2012
DOI: 10.1016/j.ijrmms.2011.12.004
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Deformation and strength anisotropy of Asan gneiss, Boryeong shale, and Yeoncheon schist

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Cited by 402 publications
(184 citation statements)
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“…Cho et al conducted a series of uniaxial compression tests with Boryeong shale and other rocks to explore the deformation and strength anisotropy. With the results by Cho et al [19], we are able to know that the coefficient of anisotropy of strength of Boryeong shale is 0.58, reflecting that the anisotropy of the Boryeong shale is a little stronger than that of the Longmaxi …”
Section: Discussionsupporting
confidence: 50%
See 1 more Smart Citation
“…Cho et al conducted a series of uniaxial compression tests with Boryeong shale and other rocks to explore the deformation and strength anisotropy. With the results by Cho et al [19], we are able to know that the coefficient of anisotropy of strength of Boryeong shale is 0.58, reflecting that the anisotropy of the Boryeong shale is a little stronger than that of the Longmaxi …”
Section: Discussionsupporting
confidence: 50%
“…Furthermore, sample deformation will be relatively large when the load direction deviates from the bedding planes, indicating that shale has a lower stiffness under these anisotropy angles. A paper from Cho et al [19] reported the experimental investigation of deformation and strength anisotropy of Asan gneiss, Boryeong shale and Yeoncheon schist in Korea which have clear evidence of transverse isotropy. From the paper we learned that the change laws of Young's modulus with the angle of anisotropy of various layered rock are of great difference.…”
Section: Discussionmentioning
confidence: 99%
“…일축압축 강도와 압열인장강도는 각각 3회의 실험결과에 대한 평 균치이며, 탄성정수는 방향별로 부착된 84개의 변형률 Table 3. Elastic constants of Asan gneiss (Cho et al, 2012) (Goodman, 1989). …”
Section: Gbm-udec 모델의 미시변수와 거시물성의 관계unclassified
“…Kim et al [27] has studied the thermal conductivity of the Asan gneiss and Boryeong shale, finding that the ratio of K PAR (thermal conductivity of parallel to bedding planes) to K PER (thermal conductivity of perpendicular to bedding planes) is 1.4, and the anisotropy of thermal conductivity in the shale is obvious. The wave velocity in a rock is usually used as a physical parameter [28,29] to predict the elastic modulus and thermal conductivity of rock. It is also affected by changes in the material and fracture development, with the wave velocity tending to decrease with an increase in temperature.…”
Section: Introductionmentioning
confidence: 99%