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Simple Correlation to Evaluate Mohr-Coulomb Failure Criterion Using Uniaxial Compressive Strength

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TLDR
In this article, a correlation between the apparent cohesion and the uniaxial compressive strength was developed based on laboratory data of more than 200 rock samples of different types obtained from the literature.
Abstract
The evaluation of Mohr-Coulomb failure criterion as well as other mechanical properties for reservoir rocks is essential for well planning, development and characterization of oil and gas reservoirs. This is because the understanding of the rock-stress relationship can solve many reservoir problems and avoid cost of remedial work. For example, a Mohr-Coulomb failure criterion may be used for borehole instability analysis, water injection design, production optimization techniques, compaction and sand production prediction, etc. A Mohr-Coulomb failure criterion is a function of the apparent cohesion (τ0) and the angle of internal friction (φ). The evaluation of these two parameters requires testing of many rock samples using an expensive and time-consuming triaxial testing set-up. In this study, a correlation between the apparent cohesion and the uniaxial compressive strength was developed. It is based on laboratory data of more than 200 rock samples of different types obtained from the literature. The correlation coefficient of the developed correlation equals to 0.82. Verification of the developed correlation using data from other references has shown an average error of estimation equal to 10%. Therefore, the Mohr-Coulomb failure criterion’s parameters as well as Poisson’s ratio can be estimated using the developed correlation based on fast and cheap measurements of the uniaxial compressive strength.

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Analogue modeling of flank instability at Mount Etna: Understanding the driving factors

TL;DR: In this paper, the authors used analog models to investigate the role of different factors in the triggering of flank instability at Mt. Etna, and showed the importance of differential buttressing at the volcano base for flank instability.
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Effect of triaxial in situ stresses and heterogeneities on absolute permeability of laminated rocks

TL;DR: In this paper, the effect of triaxial in situ stress variation on absolute permeability of homogeneous and heterogeneous sandstones was investigated and it was concluded that permeability changes due to lamination opening and closure as a result of loading magnitude and orientation.
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Leak-off mechanism and pressure prediction for shallow sediments in deepwater drilling

TL;DR: In this paper, the authors proposed two mechanisms and leak-off pressure prediction models for shallow sediments in deepwater drilling were put forward, and the calculated values of these models were compared with the measured value of shallow leakoff pressure in actual drilling.
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Relative Permeabilities of Homogeneous and Heterogeneous Laminated Rock Samples under Hydrostatic and Triaxial Stresses

TL;DR: In this paper, the authors investigated the integrated effect of rock geomechanics and fluid flow by measuring oil-water relative permeability of homogeneous and heterogeneously laminated rock samples at hydrostatic and triaxial stresses.
References
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Book

Fundamentals of rock mechanics

TL;DR: In this article, Mecanique des roches and Analyse des contraintes were used to construct Elasticite Reference Record (ER) and Elasticite reference record (ER).
Journal ArticleDOI

Failure of three sedimentary rocks in triaxial and hollow cylinder compression tests

TL;DR: In this paper, a qualitative model based on the concept of microcracks development in heterogeneous media is shown to be able to describe the failure patterns of all three British sedimentary rocks in both uniaxial and hollow cylinder compression tests.
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Strength characteristics and shear acoustic anisotropy of rock core subjected to true triaxial compression

TL;DR: In this paper, a new true triaxial cell was designed to apply independent and unequal principal stresses to the curved surfaces of cylindrical core plugs, and a series of discrete failure tests on dry specimens from two sandstone lithologies exhibiting different deformation, strength and poroperm characteristics, were conducted under azimuthal stress anisotropy ( σ 2 > σ 3 ) with σ 1 being applied axially.
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