Investigations Methods to Study Corrosion of Some Ancient Islamic Copper Coins at Faculty of Arts Museum, Sohag University, Egypt

Total Page:16

File Type:pdf, Size:1020Kb

Investigations Methods to Study Corrosion of Some Ancient Islamic Copper Coins at Faculty of Arts Museum, Sohag University, Egypt Investigations methods to study corrosion of some ancient Islamic copper coins at Faculty of arts museum, Sohag university, Egypt Ahmed Elsayed Department of Applied Science and Technology, Politecnico di Torino, 10126, Turin, Italy [email protected] Abstract Through the time, copper affected by There are different factors which effect on the deterioration factors that interact with environment. corrosion of metallic artifacts through the time for Oxygen causes corrosion of copper artifacts and example: Metal Type, Structure, Surface and Thickness forms copper oxides, meanwhile it starts to of Metal, Metal Resistance of Corrosion, burial mineralize and backs to its natural structure. Environment, pH value, the amount of Oxygen ions, This research studied five Islamic copper coins chlorine, carbons, and others, and the present at faculty of arts museum in Sohag University by environment of the metals. Copper slowly oxidizes by Examination and Analytical methods to identify the oxygen to form Cuprite (Cu 2O) which changes to corrosion nature and its effects on the coins. Tenorite (CuO). With the exists of chlorine ions it forms The Experimental Techniques were used, such nantokite (CuCl), Atacamite, Paratacamite as Stereo microscope, X-Ray Radiography, SEM- (Cu 2(OH) 3Cl), and malachite CuCo 3Cu (OH) 2. [4-6] EDX, and XRD. Results show that coins have more cracks and This research aims to identify the corrosion different corrosion layers. The chemical study (EDX- layers of five copper coins, which are stored in Faculty XRD) shows that the main element in coins is copper of arts museum, Sohag university, Egypt. These coins with some other elements such as sulfur, chloride, were registered as Islamic coins and Extracted from calcium, magnesium, aluminum, and silicon which Fustat Excavations in Egypt. These coins suffered from can be found in Egyptian soil composition or as bad storage without any treatments before storage to blemish in metals compound. stop the corrosion process, so they are completely The main compounds were copper oxides, mineralized in their plastic bag. The dimension of these Cuprite (Cu 2O), and Tenorite (CuO). Copper coins are about 1- 2.5 cm as there are missing parts of chlorides as Atacamite, Paratacamite (Cu 2(OH) 3Cl) the coins and these parts attached to others so we can’t as result of Chloride Ions. measure the right dimension of the coins as can be seen in (figure 1) Key words: Copper Coins, SEM-EDX, XRD, Corrosion. ! ! C1 C2 C4 C5 # ! INTRODUCTION ! Metals are one of the most materials which were used through ages in all life activities. The uses of metals in Egypt started from ancient Egyptian age, Christian age, Islamic age, and modern age, and the C3 workers used copper, silver, gold, and some alloys like bronze, brass, billon to make their tools [1]. Numismatic are important evidence about the speared of the commercial and affairs ways, and some secrets from the ancient worlds. Most of Coins can survive in different environmental conditions that we Fig. 1. The examined Coins can find many coins in excavations sites with different metals constitutes such as gold, Silver, copper, and some ! alloys. [2-4] 197 II. ! EXPERMINTAL oxygen amount increased in the media. It can have observed that some coins attached with others and there Different methods for Examinations and are many cracks on the surface (figure 3A& B, 4A, 5A, analysis of these Coins were used. 7B) Nondestructive X-Ray radiography [(Villa genius 500i) combined with computer and photo unit A (Fuji computer Radiography CR-IR 359)]. The coins were exposed to X-Ray waves in order to give good Fig. 3 (A) coin photos of the coins’ conditions and the corrosion layers C1 covered [7,8]. with cuprite SEM-EDX model [(JEOL-JSM 5300) attached with some with (Oxford) EDX unit] used to identify the elements Tenorite and and morphological structure of the coins [9, 10]. Atacamite Finally, XRD [Phillips PW 1840 X-Ray Diffraction] was used to identify the coin’s compositions and corrosion products [6, 11]. The 20 X operation conditions were as follows: Generator Tension {kV} 40, Generator Current {mA} 30, starting angle 2 Ɵ°= 4.025, and ending angle 2 Ɵ°= 69.975. B III. ! RESULTS AND DISCUSSION Fig. 3 (B) coin X-ray Radiography images illustrated that all C1 with coins were fully transformed and mineralized, so the crakes and coins appear in white color without any dark areas in the attached with coins (figures 2) some broken pieces 20 X A Fig. 4 (A) coin C2 covered of mixed cuprite with some Tenorite and Atacamite 30 X B Fig. 4 (B) coin C2 illustrated the crystals of Cuprite, Fig. 2. X-Ray Radiography photos of the coins and Atacamite, these photo illustrated the full mineralized of all coins and Paratacamite I. ! STEREO MICROSCOPE 60 X The investigation of the coins by using stereo Microscope, illustrated the condition of the coins in different colors. The cover of the coins is Cuprite(Cu 2O) which caused by the interaction of the coins with oxygen (figure 3-7), some black areas of Tenorite (CuO) resulted from the transformation of Cuprite when the 198 ! ! A A Fig. 5 (A) Fig. 7(A) coin coin C3 C5, mixed of covered with Atacamite cuprite with and some Paratacamite Tenorite and with Cupite Atacamite 20 X 70 X B B Fig. 5 (B) Fig. 7 (B) coin C3 coin C5, illustrated coverd of the layer of Cuprite and Atacamite some and Atacamite& Paratacamite areas. attached with 50 X another piece 30 X Paratacamite 2. ! SEM-EDX The electron microscopy which attached with EDX gives good information about the condition of the coins in a wide scale. EDX gives an indication about the coin’s elements. The results confirm that all coins are consisting of copper which is the main element with A some other elements related to soil elements and Fig. 6 (A) corrosion products [figure 8-12]. coin C4 covered of cuprite with Atacamite and Paratacamite. ! ! 100 X ! 20 X ! Fig. 8, SEM image of coin C1, shows a lot of ! cracks B Fig. 6 (B) Cu = 98.93 % coin C4, Cl = 0.20 % mixed of Ca= 0.47 % Tenorite and S = 0.39 % counts Cuprite with some Atacamite spots. ! 30 X Fig 9. EXD of coin C1 KeV ! 199 Cu = 96.57 % Cl = 0.26 % Al = 3.17 % counts 100 X KeV Fig. 10. SEM image of coin C2, Shows Fig. 15. EDX of coin C4 Atcamite layer on Cuprite Cu = 90.59 % Cl = 0.90 % Ca = 0.41 % Al = 7.48 % Mg = 0.62 % counts Fog. 16 SEM image of coin C5, illustrates Atacamite layer on Cuprite Fig 11. EXD of coin C2 KeV Cu = 98.20 % Cl = 0.72 % Ca = 0.61 % s count Al =0.28 % Si = 0.19 % 200 X KeV Fig. 12. SEM image of Coin 3 Illustrate the Fig. 17. EDX of coin C5 weakness of the corrosion layer as sponge shape on 3. ! XRD results Cu = 98.84 % The results of XRD proved that all coins are Cl = 0.37 % fully transformed which related to the oxygen Al = 0.35 % interaction with the copper as Cuprite and Tenorite counts Fe = 0.27 % compounds as major compounds. The existing of K = 0.62 % chlorine in the soil indicates that, Atacamite, Paratacamite, and Malacite are corrosion products. XRD patterns illustrated the composition KeV of coins (figure 18-22) Fig. 13. EDX of coin C3 Major: Cuprite = 56.61% Traces: Tenorite = 4.16% Atacamite= 1.89% Paratacamite= 2.65% 200 X Fig. 14. SEM image of coin C4 illustrates a lot of Fig. 18, XRD chart of Coin C1 cracks on the surface 200 Atacamite, and Paratacamite. In addition, the bad storage way in the museum by placing these coins in plastic without any restoration and conservation Major: Cuprite = 71.29 % Traces: Tenorite = 3.39 % process. These factors caused bad condition of the coins, Atacamite = 15.74 % and encourage the broken pieces to stuck together as can Paratacamite = 9.56 % be seen in the microscopy photos. Acknowledgment Author is immensely grateful to Dr. Ahmed S. Afify, ADECO CO. for Environmental Consultations, Fig. 19, XRD of coin C2 KSA) for his comments and modifications of the manuscript. REFERENCES Major: Cuprite = 61.21% Traces: Atacamite = 28.78% ""! Al-Saad, Ziad, and Bani-Hani, M. Corrosion Paratacamite = 10 % Behavior and Preservation of Islamic Silver Alloy Coins. Strategies for Saving our Cultural Heritage. Proceedings of International Conference on Strategies for Saving Indoor Metallic Collections. Cairo. 2007. Print. #"! Al-Zahrani, Abdulnaser, and Mohamed Fig. 20, XRD of coin C3 Ghoniem. "A Characterization of Coins from the Najran Hoard, Saudi Arabia, Prior to Conservation." International Journal of Conservation Science 3.3 (2012). Print. Major: Cuprite = 82.60% $"! Marabelli, Maurizio. "The Monument of Traces: Atacamite = 9.05% Paratacamite = 8.33% Marcus Aurelius: Research and Conservation." Ancient and Historic Metals: Conservation and Scientific Research (1994): 1-19. Print. %"! FitzGerald, KP, et al. "Atmospheric Corrosion of Copper and the Colour, Structure and Composition of Natural Patinas on Copper." Corrosion Science 48.9 (2006): 2480-509. Fig. 21, XRD of Coin C4 Print. &"! Shoesmith, D. Mechanism of copper corrosion in aqueous environments. A report from the Swedish National Council for Nuclear Waste’s Major: Cuprite = 66.22% scientific workshop, on November 16, 2009. Traces: Atacamite = 28.7% Malachite = 5.70% '"! Ghoniem, Mohamed. "The Characterization of a Corroded Egyptian Bronze Statue and a Study of the Degradation Phenomena." International Journal of Conservation Science 2.2 (2011). Print. ("! Pollard, A Mark. Analytical Chemistry in Archaeology. Cambridge University Press, Fig.22, XRD of coin C5 2007. Print. )"! Schreiner, M, et al. "X-Rays in Art and Archaeology: An Overview." Powder IV.
Recommended publications
  • 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
    [Show full text]
  • Final Report FAD-2010-0046 TBCC
    EUROPEAN COMMISSION JOINT RESEARCH CENTRE Institute for Reference Materials and Measurements European Union Reference Laboratory for Feed Additives JRC.DG.D.6/CvH/PRO/ag/ARES(2011)473276 EURL Evaluation Report on the Analytical Methods submitted in connection with the Application for the Authorisation of Feed Additives according to Regulation (EC) No 1831/2003 Dossier related to: FAD-2010-0046 CRL/100051 Product Name: Tribasic copper chloride (TBCC) Active Substance(s): Di copper chloride tri hydroxide; crystal form atacamite/paratacamite Rapporteur Laboratory: European Union Reference Laboratory for Feed Additives (EURL-FA) Geel, Belgium Report prepared by: Piotr Robouch (EURL-FA) Report revised by: Gerhard Buttinger (EURL-FA) Date: 02/05/2011 Report approved by: Christoph von Holst Date: 02/05/2011 EURL Evaluation Report on “Di copper chloride tri hydroxide” EXECUTIVE SUMMARY In the current application authorisation is sought under articles 4(1) for Di copper chloride tri hydroxide under the category "nutritional additives", functional group 3(b) "compounds of trace elements", according to the classification system of Annex I of Regulation (EC) No 1831/2003. Authorisation is sought for the use of the feed additive for all animal species and categories. Di copper chloride tri hydroxide (Cu2Cl(OH)3, also called tribasic copper chloride – TBCC) is a pure form of crystalline copper (II) chloride hydroxide containing a minimum of 95 % of a defined ratio of the polymorphs atacamite and paratacamite - equivalent to a minimum content of total copper of 58 %. The feed additive is intended to be incorporated into premixtures and feedingstuffs. The Applicant suggested the following maximum levels of total copper in the feedingstuffs ranging from 10 to 170 mg/kg depending on the species of interest.
    [Show full text]
  • Uranium in Situ Leaching
    IAEA-TECDOC-720 Uranium in situ leaching Proceedings Technicala of Committee Meeting held in Vienna, 5-8 October 1992 INTERNATIONAL ATOMIC ENERGY AGENC\ /A Y The IAEA doe t normallsno y maintain stock f reportso thin si s series. However, microfiche copies of these reports can be obtained from IIMIS Clearinghouse International Atomic Energy Agency Wagramerstrasse5 P.O. Box 100 A-1400 Vienna, Austria Orders shoul accompaniee db prepaymeny db f Austriao t n Schillings 100,- in the form of a cheque or in the form of IAEA microfiche service coupons which may be ordered separately from the INIS Clearinghouse. Copies of this IAEA-TECDOC may be obtained from: Nuclear Material Fued san l Cycle Technology Section International Atomic Energy Agency Wagramerstrasse 5 P.O. Box 100 A-1400 Vienna, Austria URANIU SITMN I U LEACHING IAEA, VIENNA, 1993 IAEA-TECDOC-720 ISSN 1011-4289 Printe IAEe th AustriAn y i d b a September 1993 FOREWORD The IAEA's latest published estimates show that nuclear power production worldwide will maintain modest growth well into the next century. These estimates indicate that nuclear energy production will gro averagn wo 1.5y eb % 2.5o t year %pe r worldwide ove nex e decadeso rth tw t s i t I . for this reason that despite the continuing depressed uranium market, the question of uranium supply demand an d remain issun sa e that needaddressee b o st monitoredd dan developmentsw Ne . e du , to the recent entry of the Commonwealth of Independent States and China into the uranium market, increase such a need.
    [Show full text]
  • Volborthite Cu3v2o7(OH)2 • 2H2O C 2001-2005 Mineral Data Publishing, Version 1
    Volborthite Cu3V2O7(OH)2 • 2H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic, pseudohexagonal. Point Group: 2/m. Typically as rosettelike aggregates of scaly crystals, which may have a hexagonal or triangular outline, to 5 mm. Physical Properties: Cleavage: One, perfect. Hardness = 3.5 D(meas.) = 3.5–3.8 D(calc.) = 3.52 Optical Properties: Semitransparent. Color: Dark olive-green, green, yellowish green; green to yellowish green in transmitted light. Luster: Vitreous, oily, resinous, waxy, pearly on the cleavage. Optical Class: Biaxial (–) or biaxial (+). Pleochroism: Faint. Dispersion: r<v,r>v, inclined. α = 1.820–2.01 β = 1.835–2.05 γ = 1.92–2.07 2V(meas.) = 63◦–83◦ Cell Data: Space Group: C2/m. a = 10.610(2) b = 5.866(1) c = 7.208(1) β =95.04(2)◦ Z=2 X-ray Powder Pattern: Monument No. 1 mine, Arizona, USA. 7.16 (10), 2.643 (7), 2.571 (7), 2.389 (7), 4.103 (5), 3.090 (5), 2.998 (5) Chemistry: (1) (2) (1) (2) V2O5 36.65 38.32 CuO 48.79 50.29 SiO2 1.37 H2O [11.49] 11.39 V2O3 1.70 Total [100.00] 100.00 (1) Scrava mine, Italy; by electron microprobe; V2O3 assumed for charge balance, H2Oby 5+ 3+ • • difference; corresponds to Cu2.89V1.90V0.11Si0.11O7(OH)2 2H2O. (2) Cu3V2O7(OH)2 2H2O. Occurrence: An uncommon secondary mineral in the oxidized zone of vanadium-bearing hydrothermal mineral deposits. Association: Brochantite, malachite, atacamite, tangeite, chrysocolla, barite, gypsum. Distribution: In Russia, originally from an unknown locality; later identified at the Sofronovskii copper mine, near Perm, and at Syssersk and Nizhni Tagil, Ural Mountains.
    [Show full text]
  • Articles Devoted to Silicate Minerals from Fumaroles of the Tol- Bachik Volcano (Kamchatka, Russia)
    Eur. J. Mineral., 32, 101–119, 2020 https://doi.org/10.5194/ejm-32-101-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Unusual silicate mineralization in fumarolic sublimates of the Tolbachik volcano, Kamchatka, Russia – Part 1: Neso-, cyclo-, ino- and phyllosilicates Nadezhda V. Shchipalkina1, Igor V. Pekov1, Natalia N. Koshlyakova1, Sergey N. Britvin2,3, Natalia V. Zubkova1, Dmitry A. Varlamov4, and Eugeny G. Sidorov5 1Faculty of Geology, Moscow State University, Vorobievy Gory, 119991 Moscow, Russia 2Department of Crystallography, St Petersburg State University, University Embankment 7/9, 199034 St. Petersburg, Russia 3Kola Science Center of Russian Academy of Sciences, Fersman Str. 14, 184200 Apatity, Russia 4Institute of Experimental Mineralogy, Russian Academy of Sciences, Academica Osypyana ul., 4, 142432 Chernogolovka, Russia 5Institute of Volcanology and Seismology, Far Eastern Branch of Russian Academy of Sciences, Piip Boulevard 9, 683006 Petropavlovsk-Kamchatsky, Russia Correspondence: Nadezhda V. Shchipalkina ([email protected]) Received: 19 June 2019 – Accepted: 1 November 2019 – Published: 29 January 2020 Abstract. This is the initial paper in a pair of articles devoted to silicate minerals from fumaroles of the Tol- bachik volcano (Kamchatka, Russia). These papers contain the first systematic data on silicate mineralization of fumarolic genesis. In this article nesosilicates (forsterite, andradite and titanite), cyclosilicate (a Cu,Zn- rich analogue of roedderite), inosilicates (enstatite, clinoenstatite, diopside, aegirine, aegirine-augite, esseneite, “Cu,Mg-pyroxene”, wollastonite, potassic-fluoro-magnesio-arfvedsonite, potassic-fluoro-richterite and litidion- ite) and phyllosilicates (fluorophlogopite, yanzhuminite, “fluoreastonite” and the Sn analogue of dalyite) are characterized with a focus on chemistry, crystal-chemical features and occurrence.
    [Show full text]
  • Vistore™ Copper Phibro Has Used Basic Copper Chloride Since It Was Introduced by Micronutrients
    Technical Bulletin Information from Phibro Technical Services Vistore™ Copper Phibro has used Basic Copper Chloride since it was introduced by Micronutrients. Our quality program monitors the efficacy and safety of our ingredients through detailed, routine analyses. These analyses go beyond the major element (Cu) and the contaminants (Pb, Cd, As, Hg, dioxins and furans) to include a 162 point elemental fingerprint and scans of the crystalline structure to confirm product consistency. The analytical history we have accumulated through our DQA® program provides us an understanding of potential quality issues and a basis for ensuring the quality of the Phibro Vistore Copper. Vistore Copper - A Single Chemical Formula Cu2(OH)3Cl Many Names: Multiple Crystalline Structures: • Basic Copper Chloride (AAFCO name) • Vistore Cu 580 (Phibro trade name) • Tribasic copper chloride • Intellibond® C (Micronutrients trade name) • Copper chloride hydroxide • Copper hydroxide chloride • Copper hydroxychloride • Dicopper chloride trihydroxide • Copper trihydroxyl chloride Downs, R.T. and Hall-Wallace, M. (2003) The American Mineralogist Crystal Structure Database. A variety of names, are used for Basic Copper Chloride based on different nomenclatures. All of those listed above Vistore Cu 580 are correct and describe the same compound. Although there is only one empirical formula for Basic Copper Chloride, it can crystallize in different configurations to form four different crystalline structures. Crystalline structure is dependent on the reaction conditions at the time the crystals are formed. Phibro’s choice is to provide a product that contains a mixture of the three primary crystalline structures, thereby avoiding a shift from 100% “ ” form (Atacamite) to 100% “ ” form (Botallackite). Technical Bulletin Phibro’s Chosen Path – Providing Efficacy, Food Safety and Value We have done our homework and selected a partner that will meet the most stringent quality programs.
    [Show full text]
  • Changes in Bornite (Cu5fes4) After Heating in Air: Mössbauer Effect
    Vol. 134 (2018) ACTA PHYSICA POLONICA A No. 5 Proceedings of the All-Polish Seminar on Mössbauer Spectroscopy, Goniądz, Poland, June 17–20, 2018 Changes in Bornite (Cu5FeS4) after Heating in Air: Mössbauer Effect Study M. Kądziołka-Gaweła;∗ and Z. Adamczykb aInstitute of Physics, University of Silesia in Katowice, 75 Pułku Piechoty 1a, 41-500 Chorzów, Poland bInstitute of Applied Geology, Silesian University of Technology, Akademicka 2, 44-100 Gliwice, Poland The phase transitions and structural behaviour in natural bornite sample were investigated after heat treatment in air in a temperature range of (180÷500) ◦C using high-resolution Faraday, X-ray diffraction and 57Fe Mössbauer spectroscopy studies. X-ray diffraction and the Mössbauer spectroscopy results show that polymorph phases can exist only at high temperatures, and at a temperature of 220 ◦C a process of decomposition of bornite structure starts. Hematite is a main Fe-bearing phase and Cu is located mainly in cooper oxides present in the sample after annealing at 500 ◦C. DOI: 10.12693/APhysPolA.134.1044 PACS/topics: 76.80.+y, 91.60.–x, 88.10.jn 1. Introduction 2. Experimental procedure Bornite (Cu5FeS4), also known as peacock ore, is a The natural sample of bornite was chosen for detailed widespread natural mineral that is composed of non- analyses. The bornite sample was taken from the Per- toxic and earth-abundant elements. Natural bornite mian copper-silver deposit from the Fore-Sudetic Mon- (L-bornite) crystallizes in the orthorhombic structure ocline and was collected in a Lubin mine located about with space group P bca.
    [Show full text]
  • Antlerite Cu3(SO4)(OH)4 C 2001-2005 Mineral Data Publishing, Version 1
    Antlerite Cu3(SO4)(OH)4 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 2/m 2/m 2/m. Crystals are thick tabular {010}, equant or short prismatic [001], with dominant {110}, another twenty-odd forms, to 2 cm; commonly fibrous and in cross-fiber veinlets, feltlike, granular or powdery lumps and aggregates. Physical Properties: Cleavage: {010}, perfect; {100}, poor. Tenacity: Brittle. Hardness = 3.5 D(meas.) = 3.88 D(calc.) = 3.93 Optical Properties: Translucent. Color: Emerald-green, blackish green, pale green. Streak: Pale green. Luster: Vitreous. Optical Class: Biaxial (+). Pleochroism: X = yellow-green; Y = blue-green; Z = green. Orientation: X = b; Y = a; Z = c. Dispersion: r< v,very strong. α = 1.726 β = 1.738 γ = 1.789 2V(meas.) = 53◦ Cell Data: Space Group: P nam. a = 8.244(2) b = 11.987(3) c = 6.043(1) Z = 4 X-ray Powder Pattern: Synthetic. (ICDD 7-407). 4.86 (100), 2.566 (85), 3.60 (75), 2.683 (75), 6.01 (25), 5.40 (25), 2.503 (25) Chemistry: (1) (2) SO3 22.32 22.57 CuO 66.34 67.27 H2O 10.52 10.16 insol. 0.88 Total 100.06 100.00 (1) Chuquicamata, Chile; average of two analyses. (2) Cu3(SO4)(OH)4. Occurrence: Uncommon, typically formed in the oxidized zone of copper deposits under highly acid conditions, especially in arid regions. Association: Brochantite, atacamite, chalcanthite, kr¨ohnkite,natrochalcite, linarite, gypsum. Distribution: In the USA, in Arizona, from the Antler mine, near Yucca Station, Mohave Co., large crystals at several mines in Bisbee, Cochise Co., from the Grandview mine, Grand Canyon, Coconino Co., in Copper Basin, between Skull Valley and Prescott, and at Jerome, Yavapai Co.; from the Blanchard mine, near Bingham, Hansonburg district, Socorro Co., New Mexico; in the Darwin district, Inyo Co., California; from the Northern Light mine, near Black Mountain, Mountain View district, Mineral Co.
    [Show full text]
  • Study of Corrosion Potential Measurements As a Means to Monitor the Storage and Stabilisation Processes of Archaeological Copper Artefacts
    Proceedings of Metal 2004 National Museum of Australia Canberra ACT 4-8 October 2004 ABN 70 592 297 967 Study of corrosion potential measurements as a means to monitor the storage and stabilisation processes of archaeological copper artefacts K. Leyssensa, A. Adriaensa, E. Pantosb and C. Degrignyc a Ghent University, Department of Analytical Chemistry, Krijgslaan 281 – S12, B-9000 Ghent, Belgium b CCLRC, Synchrotron Radiation Department, Daresbury Laboratory, Warrington, UK WA4 4AD c Malta Centre for Restoration, East Wing, Royal Naval Hospital, Bighi, Kalkara, Malta __________________________________________________________________________________________ Abstract Archaeological copper artefacts recovered from wet saline environments are often stored in tap water and stabilized in sodium sesquicarbonate solutions. Modification of the natural patina and development of active corrosion can occur during these processes. This implies that monitoring of storage/stabilisation processes is necessary. The focus of the study consists of examining how corrosion potential (Ecorr) measurements can contribute in providing information on the effectiveness of storage and stabilisation treatments. This paper reports on the Ecorr versus time plots of artificially prepared copper coupons (covered or not with corrosion layers) immersed in tap water and a sodium sesquicarbonate solution. Synchrotron radiation XRD was performed in parallel to understand the reactions that take place during the immersion processes. Keywords: corrosion potential measurements, XRD, copper, saline environments, storage, stabilisation, sodium sesquicarbonate, tap water 1. Introduction Archaeological copper artefacts recovered from wet saline environments should not be exposed directly to the atmosphere, especially when they contain aggressive chloride species, as the metal will then corrode at an accelerated rate in the oxygen-rich air (Scott 2002, p125).
    [Show full text]
  • Minerals Found in Michigan Listed by County
    Michigan Minerals Listed by Mineral Name Based on MI DEQ GSD Bulletin 6 “Mineralogy of Michigan” Actinolite, Dickinson, Gogebic, Gratiot, and Anthonyite, Houghton County Marquette counties Anthophyllite, Dickinson, and Marquette counties Aegirinaugite, Marquette County Antigorite, Dickinson, and Marquette counties Aegirine, Marquette County Apatite, Baraga, Dickinson, Houghton, Iron, Albite, Dickinson, Gratiot, Houghton, Keweenaw, Kalkaska, Keweenaw, Marquette, and Monroe and Marquette counties counties Algodonite, Baraga, Houghton, Keweenaw, and Aphrosiderite, Gogebic, Iron, and Marquette Ontonagon counties counties Allanite, Gogebic, Iron, and Marquette counties Apophyllite, Houghton, and Keweenaw counties Almandite, Dickinson, Keweenaw, and Marquette Aragonite, Gogebic, Iron, Jackson, Marquette, and counties Monroe counties Alunite, Iron County Arsenopyrite, Marquette, and Menominee counties Analcite, Houghton, Keweenaw, and Ontonagon counties Atacamite, Houghton, Keweenaw, and Ontonagon counties Anatase, Gratiot, Houghton, Keweenaw, Marquette, and Ontonagon counties Augite, Dickinson, Genesee, Gratiot, Houghton, Iron, Keweenaw, Marquette, and Ontonagon counties Andalusite, Iron, and Marquette counties Awarurite, Marquette County Andesine, Keweenaw County Axinite, Gogebic, and Marquette counties Andradite, Dickinson County Azurite, Dickinson, Keweenaw, Marquette, and Anglesite, Marquette County Ontonagon counties Anhydrite, Bay, Berrien, Gratiot, Houghton, Babingtonite, Keweenaw County Isabella, Kalamazoo, Kent, Keweenaw, Macomb, Manistee,
    [Show full text]
  • Literature Review on the Properties of Cuprous Oxide Cu2o and the Process of Copper Oxidation
    Technical Report TR-11-08 Literature review on the properties of cuprous oxide Cu2O and the process of copper oxidation P A Korzhavyi, B Johansson Department of Materials Science and Engineering Royal Institute of Technology October 2011 Svensk Kärnbränslehantering AB Swedish Nuclear Fuel and Waste Management Co Box 250, SE-101 24 Stockholm Phone +46 8 459 84 00 CM Gruppen AB, Bromma, 2012 CM Gruppen ISSN 1404-0344 Tänd ett lager: SKB TR-11-08 P, R eller TR. Literature review on the properties of cuprous oxide Cu2O and the process of copper oxidation P A Korzhavyi, B Johansson Department of Materials Science and Engineering Royal Institute of Technology October 2011 This report concerns a study which was conducted for SKB. The conclusions and viewpoints presented in the report are those of the author. SKB may draw modified conclusions, based on additional literature sources and/or expert opinions. A pdf version of this document can be downloaded from www.skb.se. Abstract The purpose of the present review is to provide a reference guide to the most recent data on the prop- erties of copper(I) oxide as well as on the atomic processes involved in the initial stages of oxidation of copper. The data on the structure of surfaces, as obtained from atomic-resolution microscopy studies (for example, STM) or from first-principles calculations, are reviewed. Information of this kind may be useful for understanding the atomic mechanisms of corrosion and stress-corrosion cracking of copper. SKB TR-11-08 3 Introduction The name “cuprite” of cuprous oxide Cu2O comes from the Latin “cuprum”, meaning copper.
    [Show full text]
  • CUPRITE Calcite, Which Impart a Carmine Red Color to That Cu2o Mineral (Yedlin, 1974; Morris, 1983)
    in interstices between conglomerate boulders. Also as variety “chalcotrichite” and as inclusions in CUPRITE calcite, which impart a carmine red color to that Cu2O mineral (Yedlin, 1974; Morris, 1983). 2. Clark A secondary copper mineral formed by supergene mine, Copper Harbor. 3. North Cliff mine: Fine alteration of native copper (q.v.) and copper micro-crystals showing gyroidal forms in nodules sulfides. Much of the native copper from the of copper (Moore and Beger, 1963). 4. Cliff mine: Keweenaw has films of cuprite, some of which With azurite as massive nodules cemented by formed after the mines were opened, but some of copper and, locally, silver. A few vugs lined with which, particularly from the higher levels, predates excellent crystals were found by Williams (1966). the mining (Butler and Burbank, 1929). Usually these crystals are faced by {001}, {011}, “Chalcotrichite” is a capillary or fibrous variety. and {111} of about equal development. Some Northern Peninsula. crystals show gyroidal symmetry with {321} left, and, if this is present, {211} is a major form. 5. Houghton County: 1. Centennial mine. 2. Delaware mine (Morris, 1983). 6. In stromatolites Laurium and La Salle mines, Osceola. 3. Quincy (calcite) in the Copper Harbor Conglomerate near mine, Hancock (2, 3 Morris, 1983). Gemmy red Copper Harbor with copper (q.v.), domeykite, and crystals up to 1 mm encrusting copper and quartz copper sulfides (Nishioka et al., 1983). crystals have been found on the 7th level of the Microscopic. 7. At the Central and Phoenix Quincy amygdaloid lode, 50 to 100 meters mines: As a red patina on native copper crystals, northeast of the No.
    [Show full text]