492 resultados para Asbestos, Serpentine


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Ultramafic rocks, mainly serpentinized peridotites of mantle origin, are mostly associated with the ophiolites of Mesozoic age that occur in belts along three of the margins of the Caribbean plate. The most extensive exposures are in Cuba. The ultramafic-mafic association (ophiolites) were formed and emplaced in several different tectonic environments. Mineralogical studies of the ultramafic rocks and the chemistry of the associated mafic rocks indicate that most of the ultramafic-mafic associations in both the northern and southern margins of the plate were formed in arc-related environments. There is little mantle peridotite exposed in the ophiolitic associations of the west coast of Central America, in the south Caribbean in Curacao and in the Andean belts in Colombia. In these occurrences the chemistry and age of the mafic rocks indicates that this association is mainly part of the 89 Ma Caribbean plateau province. The age of the mantle peridotites and associated ophiolites is probably mainly late Jurassic or Early Cretaceous. Emplacement of the ophiolites possibly began in the Early Cretaceous in Hispaniola and Puerto Rico, but most emplacement took place in the Late Cretaceous to Eocene (e.g. Cuba). Along the northern South America plate margin, in the Caribbean mountain belt, emplacement was by major thrusting and probably was not completed until the Oligocene or even the early Miocene. Caribbean mantle peridotites, before serpentinization, were mainly harzburgites, but dunites and lherzolites are also present. In detail, the mineralogical and chemical composition varies even within one ultramafic body, reflecting melting processes and peridotite/melt interaction in the upper mantle. At least for the northern Caribbean, uplift (postemplacement tectonics) exposed the ultramafic massifs as a land surface to effective laterization in the beginning of the Miocene. Tectonic factors, determining the uplift, exposing the peridotites to weathering varied. In the northern Caribbean, in Guatemala, Jamaica, and Hispaniola, uplift occurred as a result of transpresional movement along pre-existing major faults. In Cuba, uplift occurred on a regional scale, determined by isostatic adjustment. In the south Caribbean, uplift of the Cordillera de la Costa and Serrania del Interior exposing the peridotites, also appears to be related to strike-slip movement along the El Pilar fault system. In the Caribbean, Ni-laterite deposits are currently being mined in the central Dominican Republic, eastern Cuba, northern Venezuela and northwest Colombia. Although apparently formed over ultramafic rocks of similar composition and under similar climatic conditions, the composition of the lateritic soils varies. Factors that probably determined these differences in laterite composition are geomorphology, topography, drainage and tectonics. According to the mineralogy of principal ore-bearing phases, Dominican Ni-laterite deposits are classified as the hydrous silicate-type. The main Ni-bearing minerals are hydrated Mg-Ni silicates (serpentine and ¿garnierite¿) occurring deeper in the profile (saprolite horizon). In contrast, in the deposits of eastern Cuba, the Ni and Cooccurs mainly in the limonite zone composed of Fe hydroxides and oxides as the dominant mineralogy in the upper part of the profile, and are classified as the oxide-type.

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Surface characteristics (area, chemical reactivity) play an important role in cell response to nanomaterials. The aim of this study was to evaluate the oxidative and inflammatory effects of multi&#8722;wall carbon nanotubes (MWCNT) uncoated (P0) or coated with carboxylic polyacid or polystyrene polybutadiene polymetacrylate of methyl polymers (P1 and P2 respectively) on murine macrophages (RAW 264.7 cell line). Carbon black nanoparticles (CB, diameter 95 nm) and crocidolite fibers (diameter: 80 nm, length: < 10 &#956;m) were used as controls. Surface functional groups present on MWCNTs were analyzed by Knudsen flow reactor. The amount of acidic sites was P1> P0> P2, for basic sites was P0> P1>> P2 and for oxidizable sites was P0> P2> P1. In contact with cells, P2 formed smaller aggregates than P0 and P1, which were of similar size. Optical microscopy showed the formation of vacuoles after exposure only to P0, P1 and crocidolite. Incubation of cells with P0, P1 and crocidolite fibers induced a significant and similar decrease in metabolic activity, whereas P2 and CB had no effect. Cell number and membrane permeability were unmodified by incubation with the different particles. Incubation of macrophages with P0, P1 and crocidolite induced a dose&#8722; and time&#8722;dependent increase in mRNA expression of oxidative stress marker (HO&#8722;1, GPX1) and inflammatory mediators (TNF&#8722;a, MIP&#8722;2). No such responses were observed with P2 and CB. In conclusion, MWCNT coated with a carboxylic polyacid polymer exerted similar oxidative and inflammatory effects to uncoated MWCNT. By contrast, no such effects were observed with MWCNT coated with a polystyrene&#8722;based polymer. This kind of coating could be useful to decrease MWCNT toxicity.

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Despite the key importance of altered oceanic mantle as a repository and carrier of light elements (B, Li, and Be) to depth, its inventory of these elements has hardly been explored and quantified. In order to constrain the systematics and budget of these elements we have studied samples of highly serpentinized (&gt;50%) spinel harzburgite drilled at the Mid-Atlantic Ridge (Fifteen-Twenty Fracture zone, ODP Leg 209, Sites 1272A and 1274A). In-situ analysis by secondary ion mass spectrometry reveals that the B, Li and Be contents of mantle minerals (olivine, orthopyroxene, and clinopyroxene) remain unchanged during serpentinization. B and Li abundances largely correspond to those of unaltered mantle minerals whereas Be is close to the detection limit. The Li contents of clinopyroxene are slightly higher (0.44-2.8 mu g g(-1)) compared to unaltered mantle clinopyroxene, and olivine and clinopyroxene show an inverse Li partitioning compared to literature data. These findings along with textural observations and major element composition obtained from microprobe analysis suggest reaction of the peridotites with a mafic silicate melt before serpentinization. Serpentine minerals are enriched in B (most values between 10 and 100 mu g g(-1)), depleted in Li (most values below I mu g g(-1)) compared to the primary phases, with considerable variation within and between samples. Be is at the detection limit. Analysis of whole rock samples by prompt gamma activation shows that serpentinization tends to increase B (10.4-65.0 mu g g(-1)), H2O and Cl contents and to lower Li contents (0.07-3.37 mu g g(-1)) of peridotites, implying that-contrary to alteration of oceanic crust-B is fractionated from Li and that the B and Li inventory should depend essentially on rock-water ratios. Based on our results and on literature data, we calculate the inventory of B and Li contained in the oceanic lithosphere, and its partitioning between crust and mantle as a function of plate characteristics. We model four cases, an ODP Leg 209-type lithosphere with almost no igneous crust, and a Semail-type lithosphere with a thick igneous crust, both at I and 75 Ma, respectively. The results show that the Li contents of the oceanic lithosphere are highly variable (17-307 kg in a column of I m x I m x thickness of the lithosphere (kg/col)). They are controlled by the primary mantle phases and by altered crust, whereas the B contents (25-904 kg/col) depend entirely on serpentinization. In all cases, large quantities of B reside in the uppermost part of the plate and could hence be easily liberated during slab dehydration. The most prominent input of Li into subduction zones is to be expected from Semail-type lithosphere because most of the Li is stored at shallow levels in the plate. Subducting an ODP Leg 209-type lithosphere would mean only very little Li contribution from the slab. Serpentinized mantle thus plays an important role in B recycling in subduction zones, but it is of lesser importance for Li. (C) 2008 Elsevier Ltd. All rights reserved.

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Comprend : [Frontispice : éléments d'architecture, figures de deux soldats en armure, scène de charge de cavalerie.] [Cote : Res Z Fontanieu 103 (5)] ; [Pl. dépl. en reg. p.68 (ou 446) : art équestre. Manière de monter à cheval.] [Cote : Res Z Fontanieu 103 (5)] ; [Pl. dépl. en reg. p.72 (ou 452) : art équestre. Manière de faire tourner le cheval en une ronde ou dans une figure serpentine.] [Cote : Res Z Fontanieu 103 (5)] ; [Pl. dépl. en reg. p.78 (ou 460) : art équestre. Manière de faire monter une côte à un cheval, de lui faire sauter un obstacle.] [Cote : Res Z Fontanieu 103 (5)] ; [Pl. dépl. en reg. p.80 (ou 464) : art équestre. Manière de faire traverser un fleuve à un cheval, de lui faire traverser un pont étroit et de lui faire dominer sa peur du feu. ] [Cote : Res Z Fontanieu 103 (5)] ; [Pl. dépl. en reg. p.84 (ou 470) : art équestre. Manière de combattre avec un lance sur un cheval.] [Cote : Res Z Fontanieu 103 (5)] ; [Pl. dépl. en reg. p.86 (ou 474) : art équestre. Manière de combattre avec un lance ou avec une épéesur un cheval.] [Cote : Res Z Fontanieu 103 (5)] ; [Pl. dépl. en reg. p.88 (ou 478) : art équestre. Manière de combattre avec des arquebuses sur un cheval.] [Cote : Res Z Fontanieu 103 (5)] ; [Pl. dépl. en reg. p.90 (ou 482) : art équestre. Manière de combattre avec des arquebuses ou des épées sur un cheval.] [Cote : Res Z Fontanieu 103 (5)] ; [Pl. dépl. en reg. p.94 (ou 488) : art équestre. Manière de combattre entre un fantassin et un cavalier.] [Cote : Res Z Fontanieu 103 (5)] ; [Pl. dépl. en reg. p.96 (ou 492) : art équestre. Manière de combattre entre un fantassin et un cavalier ou entre deux cavalier armés d'épées.] [Cote : Res Z Fontanieu 103 (5)] ; [Pl. dépl. en reg. p.100 (ou 498) : art équestre. Manière de combattre entre cavaliers.] [Cote : Res Z Fontanieu 103 (5)] ; [Pl. dépl. en reg. p.102 (ou 502) : art équestre. Manière de combattre entre deux adversaires à pied.] [Cote : Res Z Fontanieu 103 (5)] ; [Pl. dépl. en reg. p.106 (ou 508) : art équestre. Scène de batailel avec charge de cavalerie.] [Cote : Res Z Fontanieu 103 (5)] ; [Vigentte p.512 : marque d'imprimeur.] [Cote : Res Z Fontanieu 103 (5)]

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[Table des matières] 1. Contexte, objet et modalités de traitement de la saisine ; Partie A : Exigences réglementaires, normatives et recensement des EPC-EPI amiante. - 2. Exigences réglementaires en matière de protection collective et individuelle contre l'amiante. - 3. Normes d'exigences pour les équipements de protection collective contre l'amiante. - 4. Aspirateurs à usage industriel. - 5. Norms d'exigences pour la protection individuelle contre l'amiante. - 6. Recensement des EPC et EPI en fonction des activités. - 7. Objectifs de la synthèse bibliographique. - 8. Rappels théoriques sur la filtration de l'air. - 9. Efficacité des équipements de protection collective contre l'amiante. - 10. Aspirateurs à usage industriel. - 11. Efficacité des équipements de protection individuelle. - 12. Comparaison de la filtration des fibres d'amiante ou autres particules non sphériques et des aérosols utilisés pour les essais normalisés (MPPS). - 13. Conclusion sur la synthèse bibliographique. - 14. Perspectives. - 15. Bibliographie. - Annexes

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Between the cities of Domodossola and Locarno, the complex ``Centovalli Line'' tectonic zone of the Central Alps outlines deformation phases over a long period of time (probably starting similar to 30 Ma ago) and under variable P-T conditions. The last deformation phases developed gouge-bearing faults with a general E-W trend that crosscuts the roots of the Alpine Canavese zone and the Finero ultramafic body. Kinematic indicators show that the general motion was mainly dextral associated with back thrusting towards the S. The &lt;2 mu m clay fractions of fault gouges from Centovalli Line consist mainly of illite, smectite and chlorite with varied illite-smectite, chlorite-smectite and chlorite-serpentine mixed-layers. Constrained with the illite crystallinity index, the thermal conditions induced by the tectonic activity show a gradual trend from anchizonal to diagenetic conditions. The &lt;2 and &lt;0.2 mu M clay fractions, and hydrothermal K-feldspar separates all provide K-Ar ages between 14.2 +/- 2.9 Ma and roughly 0 Ma, with major episodes at about 12,8, 6 and close to 0 Ma These ages set the recurrent tectonic activity and the associated fluid circulations between Upper Miocene and Recent. On the basis of the K-Ar ages and with a thermal gradient of 25-30 degrees C/km, the studied fault zones were located at a depth of 4-7 km. If they were active until now as observed in field, the exhumation was approximately 2.5-3.0 km for the last 12 Ma with a mean velocity of 0.4 mm/y. Comparison with available models on the recent Alpine evolution shows that the tectonic activity in the area relates to a continuum of the back-thrusting movements of the Canavese Line, and/or to several late-extensional phases of the Rhone-Simplon line. The Centovalli-Val Vigezzo zone therefore represents a major tectonic zone of the Central-Western Alps resulting from different interacting tectonic events. (C) 2011 Elsevier B.V. All rights reserved.

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Nanoparticles are increasingly used in various fields, including biomedicine and electronics. One application utilizes the opacifying effect of nano-TiO(2), which is frequently used as pigment in cosmetics. Although TiO(2) is believed to be biologically inert, an emerging literature reports increased incidence of respiratory diseases in people exposed to TiO(2). Here, we show that nano-TiO(2) and nano-SiO(2), but not nano-ZnO, activate the NLR pyrin domain containing 3 (Nlrp3) inflammasome, leading to IL-1&#946; release and in addition, induce the regulated release of IL-1&#945;. Unlike other particulate Nlrp3 agonists, nano-TiO(2)-dependent-Nlrp3 activity does not require cytoskeleton-dependent phagocytosis and induces IL-1&#945;/&#946; secretion in nonphagocytic keratinocytes. Inhalation of nano-TiO(2) provokes lung inflammation which is strongly suppressed in IL-1R- and IL-1&#945;-deficient mice. Thus, the inflammation caused by nano-TiO(2) in vivo is largely caused by the biological effect of IL-1&#945;. The current use of nano-TiO(2) may present a health hazard due to its capacity to induce IL-1R signaling, a situation reminiscent of inflammation provoked by asbestos exposure.

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Malignant mesothelioma is an incurable disease associated with asbestos exposure arising in the pleural cavity and less frequently in the peritoneal cavity. Platinum-based combination chemotherapy with pemetrexed is the established standard of care. Multimodality approaches including surgery and radiotherapy are being investigated. Increasing knowledge about the molecular characteristics of mesothelioma had led to the identification of novel potential targets for systemic therapy. Current evidence suggests pathways activated in response to merlin deficiency, including Pi3K/mTOR and the focal adhesion kinase, as well as immunotherapeutic approaches to be most promising. This review elaborates on the rationale behind targeted approaches that have been and are undergoing exploration in mesothelioma and summarizes available clinical results and ongoing efforts to improve the systemic therapy of mesothelioma.

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Diagnosis of pleural plaques (PPs) is commonly straightforward, especially when a typical appearance is observed in a context of previous asbestos exposure. Nevertheless, numerous causes of focal pleural thickening may be seen in routine practice. They may be related to normal structures, functional pleural thickening, previous tuberculosis, pleural metastasis, silicosis or other rarer conditions. An application of a rigorous technical approach as well as a familiarity with loco-regional anatomy and the knowledge of typical aspects of PP are required. Indeed, false-positive or false-negative results may engender psychological and medico-legal consequences or can delay diagnosis of malignant pleural involvement. Correct recognition of PPs is crucial, as they may also be an independent risk factor for mortality from lung cancer in asbestos-exposed workers particularly in either smokers or former/ex-smokers. Finally, the presence of PP(s) may help in considering asbestosis as a cause of interstitial lung disease predominating in the subpleural area of the lower lobes. The aim of this pictorial essay is to provide a brief reminder of the normal anatomy of the pleura and its surroundings as well as the various aspects of PPs. Afterwards, the common pitfalls encountered in PP diagnosis will be emphasized and practical clues to differentiate actual plaque and pseudoplaque will be concisely described.

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This paper describes the construction and performance of homemade electrodes for voltammetric purpose using cheap materials, like pipette tips and asbestos fiber. A good cost-to-benefit relation makes this devices specially designed for student use, expecting to improve the broadcasting of electroanalytical methods in Brazilian schools.

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Asbesti on yleisnimike kuitumaisille silikaattimineraaleille. Sillä on monia hyviä ominaisuuksia. Siksi sitä on käytetty useisiin eri käyttÃtarkoituksiin jo yli 4 000 vuoden ajan. Sisäänhengitettynä asbesti aiheuttaa kuitenkin vakavia terveyshaittoja, mm. asbestoosia, keuhkosyÃpää ja mesotelioomaa. Vuosina 1918-1988 Suomessa käytettiin asbestia 300 000 tonnia. Yleisintä käyttà oli 1960-70-lukujen vaihteessa. Sairauksien viive altistumisesta on 10-40 vuotta. Sairauksien esiintyminen onkin nyt suurimmillaan. Suurin osa sairauksista on hyvänlaatuisia keuhkopussin paksuuntumia eli plakkeja. Vuosittain asbestin aiheuttamiin sairauksiin, etupäässä syÃpiin, kuolee Suomessa noin 100 ihmistä. Yhteensä altistuneita arvellaan olevan 250 000. Heistä elossa on noin 50 000. Vaarallisuutensa vuoksi asbestin käyttà on useissa maissa kielletty, mutta maailmalla sitä käytetään edelleen suuria määriä. Suomessa asbestin käyttÃä rajoitettiin jo 1970-luvulla. Pieniä poikkeuksia lukuun ottamatta täyskielto tuli voimaan 1.1.1994. Suomessa asbestia esiintyy edelleen vanhoissa rakennuksissa. Asbestipurkutyà on luvanvaraista. AsbestitÃissä on huolehdittava siitä, että kukaan ei altistu asbestille. Asbestipitoisen materiaalin tunnistaminen silmämääräisesti on vaikeaa. Materiaali luokitellaan asbestipitoiseksi, jos siinä on asbestia yli 1 painoprosenttia tai jos sitä voidaan pÃlyävyytensä takia pitää vaarallisena. Asbestipitoisen materiaalin kartoituksessa voidaan käyttää rakennussuunnitelmia, vanhoja asiakirjoja kuten urakoitsijan laskuja sekä tuntemusta rakennusajan yleisistä rakennustavoista. Varmuus saadaan kuitenkin vain tutkimalla materiaali esimerkiksi laboratoriokokeissa. Tässä diplomityÃssä on pyritty selvittämään, voidaanko asbesti tunnistaa ChemPro 100 -keinonenällä. Laite perustuu ioniliikkuvuusspektrometriaan eli eri yhdisteiden erilaiseen liikkuvuuteen kaasumaisessa väliaineessa. Menetelmä on nopea ja yksinkertainen. Tutkimusta varten hankittiin asbestipitoisia materiaaleja, joista saatuja tuloksia vertailtiin toisiinsa. Nykyiset asbestintunnistusmenetelmät ovat monimutkaisia ja hitaita. Jos keinonenä pystyttäisiin kouluttamaan tunnistamaan asbestimateriaali, helpottaisi se asbestikartoituksen tekemistä.

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Among the building materials used in rural facilities, roofs are noteworthy for being largely responsible for thermal comfort, influencing the thermal balance within the shelter. This study aimed to evaluate the influence of roof on the Enthalpy (H), Thermal Load of Radiation (TLR), and Black Globe Temperature and Humidity Index (BGHI) in individual shelters for dairy calves. The design was completely randomized with three treatments: Z - zinc tile, AC - asbestos-cement tile and ACW - asbestos-cement tile painted white on the upper side. The averages were compared by the Scott Knott test at 1% probability. The results showed no statistical difference between treatments (P<0.01) and the external environment for H. For TLR, there was statistical difference among all treatments, where ACW showed the lowest TLR, 489.28 W m-2, followed by AC with 506.72 W m-2 and Z with the highest TLR, 523.55 W m-2. For BGHI, the lowest values were observed for ACW (76.8) and AC (77.4), differing significantly from Z, which obtained the highest value (81.6). The tiles with white paint on the upper side promoted the lowest TLR and the lowest BGHI, favoring the thermal environment in the shelter.

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In Tropical regions, the animal performance is often affected by climate conditions. This study aimed to evaluate covering materials in individual shelters, normally used to house dairy calves, and its influence on the calves physiology and performance. The design used was completely randomized, with a 2x3 factorial arrangement to compare the averages of 5% through the Tukey's test, i.e., both genders- and three types of covering in the shelters (Z - zinc; AC - asbestos cement; and WPAC - white-painted asbestos cement). Parameters evaluated included daily weight gain (DWG), dry matter intake (DMI), feed conversion (FC), rectal temperature (RT), and respiratory frequency (RF). Results showed significant differences (P < 0.05) among males (1.04kg/day) and females (0.74kg/day) for DWG and interaction between gender and treatment (P < 0.05) for zinc covering (0.562kg/day for females and 1.120kg/day for males). Significant differences were also observed in FI of animals housed under shelters with the covering of zinc (48.35kgDM/day for females and 96.91 kgDM/day for males). There were no significant differences (P &gt; 0.05) in the FC and the RT, and there were significant differences (P < 0.05) for RF in the Z treatments (56.9 mov.min-1), WPAC (62.2 mov.min-1) and FC (70.25 mov.min-1). It was concluded that different covering materials did not affect performance and dry matter intake of dairy calves. However, the animals' physiology of thermoregulation was altered by the different covering materials used in individual shelters.

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The research was developed to evaluate the use of different types of roofing materials regularly used in poultry houses. Measurements of thermal comfort were made through the use of techniques such as the Black Globe and Humidity Index (BGHI), the Thermal Heat Load (THL) and Enthalpy (H). Conducted in the State University of Goiás, during the months of April and May, 2011, the experiment was composed of five different treatments: AC - Asbestos cement tiles, BA -Bamboo tiles, BAP - Bamboo tiles painted in white, FB -Vegetable fiber tiles and bitumen, FBP -Vegetable fiber tiles and bitumen painted in white. The experiment consisted in 15 repetitions, which were considered the different days of measurements taken. Throughout the studied period, the time of the day considered the least comfortable was the one observed at 2:00pm, and the coverage of vegetable fiber and bitumen showed the highest value of BGHI (84.1) when compared to other types of coverage, characterizing a situation of lower thermal comfort, and no difference was found for THL and H on treatments in the studied region.