A modified empirical criterion for strength of transversely anisotropic rocks with metamorphic origin

A modified empirical criterion is proposed to determine the strength of transversely anisotropic rocks. In this regard, mechanical properties of intact anisotropic slate obtained from three different districts of Iran were taken into consideration. Afterward, triaxial rock strength criterion introdu...

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Veröffentlicht in:Bulletin of engineering geology and the environment 2013-06, Vol.72 (2), p.257-269
Hauptverfasser: Saeidi, Omid, Vaneghi, Rashid Geranmayeh, Rasouli, Vamegh, Gholami, Raoof
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container_title Bulletin of engineering geology and the environment
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creator Saeidi, Omid
Vaneghi, Rashid Geranmayeh
Rasouli, Vamegh
Gholami, Raoof
description A modified empirical criterion is proposed to determine the strength of transversely anisotropic rocks. In this regard, mechanical properties of intact anisotropic slate obtained from three different districts of Iran were taken into consideration. Afterward, triaxial rock strength criterion introduced by Rafiai was modified for transversely anisotropic rocks. The criterion was modified by adding a new parameter for taking the influence of strength anisotropy into consideration. The results obtained have shown that the parameter can be considered as the strength reduction parameter due to rock anisotropy. The modified criterion was compared to the modified Hoek–Brown (Saroglou and Tsiambaos) and Ramamurthy criteria for different anisotropic rocks. It was concluded that the criterion proposed in this paper is a more accurate and precise criterion in predicting the strength of anisotropic rocks.
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subjects Anisotropic rocks
Anisotropy
Earth and Environmental Science
Earth Sciences
Foundations
Friction
Geoecology/Natural Processes
Geoengineering
Geological engineering
Geotechnical Engineering & Applied Earth Sciences
Hydraulics
Metamorphic rocks
Nature Conservation
Original Paper
Permeability
Tensile strength
title A modified empirical criterion for strength of transversely anisotropic rocks with metamorphic origin
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