Chrysotile Asbestos
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
NMAM 9000: Asbestos, Chrysotile By
ASBESTOS, CHRYSOTILE by XRD 9000 MW: ~283 CAS: 12001-29-5 RTECS: CI6478500 METHOD: 9000, Issue 3 EVALUATION: FULL Issue 1: 15 May 1989 Issue 3: 20 October 2015 EPA Standard (Bulk): 1% by weight PROPERTIES: Solid, fibrous mineral; conversion to forsterite at 580 °C; attacked by acids; loses water above 300 °C SYNONYMS: Chrysotile SAMPLING MEASUREMENT BULK TECHNIQUE: X-RAY POWDER DIFFRACTION SAMPLE: 1 g to 10 g ANALYTE: Chrysotile SHIPMENT: Seal securely to prevent escape of asbestos PREPARATION: Grind under liquid nitrogen; wet-sieve SAMPLE through 10 µm sieve STABILITY: Indefinitely DEPOSIT: 5 mg dust on 0.45 µm silver membrane BLANKS: None required filter ACCURACY XRD: Copper target X-ray tube; optimize for intensity; 1° slit; integrated intensity with RANGE STUDIED: 1% to 100% in talc [1] background subtraction BIAS: Negligible if standards and samples are CALIBRATION: Suspensions of asbestos in 2-propanol matched in particle size [1] RANGE: 1% to 100% asbestos OVERALL PRECISION ( ): Unknown; depends on matrix and ESTIMATED LOD: 0.2% asbestos in talc and calcite; 0.4% concentration asbestos in heavy X-ray absorbers such as ferric oxide ACCURACY: ±14% to ±25% PRECISION ( ): 0.07 (5% to 100% asbestos); 0.10 (@ 3% asbestos); 0.125 (@ 1% asbestos) APPLICABILITY: Analysis of percent chrysotile asbestos in bulk samples. INTERFERENCES: Antigorite (massive serpentine), chlorite, kaolinite, bementite, and brushite interfere. X-ray fluorescence and absorption is a problem with some elements; fluorescence can be circumvented with a diffracted beam monochromator, and absorption is corrected for in this method. OTHER METHODS: This is NIOSH method P&CAM 309 [2] applied to bulk samples only, since the sensitivity is not adequate for personal air samples. -
State County Historic Site Name As Reported Development Latitude
asbestos_sites.xls. Summary of information of reported natural occurrences of asbestos found in geologic references examined by the authors. Dataset is part of: Van Gosen, B.S., and Clinkenbeard, J.P., 2011, Reported historic asbestos mines, historic asbestos prospects, and other natural occurrences of asbestos in California: U.S. Geological Survey Open-File Report 2011-1188, available at http://pubs.usgs.gov/of/2011/1188/. Data fields: State, ―CA‖ indicates that the site occurs in California. County, Name of the county in which the site is located. Historic site name as reported, The name of the former asbestos mine, former asbestos prospect, or reported occurrence, matching the nomenclature used in the source literature. Development, This field indicates whether the asbestos site is a former asbestos mine, former prospect, or an occurrence. "Past producer" indicates that the deposit was mined and produced asbestos ore for commercial uses sometime in the past. "Past prospect" indicates that the asbestos deposit was once prospected (evaluated) for possible commercial use, typically by trenching and (or) drilling, but the deposit was not further developed. "Occurrence" indicates that asbestos was reported at this site. The occurrence category includes (1) sites where asbestos-bearing rock is described in a geologic map or report and (2) asbestos noted as an accessory mineral or vein deposit within another type of mineral deposit. Latitude, The latitude of the site's location in decimal degrees, measured using the North American Datum of -
Iron.Rich Amesite from the Lake Asbestos Mine. Black
Canodian Mineralogist Yol.22, pp. 43742 (1984) IRON.RICHAMESITE FROM THE LAKE ASBESTOS MINE. BLACKLAKE. OUEBEC MEHMET YEYZT TANER,* AND ROGER LAURENT DAporternentde Gdologie,Universitd Loval, Qudbec,Qudbec GIK 7P4 ABSTRACT o 90.02(1l)', P W.42(12)',1 89.96(8)'.A notreconnais- sance,c'est la premibrefois qu'on ddcritune am6site riche Iron-rich amesite is found in a metasomatically altered enfer. Elles'ct form€ependant l'altdration hydrothermale granite sheet20 to 40 cm thick emplacedin serpentinite of du granitedans la serpentinite,dans les m€mes conditions the Thetford Mi[es ophiolite complex at the Lake Asbestos debasses pression et temperaturequi ont prdsid6d la for- mine (z16o01'N,11"22' W) ntheQuebec Appalachians.The mation de la rodingite dansle granite et de I'amiante- amesiteis associatedsdth 4lodingife 6semblage(grossu- chrysotiledans la serpentinite. lar + calcite t diopside t clinozoisite) that has replaced the primary minerals of the granite. The Quebec amesite Mots-clds:am6site, rodingite, granite, complexeophio- occurs as subhedral grains 2@ to 6@ pm.in diameter that litique, Thetford Mines, Qu6bec. have a tabular habit. It is optically positive with a small 2V, a 1.612,1 1.630,(t -'o = 0.018).Its structuralfor- INTRoDUc"iloN mula, calculated from electron-microprobe data, is: (Mg1.1Fe6.eA1s.e)(Alo.esil.df Os(OH)r.2. X-ray powder- Amesite is a raxehydrated aluminosilicate of mag- diffraction yield data dvalues that are systematicallygreater nesium in which some ferrous iron usually is found than those of amesitefrom Chester, Massachusetts,prob- replacingmapesium. The extent of this replacement ably becauseof the partial replacement of Mg by Fe. -
Chrysotile Asbestos As a Cause of Mesothelioma: Application of the Hill Causation Model
Commentary Chrysotile Asbestos as a Cause of Mesothelioma: Application of the Hill Causation Model RICHARD A. LEMEN, PHD Chrysotile comprises over 95% of the asbestos used this method, researchers are asked to evaluate nine today. Some have contended that the majority of areas of consideration: strength of association, tempo- asbestos-related diseases have resulted from exposures rality, biologic gradient, consistency, specificity, bio- to the amphiboles. In fact, chrysotile is being touted as logic plausibility, coherence, experimental evidence, the form of asbestos which can be used safely. Causa- and analogy. None of these considerations, in and of tion is a controversial issue for the epidemiologist. How itself, is determinative for establishing a causal rela- much proof is needed before causation can be estab- tionship. As Hill himself noted, “[n]one of my nine lished? This paper examines one proposed model for establishing causation as presented by Sir Austin Brad- view points can bring indisputable evidence for or ford Hill in 1965. Many policymakers have relied upon against the cause and effect hypothesis, and none can this model in forming public health policy as well as be required as a sine qua non.” In the same vein, it is deciding litigation issues. Chrysotile asbestos meets not necessary for all nine considerations to be met Hill’s nine proposed criteria, establishing chrysotile before causation is established. Instead, Hill empha- asbestos as a cause of mesothelioma. Key words: sized that the responsibility for making causal judg- asbestos; chrysotile; amphiboles; causation; mesothe- ments rested with a scientific evaluation of the totality lioma; Hill model. of the data. -
Balangeroite, a New Fibrous Silicate Related to Gageite from Balangero
American Mineralogist, Volume 6E, pages 214-219, I9E3 Balangeroite,a new fibrous silicate related to gageitefrom Balangero,Italy Ronpnro CoupecNoxr Dipartimento di Scienzqdella Terra Universitd della Calabria Castiglione scalo, 87030Cosenza, Italy GtoveNNr Fr,nnents Istituto di Mineralogia, Cristallografia e Geochimica "G. Spezia", Universitddi Torino via S. Massimo 22. 10123Torino. Itqlv eNo LRune Flone Istituto di Petrografia, Universitd di Torino and Centro di Studio per i Problemi dell'Orogeno delle Alpi Occidentalidel C.N.R., via S. Massimo22, 10123Torino, Italy Abstract Balangeroiteoccurs as brown asbestiformfibers in a paragenesiswith long-fiber chrysotile,magnetite, and native Fe-Ni in the Balangeroserpentinite (Lanzo Valley, Piedmont,Italy). It is orthorhombicwith a 13.85(4),b 13.58(3), and c 9.65(3)A;a sub-cell with c' : c/3 is stronglyevident. The X-ray powderpattern demonstrates an isostructural relationshipof the newmineral with gageite;the strongestreflections are:9.59(40)(ll0), 6.77(80)(020),3.378(45)(410), 3.278(40Xr40), 2.714(100)(050,510), 2.674(75)(150,223), and 2.516(40)(250).The fibers are elongated parallel to [fi)l], showone or more{/r/<0} cleavages, and are usuallyintergrown with chrysotile.The refractiveindexes are aboutthe same, 1.680(5),both parallel and perpendicular to [fi)l]; coloris darkbrown and yellow brown in thesetwo directions,respectively. Chemical analysis gives a unit-cellcontent of (Mgzs.zoFez2.tqFe].t3Mn?:5Ab.rzCao.ozCro.orTio.or)>rae3Si15.3sO53oe(OH)ls.sz, andthe presenceof a sub-cellwith c' = c/3 suggeststhe formula (Mg,Fe2*,Fe3*,Mn2*,!;o2sir5(O,OH)eo with contentsdivisible by 3; a similarformula is probablyalso correct for the Mn-analogue, gageite.DTA, TGA, and high-temperatureX-ray powder analysesshow structural breakdownwith a total weightloss of 9.4Voand the appearanceof olivineat 8fi)'C. -
Metamorphic Veins from the Serpentinites of the Piemonte Zone, Western Alps, Italy: a Review
Per. Mineral. (2007), 76, 127-1 doi:10.2451/2007PM0021 SPECIAL ISSUE: In honour of Ezio Callegari on his retirement http://go.to/permin An International Journal of l PERIODICO di MINERALOGIA MINERALOGY, CRYSTALLOGRAPHY, GEOCHEMISTRY, established in 1930 ORE DEPOSITS, PETROLOGY, VOLCANOLOGY and applied topics on Environment, Archaeometry and Cultural Heritage Metamorphic veins from the serpentinites of the Piemonte Zone, western Alps, Italy: a review CHIARA GROPPO 1, 2* and ROBERTO COMPAGNONI 1, 2 1 Dipartimento di Scienze Mineralogiche e Petrologiche, Università degli Studi di Torino,Via Valperga Caluso, 35, 10125 Torino, Italy 2 Centro interdipartimentale “G. Scansetti” per lo studio sull’ Asbesto e altri particolati tossici, Università degli Studi di Torino, Italy ABSTRACT. — Petrographic and micro-Raman RIASSUNTO. — Lo studio petrografico in sezione analysis of metamorphic veins occurring in sottile ed in spettroscopia micro-Raman delle vene serpentinites from the Piemonte Zone (western Alps) metamorfiche presenti nelle serpentiniti della Zona has allowed us to recognise seven different vein Piemontese (Alpi Occidentali) ha permesso di generations, developed at different P-T-X conditions. riconoscerne sette differenti generazioni, sviluppatesi The first vein generation (balangeroite + magnetite a diverse condizioni P-T-X. La prima generazione + FeNi-alloys) formed during the Alpine prograde (balangeroite + magnetite + leghe FeNi) si è formata evolution, whereas the second vein generation durante l’evoluzione prograda delle serpentiniti, -
List of Abbreviations
List of Abbreviations Ab albite Cbz chabazite Fa fayalite Acm acmite Cc chalcocite Fac ferroactinolite Act actinolite Ccl chrysocolla Fcp ferrocarpholite Adr andradite Ccn cancrinite Fed ferroedenite Agt aegirine-augite Ccp chalcopyrite Flt fluorite Ak akermanite Cel celadonite Fo forsterite Alm almandine Cen clinoenstatite Fpa ferropargasite Aln allanite Cfs clinoferrosilite Fs ferrosilite ( ortho) Als aluminosilicate Chl chlorite Fst fassite Am amphibole Chn chondrodite Fts ferrotscher- An anorthite Chr chromite makite And andalusite Chu clinohumite Gbs gibbsite Anh anhydrite Cld chloritoid Ged gedrite Ank ankerite Cls celestite Gh gehlenite Anl analcite Cp carpholite Gln glaucophane Ann annite Cpx Ca clinopyroxene Glt glauconite Ant anatase Crd cordierite Gn galena Ap apatite ern carnegieite Gp gypsum Apo apophyllite Crn corundum Gr graphite Apy arsenopyrite Crs cristroballite Grs grossular Arf arfvedsonite Cs coesite Grt garnet Arg aragonite Cst cassiterite Gru grunerite Atg antigorite Ctl chrysotile Gt goethite Ath anthophyllite Cum cummingtonite Hbl hornblende Aug augite Cv covellite He hercynite Ax axinite Czo clinozoisite Hd hedenbergite Bhm boehmite Dg diginite Hem hematite Bn bornite Di diopside Hl halite Brc brucite Dia diamond Hs hastingsite Brk brookite Dol dolomite Hu humite Brl beryl Drv dravite Hul heulandite Brt barite Dsp diaspore Hyn haiiyne Bst bustamite Eck eckermannite Ill illite Bt biotite Ed edenite Ilm ilmenite Cal calcite Elb elbaite Jd jadeite Cam Ca clinoamphi- En enstatite ( ortho) Jh johannsenite bole Ep epidote -
Nepouite Isomorphous Series
N¶epouite Ni3Si2O5(OH)4 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Orthorhombic, probable. Point Group: n.d. As crude pseudohexagonal vermiform crystals, to 1 cm; massive. Physical Properties: Hardness = 2.5 D(meas.) = 3.24 D(calc.) = [3.07{3.40] Optical Properties: Semitransparent. Color: Intense dark green to dull green. Optical Class: Biaxial ({). Pleochroism: Weak; X = dark green; Z = yellow-green. ® = 1.622 ¯ = 1.576{1.579 ° = 1.645 2V(meas.) = n.d. Cell Data: Space Group: n.d. a = 5.27{5.31 b = 9.14{9.20 c = 7.24{7.28 Z = [2] X-ray Powder Pattern: Letovice, Czech Republic. 7.31 (100), 3.63 (90), 2.501 (70), 2.894 (60), 1.530 (60), 4.55 (50b), 2.321 (40) Chemistry: (1) (2) (3) SiO2 32.84 37.0 31.60 Al2O3 0.97 0.21 Fe2O3 0.22 FeO 1.90 NiO 49.05 44.9 58.92 MgO 3.64 5.95 CaO 0.50 0.22 Na2O 0.10 K2O 0.07 + H2O 9.64 11.9 9.48 Total 98.54 100.6 100.00 (1) N¶epoui, New Caledonia. (2) Nakety, New Caledonia. (3) Ni3Si2O5(OH)4: Polymorphism & Series: Dimorphous with pecoraite; forms a series with lizardite. Mineral Group: Kaolinite-serpentine group. Occurrence: An alteration product of nickel-rich ultrama¯c rocks. Association: Serpentine, chlorite, hydrous nickel silicates, iron oxides. Distribution: From the Reis II mine, N¶epoui; near Nakety, and at Thio, New Caledonia. In the 132 North nickel mine, Widgiemooltha district, Western Australia. From Pavlos, Greece. -
Does Low Exposure to Chrysotile Pose a Health Risk?
Does Low Exposure to Chrysotile Pose a Health Risk? Dr. Tom Hesterberg Principal Toxicologist Center for Toxicology and Environmental Health American Conference Institute’s Asbestos Claims and Litigation January 30-31, 2014 San Francisco, California 5120 North Shore Drive | North Little Rock, AR 72118 | Main Line: 501.801.8500 Overview of Fiber Toxicology Studies • Basics of Fiber Toxicology • Chromosomal Effects • Fiber Biopersistence • Rodent Inhalation Studies • Thresholds for Fiber Toxicity 2 Basics of Fiber Toxicology 3 Dose The Cornerstone of Toxicology “All substances are poisons; there is none which is not a poison. The right dose differentiates a poison from a remedy.” Paracelsus (1493-1541). 4 Definition of Threshold The dose below which a given effect is not observed A threshold is a result of our bodies’ protective mechanisms 5 Doses of Common Substances Substance Normal Lethal Water 1.5 qts 15 qts Aspirin 2 tablets 90 tablets Table Salt 3 tsp. 60 tsp. Cyanide in Lima Beans 0.5 cups 11 cups Toxicity is the adverse effect caused when a chemical reaches a sufficient dose—threshold. 6 Asbestos Types Chrysotile Asbestos Crocidolite Asbestos The Three Ds of Fiber Toxicology Dose - Amount reaching the deep lung Dimension - Thin fibers deposit in the deep lung; long fibers are more toxic Durability - Dissolution and breakage; more durable fibers are more toxic Hesterberg and Hart., Inhal. Tox., 2001 8 Biopersistence Determines Toxic Potential of Fibers Long Fiber (> 20 µm) Incongruent Dissolution Congruent Dissolution Transverse Breakage Complete Altered Biological Translocation Dissolution Reactivity Macrophage Uptake Mucociliary Clearance Epithelial Cell Uptake Intracellular Degradation Translocation to Interstitium Hesterberg and Hart., Inhal. -
Characterization of Fibrous Mordenite: a First Step for the Evaluation of Its Potential Toxicity
crystals Article Characterization of Fibrous Mordenite: A First Step for the Evaluation of Its Potential Toxicity Dario Di Giuseppe 1,2 1 Department of Chemical and Geological Sciences, University of Modena and Reggio Emilia, Via G. Campi 103, I-41125 Modena, Italy; [email protected] 2 Department of Sciences and Methods for Engineering, University of Modena and Reggio Emilia, Via Amendola 2, I-42122 Reggio Emilia, Italy Received: 4 August 2020; Accepted: 28 August 2020; Published: 31 August 2020 Abstract: In nature, a huge number of unregulated minerals fibers share the same characteristics as asbestos and therefore have potential adverse health effects. However, in addition to asbestos minerals, only fluoro-edenite and erionite are currently classified as toxic/pathogenic agents by the International Agency for Research on Cancer (IARC). Mordenite is one of the most abundant zeolites in nature and commonly occurs with a fibrous crystalline habit. The goal of this paper is to highlight how fibrous mordenite shares several common features with the well-known carcinogenic fibrous erionite. In particular, this study has shown that the morphology, biodurability, and surface characteristics of mordenite fibers are similar to those of erionite and asbestos. These properties make fibrous mordenite potentially toxic and exposure to its fibers can be associated with deadly diseases such as those associated with regulated mineral fibers. Since the presence of fibrous mordenite concerns widespread geological formations, this mineral fiber should be considered dangerous for health and the precautionary approach should be applied when this material is handled. Future in vitro and in vivo tests are necessary to provide further experimental confirmation of the outcome of this work. -
Ocean Drilling Program Scientific Results Volume
Karson, J.A., Cannat, M., Miller, D.J., and Elthon, D. (Eds.), 1997 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 153 3. SERPENTINIZATION AND HYDROTHERMAL VEINING IN PERIDOTITES AT SITE 920 IN THE MARK AREA1 Yildirim Dilek,2 Angela Coulton,3 and Stephen D. Hurst4 ABSTRACT Cores from Site 920 in the Mid-Atlantic Ridge at the Kane Transform (MARK) area record polyphase deformation in two holes reaching 126 and 200 m depth in serpentinized peridotites with minor metagabbros, amphibolite gneiss, and diabase units. The majority of the recovered mantle-derived rocks are composed of serpentinized harzburgites, which display a variably elongated, medium- to coarse-grained Porphyroclastic texture produced by high-temperature crystal-plastic deformation. The Porphyroclastic texture is overprinted by an anastomosing foliation defined by dark green to black serpentine and magnetite bands that wrap around orthopyroxene porphyroclasts. These bands are composed of a variant of mesh-textured serpentine, and contain mainly lizardite ± chrysotile, whereas mesh centers consist of fine-grained lizardite + brucite. Serpentine fibers in the bands are generally wall perpendicular, suggesting that the foliation is mainly a dilational fabric. The anastomosing foliation is cut by a set of veins (VI), which contain serpentine + actinolite + chlorite ± talc and oblique-slip fibers. They display a wide range of dips with no preferred dip orientation, and indicate shearing synchronous with dilation. Compared to veins of later generations and to the pseudomorphic serpentine, serpentine in the VI veins is relatively rich in iron, with FeO (total Fe as FeO) content ranging from 4.55 to 5.76 wt%. A network of thin and discontinuous veins (V2) composed of chrysotile and mag- netite postdates the VI veins and is either parallel to the anastomosing foliation and to the mesoscopic Porphyroclastic fabric or, less commonly, is at a high angle to the foliation. -
16. Mineralogy and Geochemistry of Weathered Serpentinites, Deep Sea Drilling Project Leg 841
16. MINERALOGY AND GEOCHEMISTRY OF WEATHERED SERPENTINITES, DEEP SEA DRILLING PROJECT LEG 841 Roger Helm, Geologisches Institut, Ruhr-Universitàt2 ABSTRACT At Sites 566, 567, and 570 of Leg 84, ophiolitic serpentinite basement was covered by a sequence of serpentinitic mud that was formed by weathering of the serpentinites under sea- or pore-water conditions. Several mineralogical pro- cesses were observed: (1) The serpentinitic mud that consists mainly of chrysotile was formed from the lizardite compo- nent of the serpentinites by alteration. (2) Slightly trioctahedral smectites containing nonexpandable mica layers, trioc- tahedral smectites containing nonexpandable chlorite layers, and swelling chlorites were presumably formed from detri- tal chlorite and/or serpentine. (3) The occurrence of tremolite, chlorite, analcime, and talc can be attributed to reworking of gabbroic ophiolite rocks. (4) Dolomite, aragonite, and Mg-calcite, all authigenic, occur in the serpentinitic mud. INTRODUCTION green unweathered serpentinite are dispersed in the muddy groundmass. The serpentinitic mud shows colors from Serpentinitic muds were recovered above serpentinitic dusky blue to grayish blue. Dolomite was found in the basement rocks at Sites 566, 567, and 570. At all sites serpentinitic mud. This serpentinite occurrence within where ultramafic ophiolitic rocks were recovered, serpen- early Miocene slope sediments was probably a boulder tinitic muds with or without calcareous admixtures were transported from upslope by slumping, and little evidence recovered above the serpentinites. The muds are inter- for mixing between serpentinitic mud and typical slope preted to be the result of submarine weathering of the un- sediment was observed by the shipboard scientists (Site derlying serpentinites. The mineralogy and chemistry of 567 report, this volume).