2011 Minerals Yearbook BORON
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Origin of the Kramer Borax Deposit, Boron, CA
A 50 year retrospective 1 OUTLINE 1. A brief history of borax 2. Kramer borax deposit a) Setting and Discovery b) Mineralogy of sedimentary borates c) Stratigraphy and Lithology d) Petrography and implications for geologic setting e) Solubility studies and modeling lake characteristics f) Comparable modern analogues 3. New evidence a) Turkish and Argentinian deposits b) Boron isotopic studies 4. Broader questions – Source water controls (thermal springs), B-As-Sb association, igneous-metamorphic controls on boron in thermal waters 2 Why give this talk? 1. Old (but rusty) material to me, new to most of you 2. Desire to see if ideas have changed in the past 50+ years. 3. Citation of my work even today suggests I did something right. 4. Wish to compare Kramer work with evidence from newer borate deposits in Turkey and South America 5. A wish to evaluate these ideas in light of new evidence using tools that weren’t available in 1964 6. A chance to ponder broader questions about boron’s geochemical cycle. 7. Work done so long ago that if you ask penetrating questions I can always plead a “senior moment” 3 What was unique about my research on the Kramer deposits? • Used a combination of geological tools (Field AND lab work – rare in 1964) • Stratigraphy, Petrography, and XRD based mineralogy • Experimental solubility studies of effects of other salts on Na-borate solubilities • Field studies of other possible borate environments (Borax Lake, Teels and Columbus Marsh, NV, Death Valley, Searles Lake) • Benefits of discussions with an all-star support team with similar interests (Mary Clark, Blair Jones, G.I. -
Temperature and Relative Humidity (RH) Using Saturated Salt Solutions
THERMODYNAMICS OF 1:2 SODIUM BORATE MINERALS By LAURA SUZANNE RUHL A THESIS PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE UNIVERSITY OF FLORIDA 2008 1 © 2008 Laura Suzanne Ruhl 2 To my family, who have kept my inquisitive spirit and thirst for knowledge alive, always encouraging me, and giving me strength. 3 ACKNOWLEDGMENTS First and foremost, I thank the chair of my committee, Phil Neuhoff, for all of his time and all of the knowledge he has bestowed upon me throughout my time as his student. I would also like to thank my committee members, Ellen Martin and Guerry McClellan, for their time and support in my academic endeavors. I thank Jie Wang and Gökce Atalan for their help in the lab, for many scientific discussions and support. I also thank Derrick Newkirk for his unending encouragement and support. Major thanks go to my parents and siblings for always being there to help in any endeavor and their never-ending support and love. Lastly, I appreciate all of the never-ending encouragement from my friends and family. The National Science Foundation funded this project. 4 TABLE OF CONTENTS page ACKNOWLEDGMENTS ...............................................................................................................4 LIST OF TABLES...........................................................................................................................6 LIST OF FIGURES .........................................................................................................................7 -
Design Rules for Discovering 2D Materials from 3D Crystals
Design Rules for Discovering 2D Materials from 3D Crystals by Eleanor Lyons Brightbill Collaborators: Tyler W. Farnsworth, Adam H. Woomer, Patrick C. O'Brien, Kaci L. Kuntz Senior Honors Thesis Chemistry University of North Carolina at Chapel Hill April 7th, 2016 Approved: ___________________________ Dr Scott Warren, Thesis Advisor Dr Wei You, Reader Dr. Todd Austell, Reader Abstract Two-dimensional (2D) materials are championed as potential components for novel technologies due to the extreme change in properties that often accompanies a transition from the bulk to a quantum-confined state. While the incredible properties of existing 2D materials have been investigated for numerous applications, the current library of stable 2D materials is limited to a relatively small number of material systems, and attempts to identify novel 2D materials have found only a small subset of potential 2D material precursors. Here I present a rigorous, yet simple, set of criteria to identify 3D crystals that may be exfoliated into stable 2D sheets and apply these criteria to a database of naturally occurring layered minerals. These design rules harness two fundamental properties of crystals—Mohs hardness and melting point—to enable a rapid and effective approach to identify candidates for exfoliation. It is shown that, in layered systems, Mohs hardness is a predictor of inter-layer (out-of-plane) bond strength while melting point is a measure of intra-layer (in-plane) bond strength. This concept is demonstrated by using liquid exfoliation to produce novel 2D materials from layered minerals that have a Mohs hardness less than 3, with relative success of exfoliation (such as yield and flake size) dependent on melting point. -
Borates—Crystal Structures of Prospective Nonlinear Optical Materials: High Anisotropy of the Thermal Expansion Caused by Anharmonic Atomic Vibrations
Review Borates—Crystal Structures of Prospective Nonlinear Optical Materials: High Anisotropy of the Thermal Expansion Caused by Anharmonic Atomic Vibrations Rimma Bubnova 1,2,*, Sergey Volkov 1, Barbara Albert 3 and Stanislav Filatov 2 1 Institute of Silicate Chemistry, Russian Academy of Sciences, Makarov Emb. 2, St. Petersburg 199034, Russia; [email protected] 2 Department of Crystallography, Institute of Earth Sciences, St. Petersburg State University, University Emb. 7/9, St. Petersburg 199034, Russia; [email protected] 3 Eduard Zintl-Institute of Inorganic and Physical Chemistry, Technische Universität Darmstadt, Alarich-Weiss-Str. 12, 64287 Darmstadt, Germany; [email protected] * Correspondence: [email protected]; Tel.: +7-981-181-3262 Academic Editors: Ning Ye and Rukang Li Received: 7 February 2017; Accepted: 16 March 2017; Published: 22 March 2017 Abstract: In the present study the thermal structure evolution is reviewed for known nonlinear optical borates such as β-BaB2O4, LiB3O5, CsLiB6O10, Li2B4O7, K2Al2B2O7, and α-BiB3O6, based on single-crystal and powder X-ray diffraction data collected over wide temperature ranges. Temperature-dependent measurements of further borates are presented for the first time: α-BaB2O4 (295–673 K), β-BaB2O4 (98–693 K), LiB3O5 (98–650 K) and K2Al2B2O7 (98–348 K). In addition to the established criteria for nonlinear optical (NLO) properties of crystals, here the role of the anisotropy and anharmonicity of the thermal vibrations of atoms is analysed as well as changes in their coordination spheres and the anisotropy of the thermal expansion of the crystal structure. Non-centrosymmetric borates, especially those that have NLO properties, often show distinct anisotropies for each cation in comparison to centrosymmetric borates. -
A Specific Gravity Index for Minerats
A SPECIFICGRAVITY INDEX FOR MINERATS c. A. MURSKyI ern R. M. THOMPSON, Un'fuersityof Bri.ti,sh Col,umb,in,Voncouver, Canad,a This work was undertaken in order to provide a practical, and as far as possible,a complete list of specific gravities of minerals. An accurate speciflc cravity determination can usually be made quickly and this information when combined with other physical properties commonly leads to rapid mineral identification. Early complete but now outdated specific gravity lists are those of Miers given in his mineralogy textbook (1902),and Spencer(M,i,n. Mag.,2!, pp. 382-865,I}ZZ). A more recent list by Hurlbut (Dana's Manuatr of M,i,neral,ogy,LgE2) is incomplete and others are limited to rock forming minerals,Trdger (Tabel,l,enntr-optischen Best'i,mmungd,er geste,i,nsb.ildend,en M,ineral,e, 1952) and Morey (Encycto- ped,iaof Cherni,cal,Technol,ogy, Vol. 12, 19b4). In his mineral identification tables, smith (rd,entifi,cati,onand. qual,itatioe cherai,cal,anal,ys'i,s of mineral,s,second edition, New york, 19bB) groups minerals on the basis of specificgravity but in each of the twelve groups the minerals are listed in order of decreasinghardness. The present work should not be regarded as an index of all known minerals as the specificgravities of many minerals are unknown or known only approximately and are omitted from the current list. The list, in order of increasing specific gravity, includes all minerals without regard to other physical properties or to chemical composition. The designation I or II after the name indicates that the mineral falls in the classesof minerals describedin Dana Systemof M'ineralogyEdition 7, volume I (Native elements, sulphides, oxides, etc.) or II (Halides, carbonates, etc.) (L944 and 1951). -
The Optimization of Copper Sulfate and Tincalconite Molar Ratios on the Hydrothermal Synthesis of Copper Borates E
World Academy of Science, Engineering and Technology International Journal of Chemical and Molecular Engineering Vol:8, No:10, 2014 The Optimization of Copper Sulfate and Tincalconite Molar Ratios on the Hydrothermal Synthesis of Copper Borates E. Moroydor Derun, N. Tugrul, F. T. Senberber, A. S. Kipcak, S. Piskin anhydrous form is a pale green or gray-white powder, whereas Abstract —In this research, copper borates are synthesized by the the pentahydrate (CuSO 4·5H 2O), the most commonly reaction of copper sulfate pentahydrate (CuSO 4.5H 2O) and encountered salt, is bright blue [5]. tincalconite (Na 2O4B7.10H 2O). The experimental parameters are o Copper borates are the member of both delafossite (CuMO 2) selected as 80 C reaction temperature and 60 of reaction time. The family and the metal borate groups [1], [6], [7]. With the effect of mole ratio of CuSO 4.5H 2O to Na 2O4B7.5H2O is studied. For the identification analyses X-Ray Diffraction (XRD) and Fourier lattice structure of copper borates that can be explained with a Transform Infrared Spectroscopy (FT-IR) techniques are used. At the two-dimensional spin system; they exhibit specific features of end of the experiments, synthesized copper borate is matched with optical transparency, high electrical conductivity (1.65 S/cm 2) the powder diffraction file of “00-001-0472” [Cu(BO2)2] and and an indirect gap of 2.2 eV [8]. Copper metaborate CuBO 2 characteristic vibrations between B and O atoms are seen. The proper is considered a potential system. This is because of recent crystals are obtained at the mole ratio of 3:1. -
Diamond Dan's Mineral Names Dictionary
A Dictionary of Mineral Names By Darryl Powell Mineral Names What do they mean? Who created them? What can I learn from them? This mineral diction‐ ary is unique because it is illustrated, both with mineral drawings as well as pictures of people and places after which some minerals are named. The people pictured on this page have all made a con‐ tribution to what is formally called “mineral nomenclature.” Keep reading and you will discover who they are and what they did. In 1995, Diamond Dan Publications pub‐ lished its first full book, “A Mineral Collector’s Guide to Common Mineral Names: Their Ori‐ gins & Meanings.” Now it is twenty years later. What you will discover in this issue and in the March issue is a re‐ vised and improved version of this book. This Mineral Names Dictionary contains mineral names that the average mineral collector will encounter while collecting minerals, attending shows and visiting museum displays. In addition to the most common min‐ eral names, there are some unofficial names which you will still find on labels. Each mineral name has a story to tell or a lesson to teach. If you wanted to take the time, each name could become a topic to study. Armalcolite, for example, could quickly be‐ come a study of a mineral, first discovered on the moon, and brought back to earth by the astronauts Armstrong, Aldrin and Collins (do you see parts of their names in this mineral name?) This could lead you to a study of American astronauts landing on the moon, what it took to get there and what we discovered by landing on the moon. -
Microwave Dehydration Modelling of Tincalconite
Journal of Thermal Engineering, Vol. 4, No. 2, Special Issue 7, pp. 1803-1812, February, 2018 Yildiz Technical University Press, Istanbul, Turkey MICROWAVE DEHYDRATION MODELLING OF TINCALCONITE S. Coban1, B. Ozkarasu1, F. T. Senberber2, A. S. Kipcak1, I. Doymaz1, E. M. Derun1,* ABSTRACT Boron is known element due to wide range of application areas. Microwave dehydration has more advantages than conventional dehydraion. Differ dehydraion mechanism, higher dehydraion rate and higher level of safety are some of this advantages. Furthermore, most of minerals give better result in microwave for temperature increase. Particle size, microwave power and sample mass are parameters which effect to dehydration directly. Structure of tincalconite is suitable for the investigation of dehydration behavior by microwave because of their five moles of crystal water. Tincalconite is a type of sodium borate mineral which has a white color, trigonal system and molecule formula of Na2B4O7•5H2O. Tincalconite contains 48.8% of boron oxide(B2O3) and 29.47% of structural water. In this study, dehydration behavior of tincalconite was studied with using microwave irradiation with the power level of 180 and 360 W. The kinetic parameters of reaction were determined by using the dehydration kinetic models of Lewis, Henderson and Pabis and Wang and Singh. Tincalconite and dehydrated tincalconite characterized by the techniques of X-ray diffraction (XRD) and Raman spectroscopy. According to the results obtained tincalconite was dehydrated successfully at the microwave power level of 360 W at 14 min, on the contrary at 180 W, only the 68% of the structural water was dehydrated. Among the models, which are applied only at 360 W, Wang and Singh model best fits the data with the coefficient of regression (R2) value of 0.9965. -
Character and Distribution of Nonclastic Minerals in the Searles Lake Evaporite Deposit California
Character and Distribution of Nonclastic Minerals in the Searles Lake Evaporite Deposit California By GEORGE I. SMITH and DAVID V. HAINES I CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY BULLETIN 1181-P Prepared in cooperation with the State of California, Resources Agency, ' Department of Conservation, Division of Mines and Geology -A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1964 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library catalog card for this publication appears after page P58. For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract..---.---------------------------------------------------- PI Introduction-____________-___-___----_--_-______-____--_______-___ 3 Acknowledgments ____-_____---_-__--__--_----__-_______---____..__- 4 Mineralogy __________-_---_---------_-_--_----_-------_--__-_-____ 6 , Minerals associated with saline layers____________________________ 8 Aphthitalite.. __-____---_----_---_--___---_---__-_________ 8 Borax-----.--------------------------------------.------- 10 Burkeite__.______--____-_.._-___-._-__.____..._..______ 12 Halite ------------------------------------------------- 14 Hanksite.-_------------_-----_-------__----------_----__- 16 Nahcolite__-___-_---_-_______-___-___---_____-___-_-____ 18 ^ Sulfohalite-.--------------------------------------------- 19 Teepleite._-----------------_----_------_-------_---_-.-.- 20 ,- -
Tincalconite Crystals from Searles Lake, San Bernardino County, California A
TINCALCONITE CRYSTALS FROM SEARLES LAKE, SAN BERNARDINO COUNTY, CALIFORNIA A. Pensr aNn D. L. Sewvon, Uniwrsity oJ California, Berkeley,California. Assrnac:t The discovery of small, well-formed crystals of tincalconite in drill cores frorn Searles Lake, San Bernardino County, California, is announced. The associated minerals are described and the results of goniometric and r-ray examination of tincalconite reported. fxrnooucrroN The name tincalconite first appeared in print in 1878.1The statement in which it was contained reads as follows:- "Tincalconice (Shepard). Borax pulverulent et effi.orescent,de Californie, 32p. cent d'eau." This appeared in a section of the Bulletin headed "Extraits de diverses publications." Literature referencesare given for most of the extracts, all of which are concerned with new mineral names, but no referencesi given with the extract on tincalconite which is quoted in full above. No trace has been found of any original publication by Shepard2on this material and it seemsthat such may never have been accomplished. Mineralogists generally3considered the name tincalconite to apply to a variety of borax rather than to a distinct mineral. After half a century it was pointed out by Schallerathat "it is obvious" that Shepard's tincal- conite "was the S-hydrate of the borax series,NazO 2BzOt.5HzOidenti- cal in compositionwith 'octahedralborax'." According to Schallerit is "not very abundant but rather widespread, coating both borax and kernite." It forms from borax, the 10 hydrate of the series,by partial dehydration or from kernite, the 4 hydrate, by hydration. So far it has been found only in powdery form. Natural borax crystals such as are found embedded in the muds of Borax Lake in Lake County and SearlesLake in San Bernardino County, California, and numerous other localities are probably partly or wholly altered to the S-hydrate and so should be considered pseudomorphs of tincalconite after borax. -
The Distribution of Boron in Veins in Gale Crater with Implications for Mars Aqueous Processes and Astrobiology
Lunar and Planetary Science XLVIII (2017) 1539.pdf THE DISTRIBUTION OF BORON IN VEINS IN GALE CRATER WITH IMPLICATIONS FOR MARS AQUEOUS PROCESSES AND ASTROBIOLOGY. P. J. Gasda1, E. B. Haldeman2, R. C. Wiens1, W. Rapin3, T. Bristow4, J. Frydenvang1,5, N. Lanza1, S. Maurice3, S. Clegg1, D. Delapp1, V. Sanford2, R. McInroy1; 1Los Alamos National Laboratory ([email protected]), 2Ursinus College, 3IRAP/CNES, 4NASA Ames 5University of Copenhagen. Introduction: The study of boron on Mars sheds filled fractures and only fracture fills in Yellowknife light on martian aqueous and climate history. Boron Bay mudstone, Murray mudstone, and Stimson sand- has been detected in calcium sulfate veins in Gale stone, and observed as early as martian day (sol) 113. Crater by the ChemCam instrument on board the The majority of detections have been observed since NASA MSL rover. Possible hypotheses for boron dep- sol 1350 and at an elevation above -4435 m (Fig. 2). osition include initial enrichment in either an evaporite Relative abundances, up to ~0.08 wt.% B, are indicated layer or lacustrine clays. Late-stage groundwater either by the color scale in Fig. 2. The level of B detected in dissolved the evaporites or released boron from the the veins is highly enriched compared to estimates of B clays and these fluids were precipitated as fracture- in martian igneous rocks (~0.01–0.1 ppm) [4]. filling veins in the bedrock. Methods: ChemCam is a combined remote imager and laser-induced breakdown spectroscopy (LIBS) instrument that provides elemental emission spectra for 350–550 µm sized points on rocks from up to 7 m away from a target [1,2]. -
BULLETIN of the MINERAL RESEARCH and EXPLORATION Bulletin of the Foreign Edition 2015 151 ISSN : 0026 - 4563 CONTENTS
Bull. Min. Res. Exp. (2015) 151: 169-215 BULLETIN OF THE MINERAL RESEARCH AND EXPLORATION Bulletin of the Foreign Edition 2015 151 ISSN : 0026 - 4563 CONTENTS The late Quaternary Tectono-Stratigraphic evolution of the Lake Van, Turkey ..................................................................... Naci GÖRÜR, M. Nam›k ÇA⁄ATAY, Cengiz ZABCI, Mehmet SAKINÇ, ................................................................................................................Remzi AKKÖK, Hande fi‹LE and Sefer ÖRÇEN 1 Late Cenozoic Extensional Tectonics In Western Anatolia: Exhumation Of The Menderes Core Complex And Formation Of Related Basins ................................................................................................................................. Gürol SEYITO⁄LU and Veysel IfiIK 49 Late Pleistocene Glaciations and Paleoclimate of Turkey ............................................................................................................................. M. Akif SARIKAYA and Attila ÇINER 109 Late Permian Unconformity Around Ankara and New Age Data on The Basement Rocks, Ankara, Turkey .................................................. Mustafa SEV‹N, Mustafa DÖNMEZ, Gökhan ATICI, A. Hande ESATO⁄LU VEKL‹, ...................................................................................... Ender SARIFAKIO⁄LU, Serap ARIKAN and Havva SOYCAN 131 Mineral Research and Exploration Differentiation Processes In Late Cretaceous Ultrapotassic Volcanics Around Amasya ...................................................................................................................................