Direct and indirect assessment of the amount of naturally occurring asbestos in fractured rocks
DOI:
https://doi.org/10.21701/bolgeomin.131.3.002Keywords:
asbestos, Naturally Occurring Asbestos (NOA), fractured rocks, Discrete Fracture Networks (DFNs), fracture samplingAbstract
Naturally-Occurring Asbestos (NOA) may constitute a severe health risk when metamorphic rocks are excavated for large infrastructure projects. For public acceptance, a reliable assessment of the content of NOA is necessary for the design of the construction site, workers’ safety, and spoil management. Direct measurements of NOA content can be made by SEM-EDS analyses on an adequate number of samples. Such measurements are sufficiently precise but questions about the representativity of the samples may arise, especially when the rock units are structurally and lithologically complex. Therefore, in order to corroborate the direct assessments, alternative and indirect assessments can be performed by measuring the fracture volumetric porosity, provided that almost all the NOA is deposited as veins in the fractures of the rock mass. Statistical sampling and inference procedures can be applied to derive such an index. In this paper, an indirect assessment of NOA is reported and compared with the assessment obtained by direct measurements. The application is to a metamorphic rock formation through which a tunnel is to be driven as part of the ”Gronda di Genova” highway development in Genoa, Italy. Even though significant approximations are made, the indirect assessment is relatively close to the direct measurement.
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References
ASPI (Autostrade per l'Italia) 2011. Opera a mare nel canale di calma; parte descrittiva generale. APG9030, http://www.va.minambiente.it/File/Documento/25374 (in italian).
Botta, S., Barale, L., Compagnoni, R., Cossio, R., Piana, F., Marcelli, I., Tallone, S., Avataneo, C., Turci, F. 2020. Petrofacies for the prediction of NOA content in rocks: application to the "Gronda di Genova" tunneling project. Bulletin of Engineering Geology and the Environment, 79(1), 185-204. https://doi.org/10.1007/s10064-019-01539-6
Capponi, G., Crispini, L. 2008. Carta Geologica d'Italia alla scala 1:50.000 e note Illustrative, Foglio 213-230 (Genova). APAT, Roma.
Capponi, G., Crispini, L., Federico, L., Malatesta, C. 2016. Geology of the Eastern Ligurian Alps: a review of the tectonic units. Italian Journal of Geosciences, 135(1), 157-169. https://doi.org/10.3301/IJG.2015.06
Cravero, M., Piana, F., Ponti, S., Tallone, S., Balestro, G., Morelli, M. 2006. Analysis of fracture patterns constrained by suitable geological model. 41st US Rock Mechanics Symposium. American Rock Mechanics Association, Golden, CO. ARMA/USRMS 06-1147.
Crispini, L., Federico, L., Capponi, G., Spagnolo, C. 2009. Late orogenic transpressional tectonics in the "Ligurian Knot". Italian Journal of Geosciences, 128, 433-441. https://doi.org/10.3301/IJG.2009.128.2.433
Dershowitz W., Herda H. 1992. Interpretation of fracture spacing and intensity. 33rd U.S. Rock Mechanics Symposium, Santa Fe, New Mexico, 757-766.
Giacomini, F., Boerio, V., Polattini, S., Tiepolo, M., Tribuzio, R., Zanetti, A. 2010. Evaluating asbestos fibre concentration in metaophiolites: a case study from the Voltri Massif and Sestri-Voltaggio Zone (Liguria, NW Italy). Environmental Earth Sciences, 61, 1621-1639. https://doi.org/10.1007/s12665-010-0475-9
Groppo, C., Rinaudo, S., Cairo, D., Gastaldi, R., Compagnoni, R. 2006. Micro-Raman spectroscopy for a quick and reliable identification of serpentine minerals from ultramafics. European Journal of Mineralogy, 18(3), 319-329. https://doi.org/10.1127/0935-1221/2006/0018-0319
Hammah, R.E., Curran, J.H. 1998. Fuzzy cluster algorithm for the automatic identification of joint sets. International Journal of Rock Mechanics & Mining Sciences, 35(7), 889-905. https://doi.org/10.1016/S0148-9062(98)00011-4
Labagnara, D., Patrucco, M., Rossetti, P., Pellegrino, V. 2013. Predictive assessment of asbestos content in the Western Italian Alps: an essential tool for an effective approach to risk analysis in tunnelling operations and muck reuse. Environmental Earth Sciences, 70, 857-868. https://doi.org/10.1007/s12665-012-2174-1
Piana, F., Fioraso, G., Irace, A., Mosca, P., d'Atri, A., Barale, L., Falletti, P., Monegato, G., Morelli, M., Tallone, S., Vigna, G.B. 2017. Geology of Piemonte region (NW Italy, Alps-Apennines interference zone). Journal of Maps, 13(2), 395-405. https://doi.org/10.1080/17445647.2017.1316218
Rinaudo, S., Gastaldi, D., Belluso, E. 2003. Characterization of chrysotile, antigorite and lizardite by FT-Raman spectroscopy. Canadian Mineralogist, 41, 883-890. https://doi.org/10.2113/gscanmin.41.4.883
Turci, F., Compagnoni, R., Piana, F., Delle Piane, L., Tomatis, M., Fubini, B., Tallone, S., Fuoco, S., Bergamini, M. 2015. Geological and analytical procedures for the evaluation of asbestos-related risk in underground and surface rock excavation. Engineering Geology for Society and Territory, Vol. 5, Springer, Berlin. https://doi.org/10.1007/978-3-319-09048-1_120
Wang, X. 2005. Stereological interpretation of rock fracture traces on borehole walls and other cylindrical surfaces. PhD Thesis, Virginia Polytechnic Institute and State University, Blacksburg, Virginia.
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