Geology and Production of Saline Borate Salts
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Fall 2016 Gems & Gemology
FALL 2016 VOLUME LII THE UARTERLY JOURNAL OF THE GEMOLOGICAL INSTITUTE OF AMERICA Review of CVD Synthetic Diamonds Reversible Color Alteration of Blue Zircon Sapphires from the Russian Far East Grandidierite from Madagascar Editorial Staff Editor-in-Chief Editors, Lab Notes Contributing Editors Duncan Pay Thomas M. Moses James E. Shigley gia.edu/gems-gemology [email protected] Shane F. McClure Andy Lucas Donna Beaton Subscriptions Managing Editor Editors, Micro-World Copies of the current issue may be purchased for Stuart D. Overlin Nathan Renfro Editor-in-Chief Emeritus $29.95 plus shipping. Subscriptions are $79.99 for one [email protected] Elise A. Skalwold Alice S. Keller year (4 issues) in the U.S. and $99.99 elsewhere. Cana- John I. Koivula dian subscribers should add GST. Discounts are avail- Editor Customer Service able for group subscriptions, GIA alumni, and current Jennifer-Lynn Archuleta Editors, Gem News Martha Erickson GIA students. To purchase print subscriptions, visit [email protected] (760) 603-4502 store.gia.edu or contact Customer Service. For insti- Emmanuel Fritsch tutional rates, contact Customer Service. [email protected] Technical Editors Gagan Choudhary Tao Z. Hsu Christopher M. Breeding Database Coverage Gems & Gemology’s impact factor is 0.394, accord- [email protected] Editorial Assistants ing to the 2015 Thomson Reuters Journal Citation Jennifer Stone-Sundberg Brooke Goedert Reports (issued July 2016). G&G is abstracted in Erin Hogarth Thomson Reuters products (Current Contents: Phys- ical, Chemical & Earth -
Midterm 2 Examination Key
GLY4200C Name 90 points October 26, 2011 16 took exam - Numbers to the left of the question number in red are the number of incorrect responses. Instructor comments are in blue. Florida Atlantic University MINERALOGY -- MIDTERM 2 EXAMINATION KEY True-False - Print the letter T or F in the blank to indicate if each of the following statements is true or false. Illegible answers are wrong. (1 point each) 0 T 1. All mathematical groups, including crystallographic point and space groups, must contain an identity operation. 2 F 2. All pyramidal forms are closed. 11 F 3. As nuclei grow, their surface area/volume ratio increases. 1 F 4. Growth twins are always penetration twins. 2 T 5. Low-spin Fe3+ is smaller than high-spin Fe3+. 0 T 6.As pressure increases, minerals transform to denser structures, with atoms packed more closely together 1 T 7. Although silicon normally has CN = IV, in the lower mantle the pressures are so great that the CN of silicon is VI. 2 F 8. If two ions have the same charge, the larger ion will enter a crystal structure preferentially. 2 T 9. Crystal classes are defined by the thirty-two possible point groups. 11 F 10. Possible symmetry operations include rotation axes, mirror planes, and an inversion center. What is wrong with this statement? 0 T 11. Faces composed of all anions or all cations are very high energy. They attract ions of opposite sign, grow rapidly, and may grow themselves out of existence. 1 T 12. The calculation of the zone axis is done using the same method as a vector cross- product. -
Ultrahigh-Field Mg NMR and DFT Study of Magnesium Borate Minerals
Ultrahigh-Field 25Mg NMR and DFT Study of Magnesium Borate Minerals 1 2† 3 4 5 Bing Zhou, § Alexandra Faucher, § Robert Laskowski, Victor V. Terskikh, Scott Kroeker, Wei Sun,6,7 Jinru Lin,6 Jin-Xiao Mi,7 Vladimir K. Michaelis2* and Yuanming Pan6* 1. College of Materials Science and Engineering, Tongji University, Shanghai 21000, China 2. Department of Chemistry, University of Alberta, Edmonton, Alberta T6G 2G2, Canada 3. Institute of High Performance Computing, A*STAR, 1 Fusionopolis Way, #16-16, Connexis, Singapore 138632 4. Department of Chemistry, University of Ottawa, Ottawa, Ontario K1N 6N5 Canada 5. Department of Chemistry, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada 6. Department of Geological Sciences, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5E2, Canada 7. Fujian Provincial Key Laboratory of Advanced Materials, Department of Materials Science and Engineering, College of Materials, Xiamen University, Xiamen 361005, Fujian Province, China †Current address: Bernal Institute, University of Limerick, Limerick, Republic of Ireland §BZ and AF contributed equally *Corresponding authors: Vladimir K. Michaelis ([email protected]) and Yuanming Pan ([email protected]) Keywords: MAS NMR, grandidierite, quantum chemical calculations, WURST, CPMG, wideline, NMR crystallography 1 ABSTRACT A series of well-characterized magnesium borate minerals and synthetic analogues have been studied via ultrahigh-field 25Mg solid-state nuclear magnetic resonance (NMR) spectroscopy. Correlations between 25Mg NMR parameters and the local structure at the magnesium site(s) are highlighted and discussed. First-principles density functional theory calculations of 25Mg NMR parameters carried out with the WIEN2k software package support our experimental 25Mg NMR 25 data. Experimental Mg CQ values range from 0.7 ± 0.1 MHz in hungchaoite to 18.0 ± 0.5 MHz in 25 boracite-type Mg3B7O13Br. -
Rocks and Minerals in This Station-Based Event
Gary Vorwald NYS Rock & Mineral Supervisor Paul J. Gelinas JHS [email protected] Event Description Participants will demonstrate their knowledge of rocks and minerals in this station-based event. A team of up to 2 Approximate time: 40 – 50 Minutes Event Parameters Each team may bring: one magnifying glass One 3-ring binder (1 inch) containing information in any form from any source Materials MUST be 3-hole punched and inserted into the rings (sheet protectors allowed) The Competition Station Event: 15-24 stations with samples & questions Equal time intervals will be allotted for each station. When the signal is given, participants will begin work at their initial station. Participants may not move to the next station until prompted to do so, may not skip stations, nor return to any previously-visited station Mineral and Rock Stations The Competition HCl will not be provided, nor may it be brought to, or be used during the competition. Written descriptions as to how a specimen might react were it to be tested with HCl may be provided. The Competition Identification will be limited to specimens appearing on the Official Science Olympiad Rock and Mineral List (see www.soinc.org) Other rocks or minerals may be used to illustrate key concepts. Tournament Directors may include up to five additional specimens important to their own state. If additional specimens are to be included, all teams must be notified no later than 3 weeks prior to the competition. 2017 Rock & Mineral List Available at: https://www. soinc.org Students should place list in front of notebook Minerals are organized by mineral family Consists of: 59 Minerals 7 Metamorphic Rocks 10 Igneous Rocks 17 Sedimentary Rocks (or varieties) Minerals Native Elements 31. -
Strontium Borate) Mineral
STUDIES ON TUNELLITE (STRONTIUM BORATE) MINERAL Hüseyin GÜLENSOY and T. TEBERDAR İstanbul University, Faculty of Chemistry SUMMARY. — In these studies, the physical, chemical and mineralogical properties of the tunellite found associated with the boron mines in Turkey, which have long been known, have been investigated and the chemical compositon determined. The thermal decomposition of tunellite mineral has been studied both by dynamic and static methods. The results obtained with the methods above were checked with those obtained by Röntgenographic analysis and with the DTA studies. As a result of these studies, it has been observed that the tunellite mineral was transformed into veatchite mineral, after losing 4 molecules of its crystal water. INTRODUCTION AND HISTORY Boron minerals which are gaining ever-increasing importance in the world industry occur widespread in the northwest part of Turkey. Boron occurrences of the country are generally located in the vicinity of Bigadiç, Balıkesir, Mustafakemalpaşa, Emet and Eskişehir. Borate ores encountered in these mines are generally, ulexite and colemanite. The reserves and the grade of the ore are con- sidered favorable for economic production. Associated with the colemanite and ulexite produced from these mines, some other boron minerals are also found and the most important of these are inyoite, meyerhofferite, tertschite and howlite. These secondary minerals are locally found interbedded in the clay seams, as thin beds or nodules. In some mines, a new mineral, showing the composition of strontium borate, is found in association with colemanite and ulexite; this new mineral, which sometimes shows a prismatic struc- ture, is also found to occur closely mixed with clay having bentonite texture. -
Economic Diversification Plan for East Kern County
FEBRUARY 2017 ECONOMIC DIVERSIFICATION PLAN EAST KERN COUNTY, CA KERN COUNTY ACKNOWLEDGEMENTS TIP Strategies would like to thank the many individuals who participated in the creation of this Economic Diversification Plan. We are especially grateful to the members of the East Kern Economic Alliance who contributed their time and input throughout this planning process. Their expertise helped us gain a deep understanding of the region’s range of assets and opportunities. We are also thankful for the US Department of Defense Office of Economic Adjustment for their visionary investments and support which helped make this project a reality. We also want to thank the leadership and staff of Kern County and the Kern EDC for their essential support, guidance, and feedback during the development of this plan. EAST KERN ECONOMIC ALLIANCE KEY STAKEHOLDERS Richard Chapman, President & CEO Jennifer Wood, Mayor Gary Parsons, Economic Kern Economic Development California City Development Manager Corporation City of Ridgecrest Karina Drees, CEO and General Bill Deaver, Michelle Vance, Economic Manager Edwards Community Alliance Development Coordinator Mojave Air & Spaceport City of Tehachapi Kimberly Maevers, President Kelly Bearden, Director Ryan Rush, Field Representative Greater Antelope Valley Economic CSU-Bakersfield SBDC Kern County Board of Supervisors, Alliance 2nd District KERN COUNTY PROJECT TEAM Supervisor Zach Scrivner, Chairman of the Kern County Board of Supervisors & 2nd District Supervisor Teresa Hitchcock, Assistant County Administrative -
Trace Elements and Minerals in Fumarolic Sulfur: the Case of Ebeko Volcano, Kuriles
Hindawi Geofluids Volume 2018, Article ID 4586363, 16 pages https://doi.org/10.1155/2018/4586363 Research Article Trace Elements and Minerals in Fumarolic Sulfur: The Case of Ebeko Volcano, Kuriles E. P. Shevko,1 S. B. Bortnikova,2 N. A. Abrosimova,2 V. S. Kamenetsky ,3,4 S. P. Bortnikova,2 G. L. Panin,2 and M. Zelenski 3 1 Sobolev Institute of Geology and Mineralogy, SBRAS, Novosibirsk 630090, Russia 2Trofmuk Institute of Petroleum Geology and Geophysics, SBRAS, No. 3, Novosibirsk 630090, Russia 3Institute of Experimental Mineralogy RAS, Chernogolovka 142432, Russia 4EarthSciencesandCODES,UniversityofTasmania,PrivateBag79,Hobart,TAS7001,Australia Correspondence should be addressed to M. Zelenski; [email protected] Received 25 June 2017; Revised 13 October 2017; Accepted 14 December 2017; Published 20 March 2018 Academic Editor: Joerg Goettlicher Copyright © 2018 E. P. Shevko et al. Tis is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Native sulfur deposits on fumarolic felds at Ebeko volcano (Northern Kuriles, Russia) are enriched in chalcophile elements (As- Sb-Se-Te-Hg-Cu) and contain rare heavy metal sulfdes (Ag2S, HgS, and CuS), native metal alloys (Au2Pd), and some other low- solubility minerals (CaWO4, BaSO4). Sulfur incrustations are impregnated with numerous particles of fresh and altered andesite groundmass and phenocrysts (pyroxene, magnetite) as well as secondary minerals, such as opal, alunite, and abundant octahedral pyrite crystals. Te comparison of elemental abundances in sulfur and unaltered rocks (andesite) demonstrated that rock-forming elements (Ca, K, Fe, Mn, and Ti) and other lithophile and chalcophile elements are mainly transported by fumarolic gas as aerosol particles, whereas semimetals (As, Sb, Se, and Te), halogens (Br and I), and Hg are likely transported as volatile species, even ∘ at temperatures slightly above 100 C. -
Potash, Soda, and Borate Mineral Mining 1997 Issued October 1999
Potash, Soda, and Borate Mineral Mining 1997 Issued October 1999 EC97N-2123I 1997 Economic Census Mining Industry Series U.S. Department of Commerce Economics and Statistics Administration U.S. CENSUS BUREAU ACKNOWLEDGMENTS The staff of the Manufacturing and Con- The Geography Division staff developed struction Division prepared this report. geographic coding procedures and associ- Judy M. Dodds, Assistant Chief for Cen- ated computer programs. sus and Related Programs, was respon- The Economic Statistical Methods and Pro- sible for the overall planning, manage- gramming Division, Charles P. Pautler ment, and coordination. Patricia L. Jr., Chief, developed and coordinated the Horning, Chief, Construction and Miner- computer processing systems. Martin S. als Branch, assisted by M. Susan Bucci Harahush, Assistant Chief for Quinquen- and Susan L. DiCola, Section Chiefs, per- nial Programs, assisted by Barbara Lam- formed the planning and implementation. bert and Christina Arledge were respon- Richard Hough, Christopher D. sible for design and implementation of the Perrien, John F. Roehl, Eva J. Snapp, computer systems. Gary T. Sheridan, and Sarah B. Teichner provided primary Chief, Manufacturing and Construction staff assistance. Branch, Lori A. Guido and Roy A. Smith, Brian Greenberg, Assistant Chief for Section Chiefs, supervised the preparation Research and Methodology Programs, of the computer programs. assisted by Stacey Cole, Chief, Manufac- turing Programs Methodology Branch, and Computer Services Division, Debra Will- Robert Struble, Section Chief, provided iams, Chief, performed the computer pro- the mathematical and statistical tech- cessing. niques as well as the coverage operations. The staff of the Administrative and Cus- Jeffrey Dalzell and Cathy Ritenour pro- tomer Services Division, Walter C. -
STUDIES of BORATE MINERAI,S (ID: X-RAY CRYSTALLOG- RAPHY of INYOITE and MEYERHOFFERITE; X-RAY and MORPHOLOGICAL CRYSTALLOGRAPHY of 2Cao-3Bzo .9H2O*
STUDIES OF BORATE MINERAI,S (ID: X-RAY CRYSTALLOG- RAPHY OF INYOITE AND MEYERHOFFERITE; X-RAY AND MORPHOLOGICAL CRYSTALLOGRAPHY OF 2CaO-3Bzo .9H2O* C. L. Cunrsr, [/. S. GeologicalSuraey, Washington25, D. C. Ansrnacr fnyoite is monoclinic,P21/a, ao:10.63, bo:fi.A6, co:8.40rA, F:114.02,. 2CaO'3BrOa.9HzOistriclinic PT, ao: /.94, bo:9.452,co-7.412 A, a:101"21,,p-: l}l"7g,, t:99"49'. The findingsof Switzerin Palache(1938) for meyerhofferiteare confirmed. Powder patterns, partially indexed, are given for inyoite, meyerhofierite,and 2CaO.3BzOs.9HrO. INrnooucrroN ANDAcrwowr,ooGMENTS A systematic study of borate minerals has been continued in the pres- ent investigation with the determination of the r-ray crystallography of inyoite, 2CaO.3B2OB.13H2O, the *-ray crystallographyand morphology of the synthetic mineral 2CaO.38zOs.9HzO,and the redeterminationof the r-ray crystallography of meyerhofierite, 2CaO.3BzOt. jIJzO. Results obtained on meyerhofferite were in excellent agreementwith those previ- ously reported by Switzer in Palache (1933). Powder patterns of the three compounds have been measured and partially indexed. The work was undertaken primarily as a preliminary to the determina- tion of the structures. The writer is indebted to various colleaguesin the U. S. Geological Survey: Waldemar T. Schaller furnished the crystals studied; Mrs. Joan R. Clark made many of the calculations and film measurements; Howard T. Evans, Jr., made the goniometric measurementson and the drawing of 2CaO.3B2OB.9HsOand,also renderedmuch helpful advice; Fred A. Hildebrand prepared the powder patterns reported. ExpBnrlrpwrAr, WoRK All of the crystals used were synthetic. Schaller (personal communica- tion) has furnished the following description of the methods of prepara- tion: Inyoite (2:3:13). -
Download PDF (402K)
Geochemical Journal, Vol. 41, pp. 149 to 163, 2007 Boron isotope fractionation accompanying formation of potassium, sodium and lithium borates from boron-bearing solutions MAMORU YAMAHIRA, YOSHIKAZU KIKAWADA* and TAKAO OI Department of Chemistry, Sophia University, 7-1 Kioi-cho, Chiyoda-ku, Tokyo 102-8854, Japan (Received March 18, 2006; Accepted June 22, 2006) A series of experiments was conducted in which boron minerals were precipitated by water evaporation from solutions containing boron and potassium, sodium or lithium at 25°C, and boron isotope fractionation accompanying such mineral precipitation was investigated. In the boron-potassium ion system, K2[B4O5(OH)4]·2H2O, santite (K[B5O6(OH)4]·2H2O), KBO2·1.33H2O, KBO2·1.25H2O and sassolite (B(OH)3) were found deposited as boron minerals. Borax (Na2[B4O5(OH)4·8H2O) was found deposited in the boron-sodium ion system, and Li2B2O4·16H2O, Li2B4O7·5H2O, Li2B10O16·10H2O, LiB2O3(OH)·H2O and sassolite in the boron-lithium ion system. The boron isotopic analysis was con- 11 10 ducted for santite, K2[B4O5(OH)4]·2H2O, borax and Li2B2O4·16H2O. The separation factor, S, defined as the B/ B isotopic ratio of the precipitate divided by that of the solution, ranged from 0.991 to 1.012. Computer simulations for modeling boron mineral formations, in which polyborates were decomposed into three coor- dinated BO3 unit and four coordinated BO4 unit for the purpose of calculation of their boron isotopic reduced partition function ratios, were attempted to estimate the equilibrium constant, KB, of the boron isotope exchange between the boric – acid molecule (B(OH)3) and the monoborate anion (B(OH)4 ). -
Inyoite Cab3o3(OH)5 • 4H2O C 2001-2005 Mineral Data Publishing, Version 1
Inyoite CaB3O3(OH)5 • 4H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. Typically as crystals, short prismatic along [001], tabular on {001}, exhibiting prominent {110} and {001} and a dozen other minor forms, to 2.5 cm; in cockscomb aggregates of pseudorhombohedral crystals; also coarse spherulitic, granular. Physical Properties: Cleavage: {001}, good; {010}, distinct. Fracture: Irregular. Tenacity: Brittle. Hardness = 2 D(meas.) = 1.875 D(calc.) = 1.87 Soluble in H2O. Optical Properties: Transparent, translucent on dehydration. Color: Colorless, white on dehydration. Luster: Vitreous. Optical Class: Biaxial (–). Orientation: Y = b; X ∧ c =37◦; Z ∧ c = –53◦. Dispersion: r< v, slight. α = 1.490–1.495 β = 1.501–1.505 γ = 1.516–1.520 2V(meas.) = 70◦–86◦ Cell Data: Space Group: P 21/a. a = 10.621(1)) b = 12.066(1) c = 8.408(1) β = 114◦1.2◦ Z=4 X-ray Powder Pattern: Monte Azul mine, Argentina. 7.67 (100), 2.526 (25), 3.368 (22), 1.968 (22), 2.547 (21), 3.450 (20), 2.799 (19) Chemistry: (1) (2) B2O3 37.44 37.62 CaO 20.42 20.20 + H2O 9.46 − H2O 32.46 H2O 42.18 rem. 0.55 Total 100.33 100.00 • (1) Hillsborough, Canada; remnant is gypsum. (2) CaB3O3(OH)5 4H2O. Occurrence: Along fractures and nodular in sedimentary borate deposits; may be authigenic in playa sediments. Association: Meyerhofferite, colemanite, priceite, hydroboracite, ulexite, gypsum. Distribution: In the USA, in California, from an adit on Mount Blanco, Furnace Creek district, Death Valley, Inyo Co., and in the Kramer borate deposit, Boron, Kern Co. -
UCLA Electronic Theses and Dissertations
UCLA UCLA Electronic Theses and Dissertations Title Use of Boron in Detergents and its Impact on Reclamation Permalink https://escholarship.org/uc/item/2rw7k2r7 Author Ghavanloughajar, Maryam Publication Date 2015 Peer reviewed|Thesis/dissertation eScholarship.org Powered by the California Digital Library University of California UNIVERSITY OF CALIFORNIA Los Angeles Use of Boron in Detergents and its Impact on Reclamation A thesis submitted in partial satisfaction of the requirements for the degree Master of Science in Civil Engineering by Maryam Ghavanloughajar 2015 ABSTRACT OF THE THESIS Use of Boron in Detergents and its Impact on Reclamation By Maryam Ghavanloughajar Master of Science in Civil Engineering University of California, Los Angeles, 2015 Professor Michael K. Stenstrom, Chair Many parts of the world are experiencing severe water drought and it affects societies both economically and environmentally. Therefore, conservation practices are essential to balance water supply and demand. Greywater or wastewaters from showers and luandries, if treated well can be a reliable source for activities such as irrigation, toilet flushing and car washing. Greywaters are not as contaminated as sewage but still may require treatment before reuse. The application of insufficiently treated water for irrigation can cause harm to plants and animals. Pollutant such as boron in greywater is of particular interest because many plants are sensitive to even low concentrations. High concentrations of boron can induce toxicity, reduce growth rate and yield in plants. Therefore, proposed greywater treatment systems need to consider the sensitivity of plant species and boron concentrations and potential removal. This thesis reviews boron chemistry, its effect on plants and currently available boron removal technologies.