Chrysotile Asbestos As a Cause of Mesothelioma: Application of the Hill Causation Model
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Risk Factors for Malignant Mesothelioma
cancer.org | 1.800.227.2345 Malignant Mesothelioma Causes, Risk Factors, and Prevention Risk Factors A risk factor is anything that affects your chance of getting a disease such as cancer. Learn more about the risk factors for malignant mesothelioma. ● Risk Factors for Malignant Mesothelioma ● What Causes Malignant Mesothelioma? Prevention There's no way to completely prevent mesothelioma. But there are things you can do that might lower your risk. Learn more. ● Can Malignant Mesothelioma Be Prevented? Risk Factors for Malignant Mesothelioma A risk factor is anything that increases your chance of getting a disease such as cancer. Different cancers have different risk factors. Some risk factors, like smoking, can be changed. Others, like a person’s age or family history, can’t be changed. But having a 1 ____________________________________________________________________________________American Cancer Society cancer.org | 1.800.227.2345 known risk factor, or even many, does not mean that you will get the disease. And some people who get the disease may have few or no known risk factors. Researchers have found some factors that increase a person’s risk of mesothelioma. Asbestos The main risk factor for pleural mesothelioma is exposure to asbestos. In fact, most cases of pleural mesothelioma have been linked to high levels of asbestos exposure, usually in the workplace. Asbestos is a group of minerals that occur naturally as bundles of tiny fibers. These fibers are found in soil and rocks in many parts of the world. When asbestos fibers in the air are inhaled, they can get into the lungs. Fibers that stay in the lungs can travel to the ends of the small airways and enter the pleural lining of the lung and chest wall. -
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. -
Solitary Fibrous Tumor of the Pleura: Histology, CT Scan Images and Review of Literature Over the Last Twenty Years
DOI: 10.26717/BJSTR.2017.01.000150 Flavio Colaut. ISSN: 2574-1241 Biomed J Sci & Tech Res Case Report Open Access Solitary Fibrous Tumor of the Pleura: Histology, CT Scan Images and Review of Literature over the Last Twenty Years Giulia Bora1, Flavio Colaut2*, Gianni Segato3, Luisa Delsedime4 and Alberto Oliaro1 1Department of Thoracic Surgery, University of Turin, Italy 2Department of General Surgery and Thoracic, City Hospital , Montebelluna, (Treviso), Italy 3Department of General Surgery, S. Bortolo City Hospital, Vicenza, Italy 4Department of Pathology, University of Turin, Italy Received: June 14, 2017; Published: June 26, 2017 *Corresponding author: Flavio Colaut, Department of General Surgery, City Hospital Montebelluna, Thoracic City Hospital, via Montegrappa 1, 31044 Montebelluna (Treviso), Italy, Tel: ; Fax: 0499367643; Email: Introduction Literature up to 800 cases [1-3] have been reported, and these in case of recurrence [10,16,17]. In less than 5% of patients with Solitary fibrous tumor of the pleura is a rare neoplasm. In numbers show its rarity, despite of mesotheliomas, the most pleural SFPTs an increase of insulin-like factor II type occur and this causes refractory to therapy hypoglycaemia (Doege-Potter syndrome) similar in both sexes and there no differences in both benign and [10,18,19]. The incidence of Doege-Potter syndrome in SFPT is tumors represented. Males and females are equal distributed asbestos, tobacco or others environmental agents, were found for and the same is true for age. No correlation with exposure to malignantSome patients forms. may also present gynecomastia or galactorrhoea its development. Solitary fibrous tumor of the pleura occurs as localized neoplasms of the pleura and was initially classified as microscope and immunohistochemistry, has been possible [1]. -
Global Mesothelioma Deaths Reported
ResearchResearch Global mesothelioma deaths reported to the World Health Organization between 1994 and 2008 Vanya Delgermaa,a Ken Takahashi,a Eun-Kee Park,a Giang Vinh Le,a Toshiyuki Haraa & Tom Sorahanb Objective To carry out a descriptive analysis of mesothelioma deaths reported worldwide between 1994 and 2008. Methods We extracted data on mesothelioma deaths reported to the World Health Organization mortality database since 1994, when the disease was first recorded. We also sought information from other English-language sources. Crude and age-adjusted mortality rates were calculated and mortality trends were assessed from the annual percentage change in the age-adjusted mortality rate. Findings In total, 92 253 mesothelioma deaths were reported by 83 countries. Crude and age-adjusted mortality rates were 6.2 and 4.9 per million population, respectively. The age-adjusted mortality rate increased by 5.37% per year and consequently more than doubled during the study period. The mean age at death was 70 years and the male-to-female ratio was 3.6:1. The disease distribution by anatomical site was: pleura, 41.3%; peritoneum, 4.5%; pericardium, 0.3%; and unspecified sites, 43.1%. The geographical distribution of deaths was skewed towards high-income countries: the United States of America reported the highest number, while over 50% of all deaths occurred in Europe. In contrast, less than 12% occurred in middle- and low-income countries. The overall trend in the age- adjusted mortality rate was increasing in Europe and Japan but decreasing in the United States. Conclusion The number of mesothelioma deaths reported and the number of countries reporting deaths increased during the study period, probably due to better disease recognition and an increase in incidence. -
Epidemiology and Clinical Aspects of Malignant Pleural Mesothelioma
cancers Review Epidemiology and Clinical Aspects of Malignant Pleural Mesothelioma Fraser Brims 1,2,3 1 Curtin Medical School, Curtin University, Perth, WA 6845, Australia; [email protected] 2 Department of Respiratory Medicine, Sir Charles Gairdner Hospital, Perth, WA 6009, Australia 3 National Centre for Asbestos Related Diseases, Institute for Respiratory Health, Perth, WA 6009, Australia Simple Summary: Mesothelioma is a cancer of the lining of the lungs caused by breathing in asbestos fibres. Asbestos was widely used in industry in the last century in most developed countries and is still present in many older buildings to this day. There is no known safe level of asbestos exposure. Symptoms of mesothelioma can include worsening breathlessness, chest pain and loss of weight. There is no cure, and the treatment of mesothelioma is limited, although there have been some recent improvements in therapy. Survival is very variable although most people live for around one year after diagnosis. Efforts to improve and maintain the quality of life for patients with mesothelioma remain a priority. Abstract: Mesothelioma is a cancer predominantly of the pleural cavity. There is a clear association of exposure to asbestos with a dose dependent risk of mesothelioma. The incidence of mesothelioma in different countries reflect the historical patterns of commercial asbestos utilisation in the last century and predominant occupational exposures mean that mesothelioma is mostly seen in males. Modern imaging techniques and advances in immunohistochemical staining have contributed to an improved diagnosis of mesothelioma. There have also been recent advances in immune checkpoint inhibition, however, mesothelioma remains very challenging to manage, especially Citation: Brims, F. -
Chrysotile Asbestos
This report contains the collective views of an international group of experts and does not necessarily represent the decisions or the stated policy of the United Nations Environment Programme, the International Labour Organisation, or the World Health Organization. Environmental Health Criteria 203 CHRYSOTILE ASBESTOS First draft prepared by Dr G. Gibbs, Canada (Chapter 2), Mr B.J. Pigg, USA (Chapter 3), Professor W.J. Nicholson, USA (Chapter 4), Dr A. Morgan, UK and Professor M. Lippmann, USA (Chapter 5), Dr J.M.G. Davis, UK and Professor B.T. Mossman, USA (Chapter 6), Professor J.C. McDonald, UK, Professor P.J. Landrigan, USA and Professor W.J. Nicholson, USA (ChapterT), Professor H. Schreier, Canada (Chapter 8). Published under the joint sponsorship of the United Nations Environment Progralnme, the International Labour Organisation, and the World Health Organization, and produced within the framework of the Inter-Organization Programme for the Sound Management of Chemicals. World Health Organization Geneva, 1998 The International Programme on chemicat safety (Ipcs), esrablished in 1980, is a joint venture of the united Nations Environment programme (uNEp), the International l-abour organisation (ILo), and the world ueatttr orginization (WHO). The overall objectives of the IPCS are to establish the scientific basis for assessment of the risk to human health and the environment from exposure rc chemicals, through international peer review processes, as a prerequisiie for the promotion of chemical safety, and to provide technical assistance -
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.