Non-occupational (environmental) exposure to naturally occurring asbestos (NOA) represents a potentially important source of risk for human health in several parts of the world. Chemical reactivity of fibres surface is one of the most relevant physical-chemical property to asbestos toxicity and is commonly associateci to the presence of Fe at the surface, and in particular to its coordination and oxidation state. However, no detailed information is still available about dependence of chemical reactivity on surface iron topochemistry, which is the basis for defining structure-activity relationships. In this work the chemical reactivity of two amphibole asbestos samples, UICC crocidolite from Koegas Mine, Northern Cape (South Africa) and fibrous tremolite from Montgomery County, Maryland (USA), was investigateci after sample heating up to 1200 °c. Ex-situ X-ray powder diffraction (XRPS and the Rietveld method), scanning (SEM) and transmission (TEM) electron microscopy were used for characterizing the minerai fibres before and after the thermal treatment. In addition, thermal stability of the of the amphibole asbestos was analysed in-situ by TG/DSC. Two conventional target molecules (H202 and Hcoo-) and the DMPO spintrapping/ EPR technique were used to measure the radical activity of both pristine and thermal treated samples. Results show that, after thermal treatment, both amphibole asbestos are completely converted into hematite, cristobalite and pyroxene, stili preserving the originai fibrous morphology (pseudomorphosis). Notably, in spite of the thermal decomposition, the heated samples show a radical production comparable to that of the pristine ones.

Chemical reactivity of thermal treated naturally occurring amphibole asbestos / Ballirano, Paolo; Pacella, Alessandro; Tomatis, Maura; Turci, Francesco; Viti, Cecilia; Bloise, Andrea. - (2020). (Intervento presentato al convegno EGU General Assembly 2020 tenutosi a Online) [10.5194/egusphere-egu2020-10801].

Chemical reactivity of thermal treated naturally occurring amphibole asbestos

Paolo Ballirano;Alessandro Pacella;
2020

Abstract

Non-occupational (environmental) exposure to naturally occurring asbestos (NOA) represents a potentially important source of risk for human health in several parts of the world. Chemical reactivity of fibres surface is one of the most relevant physical-chemical property to asbestos toxicity and is commonly associateci to the presence of Fe at the surface, and in particular to its coordination and oxidation state. However, no detailed information is still available about dependence of chemical reactivity on surface iron topochemistry, which is the basis for defining structure-activity relationships. In this work the chemical reactivity of two amphibole asbestos samples, UICC crocidolite from Koegas Mine, Northern Cape (South Africa) and fibrous tremolite from Montgomery County, Maryland (USA), was investigateci after sample heating up to 1200 °c. Ex-situ X-ray powder diffraction (XRPS and the Rietveld method), scanning (SEM) and transmission (TEM) electron microscopy were used for characterizing the minerai fibres before and after the thermal treatment. In addition, thermal stability of the of the amphibole asbestos was analysed in-situ by TG/DSC. Two conventional target molecules (H202 and Hcoo-) and the DMPO spintrapping/ EPR technique were used to measure the radical activity of both pristine and thermal treated samples. Results show that, after thermal treatment, both amphibole asbestos are completely converted into hematite, cristobalite and pyroxene, stili preserving the originai fibrous morphology (pseudomorphosis). Notably, in spite of the thermal decomposition, the heated samples show a radical production comparable to that of the pristine ones.
2020
EGU General Assembly 2020
04 Pubblicazione in atti di convegno::04d Abstract in atti di convegno
Chemical reactivity of thermal treated naturally occurring amphibole asbestos / Ballirano, Paolo; Pacella, Alessandro; Tomatis, Maura; Turci, Francesco; Viti, Cecilia; Bloise, Andrea. - (2020). (Intervento presentato al convegno EGU General Assembly 2020 tenutosi a Online) [10.5194/egusphere-egu2020-10801].
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11573/1679815
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