Synthetic Phase with the Structure of Apatite
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Calcium Orthophosphates (Capo4): Occurrence and Properties
Prog Biomater DOI 10.1007/s40204-015-0045-z REVIEW PAPER Calcium orthophosphates (CaPO4): occurrence and properties Sergey V. Dorozhkin1 Received: 6 October 2015 / Accepted: 5 November 2015 Ó The Author(s) 2015. This article is published with open access at Springerlink.com Abstract The present overview is intended to point the Introduction readers’ attention to the important subject of calcium orthophosphates (CaPO4). This type of materials is of the Due to the abundance in nature (as phosphate ores) and special significance for the human beings because they presence in living organisms (as bones, teeth, deer antlers represent the inorganic part of major normal (bones, teeth and the majority of various pathological calcifications), and antlers) and pathological (i.e., those appearing due to calcium phosphates are the inorganic compounds of a special various diseases) calcified tissues of mammals. For exam- interest for human being. They were discovered in 1769 and ple, atherosclerosis results in blood vessel blockage caused have been investigated since then (Dorozhkin 2012a, 2013a). by a solid composite of cholesterol with CaPO4, while According to the databases of scientific literature (Web of dental caries and osteoporosis mean a partial decalcifica- knowledge, Scopus, Medline, etc.), the total amount of tion of teeth and bones, respectively, that results in currently available publications on the subject exceeds replacement of a less soluble and harder biological apatite 40,000 with the annual increase for, at least, 2000 papers. by more soluble and softer calcium hydrogenorthophos- This is a clear confirmation of the importance. phates. Therefore, the processes of both normal and Briefly, by definition, all known calcium phosphates pathological calcifications are just an in vivo crystallization consist of three major chemical elements: calcium (oxi- of CaPO4. -
Mineralogy and Geology of the \Vkgnerite Occurrence Co Santa Fe Mountain, Front Range, Cobrado
Mineralogy and Geology of the \Vkgnerite Occurrence co Santa Fe Mountain, Front Range, Cobrado GEOLOGICAL SURVEY PROFESSIONAL PAPER 955 Mineralogy and Geology of the Wignerite Occurance on Santa Fe Mountain, Front Range, Colorado By DOUGLAS M. SHERIDAN, SHERMAN P. MARSH, MARY E. MROSE, and RICHARD B. TAYLOR GEOLOGICAL SURVEY PROFESSIONAL PAPER 955 A detailed mineralogic study of wagnerite, a rare phosphate mineral occurring in the report area in Precambrian gneiss; this is the first recorded occurrence of wagnerite in the United States UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Main entry under title: Mineralogy and geology of the wagnerite occurrence on Santa Fe Mountain, Front Range, Colorado. (Geological Survey Professional Paper 955) Includes bibliographical references. 1. Wagnerite Colorado Santa Fe Mountain. 2. Geology Colorado Santa Fe Mountain. I. Sheridan, Douglas M., 1921- II. Series: United States Geological Survey Professional Paper 955. QE391.W3M56 549'.72 76-10335 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, B.C. 20402 Stock Number 024-001-02844-1 CONTENTS Page Metric-English equivalents .............................. Descriptive mineralogy Continued Page Abstract............................................................ 1 Wagnerite............................................... 5 Introduction.................................................... -
Calcium Orthophosphates: Occurrence, Properties and Major Applications Sergey V
lopmen e t an ev d D A s p c i p Dorozhkin, Bioceram Dev Appl 2014, 4:2 l i m c a a Bioceramics Development r t e i o DOI: 10.4172/2090-5025.1000081 c n o i s B ISSN: 2090-5025 and Applications Short communication Open Access Calcium Orthophosphates: Occurrence, Properties and Major Applications Sergey V. Dorozhkin* Kudrinskaja sq. 1-155, Moscow 123242, Russia Abstract The present overview is intended to point the readers’ attention to the important subject of calcium orthophosphates. They are of the special significance for the human beings because they represent the inorganic part of major normal (bones, teeth and antlers) and pathological (i.e., those appearing due to various diseases) calcified tissues of mammals. Therefore, the majority of the artificially prepared calcium orthophosphates of high purity appear to be well tolerated by human tissues in vivo and possess the excellent biocompatibility, osteoconductivity and bioresorbability. These biomedical properties of calcium orthophosphates are widely used to construct bone grafts. In addition, natural calcium orthophosphates are the major source of phosphorus, which are used to produce agricultural fertilizers, detergents and various phosphorus-containing chemicals. Thus, there is a great significance of calcium orthophosphates for the humankind and, here, an overview on the current knowledge on this subject is provided. Keywords: Calcium orthophosphates; Hydroxyapatite; Fluorapatite; In general, the atomic arrangement of all calcium orthophosphates Occurrence; Properties; Applications is built up around a network of orthophosphate (PO4) groups, which stabilize the entire structure. Therefore, the majority of calcium Introduction orthophosphates are sparingly soluble in water Table 1; however, all Due to the abundance in nature (as phosphate ores) and presence of them are easily soluble in acids but insoluble in alkaline solutions. -
Phosphates, Arsenates, Vanadates, Antimonates A
592 DESCRIPTIVE MINERALOGY Epistdite. A niobate of uncertain composition. Analysis shows chiefly SjOz, TiOz, NkO, H20. Monoclinic. In rectangular plates, also in aggregates of curved foha. Basal cleavage perfect. H. = 1-1.5. G. = 2.9. Color white, grayish brownish. Refractive index 1.67. Bound in pegmatite veins or in massive albite from ~llianehaab,Greenland. Plumboniobite. A niobatc of yttrium, uranium, lead, iron, etc. Amorphous. H. = 5-5'5. G. = 4.81. Color dark brown to black. Found in mica mines at Morogoro, German Enst Africa. Oxygen Salts 4. PHOSPHATES, ARSENATES, VANADATES, ANTIMONATES A. Anhydrous Phosphates, Arsenates, Vanadates, Antimonates Normal phosphoric acid is H3P04, and consequently normal phosphates I 11 m have the formulas RtPOa, R3(PO4)2 and RPO4, and similarly for the arse- nates, etc. Only a comparatively small number of species conform to this simple formula. Most species contain more than one metallic element, and in the prominent Apatite Group the radical (CaF), (CaCI) or (PbCI) enters; " in the Wagnerite Group we have similarly (kF) or (ROH). XENOTIME. Tetragonal. Axis c = 0.6187, zz' (1 11 A ill) = 55" 301, 22" (111 A 771) = 82" 22'. In crystals resembling zircon in habit; sometimes compounded with zircon in parallel position (Fig. 462, p. 173). In 972 rolled grains. Cleavage: m (110) perfect. Fracture uneven and splintery. Brittle. H. = 4-5. G. = 4.454.56. Luster resinous to vitreous. Color yellowish brown, reddish brown, hair-brown, flesh-red, grayish white, wine-yellow, pale yellow; streak pale brown, yellow- ish or reddish. Opaque. Optically + . w = 1.72. e = 1-81. -
Italian Type Minerals / Marco E
THE AUTHORS This book describes one by one all the 264 mi- neral species first discovered in Italy, from 1546 Marco E. Ciriotti was born in Calosso (Asti) in 1945. up to the end of 2008. Moreover, 28 minerals He is an amateur mineralogist-crystallographer, a discovered elsewhere and named after Italian “grouper”, and a systematic collector. He gradua- individuals and institutions are included in a pa- ted in Natural Sciences but pursued his career in the rallel section. Both chapters are alphabetically industrial business until 2000 when, being General TALIAN YPE INERALS I T M arranged. The two catalogues are preceded by Manager, he retired. Then time had come to finally devote himself to his a short presentation which includes some bits of main interest and passion: mineral collecting and information about how the volume is organized related studies. He was the promoter and is now the and subdivided, besides providing some other President of the AMI (Italian Micromineralogical As- more general news. For each mineral all basic sociation), Associate Editor of Micro (the AMI maga- data (chemical formula, space group symmetry, zine), and fellow of many organizations and mine- type locality, general appearance of the species, ralogical associations. He is the author of papers on main geologic occurrences, curiosities, referen- topological, structural and general mineralogy, and of a mineral classification. He was awarded the “Mi- ces, etc.) are included in a full page, together cromounters’ Hall of Fame” 2008 prize. Etymology, with one or more high quality colour photogra- geoanthropology, music, and modern ballet are his phs from both private and museum collections, other keen interests. -
Environmental Mineralogy Lecture (Overview with Case Studies, Methods Applied, Etc.)
Oxford Miami Chief Little Turtle 1795 Miami University, Oxford, Ohio Miami University, Oxford, Ohio 9-Mar Environmental Mineralogy Lecture (overview with case studies, methods applied, etc.) 23-Mar Sediment hosted U & V deposits of the Colorado Plateau 30-Mar Heavy metals in soils: Solid phase characterization: Overview and XRD 13-Apr Heavy metals in soils: synchrotron methods 20-Apr Heavy metals in soils: synchrotron methods 11-May Mineral water interface processes 25-May Mineral water interface processes 1-Jun Pb, Zn, F contamination from MVT deposits (Missouri, Olkush, Illinois) 15-Jun To be announced 20-Jun To be announced Go to www.cas.muohio.edu/~rakovajf/AGH.html For lecture slides and associated readings. Environmental Mineralogy: Studies of the dynamic interaction of minerals and the environment and their affect on environmental chemistry, water quality, human health, contaminant remediation, microbial processes, etc. Environmental Mineralogy is a multidisciplinary endeavor that encompasses mineralogy, geology, biology, medicine, materials science and engineering. The intersection of the biological, geological, and material sciences is exemplified no better than in the importance and interest in the structure, chemistry, and environmental significance of the phosphate mineral apatite. Apatite Ca5(PO4)3(F,OH,Cl) * Fluorapatite Ca5(PO4)3F Hydroxylapatite Ca5(PO4)3OH Chlorapatite Ca5(PO4)3Cl * The most common variety Apatite Ca5(PO4)3(F*,OH,Cl) + REE, Mn, Sr, Pb, U,… Geologic Apatite • Igneous Rocks • Metamorphic Rocks • Sedimentary -
Calcium Orthophosphates Occurrence, Properties, Biomineralization, Pathological Calcification and Biomimetic Applications
review REVIEW Biomatter 1:2, 121-164; October/November/December 2011; © 2011 Landes Bioscience Calcium orthophosphates Occurrence, properties, biomineralization, pathological calcification and biomimetic applications Sergey V. Dorozhkin Kudrinskaja sq. 1-155; Moscow, Russia Key words: calcium orthophosphates, hydroxyapatite, fluorapatite, bones, teeth, antlers, calcification, crystallization, biomimetics The present overview is intended to point the readers’ attention 1873,5 while the crystallographic faces of a natural calcium apa- to the important subject of calcium orthophosphates. tite were described in 1883.6 Furthermore, a paper on a behavior This type of materials is of special significance for human of an undisclosed calcium orthophosphate in organisms of carni- beings, because they represent the inorganic part of vores was published in 1883.7 Further, the quantitative analysis major normal (bones, teeth and antlers) and pathological 8 (i.e., those appearing due to various diseases) calcified tissues of a calcium orthophosphate was performed in 1884, followed 9 of mammals. For example, atherosclerosis results in blood by remarks by C. Glaser in 1885. In the 1880s, occurrence of 10 11-13 vessel blockage caused by a solid composite of cholesterol a calcium apatite and another calcium orthophosphate in a with calcium orthophosphates, while dental caries and metallurgical slag was discovered. Chemical reactions between osteoporosis mean a partial decalcification of teeth and bones, calcium orthophosphates and other chemicals were investigated respectively, that results in replacement of a less soluble and in 1891.14 Research papers on bone repairing are known since at harder biological apatite by more soluble and softer calcium least 1892,15 while the earliest well-documented systematic stud- hydrogenphosphates. -
Sintering and Mechanical Properties of Magnesium and Fluorine Co-Substituted Hydroxyapatites
Journal of Biomaterials and Nanobiotechnology, 2013, 4, 1-11 1 http://dx.doi.org/10.4236/jbnb.2013.41001 Published Online January 2013 (http://www.scirp.org/journal/jbnb) Sintering and Mechanical Properties of Magnesium and Fluorine Co-Substituted Hydroxyapatites Samia Nsar, Amel Hassine, Khaled Bouzouita* Laboratory of Industrial Chemistry, National School of Engineering, Sfax, Tunisia. Email: *[email protected] Received September 5th, 2012; revised October 17th, 2012; accepted November 10th, 2012 ABSTRACT Biological apatites contain several elements as traces. In this work, magnesium and fluorine co-substituted hydroxyapa- tites with the general formula Ca9Mg(PO4)6(OH)2-yFy, where y = 0, 0.5, 1, 1.5 and 2 were synthesized by the hydrother- mal method. After calcination at 500˚C, the samples were pressureless sintered between 950˚C and 1250˚C. The substi- tution of F− for OH− had a strong influence on the densification behavior and mechanical properties of the materials. Below 1200˚C, the density steeply decreased for y = 0.5 sample. XRD analysis revealed that compared to hydroxyl- fluorapatite containing no magnesium, the substituted hydroxyfluorapatites decomposed, and the nature of the decom- position products is tightly dependent on the fluorine content. The hardness, elastic modulus and fracture toughness of these materials were investigated by Vickers’s hardness testing. The highest values were 622 ± 4 GPa, 181 ± 1 GPa and 1.85 ± 0.06 MPa·m1/2, respectively. Keywords: Hydroxyapatite; Magnesium, Fluorine; Sintering; Mechanical Properties 1. Introduction tite containing magnesium and fluorine would be more suitable for dental and orthopedic applications. Hydroxyapatite (HA) is widely used in orthopedic and Hence, it is thought worthwhile to synthesize and char- reconstructive surgery thanks to its excellent bioactivity acterize Mg/F-co-substituted hydroxypatites. -
Introduction to Apatites
Chapter 1 Introduction to Apatites Petr Ptáček Additional information is available at the end of the chapter http://dx.doi.org/10.5772/62208 Abstract Apatite is the generic name, which was first introduced by German geologist A.G. Werner. These minerals and their synthetic analogs represent a major class of ionic compounds and the most common crystalline form of calcium phosphates, which are of interest of many industrial branches and scientific disciplines. Since, apatite (fluora‐ patite) is the most abundant phosphate mineral, apatite bearing phosphate rocks represents an important source of inorganic phosphorus. First chapter of this book introduces the basic concepts of nomenclature, composition, classification, crystal structure, mineralogy and properties of minerals from the supergroup of apatite. Furthermore, the minerals from the group of apatite and polysomatic apatites are described. Since, the most of the topics mentioned in this chapter will be developed in the following chapters, the key concepts provided in this chapter are important to understood before proceeding further. Keywords: Apatite, Group of Apatite, Polysomatic Apatites, Fluorapatite, Hydroxyla‐ patite, Chlorapatite, Vanadinite The minerals1 [1],[2],[3],[4],[5] from the apatite group2 [6] are classified as hexagonal or pseudo‐ hexagonal monoclinic anhydrous phosphates containing hydroxyl or halogen of the generic formula3: 1Minerals are individual components comprising rocks formed by geological processes classified according to their crystal structure and chemical composition. The total number of minerals accepted by mineralogical community is about 4000. Mineraloids are mineral-like phases including synthetic materials, human-treated substances, and some biological materials, which do not fulfill the criteria for the definition of mineral species [2]. -
Thermal Characterization of Magnesium Containing Ionomer Glasses
Thermal characterization of magnesium containing ionomer glasses ELENI MARIA KARTELIA Supervisor: Dr. A. Stamboulis Thesis submitted for the degree of MRes Biomaterials University of Birmingham School of Engineering Department of Metallurgy and Materials September, 2010 University of Birmingham Research Archive e-theses repository This unpublished thesis/dissertation is copyright of the author and/or third parties. The intellectual property rights of the author or third parties in respect of this work are as defined by The Copyright Designs and Patents Act 1988 or as modified by any successor legislation. Any use made of information contained in this thesis/dissertation must be in accordance with that legislation and must be properly acknowledged. Further distribution or reproduction in any format is prohibited without the permission of the copyright holder. ACKNOWLEDGMENTS I would like to thank my supervisor Dr. A. Stamboulis for her help and encouragement during my project. Without her support, I feel that I would not have been able to complete this work. I would also like to express my gratitude to Dr. D. Holland at University of Warwick for her helping on DSC measurements. Many thanks are given to academic staff and technicians of the School of Metallurgy and Materials. I would like to thank sincerely the Phd students Praveen Ramakrishnan, Georgina Kaklamani, Siqi Zhang and Mitra Kashani for their significant help through my experimental work. Last but not least, I would like to thank my family for their support and understanding. Special thanks to Thanos Papaioannou. 2 TABLE CAPTIONS CHAPTER 2: MATERIALS AND METHODS Table 2.1.2: Composition of Mg substituted alumino-silicate glasses. -
The Crystal Structure of Althausite, Mg.(P04)2(OH,O)(F,D)
----- ----- American Mineralogist, Volume 65, pages 488-498, 1980 The crystal structure of althausite, Mg.(P04)2(OH,O)(F,D) CHRISTIAN R0MMING Kjemisk Institutt, Universitetet i Oslo, Blindern, Oslo 3, Norway AND GUNNAR RAADE Instituttfor Geologi, Universitetet i Oslo, Blindern, Oslo 3, Norway Abstract The crystal structure of althausite was solved by direct methods and refined to a final R value of 0.022 for 1164 high-angle reflections (sin 8/A > 0.45A -I) with I> 2.50. The position of the hydrogen atom was found from a difference Fourier synthesis. The structure is ortho- rhombic Pnma with a = 8.258(2),b = 6.054(2),c = 14.383(5)A.Magnesium atoms occur in both five- and six-fold coordination, and the coordination polyhedra are highly distorted. The Mg octahedra form chains along b by edge-sharing. Hydroxyl and fluorine occur in a largely ordered distribution among two different structural sites and occupy alternating posi- tions along 'channels' parallel to b. Partial vacancy in the (OH,F) sites is confirmed, the pop- ulation factor for the F site being 81 percent. The crystal-chemical formula of althausite is therefore Mg4(P04)2(OH,0)(F,D) with Z = 4. The cleavages in althausite, {001} perfect and {101} distinct, occur along planes crossing relatively few bonds and leave the chains of Mg octahedra unbroken. Bond-strength calcu- lations for althausite and wagnerite are presented and the OH content in wagnerite is dis- cussed. Preliminary results of hydrothermal syntheses indicate the existence of a series from F- wagnerite to OH,F-wagnerite and from OH-althausite to OH,F-althausite. -
Shin-Skinner January 2018 Edition
Page 1 The Shin-Skinner News Vol 57, No 1; January 2018 Che-Hanna Rock & Mineral Club, Inc. P.O. Box 142, Sayre PA 18840-0142 PURPOSE: The club was organized in 1962 in Sayre, PA OFFICERS to assemble for the purpose of studying and collecting rock, President: Bob McGuire [email protected] mineral, fossil, and shell specimens, and to develop skills in Vice-Pres: Ted Rieth [email protected] the lapidary arts. We are members of the Eastern Acting Secretary: JoAnn McGuire [email protected] Federation of Mineralogical & Lapidary Societies (EFMLS) Treasurer & member chair: Trish Benish and the American Federation of Mineralogical Societies [email protected] (AFMS). Immed. Past Pres. Inga Wells [email protected] DUES are payable to the treasurer BY January 1st of each year. After that date membership will be terminated. Make BOARD meetings are held at 6PM on odd-numbered checks payable to Che-Hanna Rock & Mineral Club, Inc. as months unless special meetings are called by the follows: $12.00 for Family; $8.00 for Subscribing Patron; president. $8.00 for Individual and Junior members (under age 17) not BOARD MEMBERS: covered by a family membership. Bruce Benish, Jeff Benish, Mary Walter MEETINGS are held at the Sayre High School (on Lockhart APPOINTED Street) at 7:00 PM in the cafeteria, the 2nd Wednesday Programs: Ted Rieth [email protected] each month, except JUNE, JULY, AUGUST, and Publicity: Hazel Remaley 570-888-7544 DECEMBER. Those meetings and events (and any [email protected] changes) will be announced in this newsletter, with location Editor: David Dick and schedule, as well as on our website [email protected] chehannarocks.com.