Structure, Fractality, Mechanics and Durability of Calcium Silicate Hydrates
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Tobermorite Supergroup: a New Nomenclature
Mineralogical Magazine, April 2015, Vol. 79(2), pp. 485–495 The tobermorite supergroup: a new nomenclature CRISTIAN BIAGIONI*, STEFANO MERLINO AND ELENA BONACCORSI Dipartimento di Scienze della Terra, Universita` di Pisa, Via Santa Maria 53, 56126 Pisa, Italy [Received 10 July 2014; Accepted 30 September 2014; Associate Editor: S. J. Mills] ABSTRACT The name ‘tobermorites’ includes a number of calcium silicate hydrate (C-S-H) phases differing in their hydration state and sub-cell symmetry. Based on their basal spacing, closely related to the degree of hydration, 14, 11 and 9 A˚ compounds have been described. In this paper a new nomenclature scheme for these mineral species is reported. The tobermorite supergroup is defined. It is formed by the tobermorite group and the unclassified minerals plombie`rite, clinotobermorite and riversideite. Plombie`rite (‘14 A˚ tobermorite’) is redefined as a crystalline mineral having chemical composition Ca5Si6O16(OH)2·7H2O. Its type locality is Crestmore, Riverside County, California, USA. The tobermorite group consists of species having a basal spacing of ~11 A˚ and an orthorhombic sub-cell symmetry. Its general formula is Ca4+x(AlySi6Ày)O15+2xÀy·5H2O. Its endmember compositions correspond to tobermorite Ca5Si6O17·5H2O(x =1andy = 0) and the new species kenotobermorite, Ca4Si6O15(OH)2·5H2O(x =0andy = 0). The type locality of kenotobermorite is the N’Chwaning II mine, Kalahari Manganese Field, South Africa. Within the tobermorite group, tobermorite and kenotobermorite form a complete solid solution. Al-rich samples do not warrant a new name, because Al can only achieve a maximum content of 1/6 of the tetrahedral sites (y = 1). -
The Hydrated Calcium, Silicates Riversideite, Tobermorite, and Plombierite
293 The hydrated calcium, silicates riversideite, tobermorite, and plombierite. By J. D. C. McCoNNELL,M.Sc. 1)epartment of Mineralogy and Petrology, University of Cambridge. [Conmmnicated by Prof. C. E. Tilley, F.R.S., read March 26, 1953] ] NTRODUCTION. N a recent paper Taylor has shown that three distinct hydration I levels exist within the" calcium silicate hydrate (l)' group of artificial preparations (Taylor, 1953a, p. 168). The individual hydrates may be distinguished from the position of the 002 reflection in X-ray powder photographs. The d spacings corresponding to the three hydrates of this group examined during the present investigation are 1~'6, 11"3, and 9"6 ,A.. These hydrates have 1-[20 : SiO 2 molar ratios of approximately 2-0, 1.0, and 0"5 respectively. A recent examination of the minerals crestmoreite and riversideite (Taylor, 1953b) has shown that both these nfinerals are intimate inter- :growths of members of the above hydrate series with the mineral wilkeite. Both the artificial preparations and the crestmoreite-riversideite inter- growths have failed to provide material suitable for detailed optical study. During a mineralogical investigation of rocks from a dolerite-chalk contact at Ballycraigy, Larne, County Antrim, a mineral was examined and subsequently identified, from X-ray powder photographs, with the 11"3 .~. hydrate referred to above. Optical and X-ray studies on single crystals of this mineral were made and subsequently both the 14.6 and 9-6 A. hydrates were prepared from this material experimentally. X-ray powder photographs of a gelatinous material collected at Ballycraigy showed that this m~tteria] could also be identified with the 'calcium silicate hydrate (f)' group. -
Alkali-Silica Reactivity: an Overview of Research
SHRP-C-342 Alkali-Silica Reactivity: An Overview of Research Richard Helmuth Construction Technology Laboratories, Inc. With contributions by: David Stark Construction Technology Laboratories, Inc. Sidney Diamond Purdue University Micheline Moranville-Regourd Ecole Normale Superieure de Cachan Strategic Highway Research Program National Research Council Washington, DC 1993 Publication No. SHRP-C-342 ISBN 0-30cL05602-0 Contract C-202 Product No. 2010 Program Manager: Don M. Harriott Project Maxtager: Inam Jawed Program AIea Secretary: Carina Hreib Copyeditor: Katharyn L. Bine Brosseau May 1993 key words: additives aggregate alkali-silica reaction cracking expansion portland cement concrete standards Strategic Highway Research Program 2101 Consti!ution Avenue N.W. Washington, DC 20418 (202) 334-3774 The publicat:Lon of this report does not necessarily indicate approval or endorsement by the National Academy of Sciences, the United States Government, or the American Association of State Highway and Transportation Officials or its member states of the findings, opinions, conclusions, or recommendations either inferred or specifically expressed herein. ©1993 National Academy of Sciences 1.5M/NAP/593 Acknowledgments The research described herein was supported by the Strategic Highway Research Program (SHRP). SHRP is a unit of the National Research Council that was authorized by section 128 of the Surface Transportation and Uniform Relocation Assistance Act of 1987. This document has been written as a product of Strategic Highway Research Program (SHRP) Contract SHRP-87-C-202, "Eliminating or Minimizing Alkali-Silica Reactivity." The prime contractor for this project is Construction Technology Laboratories, with Purdue University, and Ecole Normale Superieure de Cachan, as subcontractors. Fundamental studies were initiated in Task A. -
Phillipsite and Al-Tobermorite Mineral Cements Produced Through Low-Temperature Water-Rock Reactions in Roman Marine Concrete Sean R
Western Washington University Western CEDAR Geology Faculty Publications Geology 2017 Phillipsite and Al-tobermorite Mineral Cements Produced through Low-Temperature Water-Rock Reactions in Roman Marine Concrete Sean R. Mulcahy Western Washington University, [email protected] Marie D. Jackson University of Utah, Salt Lake City Heng Chen Southeast University, Nanjing Yao Li Xi'an Jiaotong University, Xi'an Piergiulio Cappelletti Università degli Studi di Napoli Federico II, Naples See next page for additional authors Follow this and additional works at: https://cedar.wwu.edu/geology_facpubs Part of the Geology Commons Recommended Citation Mulcahy, Sean R.; Jackson, Marie D.; Chen, Heng; Li, Yao; Cappelletti, Piergiulio; and Wenk, Hans-Rudolf, "Phillipsite and Al- tobermorite Mineral Cements Produced through Low-Temperature Water-Rock Reactions in Roman Marine Concrete" (2017). Geology Faculty Publications. 67. https://cedar.wwu.edu/geology_facpubs/67 This Article is brought to you for free and open access by the Geology at Western CEDAR. It has been accepted for inclusion in Geology Faculty Publications by an authorized administrator of Western CEDAR. For more information, please contact [email protected]. Authors Sean R. Mulcahy, Marie D. Jackson, Heng Chen, Yao Li, Piergiulio Cappelletti, and Hans-Rudolf Wenk This article is available at Western CEDAR: https://cedar.wwu.edu/geology_facpubs/67 American Mineralogist, Volume 102, pages 1435–1450, 2017 Phillipsite and Al-tobermorite mineral cements produced through low-temperature k water-rock reactions in Roman marine concrete MARIE D. JACKSON1,*, SEAN R. MULCAHY2, HENG CHEN3, YAO LI4, QINFEI LI5, PIERGIULIO CAppELLETTI6, 7 AND HANS-RUDOLF WENK 1Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112, U.S.A. -
Charlesite, a New Mineral of the Ettringite Group, from Franklin, New Jersey
American Mineralogist, Volume 68, pages 1033-1037,1983 Charlesite, a new mineral of the ettringite group, from Franklin, New Jersey PBre J. DuxN Department of Mineral Sciences SmithsonianInstitution, Washington,D. C. 20560 DoNero R. Peecon Department of GeologicalSciences University of Michigan, Ann Arbor, Michigan 48109 PBrnn B. LBavBNs Departmentof Geology Universityof Delaware, Newark, Delaware l97ll eNo JonN L. Beuu Franklin Mineral Museum Franklin. New Jersey 07416 Abstract Charlesite,ideally C4(AI,Si)z(SO4)2(B(OH)4)(OH,O)r2.26H2Ois a member of the ettrin- gite group from Franklin, New Jersey, and is the Al analogueof sturmanite. Chemical analysisyielded CaO27.3, Al2O3 5.1, SiO2 3.1, SO3 12.8,B2o33.2, H2O 48.6, sum : 100.1 percent.-Charlesiteis hexagonal,probable spacegroup P3lc, with a = ll.16(l), c = 21.21(2)4. The strongest lines in the X-ray powder difraction pattern (d, IlIo, hkl) are: 9.70,100, 100;5.58, 80, 110;3.855,80, ll4;2.749,70,304;2.538,70,126;2.193,70,2261 404. Charlesite occurs as simple hexagonal crystals tabular on {0001} and has a perfect {10T0}cleavage. The densityis 1.77glcm3 (obs.) and 1.79glcms (calc.). Optically, charlesite is uniaxial( -) with a : | .492(3)and e : 1.475(3).It occurswith clinohedrite,ganophyllite, xonotlite, prehnite, roeblingite and other minerals in severalparageneses at Franklin, New Jersey. Charlesite is named in honor of the late Professor Charles Palache. Introduction were approved, prior to publication, by the Commission Minerals and Mineral Names. I. M. A. The An ettringite-like mineral was first described from on New specimenwas divided into three portions. -
Atomistic Modeling of Crystal Structure of Ca1.67Sihx
Cement and Concrete Research 67 (2015) 197–203 Contents lists available at ScienceDirect Cement and Concrete Research journal homepage: http://ees.elsevier.com/CEMCON/default.asp Atomistic modeling of crystal structure of Ca1.67SiHx Goran Kovačević a, Björn Persson a, Luc Nicoleau b, André Nonat c, Valera Veryazov a,⁎ a Theoretical Chemistry, P.O.B. 124, Lund University, Lund 22100, Sweden b BASF Construction Solutions GmbH, Advanced Materials & Systems Research, Albert Frank Straße 32, 83304 Trostberg, Germany c Laboratoire Interdisciplinaire Carnot de Bourgogne, UMR 6303 CNRS-Université de Bourgogne, BP 47870, F-21078 Dijon Cedex, France article info abstract Article history: The atomic structure of calcium-silicate-hydrate (C1.67-S-Hx) has been investigated by theoretical methods in Received 13 February 2014 order to establish a better insight into its structure. Three models for C-S-H all derived from tobermorite are pro- Accepted 12 September 2014 posed and a large number of structures were created within each model by making a random distribution of silica Available online xxxx oligomers of different size within each structure. These structures were subjected to structural relaxation by ge- ometry optimization and molecular dynamics steps. That resulted in a set of energies within each model. Despite Keywords: an energy distribution between individual structures within each model, significant energy differences are Calcium-Silicate-Hydrate (C-S-H) (B) Crystal Structure (B) observed between the three models. The C-S-H model related to the lowest energy is considered as the most Atomistic simulation probable. It turns out to be characterized by the distribution of dimeric and pentameric silicates and the absence of monomers. -
Minerals in Cement Chemistry: a Single-Crystal Neutron Diffraction and Raman
American Mineralogist, Volume 97, pages 1060–1069, 2012 Minerals in cement chemistry: A single-crystal neutron diffraction and Raman spectroscopic study of thaumasite, Ca3Si(OH)6(CO3)(SO4)·12H2O G. DIEGO GATTA,1,2,* GARRY J. MCINTYRE,3 JULIA G. SWANSON,4 AND STEVEN D. JACOBSEN4 1Dipartimento di Scienze della Terra, Universita’ degli Studi di Milano, Via Botticelli 23, I-20133 Milano, Italy 2CNR-Istituto per la Dinamica dei Processi Ambientali, Milano, Italy 3The Bragg Institute, Australian Nuclear Science and Technology Organisation, Locked Bag 2001, Kirrawee DC, New South Wales 2232, Australia 4Department of Earth and Planetary Sciences, Northwestern University, Evanston, Illinois 60208, U.S.A. ABSTRACT Thaumasite, Ca3Si(OH)6(CO3)(SO4)⋅12H2O, is recognized as a secondary-alteration mineral and indicator of sulfate attack in Portland cement in contact with sulfate-rich groundwater, especially in cold regions. The hydrogen positions in thaumasite have been determined from single-crystal neutron diffraction structure refinements at 300 and 22 K. No phase transitions occur within the temperature range investigated. The structure of thaumasite is largely held together by hydrogen bonding. The major structural units [CO3 groups, SO4 tetrahedra, Si(OH)6 octahedra, and Ca(OH)4(H2O)4 polyhe- dra] are interconnected via 10 distinct hydrogen bonds. Analysis of the difference-Fourier maps of the nuclear density reveals the positions of all 10 hydrogen atoms in the structure, and the hydrogen bonding becomes shorter (stronger) upon decreasing temperature to 22 K. The SO4 tetrahedron ex- pands upon decreasing temperature (i.e., negative thermal expansion at the molecular level), driven 4+ by shortening of the hydrogen bonding between [Ca3Si(OH)6(H2O)12] columns. -
Brownmillerite Ca2(Al, Fe )2O5 C 2001-2005 Mineral Data Publishing, Version 1
3+ Brownmillerite Ca2(Al, Fe )2O5 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: mm2. As square platelets, to about 60 µm; massive. Physical Properties: Hardness = n.d. D(meas.) = 3.76 D(calc.) = 3.68–3.73 Optical Properties: Semitransparent. Color: Reddish brown. Optical Class: Biaxial (–). Pleochroism: Distinct; X = Y = yellow-brown; Z = dark brown. Orientation: Y and Z lie in the plane of the platelets; extinction in that plane is diagonal. α = < 2.02 β = > 2.02 γ = > 2.02 2V(meas.) = n.d. Cell Data: Space Group: Ibm2. a = 5.584(5) b = 14.60(1) c = 5.374(5) Z = 2 X-ray Powder Pattern: Near Mayen, Germany. 2.65 (vs), 7.19 (s), 2.78 (s), 1.93 (s), 2.05 (ms), 3.65 (m), 1.82 (m) Chemistry: (1) (2) (3) TiO2 1.5 1.9 Al2O3 17.2 22.3 13.1 Fe2O3 30.5 27.6 41.9 Cr2O3 0.1 n.d. MgO n.d. n.d. CaO 46.2 44.8 43.7 insol. 4.0 LOI 0.5 Total 94.4 100.3 100.6 (1) Near Mayen, Germany; by semiquantitative spectroscopy. (2) Hatrurim Formation, Israel; corresponds to Ca1.99(Al1.09Fe0.86Ti0.05)Σ=2.00O5. (3) Do.; corresponds to Ca1.95(Fe1.31Al0.64 Ti0.06)Σ=2.01O5. Occurrence: In thermally metamorphosed limestone blocks included in volcanic rocks (near Mayen, Germany); in high-temperature, thermally metamorphosed, impure limestones (Hatrurim Formation, Israel). Association: Calcite, ettringite, wollastonite, larnite, mayenite, gehlenite, diopside, pyrrhotite, grossular, spinel, afwillite, jennite, portlandite, jasmundite (near Mayen, Germany); melilite, mayenite, wollastonite, kalsilite, corundum (Kl¨och, Austria); spurrite, larnite, mayenite (Hatrurim Formation, Israel). -
Effect of Mineralogical Changes on Mechanical Properties of Well Cement
ARMA 19–1981 Well integrity of high temperature wells: Effect of mineralogical changes on mechanical properties of well cement TerHeege, J.H. and Wollenweber, J. TNO Applied Geosciences, Utrecht, the Netherlands Marcel Naumann Downloaded from http://onepetro.org/ARMAUSRMS/proceedings-pdf/ARMA19/All-ARMA19/ARMA-2019-1981/1133466/arma-2019-1981.pdf/1 by guest on 02 October 2021 Equinor ASA, Sandsli, Norway Pipilikaki, P. TNO Structural Reliability, Delft, the Netherlands Vercauteren, F. TNO Material Solutions, Eindhoven, the Netherlands This paper w as prepared for presentation at the 53rd US Rock Mechanics/Geomechanics Symposium held in New Y ork, NY , USA , 23–26 June 2019. This paper w as selected for presentation at the symposium by an ARMA Technical Program Committee based on a technical and critical review of the paper by a minimum of tw o technical reviewers. The material, as presented, does not necessarily reflect any position of ARMA, its of ficers, or members. ABSTRACT: Wells used for steam-assisted gravity drainage (SAGD), for cyclic steam stimulation (CSS), for hydrocarbon production in areas with anomalous high geothermal gradient, or for geothermal energy extraction all are operated in high temperature environments where maintaining long term wellbore integrity is one of the key challenges. Changes in cement mineralogy and associated mechanical properties may critically affect the integrity of high temperature wells. In this study, the relation between changes in mineralogy and mechanical properties of API class G cement with 40% silica flour was investigated by exposing samples for 1-4 weeks to temperatures of 60-420°C. The effect of mineralogical changes on mechanical properties was investigated using a combination of chemical and microstructural analysis and triaxial strength tests at confining pressures of 2-15 MPa. -
Calcium Silicate Hydrate Characterization by Spectroscopic Techniques
CALCIUM SILICATE HYDRATE CHARACTERIZATION BY SPECTROSCOPIC TECHNIQUES Moisés Martín-Garridoa, Sagrario Martínez-Ramíreza, Gloria Pérezb, Ana Guerrerob aINSTITUTE FOR THE STRUCTURE OF THE MATTER (IEM-CSIC), MADRID, SPAIN. bEDUARDO TORROJA INSTITUTE FOR CONSTRUCTION SCIENCE (IETCC- CSIC), MADRID, SPAIN. 1. INTRODUCTION Calcium silicate are present in the binder of many mortars used in the Cultural Heritage, such as lime-pozzolan mortars or hydraulic mortars. After hydration the calcium silicate give rise to an amorphous hydrated calcium silicate (called C-S-H† gel) whose structure resembles that of the tobermorite and jenite minerals. However, while the C-S-H gel has no well-defined stoichiometry, the other two minerals are crystalline with a well-established chemical formula, Ca5Si6O16(OH)2·4H2O for tobermorite and Ca9Si6O18(OH)6·8H2O for jenite. Both minerals have a Ca/Si ratio of 0.83 and 1.5 respectively, while the C-S-H gel has a variable stoichiometry, presenting Ca/Si relations ranging from 0.5 to 2.1. C-S-H gel can be prepared by different methods, including i) hydrothermal reaction1 of CaO and SiO2, ii) aqueous reaction of CaO and SiO2, iii) aqueous reaction of 2 Ca(NO3)2·4H2O and Na2SiO3∙5H2O (double decomposition method ), and iv) 3 mechanochemical reaction of CaO and SiO2. Different preparation methods lead to variations in structure of C-S-H. Some disadvantages come from hydrothermal and mechanochemical synthesis since they need a long time to assess the complete hydration of the SiO2 and CaO compounds; furthermore, portlandite is formed as a secondary reaction product. Due to the low crystallinity of C-S-H gel, spectroscopic techniques such as Micro- Raman; Fourier Transformed Infrared (FT-IR) and Nuclear magnetic Resonance (NMR) are the most suitable methods to characterize the structure of the compound. -
Bentorite Ca6(Cr, Al)2(SO4)3(OH)12 • 26H2O C 2001-2005 Mineral Data Publishing, Version 1
Bentorite Ca6(Cr, Al)2(SO4)3(OH)12 • 26H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 6/m 2/m 2/m. As stout hexagonal prisms, {1010}, {1011}, {0001}, to 0.25 mm; commonly in fibrous masses, granular aggregates, and thin films. Twinning: On {1010} as composition plane. Physical Properties: Cleavage: {1010}, perfect; {0001}, distinct. Hardness = 2 D(meas.) = 2.025 D(calc.) = 2.021 Optical Properties: Transparent. Color: Bright violet. Streak: Very pale violet. Luster: Vitreous. Optical Class: Uniaxial (+). Pleochroism: O = nearly colorless; E = pale violet. Absorption: O < E. ω = 1.478(2) = 1.484(2) Cell Data: Space Group: P 63/mmc. a = 22.35 c = 21.41 Z = 8 X-ray Powder Pattern: Hatrurim Formation, Israel. 9.656 (100), 5.592 (40), 1.942 (20), 3.60 (10), 3.23 (10), 2.772 (10), 3.89 (8) Chemistry: (1) SO3 14.99 CO2 6.70 SiO2 2.50 Al2O3 1.01 Fe2O3 0.10 Cr2O3 7.48 MgO 0.00 CaO 29.90 H2O 37.70 Total 100.38 (1) Hatrurim Formation, Israel; by AA, SO3 by gravimetric analysis, CO2 and H2O by TGA; after deduction of CaO and CO2 as calcite and CaO, SiO2, H2O as truscottite, the remainder 3+ • (about 80%) corresponds to Ca5.88(Cr1.61Al0.32Fe0.02)Σ=1.95(S1.02O4)3.00(OH)11.97 28.06H2O. Mineral Group: Ettringite group. Occurrence: In low-temperature hydrothermal veins in black calcite–spurrite marble. Association: Calcite, thaumasite, truscottite, vaterite, jennite, tobermorite, brownmillerite, mayenite, melnikovite, “chlorite”. Distribution: In a marble quarry in the Hatrurim Formation, near the Arad-Sodom road, Negev Desert, Israel. -
Mayenite Ca12al14o33 C 2001-2005 Mineral Data Publishing, Version 1
Mayenite Ca12Al14O33 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Cubic. Point Group: 43m (synthetic). In rounded anhedral grains, to 60 µm. Physical Properties: Hardness = n.d. D(meas.) = 2.85 D(calc.) = [2.67] Alters immediately to hydrated calcium aluminates on exposure to H2O. Optical Properties: Transparent. Color: Colorless. Optical Class: Isotropic. n = 1.614–1.643 Cell Data: Space Group: I43d (synthetic). a = 11.97–12.02 Z = 2 X-ray Powder Pattern: Near Mayen, Germany. 2.69 (vs), 4.91 (s), 2.45 (ms), 3.00 (m), 2.19 (m), 1.95 (m), 1.66 (m) Chemistry: (1) (2) (3) SiO2 0.4 Al2O3 45.2 49.5 51.47 Fe2O3 2.0 1.5 MnO 1.4 CaO 45.7 47.0 48.53 LOI 2.2 Total 95.1 99.8 100.00 (1) Near Mayen, Germany; by semiquantitative spectroscopy. (2) Hatrurim Formation, Israel; by electron microprobe, corresponding to (Ca11.7Mg0.5)Σ=12.2(Al13.5Fe0.25Si0.10)Σ=13.85O33. (3) Ca12Al14O33. Occurrence: In thermally metamorphosed limestone blocks included in volcanic rocks (near Mayen, Germany); common in high-temperature, thermally metamorphosed, impure limestones (Hatrurim Formation, Israel). Association: Calcite, ettringite, wollastonite, larnite, brownmillerite, gehlenite, diopside, pyrrhotite, grossular, spinel, afwillite, jennite, portlandite, jasmundite (near Mayen, Germany); melilite, wollastonite, kalsilite, brownmillerite, corundum (Kl¨och, Austria); spurrite, larnite, grossite, brownmillerite (Hatrurim Formation, Israel). Distribution: From the Ettringer-Bellerberg volcano, near Mayen, Eifel district, Germany. Found at Kl¨och, Styria, Austria. In the Hatrurim Formation, Israel. From Kopeysk, Chelyabinsk coal basin, Southern Ural Mountains, Russia. Name: For Mayen, Germany, near where the mineral was first described.