Experimental and Theoretical Studies on Mechanical Properties of Complex Oxides in Concrete
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Crystal Structure of Hillebrandite: a Natural Analogue of Calcium Silicate Hydrate (CSH) Phases in Portland Cement
American Mineralogist, Volume 80, pages 841-844, 1995 Crystal structure of hillebrandite: A natural analogue of calcium silicate hydrate (CSH) phases in Portland cement YONGSHAN DAI Garber Research Center, Harbison-Walker Refractories, 1001 Pittsburgh-McKeesport Boulevard, West Miffilin, Pennsylvania 15122, U.S.A. JEFFREY E. POST Departmentof MineralSciences,SmithsonianInstitution,Washington,DC 20560,U.S.A. ABSTRACT The crystal structure of hillebrandite, Ca2Si03(OH)2, was solved and refined in space group Cmc21, a = 3.6389, b = 16.311, c = 11.829 A, to R = 0.041 using single-crystal X-ray data. The structure consists of a three-dimensional network of Ca-O polyhedra that accommodates wollastonite-type Si-O tetrahedral chains. Each of the wollastonite-type chains is an average of two symmetrically equivalent chains related by the mirror plane perpen- dicular to a. In a given structural channel of the Ca-O polyhedral network, only one chain orientation can be occupied to give reasonable Si-O distances. The 03 and 04 sites cor- responding to each vacant Si2 site are occupied by OH groups to achieve charge balance. The wollastonite-type Si-O tetrahedral chains in the hillebrandite structure resemble those reported for many calcium silicate hydrate (CSH) phases. INTRODUCTION brandite and comment upon the structural relationships Hillebrandite, Ca2Si03(OH)2, is one natural member of hillebrandite with other CSH phases. of the CaO-Si02-H20 ternary system, which includes nu- merous natural and synthetic calcium silicate hydrate EXPERIMENTAL METHODS (CSH) phases, most with a common unit-cell axis of about After an exhaustive examination of many hillebrandite 3.64 or 2 x 3.64 A and a fibrous crystal habit along this samples, a fragment ofa specimen (NMNH 95767-7) from axis. -
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. -
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. -
Cement/Clay Interactions - a Review: Experiments, Natural Analogues, and Modeling Eric C
Cement/clay interactions - A review: Experiments, natural analogues, and modeling Eric C. Gaucher, Philippe Blanc To cite this version: Eric C. Gaucher, Philippe Blanc. Cement/clay interactions - A review: Experiments, natural analogues, and modeling. Waste Management, Elsevier, 2006, 26, pp.776-788. 10.1016/j.wasman.2006.01.027. hal-00664858 HAL Id: hal-00664858 https://hal-brgm.archives-ouvertes.fr/hal-00664858 Submitted on 31 Jan 2012 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. CEMENT/CLAY INTERACTIONS – A REVIEW: EXPERIMENTS, NATURAL ANALOGUES, AND MODELING. Eric C. Gaucher*, Philippe Blanc BRGM, 3 avenue C. Guillemin, BP 6009, 45100 Orleans Cedex, France * Corresponding author. [email protected] Tel: 33.2.38.64.35.73 Fax: 33.2.38.64.30.62 1 Abstract The concept of storing radioactive waste in geological formations calls for large quantities of concrete that will be in contact with the clay material of the engineered barriers as well as with the geological formation. France, Switzerland and Belgium are studying the option of clayey geological formations. The clay and cement media have very contrasted chemistries that will interact and lead to a degradation of both types of material. -
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). -
Apophyllite-(Kf)
December 2013 Mineral of the Month APOPHYLLITE-(KF) Apophyllite-(KF) is a complex mineral with the unusual tendency to “leaf apart” when heated. It is a favorite among collectors because of its extraordinary transparency, bright luster, well- developed crystal habits, and occurrence in composite specimens with various zeolite minerals. OVERVIEW PHYSICAL PROPERTIES Chemistry: KCa4Si8O20(F,OH)·8H20 Basic Hydrous Potassium Calcium Fluorosilicate (Basic Potassium Calcium Silicate Fluoride Hydrate), often containing some sodium and trace amounts of iron and nickel. Class: Silicates Subclass: Phyllosilicates (Sheet Silicates) Group: Apophyllite Crystal System: Tetragonal Crystal Habits: Usually well-formed, cube-like or tabular crystals with rectangular, longitudinally striated prisms, square cross sections, and steep, diamond-shaped, pyramidal termination faces; pseudo-cubic prisms usually have flat terminations with beveled, distinctly triangular corners; also granular, lamellar, and compact. Color: Usually colorless or white; sometimes pale shades of green; occasionally pale shades of yellow, red, blue, or violet. Luster: Vitreous to pearly on crystal faces, pearly on cleavage surfaces with occasional iridescence. Transparency: Transparent to translucent Streak: White Cleavage: Perfect in one direction Fracture: Uneven, brittle. Hardness: 4.5-5.0 Specific Gravity: 2.3-2.4 Luminescence: Often fluoresces pale yellow-green. Refractive Index: 1.535-1.537 Distinctive Features and Tests: Pseudo-cubic crystals with pearly luster on cleavage surfaces; longitudinal striations; and occurrence as a secondary mineral in association with various zeolite minerals. Laboratory analysis is necessary to differentiate apophyllite-(KF) from closely-related apophyllite-(KOH). Can be confused with such zeolite minerals as stilbite-Ca [hydrous calcium sodium potassium aluminum silicate, Ca0.5,K,Na)9(Al9Si27O72)·28H2O], which forms tabular, wheat-sheaf-like, monoclinic crystals. -
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. -
Raman Spectroscopy and Single-Crystal High-Temperature Investigations of Bentorite, Ca6cr2(SO4)3(OH)12·26H2O
minerals Article Raman Spectroscopy and Single-Crystal High-Temperature Investigations of Bentorite, Ca6Cr2(SO4)3(OH)12·26H2O Rafał Juroszek 1,* , Biljana Krüger 2 , Irina Galuskina 1 , Hannes Krüger 2 , Martina Tribus 2 and Christian Kürsten 2 1 Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia, B˛edzi´nska60, 41-205 Sosnowiec, Poland; [email protected] 2 Institute of Mineralogy and Petrography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria; [email protected] (B.K.); [email protected] (H.K.); [email protected] (M.T.); [email protected] (C.K.) * Correspondence: [email protected]; Tel.: +48-516-491-438 Received: 28 November 2019; Accepted: 27 December 2019; Published: 30 December 2019 Abstract: The crystal structure of bentorite, ideally Ca Cr (SO ) (OH) 26H O, a Cr3+ analogue of 6 2 4 3 12· 2 ettringite, is for the first time investigated using X-ray single crystal diffraction. Bentorite crystals of suitable quality were found in the Arad Stone Quarry within the pyrometamorphic rock of the Hatrurim Complex (Mottled Zone). The preliminary semi-quantitative data on the bentorite composition obtained by SEM-EDS show that the average Cr/(Cr + Al) ratio of this sample is >0.8. Bentorite crystallizes in space group P31c, with a = b = 11.1927(5) Å, c =21.7121(10) Å, V = 2355.60(18) Å3, and Z = 2. The crystal structure is refined, including the hydrogen atom positions, to an agreement index R1 = 3.88%. The bentorite crystal chemical formula is Ca (Cr Al ) [(SO ) (CO ) ] (OH) ~25.75H O. -
Carbonation of Borehole Seals: Comparing Evidence from Short-Term Laboratory Experiments and Long-Term Natural Analogues Christopher A
Carbonation of borehole seals: Comparing evidence from short-term laboratory experiments and long-term natural analogues Christopher A. Rochelle* and Antoni E. Milodowski British Geological Survey, Environmental Science Centre, Nicker Hill, Keyworth, Nottingham, NG12 5GG, UK * Corresponding author: [email protected], tel +44 115 9363259, fax +44 115 363200 Abstract It is crucial that the engineered seals of boreholes in the vicinity of a deep storage facility remain effective for considerable timescales if the long-term geological containment of stored CO2 is to be effective. These timescales extend beyond those achievable by laboratory experiments or industrial experience. Study of the carbonation of natural Ca silicate hydrate (CSH) phases provides a useful insight into the alteration processes and evolution of cement phases over long-timescales more comparable with those considered in performance assessments. Samples from two such natural analogues in Northern Ireland have been compared with samples from laboratory experiments on the carbonation of Portland cement. Samples showed similar carbonation reaction processes even though the natural and experimental samples underwent carbonation under very different conditions and timescales. These included conversion of the CSH phases to CaCO3 and SiO2, and the formation of a well-defined reaction front. In laboratory experiments the reaction front is associated with localised Ca migration, localised matrix porosity increase, and localised shrinkage of the cement matrix with concomitant cracking. Behind the reaction front is a zone of CaCO3 precipitation that partly seals porosity. A broader and more porous/permeable reaction zone was created in the laboratory experiments compared to the natural samples, and it is possible that short-term experiments might not fully replicate slower, longer-term processes. -
BREDIGITE, LARNITE and ? DICALCIUM SILICATES from MARBLE CANYON Tnolras E
THE AMERICAN MINERALOGIST, VOL. 51, NOVEMBER_DECEMBER, 1966 BREDIGITE, LARNITE AND ? DICALCIUM SILICATES FROM MARBLE CANYON Tnolras E. Bnrocn, DepartmentoJ Geosciences,Texas T echnological College, Lubbo ck, T enas.r Alstnact The a' (bredigite), p (larnite) and 7 (unnamed) forms of dicalcium silicate (CarSiOr) occur together in the contact zone around a syenite-monzonite intrusion in Marble Canyon. Bredigite, larnite and 7 have consistant crystallographic orientations when they occur together. These relationships reflect the crystallographic direction in which the reorganiza- tion occurs when transformation from one form to another takes place. INrnooucrroN Two polymorphic forms of dicalcium silicate (CazSiOD have been de- scribed as naturally occurring minerals by Tilley (1929) and Tilley and Vincent (1948).The mineralswere found in a contact zonein Larne, Ire- Iand and given the names larnite and bredigite. Until 1964,no natural occurrencesof theseminerals had been reported from any locality in the United States. In 1963, three polymorphic forms of CazSiOawere found in the contact zone around a syenite-monzonite intrusion in 1\4arbleCavon. LocarroN AND SETTTNG Marble Canyon is in the east rim of the Diablo Plateau in Culberson County, Trans-PecosTexas, 30 miles north of the town of Van Horn and 2 miles west of State Highway 54. The canyon is about a mile long and terminates upstream in an elongate amphitheater roughly a mile and a half Iong and half a mile wide. In the center of this elongate amphitheater is an elliptical outcrop of five different types of igneous rock that are arranged in a concentric pattern. From the center out they are: (1) a coarse-grained syenite; (2) a coarse-grained green monzonitel (3) a medium-grained gray monzonite; (4) a discontinuous narrow border of olivine gabbro; and (5) small rhyolite dikes which cut the other rock types. -
Grossite and Hibonite Bearing Refractory Inclusions in the CO3.1 Chondrite Miller Range 090019. D. K. Ross1 and J. I. Simon2, 1U
49th Lunar and Planetary Science Conference 2018 (LPI Contrib. No. 2083) 2559.pdf Grossite and Hibonite Bearing Refractory Inclusions in the CO3.1 Chondrite Miller Range 090019. D. K. Ross1 and J. I. Simon2, 1University of Texas El Paso/Jacobs Technology/NASA-JSC-ARES (2224 Bay Area Blvd. Houston TX 77058, USA ([email protected]), 2NASA-Johnson Space Center-ARES ([email protected]). Introduction: We have characterized 142 refract- finer grained particles with substantial porosity. Ongo- ory objects by EDS hyperspectral X-ray mapping in the ing reaction with nebular gases produces down-temper- CO3.1 chondrite MIL 090019-13. These include 127 ature phases partially replacing earlier formed phases Ca-Al rich inclusions (CAIs), 14 amoeboidal olivine ag- and infilling porosity, leading to densified objects. gregates (AOAs) and one Al-rich chondrule. These data Most CAIs are not fully equilibrated, but exhibit miner- are being used to reveal the mineralogy, texture and alogy reflecting a considerable range of temperature, bulk composition of these inclusions, and to identify ob- with relict phases. Hibonite is typically intergrown with, jects that represent endmembers within cogenetic popu- and partially replaced by spinel, violating the predicted lations of primitive inclusions, which will be further in- crystallization order from thermodynamic calcula- vestigated by future isotopic studies. Previous work re- tions[3], in which melilite should precede spinel crystal- lated to these refractory inclusions in this chondrite also lization. appear in [1] and [2]. Twenty six inclusions are hibonite-bearing, 18 are grossite-bearing and one inclusion is corundum-rich. In seven of these inclusions, grossite and hibonite coexist. -
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.