Analyse bayésienne et élicitation d’opinions d’experts en analyse de risques et particulièrement dans le cas de l’amiante chrysotile

L’appréciation de la puissance cancérogène des fibres d’amiante chrysotile repose en grande partie sur des jugements subjectifs et incertains des experts et des analystes en raison des résultats hétérogènes et équivoques d’études épidémiologiques et toxicologiques sérieuses. L’approche probabiliste bayésienne en évaluation de risques peut formaliser l’impact des jugements subjectifs et de leurs incertitudes sur les estimations de risques, mais elle est encore peu utilisée en santé publique. Le présent travail examine la possibilité d’appliquer l’approche bayésienne dans une récente élicitation d’opinions d’experts pour estimer la toxicité du chrysotile, le degré de consensus et de divergence, ainsi que les niveaux d’incertitude des experts. Les estimations des experts concordaient assez bien sur la différence de toxicité entre chrysotile et amphiboles pour les mésothéliomes. Pour le cancer du poumon, les évaluations probabilistes étaient bien plus disparates. Dans ce cas, les jugements des experts semblaient influencés à différents degrés par des biais heuristiques, surtout les heuristiques d’affect et d’ancrage liés à la controverse du sujet et à l’hétérogénéité des données. Une méthodologie rigoureuse de préparation des experts à l’exercice d’élicitation aurait pu réduire l’impact des biais et des heuristiques sur le panel.

Fluorescent Chrysotile From Sterling Hill, New Jersey

Minerals of the serpentine group, notably chrysotile and to a lesser extent lizardite, are widely present at both Franklin and Sterling Hill. They are late-stage hydrous magnesium silicate minerals that formed by hydrothermal alteration of earlier species, among them willemite and tephroite, and are also common components of hydrothermal veins cutting the ore bodies and the enclosing marble (Dunn, 1995). Although long recognized in the area (Fowler, 1825), local serpentine was not documented as a fluorescent mineral until 2004, when a brief description of a fluorescent serpentine from Franklin appeared in The Picking Table (Cianciulli, 2004). In the present paper, we describe additional examples of fluorescent serpentine, most from Sterling Hill.

Structural and textural variations in carbonaceous chondrite matrices

Recent studies of C2 carbonaceous chondrite matrices using high resolu­tion transmission electron microscopy (HRTEM)have shown that structural details of the matrix minerals can be imaged [1-4]. The Murchison and Mighei matrices contain minerals having ordered and disordered mixed-layer structures [1,3,4] in addition to chrysotile- and lizardite-type structures [2].

Serpentinization of peridotites from the southern Mariana forearc

A detailed petrologic and mineralogic study was carried out on serpentinized peridotites dredged from the southern landward slopes of the Mariana Trench, in order to reveal the serpentinization process of these unusual rocks and to identify the sole presence of the mineral lizardite. The constituent minerals of these southern Mariana forearc peridotites are olivine, amphibole and spinel, as well as serpentine, chlorite and talc. Compared with serpentinite seamounts, the serpentinized peridotites from the southern Mariana forearc are characterized by the absence of magnetite and brucite, and the common presence of talc; besides, the serpentine mineral variety is simplex, only lizardite. Combining mineral chemistry and mineral phase relationships, we conclude that (1) the absence of magnetite in the serpentinized peridotites is due to incomplete serpentinization, other than magnetite, the iron end-member in olivine forms Fe-rich brucite and Fe-rich serpentine; (2) brucite is not stable with high silica activity, reacting with later SiO2-rich fluid and then forming lizardite, leading to a lack of brucite in these serpentinized peridotites; (3) the occurrence of talc is the result of later SiO2-rich fluid reactions with lizardite; and (4) the reason for the sole occurrence of lizardite is that the temperature condition of our study area was not high enough for the formation of antigorite (which is stable at > 500 degrees C). Despite the broad overlap of lizardite and chrysotile in growth temperature, differences in the modes of occurrence of lizardite and chrysotile, such as the scarcity of H2O, low porosity and permeability, as well as the actual situation of initial serpentinization in the study area, result in the absolute prevalence of lizardite over chrysotile in the area. (C) 2009 National Natural Science Foundation of China and Chinese Academy of Sciences. Published by Elsevier Limited and Science in China Press. All rights reserved.

Talc-bearing serpentinized peridotites from the southern Mariana forearc: implications for aseismic character within subduction zones

The serpentinized peridotites overlying the subducted zones in the Izu-Bonin-Mariana (IBM) arc system have been interpret as the cause of the low-velocity layer identified beneath the IBM froearc, in turn few earthquakes occurred along the plate boundary. Chrysotile, which is a low temperature and highly hydrated phase of serpentine with low frictional strength, has been suggested as the low velocity material in the serpentinized peridotites, besides, brucite is inferred to be likely conducive to stable sliding. However, such idea encounters challenging in our serpentinized peridotites from the southern Mariana forearc, which absent both the above minerals. The presence of talc, which characterized by its weak, low-friction and inherently stable sliding behavior, provides new clue. Here we report the occurrence of talc in serpentinized peridotites collected from the landward trench slope of the southern Mariana forearc. We infer that talc is mainly forming as a result of the reaction of serpentine minerals with silica-saturated fluids released from the subducting slab, and talc also occurs as talc veins sometimes. Due to its unique physical properties, talc may therefore play a significant role in aseismic slip in the IBM subduction zone.

Zmiany właściwości włóknistych krzemianów pod wpływem czynników fizykochemicznych

Wydział Chemii

Adverse effects of industrial multiwalled carbon nanotubes on human pulmonary cells

The aim of this study was to evaluate adverse effects of multiwalled carbon nanotubes (MWCNT), produced for industrial purposes, on the human epithelial cell line A549. MWCNT were dispersed in dipalmitoyl lecithin (DPL), a component of pulmonary surfactant, and the effects of dispersion in DPL were compared to those in two other media: ethanol (EtOH) and phosphate-buffered saline (PBS). Effects of MWCNT were also compared to those of two asbestos fibers (chrysotile and crocidolite) and carbon black (CB) nanoparticles, not only in A549 cells but also in mesothelial cells (MeT5A human cell line), used as an asbestos-sensitive cell type. MWCNT formed agglomerates on top of both cell lines (surface area 15-35 μm2) that were significantly larger and more numerous in PBS than in EtOH and DPL. Whatever the dispersion media, incubation with 100 μg/ml MWCNT induced a similar decrease in metabolic activity without changing cell membrane permeability or apoptosis. Neither MWCNT cellular internalization nor oxidative stress was observed. In contrast, asbestos fibers penetrated into the cells, decreased metabolic activity but not cell membrane permeability, and increased apoptosis, without decreasing cell number. CB was internalized without any adverse effects. In conclusion, this study demonstrates that MWCNT produced for industrial purposes exert adverse effects without being internalized by human epithelial and mesothelial pulmonary cell lines. [Authors]

Amiante et conflits d’intérêts : l’Université McGill pointée du doigt

Étude de cas / Case study

Exposición laboral de agentes químicos carcinógenos presentes en las empresas afiliadas a una ARL en Colombia 2011-2014

Objetivo: Caracterizar los sectores económicos con mayor susceptibilidad de exposición a agentes químicos carcinógenos, categorizados en el grupo 1 por la Agencia Internacional para la Investigación del Cáncer IARC (formaldehído, polvo de madera, benceno y sílice cristalina) afiliadas a una Administradora de riesgos Laborales (ARL) en Colombia entre el periodo 2011 a 2014. Método: Estudio de tipo descriptivo retrospectivo con datos históricos obtenidos desde 2011 hasta 2014. De acuerdo con el número de mediciones que se realizó en cada área y cargo de las empresas objeto de estudio, se utilizó la medición basal para determinar el estado inicial y evaluar de manera concurrente la exposición de estos cuatro agentes químicos. Resultados: En total se obtuvieron 201 mediciones de higiene industrial para cuatro agentes químicos carcinógenos. Los resultados mostraron que índice de riesgo de la exposición a agentes químicos carcinógenos en diferentes empresas, se encuentra en algunos casos en niveles altos o críticos dado que superar los valores máximos permisibles definidos por la Conferencia Americana de Higienistas Industriales de Gobierno (ACGIH). Conclusión: Los trabajadores de diferentes empresas en Colombia están expuestas a diferentes tipos de concentraciones por agentes químicos cancerígenos. Las concentraciones ambientales obtenidas en el ambiente laboral en algunos casos excedieron las concentraciones máximas permitidas, por lo que se recomienda que las empresas e instituciones del país fortalezcan las medidas de prevención, vigilancia y control para minimizar los riegos a que pueden estar expuestos sus trabajadores.

Mesoestruturas porosas a partir de materiais naturais

The MCM-41 mesoporous synthesis was done using rice hulls ash and chrysotile as natural alternative silica sources. For the using of these sources, chemical and thermic treatments were done in both materials. After chemical and thermic treatments, these materials were employed on the MCM-41 mesoctructures synthesis. The natural materials treated and employed in the synthesis were characterized by several techniques such as X-ray diffraction, N2 adsorption and desorption, scanning electronic microscopy and thermogravimetric analysis. MCM-41 standart samples synthetized with aerosil 200 commercial sílica were used to evaluation. The formed material from rice hulls ash showed values from BET specific area about 468 m².g-1, N2 adsorption and desorption isotherms and loss mass similar to reference materials. The silica from chrysotile calcined and leached was employed to mesoporous materials synthesis. The BET specific area showed values about 700 m².g-1, N2 adsorption and desorption isotherms type IV and loss mass similar to mesoporous materials. The formed material from calcined and leached chrysotile, without calcination, applied to phenol remotion carried high performance liquid chromatography and evaluated with organophilic clays with different treatments. By the characterization techniques were proved that mesoporous materials with lesser order that reference samples. The material formed from rice hulls ash without the calcination step achieved better adsorption results than organophilic clays