Electrokinetic Properties of Wavellite and Its Floatability With
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Mineral Collecting Sites in North Carolina by W
.'.' .., Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie RUTILE GUMMITE IN GARNET RUBY CORUNDUM GOLD TORBERNITE GARNET IN MICA ANATASE RUTILE AJTUNITE AND TORBERNITE THULITE AND PYRITE MONAZITE EMERALD CUPRITE SMOKY QUARTZ ZIRCON TORBERNITE ~/ UBRAR'l USE ONLV ,~O NOT REMOVE. fROM LIBRARY N. C. GEOLOGICAL SUHVEY Information Circular 24 Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie Raleigh 1978 Second Printing 1980. Additional copies of this publication may be obtained from: North CarOlina Department of Natural Resources and Community Development Geological Survey Section P. O. Box 27687 ~ Raleigh. N. C. 27611 1823 --~- GEOLOGICAL SURVEY SECTION The Geological Survey Section shall, by law"...make such exami nation, survey, and mapping of the geology, mineralogy, and topo graphy of the state, including their industrial and economic utilization as it may consider necessary." In carrying out its duties under this law, the section promotes the wise conservation and use of mineral resources by industry, commerce, agriculture, and other governmental agencies for the general welfare of the citizens of North Carolina. The Section conducts a number of basic and applied research projects in environmental resource planning, mineral resource explora tion, mineral statistics, and systematic geologic mapping. Services constitute a major portion ofthe Sections's activities and include identi fying rock and mineral samples submitted by the citizens of the state and providing consulting services and specially prepared reports to other agencies that require geological information. The Geological Survey Section publishes results of research in a series of Bulletins, Economic Papers, Information Circulars, Educa tional Series, Geologic Maps, and Special Publications. -
Hydroxyapatite and Fluorapatite in Conservative Dentistry and Oral Implantology—A Review
materials Review Hydroxyapatite and Fluorapatite in Conservative Dentistry and Oral Implantology—A Review Kamil Pajor, Lukasz Pajchel and Joanna Kolmas * Analytical Group, Department of Analytical Chemistry and Biomaterials, Faculty of Pharmacy with Laboratory Medicine Division, Medical University of Warsaw, 02-097 Warsaw, Poland * Correspondence: [email protected] Received: 29 July 2019; Accepted: 20 August 2019; Published: 22 August 2019 Abstract: Calcium phosphate, due to its similarity to the inorganic fraction of mineralized tissues, has played a key role in many areas of medicine, in particular, regenerative medicine and orthopedics. It has also found application in conservative dentistry and dental surgery, in particular, as components of toothpaste and mouth rinse, coatings of dental implants, cements, and bone substitute materials for the restoration of cavities in maxillofacial surgery. In dental applications, the most important role is played by hydroxyapatite and fluorapatite, i.e., calcium phosphates characterized by the highest chemical stability and very low solubility. This paper presents the role of both apatites in dentistry and a review of recent achievements in the field of the application of these materials. Keywords: hydroxyapatite; fluorapatite; dentistry; calcium phosphates 1. Introduction In recent decades, one has been able to observe huge progress in the field of dentistry. This results not only from the development of dental techniques and methods of therapy but also from significant developments in biomaterial engineering. The science of biomaterials is constantly increasing due to innovative modifications of already known materials or completely new biomaterials for applications in dentistry. Biodegradable polymers, bioactive ceramics, bioglass or metals covered with a layer of material facilitating osseointegration and, above all, composite materials are the main directions in the development of dental biomaterials [1–4]. -
Rare Earth Elements Deposits of the United States—A Summary of Domestic Deposits and a Global Perspective
The Principal Rare Earth Elements Deposits of the United States—A Summary of Domestic Deposits and a Global Perspective Gd Pr Ce Sm La Nd Scientific Investigations Report 2010–5220 U.S. Department of the Interior U.S. Geological Survey Cover photo: Powders of six rare earth elements oxides. Photograph by Peggy Greb, Agricultural Research Center of United States Department of Agriculture. The Principal Rare Earth Elements Deposits of the United States—A Summary of Domestic Deposits and a Global Perspective By Keith R. Long, Bradley S. Van Gosen, Nora K. Foley, and Daniel Cordier Scientific Investigations Report 2010–5220 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: 2010 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. This report has not been reviewed for stratigraphic nomenclature. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Suggested citation: Long, K.R., Van Gosen, B.S., Foley, N.K., and Cordier, Daniel, 2010, The principal rare earth elements deposits of the United States—A summary of domestic deposits and a global perspective: U.S. -
The Turquoise-Chalcosiderite-Planerite
СПИСАНИЕ НА БЪЛГАРСКОТО ГЕОЛОГИЧЕСКО ДРУЖЕСТВО, год. 80, кн. 3, 2019, с. 48–50 REVIEW OF THE BULGARIAN GEOLOGICAL SOCIETY, vol. 80, part 3, 2019, p. 48–50 Национална конференция с международно участие „ГЕОНАУКИ 2019“ National Conference with international participation “GEOSCIENCES 2019” The turquoise-chalcosiderite-planerite solid-solution series in samples from Chala deposit, Eastern Rhodopes Тюркоаз-халкосидерит-планеритова серия от твърди разтвори в образци от находище Чала, Източни Родопи Yana Tzvetanova1, Louiza Dimowa1, Elena Tacheva1, Iskra Piroeva2, Ognyan Petrov1, Aleksandar Nikolov1 Яна Цветанова1, Луиза Димова1, Елена Тачева1, Искра Пироева2, Огнян Петров1, Александър Николов1 1 Institute of Mineralogy and Crystallography, Bulgarian Academy of Sciences, Acad. G. Bonchev Str., bl. 107, 1113 Sofia, Bulgaria; E-mail: [email protected] 2 Institute of Physical Chemistry, Bulgarian Academy of Sciences, Acad. G. Bonchev Str., bl. 11, 1113 Sofia, Bulgaria Keywords: turquoise, chalcosiderite, planerite, crystal chemistry, phosphates. Introduction quoise was also reported from the Obichnik depos- it, Zvezdel-Pcheloyad ore field, Eastern Rhodopes The turquoise group, as redefined by Foord and (Kunov, Mandova, 1997). Taggart (1998), consists of 6 members: planerite, The present study aims to show the crystal chem- turquoise, faustite, aheylite, chalcosiderite and an istry of green mineral from the turquoise group from 2+ 3+ unnamed Fe –Fe analogue with the general for- Chala deposit (Spahievo ore field) with particular at- mula A0–1B6(PO4)4–x(PO3OH)x(OH)8 4H2O, where tention to planerite end-member that was approved 2+ x = 0–2. Blue turquoise has Cu at the A position and by the IMA CNMMN as a revalidated mineral in 3+ Al at the B position, whereas green⋅ chalcosiderite 1984. -
Treatment of Textile Waste Waters by Hydroxyapatite Co-Precipitation with Adsorbent Regeneration and Reuse W
Treatment of Textile Waste Waters by Hydroxyapatite Co-Precipitation with Adsorbent Regeneration and Reuse W. Lemlikchi, P. Sharrock, M. O. Mecherri, M. Fiallo, Ange Nzihou To cite this version: W. Lemlikchi, P. Sharrock, M. O. Mecherri, M. Fiallo, Ange Nzihou. Treatment of Textile Waste Waters by Hydroxyapatite Co-Precipitation with Adsorbent Regeneration and Reuse. Waste and Biomass Valorization, Springer, 2012, 3 (1), pp.75-79. 10.1007/s12649-011-9096-0. hal-01632408 HAL Id: hal-01632408 https://hal.archives-ouvertes.fr/hal-01632408 Submitted on 16 Jan 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Treatment of Textile Waste Waters by Hydroxyapatite Co-Precipitation with Adsorbent Regeneration and Reuse W. Lemlikchi • P. Sharrock • M. O. Mecherri • M. Fiallo • A. Nzihou Abstract When dissolved calcium salts are reacted in abatement and introduced calcium concentration, indicat- aqueous medium in the presence of phosphate anions, a ing the feasibility of the process. gelatinous precipitate forms. Maturation of this precipitate eventually leads to the formation of hydroxyapatites (HA). Keywords Dye removal Hydroxyapatite Adsorbent HA is a stable solid with high specific surface area, and regeneration EliminationÁ rate Á Á interesting adsorption properties. -
Preparation and Solubility of Hydroxyapatite
JOURNAL O F RESEARC H of the National Bureau of Standards - A. Ph ys ics a nd Chemistry Vol. 72A, No. 6, N ovember- December 1968 Preparation and Solubility of Hydroxyapatite E. C. Moreno,* T. M. Gregory,* and W. E. Brown* Institute for Basic Standards, National Bureau of Standards, Washington, D.C. 20234 (August 2, 1968) Two portions of a syntheti c hydroxyapatite (HA), Ca" OH(PO'}J, full y characterized by x-ray, infrared, petrographi c, and chemi cal anal yses, were heated at 1,000 °C in air and steam atmospheres, respectively. Solubility isotherms for these two samples in the syste m Ca(OH}2 -H3PO,-H20 were determined in the pH range 5 to 7 by equilibrating the solids with dilute H3 PO. solutions. Both sam ples of HA disso lved stoichiometrically. The activity products (Ca + +)'( OH - ) (pO~f' and their standard errors-obtained by a least squares adjustment of the measurements (Ca and P concentrations and pH of the saturated solutions) subject to the conditions of electroneutralit y, constancy of the activity product, and stoichiometric dissolution - were 3.73 ± 0.5 x 10- 58 for the steam-h eated HA and 2_5, ± 0.4 x 10- 55 for the air-heated HA. Allowance was made in the calculations for the presence of the ion pairs [CaHPO. lo and [CaH2P04 1+ The hi gher solubility product for the air-heated HA is as cribed either to a change in the heat of formation brought about by partial dehydration or to a state of fine subdivision resulting from a disproportionation reacti on_ The solubility product constant s were used to cal culate the points of intersection (i.e_, sin gular points) of the two HA solubility isot herms with the isotherms of CaHPO. -
Synthesis, Characterization and Process Optimization of Bone Whitlockite
nanomaterials Article Synthesis, Characterization and Process Optimization of Bone Whitlockite Sadaf Batool 1, Usman Liaqat 1 , Zakir Hussain 1,* and Manzar Sohail 2 1 School of Chemical and Materials Engineering (SCME), National University of Sciences & Technology (NUST), Sector H-12, 44000 Islamabad, Pakistan; [email protected] (S.B.); [email protected] (U.L.) 2 Department of Chemistry, School of Natural Sciences (SNS), National University of Sciences & Technology (NUST), Sector H-12, 44000 Islamabad, Pakistan; [email protected] * Correspondence: [email protected]; Tel./Fax: +0092-51-9085-5200 Received: 26 July 2020; Accepted: 20 August 2020; Published: 17 September 2020 Abstract: Whitlockite, being the second most abundant bio-mineral in living bone, finds huge applications in tissue regeneration and implants and its synthesis into its pure form has remained a challenge. Although precipitation of whitlockite phase has been reported recently in many publications, effects of various parameters to control such phase as well as conditions for the bulk preparation of this extremely important bio-mineral have not been investigated so far. In this work, we report the precipitation of pure whitlockite phase using common precursors. As reported in the literature, whitlockite is stable in a narrow pH range, therefore; optimization of pH for the stabilization of whitlockite phase has been investigated. Additionally, in order to narrow down the optimum conditions for the whitlockite precipitation, effect of temperature and heating conditions has also been studied. The obtained solids were characterized using powder X-ray diffraction (PXRD), Fourier transform infrared spectroscopy (FTIR), Raman spectroscopy, scanning electron microscopy (SEM) and thermogravimetric analysis (TGA). -
Fluorwavellite Al3(PO4)2(OH)2F⋅5H2O
Fluorwavellite Al3(PO4)2(OH)2F⋅5H2O Crystal Data: Orthorhombic. Point Group: 2/m 2/m 2/m. Prismatic crystals display {010}, (110}, and {101}, to 3 mm. Commonly in radial or bow-tie-like sprays. Physical Properties: Essentially identical to wavellite in appearance and physical properties. Cleavage: Perfect on {110}, good on {101} and {010}. Tenacity: Brittle. Fracture: Uneven to conchoidal. Hardness = 3.5 D(meas.) = 2.30(1) D(calc.) = 2.345 Optical Properties: Transparent. Color: Colorless. Streak: White. Luster: Vitreous. Optical Class: Biaxial (+). α = 1.522(1) β = 1.531(1) γ = 1.549(1) 2V(meas.) = 71(1)° 2V(calc.) = 71.2° Orientation: X = b, Y = a, Z = c. Pleochroism: None. Dispersion: Weak, r > v. Cell Data: Space Group: Pcmm. a = 9.6311(4) b = 17.3731(12) c = 9.9946(3) Z = 4 X-ray Powder Pattern: Silver Coin mine or Wood mine, USA (unspecified). 8.53 (100), 3.223 (41), 3.430 (28), 2.580 (28), 5.65 (26), 4.81 (17), 2.101 (16) Chemistry: (1) (2) (3) Al2O3 36.79 36.68 36.94 P2O5 34.66 34.31 34.29 F 4.74 4.08 4.59 H2O [26.65] [26.52] 26.11 -O = F2 2.00 1.72 1.93 Total 100.84 99.87 100.00 (1) Silver Coin mine, Valmy, Humboldt County, Nevada, USA; average of 9 electron microprobe analyses supplemented by Raman and FTIR spectroscopy, H2O calculated from structure; corresponds to Al2.96(PO4)2(OH)1.98F1.02·5H2O. (2) Wood mine, Cocke County, Tennessee, USA; average of 9 electron microprobe analyses supplemented by Raman and FTIR spectroscopy and CHN analysis, H2O calculated from structure; corresponds to Al2.98(PO4)2(OH)2.11F0.89·5H2O. -
Geology and Mineralogy This Document Consists of 90 Pages Series A
Geology and Mineralogy This document consists of 90 pages Series A UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY SELECTED ANNOTATED BIBLIOGRAPHY OF THE GEOLOGY OF URANIFEKUUS PHOSPHORITES IN THE UNITED STATES* By Diane Curtis September 1955 Trace Elements Investigations Report 532 This preliminary report is distributed without editorial and technical review for conformity with official standards and nomenclature. It is not for public inspection or quotation. #This report concerns work done on behalf of the Division of Raw Materials of the U. S. Atomic Energy Commission, USGS - TEI-532 GEOLOGY AND MINERALOGY Distribution (Series A) No. of copies Argonne National Laboratory^ .............«..o. 1 Atomic Energy Commission,, Washington .............. 2 Battelle Memorial Institute, Columbus. ............. 1 Carbide and Carbon Chemicals Company, Y-0.2 Area. ........ 1 Division of Raw Materials, Albuquerque ............. 1 Division of Raw Materials, Butte „ . , . o . » . » « 1 Division of Raw Materials, Casper. .............•<> 1 Division of Raw Materials, Denver, ............... 1 Division of Raw Materials, Hot Springs ............. 1 Division of Raw Materials, Ishpeming .............. 1 Division of Raw Materials, Phoenix ............•*. 1 Division of Raw Materials, Plant City. ............. 1 Division of Raw Materials, St. George, ............. 1 Division of Raw Materials, Salt Lake City. ........... 1 Division of Raw Materials, Washington. ............. 3 Dow Chemical Company, Pittsburg. ................ 1 Exploration Division, -
Walsh University the Remineralization Potential of Nano
Walsh University The Remineralization Potential of Nano-Hydroxyapatite in Hydrogen Peroxide Whitening Mouthwash A Thesis by Morgan McDermott Mathematics and Sciences Submitted in partial fulfillment of the requirements for a Bachelor of Science Degree with University Honors April, 2016 Accepted by the Honors Program ______________________________________________ Peter Tandler, Ph.D. Thesis Advisor Date ______________________________________________ Tom Freeland, Ph.D. Thesis Reader Date ______________________________________________ Ty Hawkins, Ph.D. Honors Director Date Abstract The purpose of this experiment was to analyze the demineralizing effects of Colgate Optic White mouthwash on hydroxyapatite tooth enamel. Nano-hydroxyapatite particles were used to make 10% solutions with RO water, artificial saliva, 2% hydrogen peroxide, and Colgate Optic White mouthwash. Small samples from these solutions were centrifuged to create an artificial tooth that was examined for demineralization upon being treated RO water, artificial saliva, 2% hydrogen peroxide, or Colgate Optic White mouthwash. Demineralization of the samples was measured by UV-Vis spectroscopy and calcium concentration was measured to compare demineralization among the four different solutions. Calcium standards and validation samples were prepared to make a calibration curve at a wavelength of 652 nm. The results of this experiment showed that calcium concentration was determined to be greatest in samples treated with Colgate Optic White mouthwash and least in samples treated with artificial saliva. RO water and 2% hydrogen peroxide both showed calcium concentrations greater than artificial saliva, but less than Colgate Optic White mouthwash. Colgate Optic White mouthwash significantly demineralizes more than the other three solutions and there was not any significant difference between RO water and 2% hydrogen peroxide. -
Evaluation of Selected Phosphate Sources for the Control of Acid
Evaluation of selected phosphate sources for the control of acid production from pyritic coal overburden by Edward Spotts A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Land Rehabilitation Montana State University © Copyright by Edward Spotts (1990) Abstract: Acid Mine Drainage (AMD) is a serious and pervasive threat to surface and groundwater quality in the eastern Appalachian coal regions and at surface area coal mines in the western United States. Recent research has indicated that the use of phosphate materials can be an effective treatment for the amelioration of AMD. Phosphate is effective at immobilizing iron and inhibiting the production of acid associated with the oxidation of FeS2. A preliminary simulated weathering study was performed to evaluate the potential of several regional phosphate sources for controlling the production of acid from pyritic coal overburden. Sources deemed most effective were tested further for application rate determination utilizing a replicated soxhlet leaching technique described by Renton et al (1988a). Phosphate sources tested in this part of the study included two apatite ores (Cominco ore and Texas Gulf ore) at an application rate of 3% by weight apatite and two byproducts of the phosphate industry (Cominco waste and Stauffer sludge) at rates of 1%, 3% and 5% apatite by weight. Results of leachate analyses indicate that all sources at all rates of application resulted in significant decreases in titratable acidity versus a control. Acidity reductions ranged from a low of 7% for samples treated with Cominco waste (1%) to a high of 67% for Texas Gulf ore-treated samples. -
Wavellite Al3(PO4)2(OH, F)3 • 5H2O C 2001-2005 Mineral Data Publishing, Version 1
Wavellite Al3(PO4)2(OH, F)3 • 5H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 2/m 2/m 2/m. Euhedral crystals uncommon, short to long prismatic, elongated and striated k [001], with {010}, {110}, {101}, {111}, {121}, with many {hk0} forms, to several mm. Commonly in flat to spherical radial aggregates, to 3 cm; may be stalactitic, in crusts, rarely opaline massive. Physical Properties: Cleavage: Perfect on {110}; good on {101}; distinct on {010}. Fracture: Uneven to subconchoidal. Tenacity: Brittle. Hardness = 3.5–4 D(meas.) = 2.36 D(calc.) = 2.37 Optical Properties: Translucent. Color: White, greenish white, green, yellow, yellowish brown, turquoise-blue, brown, brownish black, may be zoned; colorless in transmitted light. Streak: White. Luster: Vitreous to resinous, pearly. Optical Class: Biaxial (+). Pleochroism: Weak; X = greenish; Z = yellowish. Absorption: X > Z. Orientation: X = b; Y = a; Z = c. Dispersion: r> v,weak. α = 1.518–1.535 β = 1.524–1.543 γ = 1.544–1.561 2V(meas.) = 60◦–72◦ Cell Data: Space Group: P cmn. a = 9.621(2) b = 17.363(4) c = 6.994(3) Z = 4 X-ray Powder Pattern: Black River Falls, Jackson Co., Wisconsin, USA. 8.67 (100), 8.42 (100), 3.22 (60), 5.65 (50), 3.42 (42), 4.81 (25), 2.573 (25) Chemistry: (1) (2) P2O5 33.40 34.46 Al2O3 37.44 37.12 Fe2O3 0.64 F 2.79 H2O 26.45 28.42 −O=F2 1.17 Total 99.55 100.00 • (1) Clonmel, Ireland.