Stability of Sodium Sulfate Dicarbonate
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Gaylussite Na2ca(CO3)2 • 5H2O C 2001-2005 Mineral Data Publishing, Version 1
Gaylussite Na2Ca(CO3)2 • 5H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. As flattened wedge-shaped crystals with dominant {110}, {011}, {001}, smaller {010}, {100}, {101}, {112}; also as prismatic to dipyramidal crystals elongated along [100], to 6 cm. Physical Properties: Cleavage: On {110}, perfect; on {001}, imperfect. Fracture: Conchoidal. Tenacity: Very brittle. Hardness = 2.5–3 D(meas.) = 1.991 D(calc.) = 1.991 Dehydrates with efflorescence in dry air; slowly decomposes in H2O leaving CaCO3 as calcite or aragonite. Optical Properties: Transparent to translucent. Color: Colorless to pale yellow or pale gray, white; colorless in transmitted light. Streak: White to pale gray. Luster: Vitreous. Optical Class: Biaxial (–). Orientation: X = b; Z ∧ c = –15◦. Dispersion: r< v,strong, crossed. α = 1.444 β = 1.516 γ = 1.523 2V(meas.) = 34◦ Cell Data: Space Group: C2/c. a = 11.589 b = 7.780 c = 11.207 β = 102.5◦ Z=4 X-ray Powder Pattern: John Hay, Jr. Well No. 1, Wyoming, USA. 6.403 (100), 3.18 (80), 2.70 (80), 2.61 (80), 1.91 (80), 2.49 (70), 1.98 (70) Chemistry: (1) (2) CO2 30.02 29.72 SiO2 0.08 Fe2O3 0.03 MnO 0.01 MgO 0.01 CaO 19.02 18.94 Na2O 20.40 20.93 H2O 30.47 30.41 insol. 0.16 Total 100.20 100.00 • (1) Taboos-nor salt lake, Mongolia. (2) Na2Ca(CO3)2 5H2O. Occurrence: Typically in evaporites or shales from alkali lakes; rarely in veinlets cutting alkalic igneous rocks. -
Infrare D Transmission Spectra of Carbonate Minerals
Infrare d Transmission Spectra of Carbonate Mineral s THE NATURAL HISTORY MUSEUM Infrare d Transmission Spectra of Carbonate Mineral s G. C. Jones Department of Mineralogy The Natural History Museum London, UK and B. Jackson Department of Geology Royal Museum of Scotland Edinburgh, UK A collaborative project of The Natural History Museum and National Museums of Scotland E3 SPRINGER-SCIENCE+BUSINESS MEDIA, B.V. Firs t editio n 1 993 © 1993 Springer Science+Business Media Dordrecht Originally published by Chapman & Hall in 1993 Softcover reprint of the hardcover 1st edition 1993 Typese t at the Natura l Histor y Museu m ISBN 978-94-010-4940-5 ISBN 978-94-011-2120-0 (eBook) DOI 10.1007/978-94-011-2120-0 Apar t fro m any fair dealin g for the purpose s of researc h or privat e study , or criticis m or review , as permitte d unde r the UK Copyrigh t Design s and Patent s Act , 1988, thi s publicatio n may not be reproduced , stored , or transmitted , in any for m or by any means , withou t the prio r permissio n in writin g of the publishers , or in the case of reprographi c reproductio n onl y in accordanc e wit h the term s of the licence s issue d by the Copyrigh t Licensin g Agenc y in the UK, or in accordanc e wit h the term s of licence s issue d by the appropriat e Reproductio n Right s Organizatio n outsid e the UK. Enquirie s concernin g reproductio n outsid e the term s state d here shoul d be sent to the publisher s at the Londo n addres s printe d on thi s page. -
Trona Na3(CO3)(HCO3) • 2H2O C 2001-2005 Mineral Data Publishing, Version 1
Trona Na3(CO3)(HCO3) • 2H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. Crystals are dominated by {001}, {100}, flattened on {001} and elongated on [010], with minor {201}, {301}, {211}, {211}, {411},to 10 cm; may be fibrous or columnar massive, as rosettelike aggregates. Physical Properties: Cleavage: {100}, perfect; {211} and {001}, interrupted. Fracture: Uneven to subconchoidal. Hardness = 2.5–3 D(meas.) = 2.11 D(calc.) = 2.124 Soluble in H2O, alkaline taste; may fluoresce under SW UV. Optical Properties: Translucent. Color: Colorless, gray, pale yellow, brown; colorless in transmitted light. Luster: Vitreous. Optical Class: Biaxial (–). Orientation: X = b; Z ∧ c =83◦. Dispersion: r< v; strong. α = 1.412–1.417 β = 1.492–1.494 γ = 1.540–1.543 2V(meas.) = 76◦160 2V(calc.) = 74◦ Cell Data: Space Group: I2/a. a = 20.4218(9) b = 3.4913(1) c = 10.3326(6) β = 106.452(4)◦ Z=4 X-ray Powder Pattern: Sweetwater Co., Wyoming, USA. 2.647 (100), 3.071 (80), 4.892 (55), 9.77 (45), 2.444 (30), 2.254 (30), 2.029 (30) Chemistry: (1) (2) CO2 38.13 38.94 SO3 0.70 Na2O 41.00 41.13 Cl 0.19 H2O 20.07 19.93 insol. 0.02 −O=Cl2 0.04 Total 100.07 100.00 • (1) Owens Lake, California, USA; average of several analyses. (2) Na3(CO3)(HCO3) 2H2O. Occurrence: Deposited from saline lakes and along river banks as efflorescences in arid climates; rarely from fumarolic action. Association: Natron, thermonatrite, halite, glauberite, th´enardite,mirabilite, gypsum (alkali lakes); shortite, northupite, bradleyite, pirssonite (Green River Formation, Wyoming, USA). -
Carbon Mineral Ecology: Predicting the Undiscovered Minerals of Carbon
American Mineralogist, Volume 101, pages 889–906, 2016 Carbon mineral ecology: Predicting the undiscovered minerals of carbon ROBERT M. HAZEN1,*, DANIEL R. HUMMER1, GRETHE HYSTAD2, ROBERT T. DOWNS3, AND JOSHUA J. GOLDEN3 1Geophysical Laboratory, Carnegie Institution, 5251 Broad Branch Road NW, Washington, D.C. 20015, U.S.A. 2Department of Mathematics, Computer Science, and Statistics, Purdue University Calumet, Hammond, Indiana 46323, U.S.A. 3Department of Geosciences, University of Arizona, 1040 East 4th Street, Tucson, Arizona 85721-0077, U.S.A. ABSTRACT Studies in mineral ecology exploit mineralogical databases to document diversity-distribution rela- tionships of minerals—relationships that are integral to characterizing “Earth-like” planets. As carbon is the most crucial element to life on Earth, as well as one of the defining constituents of a planet’s near-surface mineralogy, we focus here on the diversity and distribution of carbon-bearing minerals. We applied a Large Number of Rare Events (LNRE) model to the 403 known minerals of carbon, using 82 922 mineral species/locality data tabulated in http://mindat.org (as of 1 January 2015). We find that all carbon-bearing minerals, as well as subsets containing C with O, H, Ca, or Na, conform to LNRE distributions. Our model predicts that at least 548 C minerals exist on Earth today, indicating that at least 145 carbon-bearing mineral species have yet to be discovered. Furthermore, by analyzing subsets of the most common additional elements in carbon-bearing minerals (i.e., 378 C + O species; 282 C + H species; 133 C + Ca species; and 100 C + Na species), we predict that approximately 129 of these missing carbon minerals contain oxygen, 118 contain hydrogen, 52 contain calcium, and more than 60 contain sodium. -
Update of State of Nevada Research on Waste Package Environments in Yucca Mountain
Update of State of Nevada research on waste package environments in Yucca Mountain By Maury Morgenstein Geosciences Management Institute, Inc. [email protected] 1 Are we doing a good job in defining the service environment? The characterization of existing conditions addresses environmental conditions during the initial waste loading period. Thus, a major constituent now in tunnel dust - rock flower (aluminum silicates) may not be a major constituent during and after the heat up period. 2 Vadose water seeping into the tunnels during the heat-up period through fracture flow and drip has the potential to form brine solutions. With evaporation a variety of single and double salts can form. With increasing raise in repository temperature these salts have the potential to become airborne dust. When repository temperature falls and humidity rises salts present as rock flower coated-dust particles or as salt dust may deliquesce and form brine solutions that have the potential to corrode the waste package. 3 SEM and EDS of Dust Particles off of the tunnel wall SPC01019444 Mixture of Na, K, Ca, Cl, and sulfate 4 4 Dust Particles off of the tunnel wall Mixture of SPC01019444 Ca and Mg chloride and sulfate salts on rock flower 5 5 Dust Particles off of the tunnel wall Rock flower with SPC01019444 calcite, chloride and sulfate salts 6 6 Dust Particles off of air pipe SPC01019441 Mixture of Mg, Na, Ca, and K carbonate, sulfate, and phosphates on rock flower 7 7 Dust particles off of air pipe SPC01019411 Rock flower K-aluminum silicate 8 8 Service Environmental Parameters How complex are these parameters through the lifetime of waste containment? • Fixed Surfaces • Mobile Surfaces • Variable vadose water compositions • Variable vadose water flux • Relative humidity and deliquescence • Temperature • Convection • Decay 9 Salts on Fixed and Mobile Surfaces How have we defined the salts that might be present after closure? The following lists are from: C. -
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). -
Phase Relations of Nahcolite and Trona at High P-T Conditions
Journal of MineralogicalPhase and relationsPetrological of nahcolite Sciences, and Volume trona 104, page 25─ 36, 2009 25 Phase relations of nahcolite and trona at high P-T conditions *,** * Xi LIU and Michael E. FLEET *Department of Earth Sciences, University of Western Ontario, London, ON N6A 5B7, Canada **School of Earth and Space Sciences, Peking University, Beijing 100871, P.R. China Using cold-seal hydrothermal bomb and piston-cylinder apparatus, we have carried out both forward and rever- sal experiments to investigate the phase boundary between nahcolite (NaHCO3) and trona (NaHCO3⋅Na2CO3⋅ 2H2O). We found that the temperature of this phase boundary remains low at least up to 10 kbar, so that this phase transformation maintains its univariant nature in our investigated P-T space. The locus of this phase - boundary in a log(pCO2) T space is defined as log(pCO2) = 0.0240(±0.0001)T – 9.80(±0.06) (with pCO2 in bar and T in K), in excellent agreement with earlier 1 atm experiments at different partial pressures of CO2 (pCO2) and theoretical calculation. Using this equation and literature thermodynamic data, the entropy of trona at 298.15 K is constrained to be 303.8 J mol−1 K−1, essentially identical to earlier estimates from different methods. Our experimental results have also been used to constrain the genesis of nahcolite in some fluid inclusions of diverse origins, and it is suggested that nahcolite in these occurrences is most likely a daughter mineral which crystallized from the fluids as temperature decreased, rather than an accidentally trapped phase. Keywords: Nahcolite, Trona, Phase relations, Entropy, Fluid inclusions INTRODUCTION 2002). -
A POTENTIAL MARTIAN ANALOG T. Liu and DL
41st Lunar and Planetary Science Conference (2010) 2024.pdf MINERALOGICAL COMPOSITIONS OF THE EVAPORITES AT LEWIS CLIFF ICE TONGUE, ANTARCTICA: A POTENTIAL MARTIAN ANALOG T. Liu and D. L. Bish, Department of Geological Sciences, Indiana University, 1001 E. 10th St., Bloomington, IN 47405, USA email: [email protected]. Introduction: Numerous recent orbital and rover freezer until time of analysis, and sample preparation studies of Mars have documented the occurrence of a was done in a cold room at 4ºC, using pre-cooled variety of hydrated minerals commonly associated preparation equipment (i.e., mortar and pestle, with evaporite deposits, e.g., hydrated varieties of spatulas, specimen mount, etc.). X-ray powder Mg-, Ca- and Fe- sulfates such as gypsum, epsomite, diffraction (XRD) measurements used a Bruker D8 and jarosite. Evaporite minerals are often used to Advance diffractometer with Cu Kα radiation and a document the evolution of natural waters resulting SolX energy-dispersive detector, and measurements from past water-rock interactions, but these minerals were done under ambient room temperature form on Earth under a wide range of conditions. immediately after mounting the specimens. Relative Formation environments include a wide range in humidity (RH) at the time of field collection was water:rock ratios and temperatures. As emphasized ~50%, so the environment surrounding samples by [1], the formation of evaporite minerals under during XRD data measurement was maintained at low-temperature conditions at low water:rock ratios 50%. Specimens were measured using rapid scan is one of the least understood scenarios but is perhaps rates to minimize the possibility of modification at most applicable to evaporite formation on Mars. -
NIR Reflectance Spectroscopy of Hydrated and Anhydrous Sodium Carbonates at Different Temperatures S
NIR reflectance spectroscopy of hydrated and anhydrous sodium carbonates at different temperatures S. de Angelis, C. Carli, F. Tosi, P. Beck, O. Brissaud, B. Schmitt, S. Potin, M.C. de Sanctis, F. Capaccioni, G. Piccioni To cite this version: S. de Angelis, C. Carli, F. Tosi, P. Beck, O. Brissaud, et al.. NIR reflectance spectroscopy of hydrated and anhydrous sodium carbonates at different temperatures. Icarus, Elsevier, 2019, 317, pp.388-411. 10.1016/j.icarus.2018.08.012. hal-02415147 HAL Id: hal-02415147 https://hal.archives-ouvertes.fr/hal-02415147 Submitted on 30 Jul 2021 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. De Angelis et al. 2019, Icarus, 317, 388-411 1 NIR reflectance spectroscopy of hydrated and anhydrous sodium 2 carbonates at different temperatures 3 4 S. De Angelis1, C. Carli1, F. Tosi1, P. Beck2, O. Brissaud2, B. Schmitt2, S. Potin2, M.C. 5 De Sanctis1, F. Capaccioni1, G. Piccioni1 6 7 1 Istituto di Astrofisica e Planetologia Spaziali, Via del Fosso del Cavaliere, I-00133 Roma, Italy 8 2 Université Grenoble Alpes, CNRS, Institut de Planétologie et d’Astrophysique de Grenoble (IPAG), 38058 9 Grenoble Cédex 9, France 10 11 Abstract 12 13 Recent space-based observations have revealed or suggested the existence of various types of 14 carbonate salts in several Solar System bodies, such as Mars, Ceres, Enceladus, and Europa. -
A Refinement of the Crystal Structure of Na2 C0 3 • H2 0
JOURNAL O F RESEARCH of the National Bureau of Standards - A. Physics and Chemistry Vol. 74A, No. 3, May- June 1970 A Refinement of the Crystal Structure of Na2 C0 3 • H2 0 B. Dickens, F. A. Maue r, and W. E. Brown* Institute for Materi als Research, National Bureau of Standards Washington, D.C. 20234 (January 28, 1970) The c rystal structure of synthe ti c Na2 Co.,,· H2O. has been refin ed us in g 1231 unique x·ray dif· fr~c tlOn data c~ l ec l e d by the peak height m ~ th o d on a diffractomete r. R = 0.034. The unit cell is a - 6.474(2), b- 1O.724(3) and c=5.259(2) A with z = 4 a nd s pace group P2,ab. The calc ulated de nsit y IS the same as the observe d dens it y, 2.26 g. c m- 3 . The structure cont ain s sheets of C0.§- ions bonded to Na+ IOn s a nd water molecul es roughly halfw ay betw een the s heets. Each C02- bonds ed rre· wise to both Na+ ions. The Na+ ions have irregul ar but simila r coordi nations of seve n "' ~ i ghb o r s . Ea~h wa ter molec ule is bonded to both Na+ ions and form s hydrogen bonds to bot h neig hboring Co. ~ - layers. Key words : Crystal struc ture; hyd rated carbonates; hydrogen bonding; sodium carbonate; the rmonatrite; x·ray diffracti on. 1. Introduction of aqueous solution a t 60 °C. -
Kogarkoite Na3(SO4)F C 2001-2005 Mineral Data Publishing, Version 1
Kogarkoite Na3(SO4)F c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic, pseudorhombohedral. Point Group: 2/m. As tabular to pseudorhombohedral crystals, to 2 cm, and in grains and earthy aggregates. Twinning: Common, by rotation about [102] (pseudohexagonal [0001]), giving intergrown and contact trillings. Physical Properties: Hardness = 3.5 D(meas.) = 2.66(6) D(calc.) = 2.679 Slowly soluble in H2O; fluoresces cream to pale blue under SW UV and green under LW UV. Optical Properties: Transparent to translucent. Color: Colorless, pale sky-blue, pale pink, lilac. Streak: White. Luster: Vitreous to dull. Optical Class: Biaxial (+), nearly uniaxial (+). Pleochroism: Slight. ω = 1.435 = 1.439 α = 1.439(1) β = 1.439(1) γ = 1.442(1) 2V(meas.) = 0◦ to very small. Cell Data: Space Group: P 21/m (synthetic). a = 18.079(2) b = 6.958(1) c = 11.443(2) β = 107.71◦ Z=12 X-ray Powder Pattern: Synthetic. 3.48 (100), 2.991 (85), 2.718 (85), 2.705 (85), 2.1419 (85), 3.80 (70), 2.564 (70) Chemistry: (1) (2) SO3 43.41 43.51 Na2O 50.1 50.52 K2O 0.07 F 10.10 10.32 Cl 0.02 −O=(F, Cl)2 4.26 4.35 Total 99.44 100.00 (1) Mt. Alluaiv, Kola Peninsula, Russia; here recalculated to oxides. (2) Na3(SO4)F. Occurrence: A sublimate from steam around a hot spring (Hortense Hot Spring, Colorado, USA); in nepheline syenite pegmatite veins in a differentiated alkalic massif (Mt. Alluaiv, Kola Peninsula, Russia); in sodalite–syenite xenoliths associated with an intrusive alkalic gabbro–syenite complex (Mont Saint-Hilaire, Canada). -
Natron Na2co3 • 10H2O C 2001-2005 Mineral Data Publishing, Version 1
Natron Na2CO3 • 10H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: m. Granular to fine crystalline, as crusts, efflorescences, and coatings. Twinning: On {001}. Physical Properties: Cleavage: Distinct on {001}; imperfect on {010}; in traces on {110}. Fracture: Conchoidal. Tenacity: Brittle. Hardness = 1–1.5 D(meas.) = 1.478 D(calc.) = 1.458 Soluble in H2O, alkaline taste; dehydrates rapidly in air forming thermonatrite. Optical Properties: Semitransparent. Color: Colorless to white, may be yellow or gray due to impurities; colorless in transmitted light. Luster: Vitreous. Optical Class: Biaxial (–). Orientation: X = b; Z ∧ c ' 41◦. Dispersion: r> v,perceptible, crossed. α = 1.405(3) β = 1.425(3) γ = 1.440(3) 2V(meas.) = Large. Cell Data: Space Group: Cc (synthetic). a = 12.83(2) b = 9.026(9) c = 13.44(5) β = 123.0(5)◦ Z=4 X-ray Powder Pattern: Synthetic. (ICDD 15-800). 3.04 (100), 3.02 (70), 2.894 (60), 5.37 (45), 3.94 (30), 3.45 (25), 4.50 (20) Chemistry: (1) (2) SO3 0.83 CO2 15.66 15.38 MgO 0.15 CaO 0.18 Na2O 21.50 21.66 Cl 0.41 H2O 61.69 62.96 Total 100.42 100.00 • (1) Hall, Austria. (2) Na2CO3 10H2O. Occurrence: Formed on the margins around soda-rich lakes, or as a precipitate on lake bottoms during cold weather; as an efflorescence on lavas; rare in differentiated alkaline massifs. Association: Thermonatrite, trona, mirabilite, gaylussite, gypsum, calcite. Distribution: Many reported occurrences may be of thermonatrite, an easily-obtained alteration product.