Bond Paths and Van Der Waals Interactions in Orpiment, As2s3
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Theoretical Studies on As and Sb Sulfide Molecules
Mineral Spectroscopy: A Tribute to Roger G. Bums © The Geochemical Society, Special Publication No.5, 1996 Editors: M. D. Dyar, C. McCammon and M. W. Schaefer Theoretical studies on As and Sb sulfide molecules J. A. TOSSELL Department of Chemistry and Biochemistry University of Maryland, College Park, MD 20742, U.S.A. Abstract-Dimorphite (As4S3) and realgar and pararealgar (As4S4) occur as crystalline solids con- taining As4S3 and As4S4 molecules, respectively. Crystalline As2S3 (orpiment) has a layered structure composed of rings of AsS3 triangles, rather than one composed of discrete As4S6 molecules. When orpiment dissolves in concentrated sulfidic solutions the species produced, as characterized by IR and EXAFS, are mononuclear, e.g. ASS3H21, but solubility studies suggest trimeric species in some concentration regimes. Of the antimony sulfides only Sb2S3 (stibnite) has been characterized and its crystal structure does not contain Sb4S6 molecular units. We have used molecular quantum mechanical techniques to calculate the structures, stabilities, vibrational spectra and other properties of As S , 4 3 As4S4, As4S6, As4SIO, Sb4S3, Sb4S4, Sb4S6 and Sb4SlO (as well as S8 and P4S3, for comparison with previous calculations). The calculated structures and vibrational spectra are in good agreement with experiment (after scaling the vibrational frequencies by the standard correction factor of 0.893 for polarized split valence Hartree-Fock self-consistent-field calculations). The calculated geometry of the As4S. isomer recently characterized in pararealgar crystals also agrees well with experiment and is calculated to be about 2.9 kcal/mole less stable than the As4S4 isomer found in realgar. The calculated heats of formation of the arsenic sulfide gas-phase molecules, compared to the elemental cluster molecules As., Sb, and S8, are smaller than the experimental heats of formation for the solid arsenic sulfides, but shown the same trend with oxidation state. -
Orpiment As2s3 C 2001-2005 Mineral Data Publishing, Version 1
Orpiment As2S3 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. Commonly in foliated columnar or fibrous aggregates, with cleavages as much as 60 cm across; may be reniform or botryoidal; also granular or powdery; rarely as prismatic crystals, to 10 cm. Twinning: On {100}. Physical Properties: Cleavage: Perfect on {010}, imperfect on {100}; cleavage lamellae are flexible. Tenacity: Sectile. Hardness = 1.5–2 VHN = n.d. D(meas.) = 3.49 D(calc.) = 3.48 Optical Properties: Transparent. Color: Lemon-yellow to golden or brownish yellow. Streak: Pale lemon-yellow. Luster: Resinous, pearly on cleavage surface. Optical Class: Biaxial (–). Pleochroism: In reflected light, strong, white to pale gray with reddish tint; in transmitted light, Y = yellow, Z = greenish yellow. Orientation: X = b; Z ∧ c = 2◦. Dispersion: r> v,strong. α = 2.4 (Li). β = 2.81 (Li). γ = 3.02 (Li). 2V(meas.) = 76◦ Anisotropism: Barely observable because of strong internal reflections. R1–R2: (400) 33.0–36.5, (420) 31.0–35.2, (440) 28.9–33.9, (460) 27.4–31.5, (480) 26.0–30.3, (500) 24.9–29.3, (520) 24.0–28.4, (540) 23.3–27.8, (560) 22.8–27.3, (580) 22.3–26.9, (600) 22.0–26.5, (620) 21.7–26.3, (640) 21.5–26.0, (660) 21.2–25.7, (680) 21.0–25.5, (700) 20.8–25.3 Cell Data: Space Group: P 21/n. a = 11.475(5) b = 9.577(4) c = 4.256(2) β =90◦41(5)0 Z=4 X-ray Powder Pattern: Baia Sprie (Fels˝ob´anya), Romania. -
10700 Orpiment, King's Yellow PY 39
10700 Orpiment, King's Yellow PY 39 Chemical composition: yellow sulphide of arsenic As2S3 The origin of the modern name is derived from the Latin term auripigmentum or auripigmento, literally meaning gold paint. Orpiment was once widely used, particularly in the East, but has now fallen into disuse because of its limited supply and because of its poisonous character. The principal sources in ancient times appear to have been in Hungary, Macedonia, Asia Minor and perhaps in various parts of Central Asia. There was a large deposit near Julamerk in Kurdistan. Current deposits of orpiment are in Romania, Hungary, Germany, Greece, France, Italy, Iran, Peru, China, Japan and the western United States. Orpiment occurs as a low temperature product in hydrothermal veins, as a volcanic sublimation product, as a hot spring deposit and in fire mines. It is often associated with stibnite, pyrite, realgar, calcite and gypsum. Orpiment occurs in many places but not in large quantities. Orpiment is usually described as a lemon or canary yellow or sometimes as a golden or brownish yellow with a fair covering power. Microscopically, orpiment is crystalline and may contain orange-red particles of realgar, to which it is closely related. The larger particles glisten by reflected light and have a waxy-looking surface. The toxicity of the arsenic sulfide pigments has been known since early times. The toxic properties of orpiment have been used to advantage to repel insects. Orpiment is said to be incompatible with lead- or copper-containing pigments. Orpiment is not stable in lime and therefore can not be used for fresco, a fact noted by Cennino Cennini inn the fifteenth century. -
Single Crystal Raman Spectroscopy of Selected Arsenite, Antimonite and Hydroxyantimonate Minerals
SINGLE CRYSTAL RAMAN SPECTROSCOPY OF SELECTED ARSENITE, ANTIMONITE AND HYDROXYANTIMONATE MINERALS Silmarilly Bahfenne B.App.Sci (Chem.) Chemistry Discipline This thesis is submitted as part of the assessment requirements of Master of Applied Science Degree at QUT February 2011 KEYWORDS Raman, infrared, IR, spectroscopy, synthesis, synthetic, natural, X-ray diffraction, XRD, scanning electron microscopy, SEM, arsenite, antimonate, hydroxyantimonate, hydrated antimonate, minerals, crystal, point group, factor group, symmetry, leiteite, schafarzikite, apuanite, trippkeite, paulmooreite, finnemanite. i ii ABSTRACT This thesis concentrates on the characterisation of selected arsenite, antimonite, and hydroxyantimonate minerals based on their vibrational spectra. A number of natural arsenite and antimonite minerals were studied by single crystal Raman spectroscopy in order to determine the contribution of bridging and terminal oxygen atoms to the vibrational spectra. A series of natural hydrated antimonate minerals was also compared and contrasted using single crystal Raman spectroscopy to determine the contribution of the isolated antimonate ion. The single crystal data allows each band in the spectrum to be assigned to a symmetry species. The contribution of bridging and terminal oxygen atoms in the case of the arsenite and antimonite minerals was determined by factor group analysis, the results of which are correlated with the observed symmetry species. In certain cases, synthetic analogues of a mineral and/or synthetic compounds isostructural or related to the mineral of interest were also prepared. These synthetic compounds are studied by non-oriented Raman spectroscopy to further aid band assignments of the minerals of interest. Other characterisation techniques include IR spectroscopy, SEM and XRD. From the single crystal data, it was found that good separation between different symmetry species is observed for the minerals studied. -
Crystalloluminescence and Temporary Mechanoluminescence of As203 Crystals
Pratr~na, Vol. 18, No. 2, February 1982, pp. 127-135. © Printed in India. Crystalloluminescence and temporary mechanoluminescence of As203 crystals B P CHANDRA, P R TUTAKNE, A C BIYANI and B MAJUMDAR Department of Physics, Government Science College, Raipur 492 002, India MS received 24 August 1981 ; revised 21 December 1981 Abstract. Crystalloluminescence and temporary mechanoluminescence of AsaOa crystals are investigated. The crystalloluminescence spectra are similar to the photo- luminescence and mechanolumineseence (of fresh crystals, in COz atmosphere) spectra. The mechanoluminescence spectra of freshly grown crystals taken in air consist of the superposition of the photoluminescence and nitrogen emissions. The mechano- luminescence spectra of old crystals of AssO3 consist of only the nitrogen emission. The total number of crystalloluminescence flashes is linearly related to the total mass of the crystals grown. The mechanoluminescence intensity increases with the mass of the crystals. The mechanoluminescence intensity decreases with the age of the crys- tals and the rate of decrease increases with increasing temperature of the crystals. Different possibilities of crystalloluminescence and mechanoluminescence excitations in AssOs crystals are exlSlored and it is concluded that crystalloluminescence and mechanoluminescence are of different origins. Keywords. Crystalloluminescence; mechanoluminescence; photoluminescence; crys- tal-fracture; As~Os crystals. 1. Introduction Crystalloluminescence (CRL), the emission of light during crystallization of certain substances from solution and mechanoluminescence (ML), the emission of light during mechanical deformation of certain solids are known for a long time (Harvey 1957). It has been reported from time to time that the CRL and ML should be correlated in their excitation mechanism (Trautz 1905; Gernez 1905; Weiser 1918; Belyaev et al 1963; Takeda et al 1973). -
STRONG and WEAK INTERLAYER INTERACTIONS of TWO-DIMENSIONAL MATERIALS and THEIR ASSEMBLIES Tyler William Farnsworth a Dissertati
STRONG AND WEAK INTERLAYER INTERACTIONS OF TWO-DIMENSIONAL MATERIALS AND THEIR ASSEMBLIES Tyler William Farnsworth A dissertation submitted to the faculty at the University of North Carolina at Chapel Hill in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of Chemistry. Chapel Hill 2018 Approved by: Scott C. Warren James F. Cahoon Wei You Joanna M. Atkin Matthew K. Brennaman © 2018 Tyler William Farnsworth ALL RIGHTS RESERVED ii ABSTRACT Tyler William Farnsworth: Strong and weak interlayer interactions of two-dimensional materials and their assemblies (Under the direction of Scott C. Warren) The ability to control the properties of a macroscopic material through systematic modification of its component parts is a central theme in materials science. This concept is exemplified by the assembly of quantum dots into 3D solids, but the application of similar design principles to other quantum-confined systems, namely 2D materials, remains largely unexplored. Here I demonstrate that solution-processed 2D semiconductors retain their quantum-confined properties even when assembled into electrically conductive, thick films. Structural investigations show how this behavior is caused by turbostratic disorder and interlayer adsorbates, which weaken interlayer interactions and allow access to a quantum- confined but electronically coupled state. I generalize these findings to use a variety of 2D building blocks to create electrically conductive 3D solids with virtually any band gap. I next introduce a strategy for discovering new 2D materials. Previous efforts to identify novel 2D materials were limited to van der Waals layered materials, but I demonstrate that layered crystals with strong interlayer interactions can be exfoliated into few-layer or monolayer materials. -
Allchar Mineral Assemblage 3
Geologica Macedonica, Vol. 15-16, p. 1-23 (2001-2002) Suppl. GEOME2 SSN 0352 - 1206 Manuscript received: December 15, 200 1 UDC: 553.08 (497 .7) Accepted: March 3, 2002 Original scientific paper ~• ALLCHAR l\1INERAL ASSEMBLAGE l 3 l 4 Blazo Boev , Vladimir Bermanec , Todor Serafimovski\ Sonja Lepitkova , Snezana Mikulcic , 5 5 5 Marin ~oufek\ Gligor Jovanovski , Trajce Stafilov , Metodija Najdoski IDepartment ofPetrology, Mineralogy and Geochemistry, Faculty ofMining and Geology, "Sv. Kiril i Metodij" University, Goce Delcev 89, MK-2000 Stip, Republic ofMacedonia 2Department ofMineral Deposits, Faculty ofMining and Geology, "Sv. Kiril i Metodij" University, Goce Delcev 89, MK-2000 Stip, Republic of Macedonia 3Institute ofMineralogy and Petrology, Department ofGeology, Faculty ofScience, University ofZagreb, Horvatovac bb, HR-JOOOO Zagreb, Croatia 4Department ofMineralogy and Petrology, Croatian Natural History Museum, Demetrova I, HR-JOOOO Zagreb, Croatia 5Institute of Chemistry, Faculty ofScience, "Sv. Kiril i Metodij" University, P.o. Box 162, MK-JOOI Skopje, Republic ofMacedonia Abstract. The paper is a summary of investigatioris carried out on minerals of the Allchar deposit. It discusses the TI-As-Sb-Au mineral ill emblage after detailed and intense research work. Four types of mineralization have been distinguished based on the mineral assemblage present: I. The first ly pe is characterised by high c ment of iron and sulphur, but lower arsenic and thalli um contenl. The pyrite-marcasite mineral assemblage is characterized by the presence of some quantities of arsenic-pyrite. 2. The second type is characterized by the high antimony and low iron and thallium content. Stibnite is the most common mineral in the group. -
Twinnite Pb(Sb, As)2S4 C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Triclinic, Probable; Pseudo-Orthorhombic
Twinnite Pb(Sb, As)2S4 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Triclinic, probable; pseudo-orthorhombic. Point Group: 2/m 2/m 2/m, apparent. As grains, to 1.5 mm. Twinning: Polysynthetic, the trace of the composition plane parallel to {100}. Physical Properties: Cleavage: Perfect on {100}. Tenacity: Brittle. Hardness = n.d. VHN = 147 (50 g load). D(meas.) = n.d. D(calc.) = 5.323 (for Sb:As=3:2). Optical Properties: Opaque. Color: Black; white in polished section. Streak: Black, with a slightly brownish tint. Luster: Metallic. Pleochroism: Strong, displaying twin lamellae. R1–R2: (400) 39.1–45.2, (420) 38.2–44.7, (440) 37.3–44.2, (460) 36.6–43.7, (480) 36.2–43.2, (500) 35.8–42.9, (520) 35.5–42.5, (540) 35.0–42.0, (560) 34.4–41.4, (580) 34.0–40.8, (600) 33.5–40.0, (620) 33.2–39.4, (640) 32.8–38.7, (660) 32.3–38.1, (680) 31.7–37.5, (700) 31.0–37.0 Cell Data: Space Group: P nmn pseudocell. a = 19.6(2) b = 7.99(5) c = 8.60(5) α =90◦ β =90◦ γ =90◦ Z=8 X-ray Powder Pattern: Madoc, Canada. 3.51 (100), 2.344 (80), 2.78 (70), 4.18 (50), 3.91 (50), 2.689 (50), 2.645 (50) Chemistry: (1) (2) (3) Pb 41 39.3 38.7 Sb 28 28.1 24.8 As 11 8.9 12.0 S 23 23.7 23.9 Total 103 100.0 99.4 (1) Madoc, Canada; by electron microprobe, corresponding to Pb1.10(Sb1.28As0.82)Σ=2.10S4.00. -
Nonlinear Mixing Characteristics of Reflectance Spectra of Typical
minerals Article Nonlinear Mixing Characteristics of Reflectance Spectra of Typical Mineral Pigments Shuqiang Lyu 1,2, Die Meng 1,2, Miaole Hou 1,2,* , Shuai Tian 3, Chunhao Huang 1,2 and Jincheng Mao 1,2 1 School of Geomatics and Urban Spatial Informatics, Beijing University of Civil Engineering and Architecture, Beijing 102616, China; [email protected] (S.L.); [email protected] (D.M.); [email protected] (C.H.); [email protected] (J.M.) 2 Beijing Key Laboratory for Architectural Heritage Fine Reconstruction & Health Monitoring, Beijing 102616, China 3 Chinese Academy of Cultural Heritage, Beijing 100029, China; [email protected] * Correspondence: [email protected]; Tel.: +86-139-1096-1145 Abstract: Hyperspectral technology has been used to identify pigments that adhere to the surfaces of polychrome artifacts. However, the colors are often produced by the mixing of pigments, which requires that the spectral characteristics of the pigment mixtures be considered before pigment un- mixing is conducted. Therefore, we proposed an experimental approach to investigate the nonlinear degree of spectral reflectance, using several mixing models, and to evaluate their performances in the study of typical mineral pigments. First, five mineral pigments of azurite, malachite, cinnabar, orpi- ment, and calcite were selected to form five groups of samples, according to their different mass ratios. Second, a fully constrained least squares algorithm based on the linear model and three algorithms based on the nonlinear model were employed to calculate the proportion of each pigment in the mixtures. We evaluated the abundance accuracy as well as the similarity between the measured and reconstructed spectra produced by those mixing models. -
The Koman Dawsonite and Realgar–Orpiment Deposit, Northern Albania
413 The Canadian Mineralogist Vol. 41, pp. 413-427 (2003) THE KOMAN DAWSONITE AND REALGAR–ORPIMENT DEPOSIT, NORTHERN ALBANIA: INFERENCES ON PROCESSES OF FORMATION VINCENZO FERRINI§ Dipartimento di Scienze della Terra, Università degli Studi di Roma “La Sapienza”, P.le A. Moro, 5, I–00185 Roma, Italy LUCIO MARTARELLI Centro di Studio per gli Equilibri Sperimentali in Minerali e Rocce del C.N.R., P.le A. Moro, 5, I–00185 Roma, Italy CATERINA DE VITO Dipartimento di Scienze della Terra, Università degli Studi di Roma “La Sapienza”, P.le A. Moro, 5, I–00185 Roma, Italy ALEKSANDER ÇINA AND TONIN DEDA Geological Survey of Albania, Rruga Vasil Shanto, Tirana, Albania ABSTRACT The deposit of dawsonite and realgar–orpiment in the Koman area, northern Albania, is aligned along the NE–SW-trending tectonic line joining the Krasta–Cukal and Mirdita structural-tectonic zones. The deposit contains the following main paragenetic assemblages: i) marcasite – greigite (Fe-sulfide stage), ii) stibnite – realgar – orpiment (As–Sb-sulfide stage), iii) dolomite – calcite – dawsonite – aragonite – barite – gypsum (carbonate–sulfate stage), iv) native As – gibbsite (supergene stage). There was lithostratigraphic control of mineralization; carbonate-rich wallrocks reacted with the mineralizing fluids emanating from a bur- ied magmatic body and migrating along Albanian transversal faults, rather than argillaceous lithotypes. Values of ␦18O and ␦13C indicate that dawsonite and hydrothermal dolomite are derived at the expense of carbonate rocks, which occur extensively in the stratigraphic sequence of the host rocks. The water:rock ratio during the carbonate–sulfate stage of deposition was probably small. Moreover, oxygen and carbon isotopic exchange during metasomatic transformation of the rocks, recrystallization and late involvement of groundwater, probably all occurred. -
Hutchinsonite (Pb, Tl)2As5s9 C 2001-2005 Mineral Data Publishing, Version 1
Hutchinsonite (Pb, Tl)2As5S9 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 2/m 2/m 2/m. Crystals are prismatic to acicular k [001], to 1 cm; also as radiating tufts. Physical Properties: Cleavage: Good on {010}. Fracture: Conchoidal. Tenacity: Brittle. Hardness = 1.5–2 VHN = 170 D(meas.) = 4.6–4.7 D(calc.) = 4.58 Optical Properties: Opaque, translucent in thin fragments. Color: Scarlet-vermilion to deep cherry-red, with strong red internal reflections; transmits red light in thin fragments. Luster: Adamantine to submetallic. Optical Class: Biaxial (–). Orientation: X = a; Y = b; Z = c. Dispersion: r< v,extreme. α = 3.078(18) β = 3.176(3) γ = 3.188(3) 2V(meas.) = 37◦ (589). Anisotropism: Strong. R1–R2: (400) 32.6–36.9, (420) 31.8–35.9, (440) 31.2–35.2, (460) 30.5–34.3, (480) 29.5–33.2, (500) 29.0–32.1, (520) 29.1–31.3, (540) 28.8–30.4, (560) 28.0–29.4, (580) 26.9–28.4, (600) 26.0–27.6, (620) 25.3–26.8, (640) 24.8–26.4, (660) 24.3–26.0, (680) 23.9–25.6, (700) 23.6–25.3 Cell Data: Space Group: P bca. a = 1.809(6) b = 35.48(1) c = 8.167(3) Z = 8 X-ray Powder Pattern: Binntal, Switzerland. 2.74 (100), 3.79 (70), 3.05 (60), 4.44 (50), 2.39 (30), 2.22 (30), 1.907 (30) X-ray Powder Pattern: Quiruvilca, Peru. (ICDD 42-1388). -
Christite, a New Thallium Mineral from the Carlin Gold Deposit, Nevada
American Mineralogist, Volume62, pages421425, 1977 Christite,a newthallium mineral from the Carlin golddeposit, Nevada ARruuRS. Rlorxn U.S. GeologicalSuruey, Menlo Park, California 94025 FnnNr W. Dlcrsor Departmentof Geology,Stanford Uniuersity St anfo rd, Cal ift rnia 9430 5 JoHNF. Slecr U.S. GeologicalSuruey, Reston, Virginia 22092 lNn KevtNL. Bnowx ChemistryDiuision, Diuision of Scientffic and IndustrialResearch, Petone, New Zealand Abstract Christite,TlHgAsSr, occurs with realgar,orpiment, and loranditein bariteveins and with realgar,lorandite, and getchellitein mineralizedcarbonaceous silty dolomite in the Carlin gold deposit,north-central Nevada. The mineralis namedfor Dr. CharlesL. Christof the U.S. GeologicalSurvey. The color is crimsonor deep red, but variesto bright orangein thinnerplates and crystals;the streakis bright orange,and the lusteris adamantine.The mineralis monoclinic,space group P2,/n,a -- 6.113(l),b = 16.188(4),c = 6.1Il(l) A, with0 : 96.71(2)',Z = 4, and cell volume: 600.6A8. Strongest X-ray powderdiffraction lines, in A, andtheir relative intensities are2.98 (10),3.62 (8),3.49 (6),2.692(6),2.216 (5),4.03 (6), and 3.36(5). Electronmicroprobe analyses gave Tl 35.2,Hg 35.1,As 13.1,S 16.6,sum 100.0 weight percent.The mineraloccurs in smallsubhedral to anhedralgrains which usuallylack well-developedforms but may showa bladedor flattenedhabit. Synthetic crystals are tabular, show{010) and {T0l}pinacoids, and {1l0} and {01l} prisms,and haveperfect {010}, excellent {ll0} and {001},and good {T0l} cleavages.Vickers hardness varied from 28.3-34.6and averaged31.5 kg mm-' (10 determinations).Density of syntheticTlHgAsSs is 6.2(2)(meas) and6.37g cm-e (calc).In reflectedlight christiteis grayish-whitewith a faint blue tint, lacks visiblebireflectance, is anisotropic,and has a brilliant red-orangeinternal reflection.