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Preliminary communication

https://doi.org/10.14256/JCE.3266.2021

Deformation anisotropy of soft rock

Slobodan Živaljević
Zvonko Tomanović
Borko Miladinović


Full text: croatian pdf 4.032 Kb

page 129-141

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Full text: english pdf 4.028 Kb

page 129-141

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Abstract

Bedding, being a typical feature of sedimentary rocks, is a cause of inherent anisotropy of deformation properties of rock mass. Results of uniaxial and triaxial, short-term and creep tests conducted by the authors on the specimens of a soft sedimentary rock - marl are presented in this paper. Interpolation of results of the short-term tests enabled for determining the parabolic dependence of secant modulus of deformability on angle (a) between load and natural bedding planes in the interval from 0 to 90 degrees. The time-dependent deformation response is described by determining the dependence of parameters of the modified Wallner’s model on the angle a in the interval from 45 to 90 degrees, based on the results of the performed creep tests.

Keywords

soft rock; creep; anisotropy; bedding; secant modulus; triaxial; marl

Hrčak ID:

295872

URI

https://hrcak.srce.hr/295872

Publication date:

14.3.2023.

Article data in other languages: croatian

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