Talc and Asbestos
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Fire Retardancy of Polypropylene/Kaolinite Composites Marcos Batistella, Belkacem Otazaghine, Rodolphe Sonnier, Carlos Petter, José-Marie Lopez-Cuesta
Fire retardancy of polypropylene/kaolinite composites Marcos Batistella, Belkacem Otazaghine, Rodolphe Sonnier, Carlos Petter, José-Marie Lopez-Cuesta To cite this version: Marcos Batistella, Belkacem Otazaghine, Rodolphe Sonnier, Carlos Petter, José-Marie Lopez-Cuesta. Fire retardancy of polypropylene/kaolinite composites. Polymer Degradation and Stability, Elsevier, 2016, 129, pp.260-267. 10.1016/j.polymdegradstab.2016.05.003. hal-02906432 HAL Id: hal-02906432 https://hal.archives-ouvertes.fr/hal-02906432 Submitted on 26 May 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. Fire retardancy of polypropylene/kaolinite composites * Marcos Batistella a, c, , Belkacem Otazaghine b, Rodolphe Sonnier b, Carlos Petter c, Jose-Marie Lopez-Cuesta b a Federal University of Santa Catarina, R. Eng. Agronomico^ Andrei Cristian Ferreira, s/n e Trindade, Florianopolis, SC, CEP 88040-900, Brazil b Ecole des Mines d’Ales, Centre des Materiaux (C2MA) e Pole^ Materiaux Polymeres Avances, 6 Avenue de Clavieres, 30319, Ales Cedex, France c Federal University of Rio Grande do Sul, Av. Bento Gonçalves, 9500, Porto Alegre, CEP 91501-970, Brazil abstract In this study the influence of surface modification of kaolinite with trisilanolisooctyl Polyhedral Oligo- SilSesquioxane (POSS) in polypropylene composites was evaluated in terms of thermal stability and fire retardancy and compared with talc. -
Wollastonite–A Versatile Industrial Mineral
Industrial Minerals of the United States Wollastonite–A Versatile Industrial Mineral What is Wollastonite? Wollastonite is a chemically simple mineral named in honor of English mineralogist and chemist Sir W.H. Wollaston (1766–1828). It is composed of calcium (Ca) and silicon and oxygen (SiO2, silica) with the chemical formula CaSiO3. Although much wollastonite is relatively pure CaSiO3, it can contain some iron, magnesium, (Above and right) Hand specimens of manganese, aluminum, potassium, wollastonite showing acicular crystal clusters. sodium, or strontium substituting for calcium in the mineral structure. Pure wollastonite is bright white; the geologic conditions during formation What Makes Wollastonite and host rock composition. The type and amount of impurities can Useful? produce gray, cream, brown, pale- Lewis Deposit, mined by NYCO green, or red colors. Minerals, Inc., in the Adirondack Wollastonite has several physical Mountains in Essex County, was properties that make it useful as an formed by the recrystallization of industrial mineral: Geology of U.S. Precambrian carbonate rocks inter- Wollastonite Deposits layered with high-grade metamor- ∑ Wollastonite is largely inert, phic rocks. Nearby reserves are although it will dissolve in concen- Wollastonite is formed by two contained in the Oak Hill and trated hydrochloric acid. It will not processes. The first occurs when Deerhead deposits. The ore bodies react with other components of silica and limestone are raised to a consist of the minerals wollastonite, manufactured products either during temperature of 400°–450°C, either garnet, and diopside with as much as or after the manufacturing process. because of deep burial (regional 60 percent of the bodies being ∑ During crushing, wollastonite metamorphism) or by being baked wollastonite. -
Talc and Pyrophyllite
TALC AND PYROPHYLLITE By Robert L. Virta Domestic survey data and tables were prepared by Raymond I. Eldridge III, statistical assistant, and the world production table was prepared by Glenn J. Wallace, international data coordinator. The mineral talc is a hydrous magnesium silicate. A massive recommended against listing asbestiform talc and talcose rock is called steatite, and an impure massive variety is nonasbestiform talc in its 10th report on carcinogens (U.S. known as soapstone. Talc is used commercially because of its Department of Health and Human Services, Public Health fragrance retention, luster, purity, softness, and whiteness. Service, 2001; National Paint and Coatings Association, Other commercially important properties of talc are its chemical January 2001, NTP skips over talc, accessed January 8, 2001, at inertness, high dielectric strength, high thermal conductivity, URL http://www.paint.org/ind_issue/current/jan/issue05.htm). low electrical conductivity, and oil and grease adsorption. In 2000, the U.S. Department of Defense authorized the Major markets for talc are ceramics, paint, paper, and plastics. disposal of 907 metric tons (t) of block and lump talc, which is Pyrophyllite is a hydrous aluminum silicate with a structure the entire uncommitted inventory in that category, from the similar to talc. Such properties as chemical inertness, high National Defense Stockpile. dielectric strength, high melting point, and low electrical conductivity make it useful for ceramic and refractory Production applications. Talc.—In 2000, seven companies operating nine mines in five Legislation and Government Programs States produced soapstone, steatite, and talc. All were open pit mines. The producers were, in decreasing order of production, The National Toxicology Program (NTP) of the U.S. -
Wollastonite
Strictly private and confidential Wollastonite A versatile mineral which can support sustainable farming 07 June 2019 Business Risk Analysis – Visionary Execution Strictly private and confidential 2 Disclaimer & Forward-Looking Statements Cautionary Statement on Forward-Looking Information & Statements: This presentation contains certain forward-looking information and statements which may not be based on fact, including without limitation, statements regarding the Company’s expectations in respect of its future financial position, business strategy, future exploration and production, mineral resource potential, exploration drilling, permitting, access to capital, events or developments that the Company expects to take place in the future. All statements, other than statements of historical facts, are forward-looking information and statements. The words “believe”, “expect”, “anticipate”, “contemplate”, “target”, “plan”, “intends”, “continue”, “budget”, “estimate”, “may”, “will”, “aim”, “goal” and similar expressions identify forward-looking information and statements. In addition to the forward-looking information and statements noted above, this presentation includes those that relate to: the expected results of exploration activities; the estimation of mineral resources; the ability to identify new mineral resources and convert mineral resources into mineral reserves; ability to raise additional capital and complete future financings; capital expenditures and costs, including forecasted costs; the ability of the Company to comply with -
The Conversion of Wollastonite to Caco3 Considering Its Use for CCS Application As Cementitious Material
applied sciences Article The Conversion of Wollastonite to CaCO3 Considering Its Use for CCS Application as Cementitious Material Kristoff Svensson *, Andreas Neumann, Flora Feitosa Menezes, Christof Lempp and Herbert Pöllmann Institute for Geosciences and Geography, Martin-Luther-University of Halle-Wittenberg, Von-Seckendorff-Platz 3, 06120 Halle (Saale), Germany; [email protected] (A.N.); fl[email protected] (F.F.M.); [email protected] (C.L.); [email protected] (H.P.) * Correspondence: [email protected]; Tel.: +49-345-55-26138 Received: 21 December 2017; Accepted: 8 February 2018; Published: 20 February 2018 Featured Application: Building materials and CCS. Abstract: The reaction of wollastonite (CaSiO3) with CO2 in the presence of aqueous solutions (H2O) and varied temperature conditions (296 K, 323 K, and 333 K) was investigated. The educts (CaSiO3) and the products (CaCO3 and SiO2) were analyzed by scanning electron microscopy (SEM), powder X-ray diffraction (PXRD), and differential scanning calorimetry with thermogravimetry coupled with a mass spectrometer and infrared spectrometer (DSC-TG/MS/IR). The reaction rate increased significantly at higher temperatures and seemed less dependent on applied pressure. It could be shown that under the defined conditions wollastonite can be applied as a cementitious material for sealing wells considering CCS applications, because after 24 h the degree of conversion from CaSiO3 to CaCO3 at 333 K was very high (>90%). As anticipated, the most likely application of wollastonite as a cementitious material in CCS would be for sealing the well after injection of CO2 in the reservoir. -
Swelling Capacity of Mixed Talc-Like/Stevensite Layers in White/Green Clay
This is a preprint, the final version is subject to change, of the American Mineralogist (MSA) Cite as Authors (Year) Title. American Mineralogist, in press. DOI: https://doi.org/10.2138/am-2020-6984 1 1 Plagcheck: no concerns 2 Tables?: 3 small 3 Word Count: ~9,100 4 Prod notes: make sure tables in file before RE 5 6 7 8 Swelling capacity of mixed talc-like/stevensite layers in white/green clay 9 infillings (‘deweylite’/‘garnierite’) from serpentine veins of faulted 10 peridotites, New Caledonia 11 REVISION 2 12 Lionel FONTENEAU 1, Laurent CANER 2*, Sabine PETIT 2, Farid JUILLOT 3, Florian 13 PLOQUIN 3, Emmanuel FRITSCH 3 14 15 1Corescan Pty Ltd, 1/127 Grandstand Road, 6104 Ascot, WA, Australia 16 2 Université de Poitiers, Institut de Chimie des Milieux et Matériaux de Poitiers, IC2MP UMR 17 7285 CNRS, 5 rue Albert Turpain, TSA51106, 86073 Poitiers cedex 9, France 18 * Corresponding author, e-mail: [email protected] 19 3 Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie (IMPMC), Sorbonne 20 Universités – Université Pierre et Marie Curie UPMC, UMR CNRS 7590, Museum National 21 d’Histoire Naturelle, UMR IRD 206, 101 Promenade Roger Laroque, Anse Vata, 98848, 22 Nouméa, New Caledonia 23 24 25 Abstract: White (Mg-rich) and green (Ni-rich) clay infillings (‘deweylite’/‘garnierite’) found 26 in serpentine veins of faulted peridotite formations from New Caledonia consist of an intimate 27 mixture of fine-grained and poorly ordered 1:1 and 2:1 layer silicates, commonly referred to 28 as non-expandable serpentine-like (SL) and talc-like (TL) minerals. -
Commodities, Part 5 Strontium, Sodium Sulfate, Trona (Soda Ash), Talc, Lithium, Summary Comments Safety Reminders
ME571/GEO571 Geology of Industrial Minerals Spring 2018 Commodities, Part 5 strontium, sodium sulfate, trona (soda ash), talc, lithium, summary comments Safety Reminders Commodity presentations—send me your powerpoints April 28 AIPG meeting and Field trip in afternoon (perlite mine or carbonatites) Research Projects presentation April 30 Finals, written Project due May 4 No class May 7 Strontium Strontium—introduction • Sr • 15th abundant element • does not occur naturally as an element, in compounds • No production in the United States since 1959 • celestite or celestine SrSO4 (same structure as barite) 56.4% Sr • strontianite SrCO3, 70.1% Sr Celesitite http://www.zeuter.com/~tburden Strontianite http://www.zeuter.com/~tburden Strontium and strontianite are named after Stronian, a village in Scotland near which the mineral was discovered in 1790 by Adair Crawford and William Cruickshank A critical mineral Strontium—uses • faceplate glass of color television picture tubes, 77% • ferrite ceramic magnets, 8% • pyrotechnics and signals, 9% – fireworks (red flame) – flares • other applications, 6% – refining zinc – optical materials Strontium—production USGS Mineral Yearbooks metric tons Strontium—geology • association with rocks deposited by the evaporation of sea water (evaporites) • igneous rocks • Brines • Barite and calcite must be removed— costly Sodium sulfate Sodium sulfate—introduction • disodium sulfate (Na2SO4), • inorganic chemical • Thenardite Na2SO4 • Hanksite Na22K(SO4)9(CO3)2Cl • Glauberite Na2Ca(SO4)2 Sodium sulfate—uses -
The Cordierite Formation in Mechanically Activated Talc-Kaoline-Alumina-Basalt-Quartz Ceramic System D
Vol. 127 (2015) ACTA PHYSICA POLONICA A No. 4 Proceedings of the 4th International Congress APMAS2014, April 24-27, 2014, Fethiye, Turkey The Cordierite Formation in Mechanically Activated Talc-Kaoline-Alumina-Basalt-Quartz Ceramic System D. Kirsever*, N. Karakus, N. Toplan, H.O. Toplan Sakarya University, Metalurgy and Materials Engineering, 54187 Sakarya, Turkey The powder mixtures of Talc-Kaolinite-Alumina-Basalt-Quartz were mechanically activated in a planetary ball mill for 1 hour. The structural alterations and thermal behaviour of the powder mixture were examined by X-ray diraction (XRD), scanning electron microscopy (SEM) and thermal analysis (TG-DTA). The results showed that the mechanical activation led to amorphisation and decreased the temperature of cordierite formation. DOI: 10.12693/APhysPolA.127.1042 PACS: 81.05.Je 1. Introduction a high-energy ball mill. In this process, a small quantity of the blended elemental powder mixture is loaded into a Cordierite, which chemical composition is container, along with the grinding media, and the whole 2MgO 2Al O 5SiO , is one of the phases of the · 2 3· 2 mass is agitated at a high speed for a predetermined ternary MgOSiO Al O system, along with mullite, 2 2 3 length of time [5]. The mechano-activation treatment cristobalite, tridymite, enstatite, forsterite, sapphirine, might promote: the amorphization of treated material, etc. Cordierite-based materials have a great importance noticeable change of the microstructure, size and shape in modern technology due to their excellent properties, of particles, etc. Furthermore, ultra-ne grinding kinetic such as low thermal expansion coecient, high refrac- investigation indicates the mechano-chemical reduction toriness, low dielectric constant, high thermal shock of the original particles of talc/mica, which appears to resistance and good mechanical properties [1]. -
Experimental Study of Mineral Carbonation of Wollastonite For
DEGREE PROJECT IN TECHNOLOGY, FIRST CYCLE, 15 CREDITS STOCKHOLM, SWEDEN 2019 Experimental Study of Mineral Carbonation of Wollastonite for Increased CO2 Uptake DINA BABIKER MATILDA AHLSTRAND KTH ROYAL INSTITUTE OF TECHNOLOGY SCHOOL OF ARCHITECTURE AND THE BUILT ENVIRONMENT TRITA TRITA-ABE-MBT-19533 www.kth.se Abstract The cement and concrete industry stand for approximately 8% of the global CO2 emissions. The demand of concrete and cement is expected to increase rapidly with the growing world population and increased urbanization. This makes it of the utmost importance for the industry to try to mitigate its emissions. One way to reduce the industry’s environmental impact is by mineral carbonation curing through which CO2 can be sequestered in the concrete. This investigation studied the CO2 uptake of wollastonite (CaSiO3) which can be used for mineral carbonation. The CO2 uptake of different brands of wollastonite powders for different temperatures, pressures and water to solid ratios were tested through carbonation, and the samples were then analyzed through XRD, SEM and particle size analysis. The results showed large differences in CO2 uptake between the brands of wollastonite powders. They also indicate that lower temperatures lead to higher CO2 uptake but also possibly slow down the reaction rate and that higher CO2 pressures seem to increase CO2 uptake though the effect is small. There was significant variation of the effects of the water to solid ratios on CO2 uptake between the tested brands. The morphology of the powders also seemed to be of little relevance as an amorphous and crystalline powder were the two best performing powders, similarly particle size is not indicated by the result to have a large effect on CO2 uptake, though further studies are required to fully determine the effect of the morphology and particle size. -
Talc Processing
11.26 Talc Processing 11.26.1 Process Description1-9 . Talc, which is a soft, hydrous magnesium silicate (3Mg0 4Si02 H20), is used in a wide range of industries including the manufacture of ceramics, paints, paper, and asphalt roofing. The end-uses for talc are determined by variables such as chemical and mineralogical composition, particle size and shape, specific gravity, hardness, and color. There is no Source Classification Code (SCC) for the source category. Over 95 percent of the talc ore produced in the United States comes from open-pit mines. Mining operations usually consist of conventional drilling and blasting methods. Figure 11.26-1 is a process flow diagram for a typical domestic talc plant. Talc ore generally is hauled to the plant by truck from a nearby mine. The ore is crushed, typically in a jaw crusher, and screened. The coarse (oversize) material then is returned to the crusher. Rotary dryers may be used to dry the material. Secondary grinding is achieved with pebble mills or roller mills, producing a product that is 44 to 149 micrometers ( m) (325 to 100 mesh) in size. Some roller mills are designed to use heated air to dry the material as it is being ground. Hammer mills or steam- or compressed air- powered jet mills may be used to produce additional final products. Air classifiers (separators), generally in closed circuit with the mills, separate the material into coarse, coarse-plus-fine, and fine fractions. The coarse and coarse-plus-fine fractions then are stored as products. The fines may be concentrated using a shaking table (tabling process) to separate product containing small quantities of nickel, iron, cobalt, or other minerals and then may undergo a one-step flotation process. -
What We Know About Subduction Zones from the Metamorphic Rock Record
What we know about subduction zones from the metamorphic rock record Sarah Penniston-Dorland University of Maryland Subduction zones are complex We can learn a lot about processes occurring within active subduction zones by analysis of metamorphic rocks exhumed from ancient subduction zones Accreonary prism • Rocks are exhumed from a wide range of different parts of subduction zones. • Exhumed rocks from fossil subduction zones tell us about materials, conditions and processes within subduction zones • They provide complementary information to observations from active subduction systems Tatsumi, 2005 The subduction interface is more complex than we usually draw Mélange (Bebout, and Penniston-Dorland, 2015) Information from exhumed metamorphic rocks 1. Thermal structure The minerals in exhumed rocks of the subducted slab provide information about the thermal structure of subduction zones. 2. Fluids Metamorphism generates fluids. Fossil subduction zones preserve records of fluid-related processes. 3. Rheology and deformation Rocks from fossil subduction zones record deformation histories and provide information about the nature of the interface and the physical properties of rocks at the interface. 4. Geochemical cycling Metamorphism of the subducting slab plays a key role in the cycling of various elements through subduction zones. Thermal structure Equilibrium Thermodynamics provides the basis for estimating P-T conditions using mineral assemblages and compositions Systems act to minimize Gibbs Free Energy (chemical potential energy) Metamorphic facies and tectonic environment SubduconSubducon zone metamorphism zone metamorphism Regional metamorphism during collision Mid-ocean ridge metamorphism Contact metamorphism around plutons Determining P-T conditions from metamorphic rocks Assumption of chemical equilibrium Classic thermobarometry Based on equilibrium reactions for minerals in rocks, uses the compositions of those minerals and their thermodynamic properties e.g. -
Wollastonite Casio3 C 2001 Mineral Data Publishing, Version 1.2 ° Crystal Data: Monoclinic Or Triclinic
Wollastonite CaSiO3 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Monoclinic or triclinic. Point Group: 2=m or 1: Crystals tabular 100 k f g or 001 , or short to long prismatic, to 20 cm. Commonly cleavable, parallel ¯brous, or compact, f g massive. Twinning: Common; twin axis [010], composition plane 100 . f g Physical Properties: Cleavage: 100 perfect; 001 and 102 , good; (100) (001) = f g f g f g ^ 84.5±. Fracture: Uneven. Tenacity: Brittle. Hardness = 4.5{5. D(meas.) = 2.86{3.09 D(calc.) = 2.90 May exhibit yellow catholuminescence. Optical Properties: Transparent to translucent. Color: White, colorless, brown, red, yellow, pale green; colorless in thin section. Streak: White. Luster: Vitreous, pearly on cleavage. Optical Class: Biaxial ({). Orientation: X c = 30 {44 ; Y b = 0 {5 ; Z a = ^ ± ± ^ ± ± ^ 37±{50±. Dispersion: r > v; weak. ® = 1.616{1.640 ¯ = 1.628{1.650 ° = 1.631{1.653 2V(meas.) = 36±{60± Cell Data: Space Group: P 21=a: a = 15.409(3) b = 7.322(1) c = 7.063(1) ¯ = 95:30(2)± Z = 12, or Space Group: P 1: a = 7.94 b = 7.32 c = 7.07 ® = 90±20 ¯ = 95±220 ° = 103±260 Z = 6 X-ray Powder Pattern: Sampo mine, Okayama Prefecture, Japan (1A). 3.314 (100), 3.83 (84), 3.51 (77), 3.086 (58), 2.302 (52), 2.556 (44), 1.759 (35) Chemistry: (1) (2) (1) (2) SiO2 50.82 50.24 CaO 48.16 35.93 Al2O3 0.46 Na2O 0.12 Fe2O3 trace K2O 0.07 + FeO 0.18 5.54 H2O 0.08 0.00 MnO 0.03 8.16 S 0.14 MgO 0.22 0.07 Total 99.68 100.54 (1) Remonmaki, Finland; corresponds to (Ca1:01Mg0:01)§=1:02Si0:99O3: (2) North mine, Broken Hill, New South Wales, Australia; corresponds to (Ca0:76Mn0:14Fe0:09)§=0:99(Si1:00Al0:01)§=1:01O3: Polymorphism & Series: 1A, 2M, 3A, 4A, 5A, 7A polytypes.