnetic hysteresis and retain remanent magnetization (i.e. behaves like ferromagnets.) I Above the Curie temperature, becomes paramagnetic. I Magnetite (Fe3O4), maghemite, pyrrhotite and goethite (' rust). Magnetic properties of rocksI I Matrix minerals are mainly silicates or carbonates, which are diamagnetic. I Secondary minerals (e.g., clays) have paramagnetic properties. I So, the bulk of constituent minerals have a magnetic susceptibility but not remanent magnetic properties. I Variable concentrations of ferrimagnetic and matrix minerals result in a wide range of susceptibilities in rocks. Magnetic properties of rocksII I I The weak and variable concentration of ferrimagnetic minerals plays a key role in determining the magnetic properties of the rock. Magnetic properties of rocks III I Important factors influencing rock magnetism: I The type of ferrimagnetic mineral. -
Unerring in Her Scientific Enquiry and Not Afraid of Hard Work, Marie Curie Set a Shining Example for Generations of Scientists
Historical profile Elements of inspiration Unerring in her scientific enquiry and not afraid of hard work, Marie Curie set a shining example for generations of scientists. Bill Griffiths explores the life of a chemical heroine SCIENCE SOURCE / SCIENCE PHOTO LIBRARY LIBRARY PHOTO SCIENCE / SOURCE SCIENCE 42 | Chemistry World | January 2011 www.chemistryworld.org On 10 December 1911, Marie Curie only elements then known to or ammonia, having a water- In short was awarded the Nobel prize exhibit radioactivity. Her samples insoluble carbonate akin to BaCO3 in chemistry for ‘services to the were placed on a condenser plate It is 100 years since and a chloride slightly less soluble advancement of chemistry by the charged to 100 Volts and attached Marie Curie became the than BaCl2 which acted as a carrier discovery of the elements radium to one of Pierre’s electrometers, and first person ever to win for it. This they named radium, and polonium’. She was the first thereby she measured quantitatively two Nobel prizes publishing their results on Boxing female recipient of any Nobel prize their radioactivity. She found the Marie and her husband day 1898;2 French spectroscopist and the first person ever to be minerals pitchblende (UO2) and Pierre pioneered the Eugène-Anatole Demarçay found awarded two (she, Pierre Curie and chalcolite (Cu(UO2)2(PO4)2.12H2O) study of radiactivity a new atomic spectral line from Henri Becquerel had shared the to be more radioactive than pure and discovered two new the element, helping to confirm 1903 physics prize for their work on uranium, so reasoned that they must elements, radium and its status. -
Magnetism, Magnetic Properties, Magnetochemistry
Magnetism, Magnetic Properties, Magnetochemistry 1 Magnetism All matter is electronic Positive/negative charges - bound by Coulombic forces Result of electric field E between charges, electric dipole Electric and magnetic fields = the electromagnetic interaction (Oersted, Maxwell) Electric field = electric +/ charges, electric dipole Magnetic field ??No source?? No magnetic charges, N-S No magnetic monopole Magnetic field = motion of electric charges (electric current, atomic motions) Magnetic dipole – magnetic moment = i A [A m2] 2 Electromagnetic Fields 3 Magnetism Magnetic field = motion of electric charges • Macro - electric current • Micro - spin + orbital momentum Ampère 1822 Poisson model Magnetic dipole – magnetic (dipole) moment [A m2] i A 4 Ampere model Magnetism Microscopic explanation of source of magnetism = Fundamental quantum magnets Unpaired electrons = spins (Bohr 1913) Atomic building blocks (protons, neutrons and electrons = fermions) possess an intrinsic magnetic moment Relativistic quantum theory (P. Dirac 1928) SPIN (quantum property ~ rotation of charged particles) Spin (½ for all fermions) gives rise to a magnetic moment 5 Atomic Motions of Electric Charges The origins for the magnetic moment of a free atom Motions of Electric Charges: 1) The spins of the electrons S. Unpaired spins give a paramagnetic contribution. Paired spins give a diamagnetic contribution. 2) The orbital angular momentum L of the electrons about the nucleus, degenerate orbitals, paramagnetic contribution. The change in the orbital moment -
Relationships Between Magnetic Parameters, Chemical Composition and Clay Minerals of Topsoils Near Coimbra, Central Portugal
Nat. Hazards Earth Syst. Sci., 12, 2545–2555, 2012 www.nat-hazards-earth-syst-sci.net/12/2545/2012/ Natural Hazards doi:10.5194/nhess-12-2545-2012 and Earth © Author(s) 2012. CC Attribution 3.0 License. System Sciences Relationships between magnetic parameters, chemical composition and clay minerals of topsoils near Coimbra, central Portugal A. M. Lourenc¸o1, F. Rocha2, and C. R. Gomes1 1Centre for Geophysics, Earth Sciences Dept., University of Coimbra, Largo Marquesˆ de Pombal, 3000-272 Coimbra, Portugal 2Geobiotec Centre, Geosciences Dept., University of Aveiro, 3810-193 Aveiro, Portugal Correspondence to: A. M. Lourenc¸o ([email protected]) Received: 6 September 2011 – Revised: 27 February 2012 – Accepted: 28 February 2012 – Published: 14 August 2012 Abstract. Magnetic measurements, mineralogical and geo- al., 1980). This methodology is fast, economic and can be ap- chemical studies were carried out on surface soil samples plied in various research fields, such as environmental mon- in order to find possible relationships and to obtain envi- itoring, pedology, paleoclimatology, limnology, archeology ronmental implications. The samples were taken over a and stratigraphy. Recent studies have demonstrated the ad- square grid (500 × 500 m) near the city of Coimbra, in cen- vantages and the potential of the environmental magnetism tral Portugal. Mass specific magnetic susceptibility ranges methods as valuable aids in the detection and delimitation between 12.50 and 710.11 × 10−8 m3 kg−1 and isothermal of areas affected by pollution (e.g. Bityukova et al., 1999; magnetic remanence at 1 tesla values range between 253 Boyko et al., 2004; Blaha et al., 2008; Lu et al., 2009; and 18 174 × 10−3 Am−1. -
An Overview of Representational Analysis and Magnetic Space Groups
Magnetic Symmetry: an overview of Representational Analysis and Magnetic Space groups Stuart Calder Neutron Scattering Division Oak Ridge National Laboratory ORNL is managed by UT-Battelle, LLC for the US Department of Energy Overview Aim: Introduce concepts and tools to describe and determine magnetic structures • Basic description of magnetic structures and propagation vector • What are the ways to describe magnetic structures properly and to access the underlying physics? – Representational analysis – Magnetic space groups (Shubnikov groups) 2 Magnetic Symmetry: an overview of Representational Analysis and Magnetic Space groups Brief History of magnetic structures • ~500 BC: Ferromagnetism documented Sinan, in Greece, India, used in China ~200 BC • 1932 Neel proposes antiferromagnetism • 1943: First neutron experiments come out of WW2 Manhatten project at ORNL • 1951: Antiferromagnetism measured in MnO and Ferrimagnetism in Fe3O4 at ORNL by Shull and Wollan with neutron scattering • 1950-60: Shubnikov and Bertaut develop methods for magnetic structure description • Present/Future: - Powerful and accessible experimental and software tools available - Spintronic devices and Quantum Information Science 3 Magnetic Symmetry: an overview of Representational Analysis and Magnetic Space groups Intrinsic magnetic moments (spins) in ions • Consider an ion with unpaired electrons • Hund’s rule: maximize S/J m=gJJ (rare earths) m=gsS (transtion metals) core 2+ Ni has a localized magnetic moment of 2µB Ni2+ • Magnetic moment (or spin) is a classical -
Rock and Paleomagnetic Investigations Technical Detailed
NWM-USGS-GPP-06 RO Rock and Paleomagnetic Investigations Technical Detailed Procedure GPP-O NNWSI Project Quality Assurance Program U.S. Geological Survey Effective Date: pepared by: Joseph Rosenbaum Technical Reviewer: Richard Reynolds 'Branch Chief: Adel Zohdy NNWI Project Coordinator: W. Dudley Quality Assurance: P. L. Bussolini 8502210165 841130 PDR WASTE PDR Wm-II NWM-USGS-GPP- 06, RO NWM-USGS-GPP- o RO Page 2 of 13 Rock and Paleomagnetic Investigations 1.0 PURPOSE 1.1 This procedure provides a means of assuring the accuracy, validity, and applicability of the methods used to determine paleomagnetic and rock magnetic properties. 1.2 The procedure documents the USGS responsibilities for quality assurance training and enforcement, the processes and authority for procedure modification and revision, the requirements for procedure and personnel interfacing, and to whom the procedure applies. 1.3 The procedure describes the system components, the principles of the methods used, and the limits of their use. 1.4 The procedure describes the detailed methods to be used, where applicable, for system checkout and maintenance, calibration, operation and performance verification. 1.5 The procedure defines the requirements for data acceptance, documentation and control; and provides a means of data traceability. 1.6 The procedure provides a guide for USGS personnel and their contractors engaged to determining paleomagnetic and rock mag- netic properties and a means by which the Department of Energy (DOE) and the Nuclear Regulatory Commission (NRC) can evaluate these activities in meeting requirements for the NNWSI repository. 2.0 SCOPE OF COMPLIANCE 2.1 This procedure applies to all USGS personnel, and persons assigned by the USGS, who perform work on the procedure as described by the work activity given in Section 1.1, or use data from such activities, if the activities or data are deemed by the USGS Project Coordinator to potentially affect public health and safety as related to a nuclear waste repository. -
Selecting the Optimal Inductor for Power Converter Applications
Selecting the Optimal Inductor for Power Converter Applications BACKGROUND SDR Series Power Inductors Today’s electronic devices have become increasingly power hungry and are operating at SMD Non-shielded higher switching frequencies, starving for speed and shrinking in size as never before. Inductors are a fundamental element in the voltage regulator topology, and virtually every circuit that regulates power in automobiles, industrial and consumer electronics, SRN Series Power Inductors and DC-DC converters requires an inductor. Conventional inductor technology has SMD Semi-shielded been falling behind in meeting the high performance demand of these advanced electronic devices. As a result, Bourns has developed several inductor models with rated DC current up to 60 A to meet the challenges of the market. SRP Series Power Inductors SMD High Current, Shielded Especially given the myriad of choices for inductors currently available, properly selecting an inductor for a power converter is not always a simple task for designers of next-generation applications. Beginning with the basic physics behind inductor SRR Series Power Inductors operations, a designer must determine the ideal inductor based on radiation, current SMD Shielded rating, core material, core loss, temperature, and saturation current. This white paper will outline these considerations and provide examples that illustrate the role SRU Series Power Inductors each of these factors plays in choosing the best inductor for a circuit. The paper also SMD Shielded will describe the options available for various applications with special emphasis on new cutting edge inductor product trends from Bourns that offer advantages in performance, size, and ease of design modification. -
Chapter 6 Antiferromagnetism and Other Magnetic Ordeer
Chapter 6 Antiferromagnetism and Other Magnetic Ordeer 6.1 Mean Field Theory of Antiferromagnetism 6.2 Ferrimagnets 6.3 Frustration 6.4 Amorphous Magnets 6.5 Spin Glasses 6.6 Magnetic Model Compounds TCD February 2007 1 1 Molecular Field Theory of Antiferromagnetism 2 equal and oppositely-directed magnetic sublattices 2 Weiss coefficients to represent inter- and intra-sublattice interactions. HAi = n’WMA + nWMB +H HBi = nWMA + n’WMB +H Magnetization of each sublattice is represented by a Brillouin function, and each falls to zero at the critical temperature TN (Néel temperature) Sublattice magnetisation Sublattice magnetisation for antiferromagnet TCD February 2007 2 Above TN The condition for the appearance of spontaneous sublattice magnetization is that these equations have a nonzero solution in zero applied field Curie Weiss ! C = 2C’, P = C’(n’W + nW) TCD February 2007 3 The antiferromagnetic axis along which the sublattice magnetizations lie is determined by magnetocrystalline anisotropy Response below TN depends on the direction of H relative to this axis. No shape anisotropy (no demagnetizing field) TCD February 2007 4 Spin Flop Occurs at Hsf when energies of paralell and perpendicular configurations are equal: HK is the effective anisotropy field i 1/2 This reduces to Hsf = 2(HKH ) for T << TN Spin Waves General: " n h q ~ q ! M and specific heat ~ Tq/n Antiferromagnet: " h q ~ q ! M and specific heat ~ Tq TCD February 2007 5 2 Ferrimagnetism Antiferromagnet with 2 unequal sublattices ! YIG (Y3Fe5O12) Iron occupies 2 crystallographic sites one octahedral (16a) & one tetrahedral (24d) with O ! Magnetite(Fe3O4) Iron again occupies 2 crystallographic sites one tetrahedral (8a – A site) & one octahedral (16d – B site) 3 Weiss Coefficients to account for inter- and intra-sublattice interaction TCD February 2007 6 Below TN, magnetisation of each sublattice is zero. -
Coexistence of Superparamagnetism and Ferromagnetism in Co-Doped
Available online at www.sciencedirect.com ScienceDirect Scripta Materialia 69 (2013) 694–697 www.elsevier.com/locate/scriptamat Coexistence of superparamagnetism and ferromagnetism in Co-doped ZnO nanocrystalline films Qiang Li,a Yuyin Wang,b Lele Fan,b Jiandang Liu,a Wei Konga and Bangjiao Yea,⇑ aState Key Laboratory of Particle Detection and Electronics, University of Science and Technology of China, Hefei 230026, People’s Republic of China bNational Synchrotron Radiation Laboratory, University of Science and Technology of China, Hefei 230029, People’s Republic of China Received 8 April 2013; revised 5 August 2013; accepted 6 August 2013 Available online 13 August 2013 Pure ZnO and Zn0.95Co0.05O films were deposited on sapphire substrates by pulsed-laser deposition. We confirm that the magnetic behavior is intrinsic property of Co-doped ZnO nanocrystalline films. Oxygen vacancies play an important mediation role in Co–Co ferromagnetic coupling. The thermal irreversibility of field-cooling and zero field-cooling magnetizations reveals the presence of superparamagnetic behavior in our films, while no evidence of metallic Co clusters was detected. The origin of the observed superparamagnetism is discussed. Ó 2013 Acta Materialia Inc. Published by Elsevier Ltd. All rights reserved. Keywords: Dilute magnetic semiconductors; Superparamagnetism; Ferromagnetism; Co-doped ZnO Dilute magnetic semiconductors (DMSs) have magnetic properties in this system. In this work, the cor- attracted increasing attention in the past decade due to relation between the structural features and magnetic their promising technological applications in the field properties of Co-doped ZnO films was clearly of spintronic devices [1]. Transition metal (TM)-doped demonstrated. ZnO is one of the most attractive DMS candidates The Zn0.95Co0.05O films were deposited on sapphire because of its outstanding properties, including room- (0001) substrates by pulsed-laser deposition using a temperature ferromagnetism.