Calculating the cohesion and internal friction angle of volcanic rocks and rock masses

Marlene Villeneuve, M. J. Heap

Publikation: Beitrag in FachzeitschriftArtikelForschungBegutachtung

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Rock failure criteria are key input parameters for models designed to better understand the stability of volcanic rock masses. Cohesion and friction angle are the two defining material variables for the Mohr-Coulomb failure criterion. Although these can be determined from laboratory deformation experiments, they are rarely reported. Tabulated data for volcanic rocks, calculated using published triaxial results, show that cohesion and friction angle decrease with increasing porosity. If porosity is known, these empirical fits can provide laboratory-scale cohesion and friction angle estimations. We present a method to upscale these parameters using the generalised Hoek-Brown failure criterion, discuss the considerations and assumptions associated with the upscaling, and provide recommendations for potential end-users. A spreadsheet is provided so that modellers can (1) estimate cohesion and friction angle and (2) upscale these values for use in large-scale volcano modelling. Better constrained input parameters will increase the accuracy of large-scale volcano stability models.
Seiten (von - bis)279-293
PublikationsstatusVeröffentlicht - 23 Nov. 2021

Bibliographische Notiz

Funding Information:
M. Heap acknowledges support from the Institut Uni-versitaire de France (IUF). We acknowledge the insightful and constructive review from Fabian Wadsworth and two anonymous reviewers who helped improve this manuscript.

Publisher Copyright:
© 2021 Volcanica. All rights reserved.

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