2015
DOI: 10.1007/s00603-015-0708-z
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A nonlinear criterion for triaxial strength of inherently anisotropic rocks

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Cited by 107 publications
(37 citation statements)
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“…We take five sets of triaxial and uniaxial compression data from the database mentioned in Section 2.4 for example to calculate the parameter . These experimental data are respectively collected from the tests on dry phyllite, dry orthoquartzite, dry slate [35], chlorite schist, and biotite schist [36].…”
Section: Parabolic Criterion For Transversely Isotropic Rockmentioning
confidence: 99%
See 1 more Smart Citation
“…We take five sets of triaxial and uniaxial compression data from the database mentioned in Section 2.4 for example to calculate the parameter . These experimental data are respectively collected from the tests on dry phyllite, dry orthoquartzite, dry slate [35], chlorite schist, and biotite schist [36].…”
Section: Parabolic Criterion For Transversely Isotropic Rockmentioning
confidence: 99%
“…Database. Abundant experimental data including 358 triaxial and 88 uniaxial compression tests corresponding to 12 types of rocks are collected from published articles [35][36][37] to investigate the performance of the proposed criterion and characteristics parameters. As shown in Figure 1, all of the rocks are processed for cylindrical specimens with different bedding angles.…”
Section: Introductionmentioning
confidence: 99%
“…R-square (R 2 ) and average absolute relative error percentage (AAREP) were utilized to estimate the proposed model. AAREP is defined as [31,32],…”
Section: Verification Of the Model On Simulated Production Datasetmentioning
confidence: 99%
“…With the development of economy, a large number of rock projects are emerging. To guarantee the safety of these projects, it is very important to study the mechanical properties of rock (Singh, et al 2015 ; Nadimi et al 2011 ; Wang et al 2014 ; Yang et al 2015 ; Nadimi and Shahriar 2014 ; Chen et al 2016a , b ; Lai et al 2016 ), which as a kind of natural geological material contains many flaws (for instance, joints, micro cracks, faults, etc.). The existence of these flaws complicates the mechanical behavior of rock.…”
Section: Introductionmentioning
confidence: 99%