Cost-Effective Cementitious Material Compatible with Yucca Mountain Repository Geochemistry

Total Page:16

File Type:pdf, Size:1020Kb

Cost-Effective Cementitious Material Compatible with Yucca Mountain Repository Geochemistry ORNL/TM-2004/296 Cost-Effective Cementitious Material Compatible with Yucca Mountain Repository Geochemistry December 2004 Prepared by Les Dole1 Catherine Mattus1 Mostafa Fayek2 Lawrence M. Anovitz1 Juan J. Ferrada1 David J. Wesolowski1 Don Olander3 Don A. Palmer1 Lee R. Riciputi1 Lætitia Delmau1 Sergé Ermichev4* Vyacheslav I. Shapovalov4* ___________________ 1 Oak Ridge National Laboratory, 2 University of Tennessee, 3 University of California Berkeley, 4 MINATOM VNIIEF, Sarov, * funded by ISTC programs ORNL/TM-2004/296 COST-EFFECTIVE CEMENTITIOUS MATERIAL COMPATIBLE WITH YUCCA MOUNTAIN REPOSITORY GEOCHEMISTRY December 2004 Les Dole1 , Catherine Mattus1, Mostafa Fayek2, Lawrence M. Anovitz1, Juan J. Ferrada1, David J. Wesolowski1, Don Olander3, Don A. Palmer1, Lee R. Riciputi1, Lætitia Delmau1, Sergé Ermichev4*, Vyacheslav I. Shapovalov4* 1 Oak Ridge National Laboratory, 2 University of Tennessee, 3 University of California Berkeley, 4 MINATOM VNIIEF, Sarov, *funded by ISTC programs. Contact: Les Dole, 865-576-4319, [email protected], Nuclear Science and Technology Division, Oak Ridge National Laboratory Prepared by OAK RIDGE NATIONAL LABORATORY P.O. Box 2008 Oak Ridge, Tennessee 37831-6254 managed by UT-Battelle, LLC for the U.S. DEPARTMENT OF ENERGY under contract DE-AC05-00OR22725 TABLE OF CONTENTS List of Figures .............................................................................................................................................vii List of Tables ...............................................................................................................................................ix Acroynyms ...................................................................................................................................................xi Summary of Needed Research......................................................................................................................1 Introduction...............................................................................................................................................1 Meeting YMP Needs ................................................................................................................................1 Recommended Experimental Studies and Analyses.................................................................................3 Natural Analog Studies.............................................................................................................................4 Responsibilities.........................................................................................................................................5 Introduction...................................................................................................................................................5 Scientific Basis for Using High-Silica Cements ...........................................................................................6 Yucca Mountain Project Concerns with the Uses of Cements in the YM Repository .............................6 Summary of Concerns..........................................................................................................................6 Addressing YMP Concerns ..................................................................................................................7 Silicates Suppress the Formation of Calcium Hydroxide ................................................................7 Fine Pore Distribution in High-Silica Cements Reduces the Release of Moisture........................19 Silica-Saturated Cement Leachates Will Not Dissolve Adjacent Vitreous Tuff............................22 Pozzolanic Additives Are Water-Reducing Agents and Minimize the Need for Surfactants........22 High-Silica Cements Limit the Bioavailability of Nutrients..........................................................23 Natural and Anthropogenic Analogs Can Predict Long-Term Performance .................................24 Research Needs...........................................................................................................................................25 Need 1: Develop and Test Cost-Effective, High-Silica Cementitious Materials for Construction of Yucca Mountain (YM) Inverts, Drift Liners, and Bulkheads.................................................................25 Preliminary Analysis of Potential Cost Savings.................................................................................29 Potential Economic Impacts of Substituting a Conservative 100-mm Thickness of Fiber- Rreinforced Shotcrete ....................................................................................................................31 Economic Impact of Using a More Likely 50-mm Thickness of Shotcrete...................................31 Summary and Comparisons of Preliminary Economic Analyses ..................................................31 The Laboratory Tasks to Support these Objectives............................................................................31 Need 2: Establish Long-Term Performance of High-Silica Concretes by Studying and Characterizing Natural and Anthropogenic Analogs in order To Predict the Long-Term Performance (>300,000 years) of these Materials ..................................................................................32 Anthropogenic Analog Studies...........................................................................................................33 Roman Cements .............................................................................................................................35 Natural Analogs .............................................................................................................................36 Need 3: Negotiate and Coordinate Work Plans with Parallel Russian Program under an International Science and Technology Center (ISTC) Agreement with the Russian Federation ...........38 Description of Tasks ...............................................................................................................................38 Laboratory Studies .............................................................................................................................39 Selection of Materials and Formulations............................................................................................39 Preparation of Test Specimens and Physical Testing.........................................................................40 Fresh Paste .....................................................................................................................................40 Exposure Testing Using Intact Cement Monoliths ........................................................................43 Flow-Through Exposure Testing ...................................................................................................47 Effects of High Temperatures on High-Silica Concretes...............................................................50 Biodegradation Studies ..................................................................................................................51 Chemical Analyses of Solid and Liquid Phases and Mineralogical Changes................................51 v Characterize and Detect the Phases that Form due to Interaction with Groundwater....................51 Cost Comparison Study .................................................................................................................51 Models of the Aging of Cementitious Materials............................................................................52 Anthropogenic Analog Tasks.............................................................................................................53 Natural Analog Tasks.........................................................................................................................53 Laboratory Examination on Anthropogenic and Natural Samples ................................................54 Work Breakdown, Costs, and Schedule......................................................................................................55 References...................................................................................................................................................61 Appendix A: Letters and Messages of Support...........................................................................................71 Appendix B: Natural Analog Site Detailed Descriptions............................................................................79 Marble Canyon, West Texas...................................................................................................................81 Hueco Limestone....................................................................................................................................82 Bone Springs Limestone.........................................................................................................................82 Christmas Mountains, West Texas .........................................................................................................84 Hatrurim Formation (Mottled Zone), Israel............................................................................................87 Scawt Hill, Larne, Co. Antrim, Northern Ireland, UK .......................................................................89 Appendix C: Annotated Bibliography.........................................................................................................93
Recommended publications
  • The Mineralogical Magazine
    THE MINERALOGICAL MAGAZINE AND JOURNAL OF THE MINERALOGICAL SOCIETY ~._---_.~----- -~---- No. 138. September, 1932. Vol. XXIII. On bultfonteinite, n, new fluorine-bearing hydrous calcium silicate from South Africa. By JOHN PARRY1 (chemical study), ALPHEUS F. WILLIAMS, De Beers Consolidated Mines, Kimberley, Union of South Africa, and F. E. WRIGHT (crystallographical and optical study), Geophysical Laboratory, Carnegie Institution of Washington, D.C.. [Read June 7,1932.] ----- HIS new mineral was first found by a miner named Cann in 1903 T or 1904 on the 480-foot level of the Bultfontein mine at Kim- berley. It occurred, associated with calcite, apophyllite, and natrolite, in a large' horse' of dolerite and shale fragments enclosed in kim- berlite. This huge inclusion, several hundred feet in height, un- doubtedly formed part of the country-rock that now encloses the kimberlite pipe. The specimens of the new mineral were considered to be natrolite and were presented to Mr. A. F. Williams. Several years later the same mineral was found by Mr. C. E. Adams in the Dutoitspan mine, which is located about half a mile from the Bult- fontein mine; he presented his specimens tothe MacGregor Museum at Kimberley. Recently, Mr. Miller, Underground Manager of the Jagers- fontein mine in Orange River Colony, discovered the new mineral in that mine, which is located 100 miles south-east of Kimberley. 1 Mr. John Parry, Chief Chemist of the De Beers Consolidated Mines at Kim. berley, died on October 6, 1931. M 146 J. PARRY, A. F. WILLIAMS,AND F. E. WRIGHT ON After the description of the new mineral afwillite1 had been pub- lished, Mr.
    [Show full text]
  • Olmiite, Camn[Sio3(OH)](OH), the Mn-Dominant Analogue of Poldervaartite, a New Mineral Species from Kalahari Manganese Fields (Republic of South Africa)
    Mineralogical Magazine, April 2007, Vol. 71(2), pp. 193–201 Olmiite, CaMn[SiO3(OH)](OH), the Mn-dominant analogue of poldervaartite, a new mineral species from Kalahari manganese fields (Republic of South Africa) 1, 2 3 4 1 1 P. BONAZZI *, L. BINDI ,O.MEDENBACH ,R.PAGANO ,G.I.LAMPRONTI AND S. MENCHETTI 1 Dipartimento di Scienze della Terra, Universita` degli Studi di Firenze, Via La Pira, 4, I-50121, Firenze, Italy 2 Museo di Storia Naturale, sezione di Mineralogia, Universita` di Firenze, Via La Pira 4, I-50121 Firenze, Italy 3 Institut fu¨r Geologie, Mineralogie und Geophysik, Ruhr-Universita¨t Bochum, Universita¨tsstraße 150, D-44780 Bochum, Germany 4 P.O. Box 37, I-20092 Cinisello, Milano, Italy [Received 10 April 2007; Accepted 12 July 2007] ABSTRACT Olmiite, ideally CaMn[SiO3(OH)](OH), is a newly identified mineral from the N’Chwaning II mine of the Kalahari manganese fields (Republic of South Africa), which occurs as a product of hydrothermal alteration associated with poldervaartite, celestine, sturmanite, bultfonteinite and hematite. The mineral occurs as wheat-sheaf aggregates consisting of pale to intense reddish pink minute crystals. Olmiite is transparent with vitreous lustre, and exhibits deep-red fluorescence under short-wave UV-light. The mineral is brittle, with irregular fracture. Streak is white and Mohs hardness is 5À5Ý. No cleavage was observed. The measured density (pycnometer method) is 3.05(3) g/cm3. The calculated density is 3.102 g/cm3 or 3.109 g/cm3 using the unit-cell volume from single-crystal or powder data, respectively. Olmiite is biaxial positive, with refractive indices a = 1.663(1), b = 1.672(1), g = 1.694(1) (589 nm), 2Vmeas = 71.8(1)º, 2Vcalc = 66(8)º.
    [Show full text]
  • New Mineral Names*
    American Mineralogist, Volume 71, pages 227-232, 1986 NEW MINERAL NAMES* Pers J. Dulw, Gsoncr Y. CHao, JonN J. FrrzperRrcr, RrcHeno H. LaNcr-nv, MIcHeer- FrerscHnn.aNo JRNBIA. Zncznn Caratiite* sonian Institution. Type material is at the Smithsonian Institu- tion under cataloguenumbers 14981I and 150341.R.H.L. A. M. Clark, E. E. Fejer, and A. G. Couper (1984) Caratiite, a new sulphate-chlorideofcopper and potassium,from the lavas of the 1869 Vesuvius eruption. Mineralogical Magazine, 48, Georgechaoite* 537-539. R. C. Boggsand S. Ghose (1985) GeorgechaoiteNaKZrSi3Or' Caratiite is a sulphate-chloride of potassium and copper with 2HrO, a new mineral speciesfrom Wind Mountain, New Mex- ideal formula K4Cu4Or(SO4).MeCl(where Me : Na and,zorCu); ico. Canadian Mineralogist, 23, I-4. it formed as fine greenacicular crystalsin lava of the 1869 erup- S. Ghose and P. Thakur (1985) The crystal structure of george- tion of Mt. Vesuvius,Naples, Italy. Caratiite is tetragonal,space chaoite NaKZrSi3Or.2HrO. Canadian Mineralogist, 23, 5-10. group14; a : 13.60(2),c : a.98(l) A, Z:2.The strongestlines of the powder partern arc ld A, I, hkll: 9.61(l00Xl l0); Electron microprobe analysis yields SiO, 43.17, 7-xO229.51, 6.80(80X200); 4.296(60X3 I 0); 3.0I 5( 100b)(a 20,32r); 2.747 (7 0) NarO 7.42,IGO I1.28, HrO 8.63,sum 100.010/0,corresponding (4 I t); 2.673(60X5 I 0); 2.478(60)(002); 2. 3 8 8(70Xa 3 l, 50I ); to empirical formula Na, orl(oru(Zro rrTio o,Feo o,)Si, or Oe' 2.
    [Show full text]
  • New Mineral Names*,†
    American Mineralogist, Volume 101, pages 2570–2573, 2016 New Mineral Names*,† DMITRIY I. BELAKOVSKIY1, OLIVIER C. GAGNE2, AND YULIA UVAROVA3 1Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18 korp. 2, Moscow 119071, Russia 2Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba, R3T 2N2, Canada 3CSIRO Mineral Resources, CSIRO, ARRC, 26 Dick Perry Avenue, Kensington, Western Australia 6151, Australia IN THIS ISSUE This New Mineral Names has entries for 9 new mineral species, including dmisokolovite, geschieberite, imayoshiite, palladosilicide, plášilite, raisaite, shchurovskyite, svornostite, and vanackerite. GESCHIEBERITE* AND SVORNOSTITE* 3.681 (18; 311), 3.403 (12; 013), 3.304 (15; 401,113), 3.006 (17; 122). The unit-cell parameters refined from powder-diffraction data are: a = J. Plášil, J. Hloušek, A.V. Kasatkin, R. Škoda, M. Novàk and J. Čejka 13.786(5), b = 7.278(3), c = 11.536(4) Å, V = 1157.4 Å3. Single-crystal (2015) Geschieberite, K (UO )(SO ) (H O) , a new uranyl sulfate 2 2 4 2 2 2 X-ray diffraction data collected on a crystal of size 0.19 × 0.11 × 0.09 mm mineral from Jáchymov. Mineralogical Magazine, 79(1), 205–216. refined to R = 0.028 for 1882 unique reflections with I ≥ 3σ(I) shows J. Plášil, J. Hloušek, A.V. Kasatkin, M. Novák, J. Čejka and L. Lapčák 1 geschieberite is orthorhombic, Pna2 , with a = 13.7778(3), b = 7.2709(4), (2015) Svornostite, K Mg[(UO )(SO ) ] ∙8H O , a new uranyl sulfate 1 2 2 4 2 2 2 c = 11.5488(2) Å, V = 1156.92 Å3, Z = 4.
    [Show full text]
  • Bultfonteinite Ca2sio2(OH; F)4 C 2001 Mineral Data Publishing, Version 1.2 ° Crystal Data: Triclinic
    Bultfonteinite Ca2SiO2(OH; F)4 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Triclinic. Point Group: 1: As radiating prismatic acicular crystals and radial spherules, to 2 cm. Twinning: Interpenetrating on 100 and 010 ; polysynthetic. f g f g Physical Properties: Cleavage: Good on 100 and 010 . Fracture: Conchoidal. Hardness = 4.5 D(meas.) = 2.73 D(calc.) =f2.74g f g Optical Properties: Transparent. Color: Pale pink to colorless. Luster: Vitreous. Optical Class: Biaxial (+). Orientation: Z 0 c = 27±{29± on 010 ; Z 0 c = 46±{48± on 100 . Dispersion: r > v; barely perceptibl^e. ® = 1.587(2) f ¯ =g [1.59^0] ° = 1.597(2) f g 2V(meas.) = 70± Cell Data: Space Group: P 1: a = 10.992(4) b = 8.185(2) c = 5.671(1) ® = 93±570 ¯ = 90±190 ° = 89±510 Z = 4 X-ray Powder Pattern: Bultfontein mine, Kimberley, South Africa. 1.93 (100), 8.12 (60), 2.92 (60), 2.88 (60), 2.037 (50), 4.06 (40), 3.50 (40) Chemistry: (1) (2) SiO2 26.50 24.06 B2O3 0.02 Al2O3 0.72 1.37 CaO 54.20 53.59 Na2O 0.04 F 8.81 7.90 + H2O 10.78 H2O¡ 0.75 H2O 13.36 CO2 4.65 P2O5 0.02 O = F 3.71 3.33 ¡ 2 Total 99.88 99.85 (1) Bultfontein mine, Kimberley, South Africa. (2) Fuka, Japan; corresponds to (Ca2:04 (Si0:96Al0:06)§=1:02O2:13[(OH)2:87F1:00]§=3:87: Occurrence: In a large \horse" of diabase and shale fragments in a kimberlite pipe (Bultfontein mine, Kimberley, South Africa); in a contact zone in thermally metamorphosed limestone (Crestmore, California, USA).
    [Show full text]
  • Bultfonteinite from Crestmore, California
    BULTFONTEINITE FROM CRESTMORE, CALIFORNIA Josneu Munoocu, Univers,ityoJ CaliJornia at Los Angeles, Los Angeles, Cal iJorn i a. AssrRlcr The rare mineral bultfonteinite has been found in the contact zone at Cresrmore, California, in association with afwillite and scawtite. It occurs with these as microscopic, twinned individuals, much finer grained than the enclosing minerals. Opticai and micro- chemical observations indicated that it is bultfonteinite, and this is confirmed by r-ray powder pattern, which matches that of the t1'pe material. This is the first locality for this mineral outside of South Africa The powder pattern shows the following spacings and intensities for the strongest lines: 8.16 A-7; 3.51 A-5; 3.+O A-5; 2.92 A-1O;2.385 A-10; -1.93 A-10. X-ray measurements on a crystal sliver from the type locality give cell-dimensions and ansles as follows: ao:8.34A bo:11.18A co:5.68A I:88'24/ p :86" 06' v:90o 00' These agree very closely with morphological measurements by Wright, provided his o and b axes are exchanged, and the value for the new D axis is doubled. The transformation formula, Wright to Murdoch is0I0/20O/0f1. The rare mineral Bultfonteinite was discoveredabout 1903 or 1904 in the Bultfontein mine, in the Kimberley District, South Africa. Several years later it appeared in the Dutoitspan mine in the same district, and shortly before 1932 it was found also at the Jagersfontein mine in the Orange River Colony, somehundred miles southeastof Kimberley. When first collected, it was thought to be natrolite, but was later recognized by A.
    [Show full text]
  • New Mineral Names*,†
    American Mineralogist, Volume 100, pages 1319–1332, 2015 New Mineral Names*,† FERNANDO CÁMARA1, OLIVIER C. GAGNÉ2, DMITRIY I. BELAKOVSKIY3 AND YULIA UVAROVA4 1Dipartimento di Scienze della Terrá, Universitá di degli Studi di Torino, Via Valperga Caluso, 35-10125 Torino, Italy 2Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada 3Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18 korp. 2, Moscow 119071, Russia 4Mineral Resources Flagship, CSIRO, ARRC, 26 Dick Perry Avenue, Kensington, Western Australia 6151, Australia IN THIS ISSUE This New Mineral Names has entries for 25 new minerals, including alcaparrosaite, bastnäsite-(Nd), calciolangbeinite, chovanite, chromio-pargasite (ehimeite), chukhrovite-(Ca), dzhuluite, eltyubyuite, ferrisepiolite, hereroite, hielscherite, iseite, itsiite, jakobssonite, kazanskiite, meisserite, nashite, omsite, schindlerite, tanohataite, tazzoliite, vapnikite, vladkrivovichevite, wernerbaurite, and wopmayite. ALCAPARROSAITE* r < v. The optical orientation is X = b; Y ^ c = 27° in the obtuse A.R. Kampf, S.J. Mills, R.M. Housley, P.A. Williams, and M. angle β. No pleochroism was observed. The average of 4 electron 4+ 3+ probe analyses gives [wt% (range)]: Na2O 0.32 (0.16–0.51), K2O Dini (2012) Alcaparrosaite, K3Ti Fe (SO4)4O(H2O)2, a new hydrophobic Ti4+ sulfate from Alcaparrosa, Chile. Mineralogi- 20.44 (20.30–20.67), Fe2O3 11.58 (11.41–11.71), TiO2 11.77 cal Magazine, 76(4), 851–861. (11.54–12.18), P2O5 0.55 (0.48–0.68), SO3 47.52 (46.57–48.06), H2O 5.79 (calculated from structure refinement); total 97.97 wt%. 4+ 3+ 4+ This gives the empirical formula (K2.89Na0.07)Σ2.96Ti0.98Fe0.97(S0.99 Alcaparrosaite (IMA 2011-024), ideally K3Ti 3+ P0.01O4)4O0.72(OH)0.28(H2O)2 based on 19 O pfu.
    [Show full text]
  • Lsosh20, a New Mineral from Fuka, Okayama Prefecture, Japan
    Clinotobermorite, CaSSi6(O,OH)lSoSH20, a new mineral from Fuka, Okayama Prefecture, Japan C. HENMI Department of Earth Sciences, Faculty of Science, Okayama University, Okayama 700 Japan AND 1. KUSACHI Department of Earth Sciences, Faculty of Education, Okayama University, Okayama 700 Japan Abstract Clinotobermorite, CasSi6(0,OHhs.5H20, has been found as a vein-forming mineral in gehlenite- spurrite skarns at Fuka, Okayama Prefecture. It is associated with tobermorite, piombierite, apophyllite, and calcite. The cIinotobermorite is colourless or white and occurs as tabular or acicular crystals. It is monoclinic with the space group Ce or C2le. The unit cell dimensions are a 11.331, b 7.353, c 22.67 A, ~ 96.59°. Microtwinning and stacking disorder on (001) are observed. On heating the cIinotobermorite at 300°C, the 002 spacing is reduced from 11.3 to 9.3 A. Its refractive indices are IX1.575, ~1.580, y 1.585, and the density 2.58 g/cm3 (meas.), 2.69 g/cm3 (calc). The Moh's hardness is 4.5. Calculation of the analytical data on the basis of six tetrahedral cations shows that this mineral has a simplified chemical formula Cas.3Si6(0,OH,F)1s.5H20. The chemical composition and the unit cell are closely related to those of tobermorite. It is most likely that clinotobermorite is a low-temperature polymorph of tobermorite. KEYWORDS:clinotobermorite, new mineral, tobermorite, Okayama Prefecture, Japan. Introduction morite. The mineral species and its name have TOBERMORITE (11.3 A tobermorite), plombier- been approved by the Commission on New ite (14 A tobermorite), tacharanite (12.6 A Minerals and Mineral Names, International tobermorite), riversideite (9.3 A tobermorite) Mineralogical Association, in May 1990.
    [Show full text]
  • Nchwaningite, Mn~+Si03(OH)2'H20, a New Pyroxene-Related Chain Silicate from the N'chwaning Mine, Kalahari Manganese Field, South Africa
    American Mineralogist. Volume 80, pages 377-386, 1995 Nchwaningite, Mn~+Si03(OH)2'H20, a new pyroxene-related chain silicate from the N'chwaning mine, Kalahari manganese field, South Africa DANIEL NYFELER, THOMAS ARMBRUSTER Laboratorium rur chemische und mineralogische Kristallographie, Universitiit Bern, Freiestrasse 3, CH-3012 Bern, Switzerland ROGER DIXON Museum of the Geological Survey, PB X1l2, 0001 Pretoria, South Africa VLADIMIR BERMANEC Department of Mineralogy and Petrology of Faculty of Science, University of Zagreb, Demetrova I, 41000 Zagreb, Croatia ABSTRACT Nchwaningite, Mn~+ Si03(OH)2' H20, is an orthorhombic chain silicate [space group Pea2" Z = 4, a = 12.672(9), b = 7.217(3), e = 5.341(2) A], occurring as aggregates shaped like pin cushions, together with calcite, bultfonteinite, and chlorite at N'chwaning mine, located in the Kalahari manganese field, northern Cape Province, South Africa. The ag- gregates consist of light brown, transparent needles, which average 1.0 x 0.1 x 0.05 mm in size. Nchwaningite is named after the mine N'chwaning II, where it was found first. Nchwaningite is biaxially negative with the refractive indices ex= 1.681(2), fJ = 1.688(2), b, Y = a, Z = c. Nchwaningite 'Y= 1.690(2), 2 ~ = 54.4(4)°. The optical orientation is X = has two perfect cleavages parallel to (010) and (100). The calculated density is 3.202 glcm3. The chemical composition, as determined by electron microprobe analyses, indicates mi- nor substitutions of Mg for Mn. The crystal structure, including H positions, was solved and refined from X-ray single- crystal data to R = 2.14%, Rw = 2.91%.
    [Show full text]
  • AND ORE-FORMING MINERALS (December 30, 2019) ______
    THE CANADIAN MINERALOGIST LIST OF SYMBOLS FOR ROCK- AND ORE-FORMING MINERALS (December 30, 2019) ____________________________________________________________________________________________________________ Ac acanthite Adr andradite Ast astrophyllite Brl beryl Act actinolite Ang angelaite At atokite Bll beryllonite Ae aegirine Agl anglesite Au gold Brz berzelianite Aen aenigmatite Anh anhydrite Aul augelite Bet betafite Aes aeschynite-(Y) Ani anilite Aug augite Bkh betekhtinite Aik aikinite Ank ankerite Aur auricupride Bdt beudantite Akg akaganeite Ann annite Aus aurostibite Beu beusite Ak åkermanite An anorthite Aut autunite Bch bicchulite Ala alabandite Anr anorthoclase Aw awaruite Bt biotite* Ab albite Atg antigorite Axn axinite-(Mn) Bsm bismite Alg algodonite Sb antimony Azu azurite Bi bismuth All allactite Ath anthophyllite Bdl baddeleyite Bmt bismuthinite Aln allanite Ap apatite* Bns banalsite Bod bohdanowiczite Alo alloclasite Arg aragonite Bbs barbosalite Bhm böhmite Ald alluaudite Ara aramayoite Brr barrerite Bor boralsilite Alm almandine Arf arfvedsonite Brs barroisite Bn bornite Alr almarudite Ard argentodufrénoysite Blt barylite Bou boulangerite Als alstonite Apn argentopentlandite Bsl barysilite Bnn bournonite Alt altaite Arp argentopyrite Brt baryte, barite Bow bowieite Aln alunite Agt argutite Bcl barytocalcite Brg braggite Alu alunogen Agy argyrodite Bss bassanite Brn brannerite Amb amblygonite Arm armangite Bsn bastnäsite Bra brannockite Ams amesite As arsenic Bau baumstarkite Bnt braunite Amp amphibole* Ass arseniosiderite
    [Show full text]
  • Crystal Structure of Bultfonteinite, Ca4[Sio3(OH)]2F2·2H2O, from N’Chwaning II Mine (Kalahari Manganese Field, Republic of South Africa)
    atti Soc. tosc. Sci. nat., Mem., Serie a, 115 (2010) pagg. 9-15, figg. 3, tabb. 5; doi: 10.2424/ASTSN.M.2010.02 C. Biagioni (*), E. Bonaccorsi (*), S. Merlino (*) CRySTaL structure OF bultfonteiNiTE, Ca4[SiO3(OH)]2F2·2H2O, from N’CHWaNiNG ii MiNE (KaLaHaRi MaNGaNESE FiELD, REPUBLiC OF SOUTH aFRiCa) Abstract - The finding of well-crystallized specimens of with tobermorite and afwillite. Bultfonteinite was also bultfonteinite from the N’Chwaning II mine (Kalahari identified in the Wessels and N’Chwaning II mines Manganese Field, Republic of South africa) in the 1980s (Kalahari Manganese Field, Republic of South africa; allowed the collection of new data about the crystal structure Von Bezing et al., 1991); its origin is related to an of this calcium silicate hydrate. The crystal structure study is in agreement with the general features outlined by Mciver important hydrothermal process, known as the Wes- (1963) and allows the description of a reasonable hydrogen- sels alteration event, occurred about 1.0-1.25 Ga ago bond scheme. (Gutzmer & Beukers, 1996). The widespread twinning shown by bultfonteinite Key words - Bultfonteinite, C-S-H, crystal structure, made the crystal structure determination difficult; the N’Chwaning ii mine, Republic of South africa. cell parameters were determined by Murdoch (1955), whereas Megaw & Kelsey (1955) identified the twin Riassunto - Struttura cristallina della bultfonteinite, laws: according to them, twinning takes place accord- Ca4[SiO3(OH)]2F2·2H2O, dalla N’Chwaning II mine (Kala- ing to axes normal to the (100) and/or (010) planes, with hari Manganese Field, Repubblica Sudafricana). il ritrova- an angle between the two twin axes of about 90°.
    [Show full text]
  • Mineral Species Found at Franklin and Sterling Hill, NJ
    Mineral Species Found at Franklin and Sterling Hill, NJ This list is current as of September 2008 and is revised annually by the Mineral List Committee of the Franklin- Ogdensburg Mineralogical Society. Species unique to the Franklin-Sterling Hill area are in bold type. A D J P T Acanthite Datolite Jacobsite Parabrandtite Talc Actinolite Descloizite Jarosewichite Paragonite Tennantite Adamite Devilline Jerrygibbsite Pararammelsbergite Tephroite Adelite Digenite Johannsenite Pararealgar Tetrahedrite Aegirine Diopside Johnbaumite Parasymplesite Thomsonite-Ca Akrochordite Djurleite Junitoite Pargasite Thorite Albite Dolomite Pectolite Thortveitite Allactite Domeykite K Pennantite Thorutite Allanite-(Ce) Dravite Kaolinite Petedunnite Tilasite Alleghanyite Duftite Kentrolite Pharmacolite Titanite Almandine Dundasite Kittatinnyite Pharmacosiderite Todorokite Analcime Dypingite Kolicite Phlogopite Torreyite Anandite Köttigite Picropharmacolite Tremolite Anatase E Kraisslite Piemontite Turneaureite Andradite Edenite Kutnahorite Powellite Anglesite Epidote Prehnite U Anhydrite Pumpellyite-(Mg) Epidote-(Pb) L Uraninite Annabergite Epsomite Pyrite Uranophane-alpha Anorthite Larsenite Pyroaurite Erythrite Laumontite Uranospinite Anorthoclase Esperite Pyrobelonite Uvite Antlerite Lawsonbauerite Pyrochroite Euchroite Lead Apatite-(CaF) Eveite Pyrophanite Apophyllite-(KF) Legrandite Pyrosmalite-(Mn) V Apophyllite-(KOH) Lennilenapeite Pyroxmangite Vesuvianite Aragonite F Leucophoenicite Pyroxferroite Villyaellenite Arsenic Fayalite Linarite Pyrrhotite
    [Show full text]