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Washington State Minerals Checklist
Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite -
Litharge from Laurion. a Medical and Metallurgical Commodity from South Attika Thilo Rehren, Doris Vanhove, Herman F
L'antiquité classique Litharge from Laurion. A medical and metallurgical commodity from South Attika Thilo Rehren, Doris Vanhove, Herman F. Mussche, Mary Oikonomakou Citer ce document / Cite this document : Rehren Thilo, Vanhove Doris, Mussche Herman F., Oikonomakou Mary. Litharge from Laurion. A medical and metallurgical commodity from South Attika. In: L'antiquité classique, Tome 68, 1999. pp. 299-308. doi : 10.3406/antiq.1999.1348 http://www.persee.fr/doc/antiq_0770-2817_1999_num_68_1_1348 Document généré le 10/09/2015 Litharge from Laurion A medical and metallurgical commodity from South Attika Introduction During the first century AD, both Dioskourides of Anazarbos and Pliny the Elder discuss in some detail the preparation of lithargyros 'silver stone1 and spuma argenti 'scum of silver' for medical use of which Pliny in his Naturalis Historia (33, 1 10) says: «It is used to make an eye-wash and for women's skin to remove ugly scares and spots and as a hair-wash. Its effect is to dry, to soften, to cool, to act as a gentle purge, to fill up cavities caused by ulcers and to soften tumours... it also removes erysipelas and likewise chilblains....» (transi. H. Rackman [Loeb]) Both authors apparently rely on the same source of information. Nevertheless Pliny gives some additional information concerning the metallurgical background of its production1. Dioskourides in his De Materia Medica (V, 87) says about lithargyros that «one is made from sand called molybditis which is roasted until it is totally burned, another from silver, a third from lead. The Attic is excellent, the second is from Spain, followed by those from Dikaiarchia and Sicily» and Pliny (o.e. -
A Pxrf in Situ Study of 16Th–17Th Century Fresco Paints from Sviyazhsk (Tatarstan Republic, Russian Federation)
minerals Article A pXRF In Situ Study of 16th–17th Century Fresco Paints from Sviyazhsk (Tatarstan Republic, Russian Federation) Rezida Khramchenkova 1,2, Corina Ionescu 2,3,*, Airat Sitdikov 1,2,4, Polina Kaplan 1,2, Ágnes Gál 3 and Bulat Gareev 1 1 Analytical and Restoration Department, Institute of Archaeology of Tatarstan Academy of Science, 30, Butlerova St., 420012 Kazan, Tatarstan, Russia; [email protected] (R.K.); [email protected] (A.S.); [email protected] (P.K.); [email protected] (B.G.) 2 Archeotechnologies & Archeological Material Sciences Laboratory, Institute of International Relations, History and Oriental Studies, Kazan (Volga Region) Federal University, 18 Kremlevskaya Str., 420000 Kazan, Tatarstan, Russia 3 Department of Geology, Babe¸s-BolyaiUniversity, 1 Kogălniceanu Str., 400084 Cluj-Napoca, Romania; [email protected] 4 Laboratory of Isotope and Element Analysis, Institute of Geology and Petroleum Technologies, Kazan (Volga Region) Federal University, 18 Kremlevskaya Str., 420000 Kazan, Tatarstan, Russia * Correspondence: [email protected] Received: 13 December 2018; Accepted: 13 February 2019; Published: 15 February 2019 Abstract: Twenty frescoes from “The Assumption” Cathedral located in the island town of Sviyazhsk (Tatarstan Republic, Russian Federation)—dated back to the times of Tsar Ivan IV “the Terrible”—were chemically analyzed in situ with a portable X-ray fluorescence (pXRF) spectrometer. The investigation focused on identifying the pigments and their combinations in the paint recipes. One hundred ninety-three micropoints randomly chosen from the white, yellow, orange, pink, brown, red, grey, black, green, and blue areas were measured for major and minor elements. The compositional types separated within each color indicate different recipes. -
B Clifford Frondel
CATALOGUE OF. MINERAL PSEUDOMORPHS IN THE AMERICAN MUSEUM -B CLIFFORD FRONDEL BU.LLETIN OF THEAMRICANMUSEUM' OF NA.TURAL HISTORY. VOLUME LXVII, 1935- -ARTIC-LE IX- NEW YORK Tebruary 26, 1935 4 2 <~~~~~~~~~~~~~7 - A~~~~~~~~~~~~~~~, 4~~~~~~~~~~~~~~~~~~~~~~~~~~~~~4 4 4 A .~~~~~~~~~~~~~~~~~~~~~~~~~~4- -> " -~~~~~~~~~4~~. v-~~~~~~~~~~~~~~~~~~t V-~ ~~~~~~~~~~~~~~~~ 'W. - /7~~~~~~~~~~~~~~~~~~~~~~~~~~7 7-r ~~~~~~~~~-A~~~~ ~ ~ ~ ~ ~ ~ ~ ~ ~ -'c~ ~ ~ ' -7L~ ~ ~ ~ ~ 7 54.9:07 (74.71) Article IX.-CATALOGUE OF MINERAL PSEUDOMORPHS IN THE AMERICAN MUSEUM OF NATURAL HISTORY' BY CLIFFORD FRONDEL CONTENTS PAGE INTRODUCTION .................. 389 Definition.389 Literature.390 New Pseudomorphse .393 METHOD OF DESCRIPTION.393 ORIGIN OF SUBSTITUTION AND INCRUSTATION PSEUDOMORPHS.396 Colloidal Origin: Adsorption and Peptization.396 Conditions Controlling Peptization.401 Volume Relations.403 DESCRIPTION OF SPECIMENS.403 INTRODUCTION DEFINITION.-A pseudomorph is defined as a mineral which has the outward form proper to another species of mineral whose place it has taken through the action of some agency.2 This precise use of the term excludes the regular cavities left by the removal of a crystal from its matrix (molds), since these are voids and not solids,3 and would also exclude those cases in which organic material has been replaced by quartz or some other mineral because the original substance is here not a mineral. The general usage of the term is to include as pseudomorphs both petrifactions and molds, and also: (1) Any mineral change in which the outlines of the original mineral are preserved, whether this surface be a euhedral crystal form or the irregular bounding surface of an embedded grain or of an aggregate. (2) Any mineral change which has been accomplished without change of volume, as evidenced by the undistorted preservation of an original texture or structure, whether this be the equal volume replacement of a single crystal or of a rock mass on a geologic scale. -
Oxidized Zinc Deposits of the United States Part 2
Oxidized Zinc Deposits of the United States Part 2. Utah By ALLEN V. HEYL GEOLOGICAL SURVEY BULLETIN 1135-B A detailed study of the supergene zinc deposits of Utah UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printin~ Office Washin~ton 25, D.C. CONTENTS Page Abstract ____________________ ~------------------------------------- B1 Introduction______________________________________________________ 1 Fieldwork____________________________________________________ 1 Acknowledgments_____________________________________________ 2 Geology__________________________________________________________ 2 Location of the deposits________________________________________ 2 ~ineralogy___________________________________________________ 3 Secondary zinc minerals_ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 4 Smithsonite___ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 4 H emimorphite (calamine) __ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 6 Hydrozincite___ _ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ 7 Aurichalcite_____ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ 7 VVurtzite_____________________________________________ 8 Other secondary zinc minerals___________________________ 8 Associated minerals__ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ -
Pb-Rich Slags, Minerals, and Pollution Resulted from a Medieval Ag-Pb Smelting and Mining Operation in the Silesian-Cracovian Region (Southern Poland)
minerals Article Pb-Rich Slags, Minerals, and Pollution Resulted from a Medieval Ag-Pb Smelting and Mining Operation in the Silesian-Cracovian Region (Southern Poland) Jerzy Cabała 1,*, Rafał Warchulski 1, Dariusz Rozmus 2, Dorota Srodek´ 1 and Eligiusz Szeł˛eg 1 1 Faculty of Natural Sciences, University of Silesia, Bedzinska 60 Street, 41-200 Sosnowiec, Poland; [email protected] (R.W.); [email protected] (D.S.);´ [email protected] (E.S.) 2 The City Museum ”Sztygarka”, Legionów Polskich 69, 41-300 D ˛abrowa-Górnicza, Poland; [email protected] * Correspondence: [email protected] Received: 25 November 2019; Accepted: 24 December 2019; Published: 28 December 2019 Abstract: Since the 12th century in the Silesian-Cracovian area, lead, litharge, and silver have been produced by the pyrometallurgical processing of Pb-Ag-Zn ore. Slags and soils contaminated with heavy metals (Zn, Pb, Cd, Fe, Mn, As) were the subject of this research. Samples were collected during archaeological works in the area of early medieval metallurgical settlement. The main goals of the analyses (Scanning Electron Miscroscopy-Energy Dispersive Spectroscopy (SEM-EDS), Electron Probe Microanalyzer (EPMA), X-ray diffraction (XRD), Atomic Absorption Spectroscopy (AAS)) were the determination of the mineralogical composition of furnace batches and smelting temperatures and conditions. In soils, the anthropogenic phases enriched in Pb, Zn, Fe, Mn, P, and primary minerals like goethite, ferrihydrite, sphalerite, galena, smithsonite, minrecordite, cerussite, gypsum, anglesite, jarosite, and hemimorphite were identified. The soil from former metallurgical settlements contained up to 1106 mg kg 1 Pb, 782 mg kg 1 Zn, 4.7 mg kg 1 Cd in the fine fraction. -
Dissolution of the (001) Surface of Galena: an in Situ Assessment of Surface Speciation by ß Uid-Cell Micro-Raman Spectroscopy
American Mineralogist, Volume 92, pages 518–524, 2007 Dissolution of the (001) surface of galena: An in situ assessment of surface speciation by ß uid-cell micro-Raman spectroscopy GIOVANNI DE GIUDICI,1,* PIERCARLO RICCI,2 PIERFRANCO LATTANZI,1,3 AND ALBERTO ANEDDA2,3 1Dipartimento di Scienze della Terra, Università degli Studi di Cagliari, via Trentino 51, I-09127 Cagliari, Italy 2Dipartimento di Fisica, Università degli Studi di Cagliari, Cittadella di Monserrato, S.S. 554, I-09042 Monserrato (CA), Italy 3Laboratorio LIMINA, Università degli Studi di Cagliari, Cittadella di Monserrato, S.S. 554, I-09042 Monserrato (CA), Italy ABSTRACT The chemical evolution of the galena (001) cleavage surface dissolving in oxygen-saturated so- lutions was investigated by ß uid-cell micro-Raman Spectroscopy (μRS) and solution chemistry. In this novel design of μRS apparatus, the solution in the ß uid cell is continuously renewed. A fairly thick (several tens to hundreds of nanometers) layer forms at the galena surface in solutions with pH between 1 and 5.8. This surface layer is composed of Pb oxides, sulfates, and metastable species of sulfur. Native sulfur forms at pH 1 and 4.6, but is not a predominant surface species at pH 5.8. Dis- solution rates, measured by solution chemistry, decrease with pH and reaction time. The formation of Pb oxides in these experiments at such low pH values contrasts with thermodynamic predictions based on properties at the macroscale (bulk solution). The in situ assessment of surface speciation conÞ rms that sulfur can partially oxidize at the interface, and indicates that this process of sulfur oxidation depends on pH. -
Chapter 7. Mineral Pigments: the Colourful Palette of Nature
EMU Notes in Mineralogy, Vol. 20 (2019), Chapter 7, 283–322 Mineral pigments: the colourful palette of nature Ina REICHE National Museum, Berlin and CNRS, Paris e-mail: [email protected] The use of minerals as pigments in art and on archaeological objects, from the use of ochre in prehistoric caves to the elaborate transformation and use in ancient and modern artist palettes, is reviewed in this chapter. Starting from the purposes of the study of pigments, the chapter presents current trends in the study of coloured minerals in cultural heritage science. It emphasizes through the use of case studies the potential of these minerals in terms of information about former ways of life and especially the artistic techniques employed in ancient times. This information is gained through knowledge of geological and physicochemical processes acting on minerals and on artefacts produced by human activities. Some new trends are presented as the state of the art of how to master most of the methods and techniques useful for investigating our common cultural heritage. 1. Introduction Besides ancient glasses, ceramics and metals, mineral pigments are among the most studied materials in cultural heritage sciences. This is due to the fact that pigments play a crucial role in cultural heritage because of the wide colour palette they can provide. Beautiful colours are very decorative and persist over very long time scales so that they can even be preserved on objects dating back to the Stone Age. The available paint palette for artists evolved continuously from the use of coloured minerals or other naturally available materials such as charcoal to more elaborated paint palettes including synthetic pigments and colourants in modern and contemporaneous times. -
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). -
Crystal Structure, Morphology and Formation Mechanism of a Novel
Crystal structure, morphology and formation mechanism of a novel polymorph of lead dioxide, γ-PbO 2 Hiba Kabbara, Jaafar Ghanbaja, Abdelkrim Redjaïmia, Thierry Belmonte To cite this version: Hiba Kabbara, Jaafar Ghanbaja, Abdelkrim Redjaïmia, Thierry Belmonte. Crystal structure, morphology and formation mechanism of a novel polymorph of lead dioxide, γ-PbO 2. Jour- nal of Applied Crystallography, International Union of Crystallography, 2019, 52 (2), pp.304-311. 10.1107/S1600576719001079. hal-02105360 HAL Id: hal-02105360 https://hal.univ-lorraine.fr/hal-02105360 Submitted on 20 Apr 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. electronic reprint ISSN: 1600-5767 journals.iucr.org/j Crystal structure, morphology and formation mechanism of a novel polymorph of lead dioxide, γ-PbO2 Hiba Kabbara, Jaafar Ghanbaja, Abdelkrim Redja¨ımia and Thierry Belmonte J. Appl. Cryst. (2019). 52, 304–311 IUCr Journals CRYSTALLOGRAPHY JOURNALS ONLINE Copyright c International Union of Crystallography Author(s) of this article may load this reprint on their own web site or institutional repository provided that this cover page is retained. Republication of this article or its storage in electronic databases other than as specified above is not permitted without prior permission in writing from the IUCr. -
Minium Pb Pb4+O4
2+ 4+ Minium Pb2 Pb O4 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Tetragonal. Point Group: 4/m 2/m 2/m. Scaly; commonly earthy, pulverulent, massive. Physical Properties: Hardness = 2.5 D(meas.) = 8.9–9.2 (synthetic). D(calc.) = [8.92] Optical Properties: Semitransparent. Color: Scarlet to brownish red, may have a yellowish tint; red in transmitted light. Streak: Yellow-orange. Luster: Dull to slightly greasy. Optical Class: Uniaxial; may be weakly birefringent with anomalous green interference colors. Pleochroism: Strong; X = deep reddish brown; Z = nearly colorless. Orientation: Extinction parallel; elongation negative. n = 2.42(2) (Li). Cell Data: Space Group: P 42/mbc (synthetic). a = 8.811(5) c = 6.563(3) Z = 4 X-ray Powder Pattern: Synthetic. 3.38 (100), 2.903 (50), 2.787 (45), 2.632 (30), 1.775 (30), 3.113 (20), 1.903 (20) Chemistry: (1) (2) PbO2 34.89 Pb3O4 97.02 Fe2O3 2.70 ZnO 0.26 PbO 65.11 CaO trace SiO2 trace Total 99.98 100.00 2+ 4+ (1) Santa Marta, Spain. (2) Pb2 Pb O4. Occurrence: A rare secondary mineral in some highly oxidized lead-bearing mineral deposits; may form during mine fires. Association: Galena, cerussite, massicot, litharge, lead, wulfenite, mimetite. Distribution: Many localities, but only in small amounts. In Germany, at Langhecke, Hesse; Badenweiler, Baden-W¨urttemberg; Bleialf, Eifel district; Horhausen, Rhineland-Palatinate, and many other places. At Mies (Meˇzica),Slovenia. From Leadhills, Lanarkshire, Scotland. At Castelberg, near St. Avold, Moselle, France. From L˚angban,V¨armland,Sweden. At Sarrabus, Sardinia, Italy. -
Sending Laurion Back to the Future: Bronze Age Silver and the Source of Confusion, Internet Archaeology 56
This PDF (landscape to accommodate the table data) is a simplified version of the original article published in Internet Archaeology. All links and images connect back to the original version online. Please cite this as: Wood J. R., Hsu, Y-T and Bell, C. 2021 Sending Laurion Back to the Future: Bronze Age Silver and the Source of Confusion, Internet Archaeology 56. https://doi.org/10.11141/ia.56.9 Sending Laurion Back to the Future: Bronze Age Silver and the Source of Confusion Jonathan R. Wood, Yi-Ting Hsu and Carol Bell Silver stag rhyton (SG388) from Mycenae in the National Museum of Athens (NMA388). Photo by Zde (CC-BY-SA-3.0) Silver-bearing lead ores at Laurion in Attica were considered to have been first exploited with the introduction of coinage sometime around the birth of Classical Greece. However, in the late 20th century this chronology was radically revised earlier, to the Bronze Age, largely supported by lead isotope analyses (LIA). Here, we acknowledge that lead and silver metallurgy emerged from the earliest times but we propose that any correlation between these metals in the archaeological record is not a consequence of a geological association between lead and silver in ores such as galena until the middle of the first millennium BCE. We suggest that ancient metallurgists recognised that silver minerals (such as horn silver) dispersed in host rocks could be concentrated in molten lead and that LIA signatures of Bronze Age silver artefacts reflect the use of exogenous lead to extract silver, perhaps applying processes similar to those used to acquire silver in Bronze Age Siphnos.