Authors
Jasmine R Petriglieri, Luca Barale, Maura Tomatis, Alessandro Cavallo, Chiara De Giuli, Maria Rosaria Bruno, Angelo Olori, Biagio Maria Bruni, Paolo Ballirano, Elena Belluso, Fabrizio Piana, Alessandro Pacella, Antonella Campopiano, Francesco Turci
Published in
Journal of hazardous materials. Volume 516. Pages 143415. Aug 27, 2026. Epub Aug 27, 2026.
Abstract
Hazard assessment of naturally occurring asbestos and asbestos-like minerals (NOA) is hindered by the lack of standardized criteria for quantifying asbestos-like morphology. This work introduces the fibrosity parameter (Fp), an experimental approach for classifying suspected fibrous minerals. Fp combines standardized mechanical stress with automated morphometric analysis to evaluate changes in the percentage of elongate mineral particles (EMP) during milling. The approach was tested on five antigorite and three tremolite samples spanning fibrous, lamellar, and prismatic morphologies, using crocidolite, amosite, MMVF, and talc as references. Fp is defined by EMP% after 20 min of milling (EMP20%) and the slope of EMP% between 2 and 20 min (S). Thresholds of EMP20% = 50% and S = -1 distinguished four morphological scenarios: 1) asbestos or asbestos-like, 2) precautionary asbestos-like, 3) non-asbestos-like, and 4) non-asbestos. Fibrous antigorite samples and one tremolite retained high EMP contents and behaved comparably to asbestos references, whereas another macroscopically fibrous tremolite progressively lost fibrosity and was classified as non asbestos-like. Thus, macroscopic fibrosity is not a reliable proxy for asbestos-like fragmentation behaviour. Fp provides a quantitative and reproducible morphological screening tool that complements broader hazard assessment. However, Fp is not a stand-alone predictor of pathogenicity.
PMID:
42679572
Bibliographic data and abstract were imported from PubMed on 02 Sep 2026.
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