1968
DOI: 10.1016/0148-9062(68)90005-3
|View full text |Cite
|
Sign up to set email alerts
|

Determination of the stress in rock unaffected by boreholes or drifts, from measured strains or deformations

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
17
0

Year Published

2008
2008
2022
2022

Publication Types

Select...
4
2
1

Relationship

0
7

Authors

Journals

citations
Cited by 88 publications
(17 citation statements)
references
References 3 publications
0
17
0
Order By: Relevance
“…Therefore, the previous stress coordinates have to be changed for the inclined wells [30]. Then, the borehole induced stresses for an inclined well are:…”
Section: Induced Principal Stressesmentioning
confidence: 99%
See 2 more Smart Citations
“…Therefore, the previous stress coordinates have to be changed for the inclined wells [30]. Then, the borehole induced stresses for an inclined well are:…”
Section: Induced Principal Stressesmentioning
confidence: 99%
“…The Mohr-Coulomb criterion, which is one of the most common geomechanical failure criteria in the literature, is [30]: (22) where UCS represents the Uniaxial Compressive Strength of the rock and q is a parameter that depends on the friction angle, :…”
Section: -Failure Criteria Analysis For Determination Of the Breakoumentioning
confidence: 99%
See 1 more Smart Citation
“…The stress and strain solutions for a cavity and surrounding crack(s) in an infinite elastic plane are abundant in the literature. Earlier analytical solutions were developed for the problem of a radial crack attached to a circular cavity by use of the complex-variable theory of elasticity (Bowie 1956;Hsu 1975), or by direct solution of the Airy stress functions in the real plane Rooke 1973, 1979). Later, the elastic dislocation theory was widely used for this purpose.…”
Section: Solutionmentioning
confidence: 99%
“…The stress state in the elastic region (or non-yielding zone, r R) can be calculated with Equations (37)- (39). The radial stress at the interface R can be obtained by considering the stress state [(2 h − R ), h , R ] at r = R, which must satisfy the yield criterion (Equation (9a)):…”
Section: Special Casementioning
confidence: 99%