• 한국암반공학회:학술대회논문집
• /
• 한국암반공학회 2011년도 추계 총회 및 창립 30주년 기념 심포지엄
• /
• pp.89-97
• /
• 2011

Brittle failure of rock is a classical rock mechanics problem. Rock failure not only involves initiation and propagation of single crack, but also is a complex problem associated with initiation, propagation and coalescence of many cracks. As the most important feature of rock material properties is the heterogeneity, the Weibull statistical distribution is employed in the rock failure process analysis (RFPA) method to describe the heterogeneity in rock properties. In this paper, the applications of the RFPA method in geotechnical engineering and rockburst modeling are introduced with emphasis, which can provide some references for relevant researches.

• 한국환경복원기술학회지
• /
• 제4권3호
• /
• pp.49-54
• /
• 2001

It is common that the soil layer is a few meters below the earth's surface and the rock mass is below the soil layer in the view of geological characteristics in Korea. And the boundary between rock and soil is clearly divided. When dealing with the stability of rock masses, as in the case of rock slopes or dam foundations, the majority of the collapses is not within the soil layer, but within the soil-rock boundary. Therefore it is important to identify the shear strength characteristics between soil-rock boundary. And then in the method of reinforcement on landslide this chose a cut slope near Daemo elementary school in Seoul, surveyed shear strength between soil-rock contacts and considered a large scale collapse using a limit equilibrium method.

• 한국환경복원기술학회지
• /
• 제5권3호
• /
• pp.9-14
• /
• 2002

It is common that the soil layer is few meters below the earth surface and there are rock masses below the soil layer in the view of geological characteristics in Korea. The boundary between rock and soil is clearly divided. When dealing with the stability of rock masses, as in the case of rock slopes or dam foundations, the majority of the collapses is not within the soil layer, but within the soil-rock boundary. Therefore, it is important to identify the shear strength characteristics between soil-rock contacts. It has been common practice to assume that the strength of the soil or shale represents the minimum strength present. However, it has been suggested by Patton(1968) that such an assumption may not be valid and that lower shear strengths might be obtained along the soil-rock interface than for either material alone. Then, in this thesis, introduce rock and residual soil shear strength tests and the specimen preparation and testing procedures are described in detail and also the testing results are presented and discussed.

• 터널과지하공간
• /
• 제11권3호
• /
• pp.217-224
• /
• 2001

암석은 지질학적 생성과정으로 인해 많은 역학적 결함을 포함하고 있으며 이러한 결함 사이에는 암석 브릿지가 존재하게 된다. 이러한 암석 브릿지에서의 균열의 전파 및 결합(coalescence)과정은 사면, 기초, 터널 등의 안정성에 영향을 미치게 된다. 본 연구에서는 단축압축 하에서 균열의 형상변화에 따른 암석 브릿지에서의 균열의 개시, 전파 및 결합거동 변화에 대해 알아보았다. 여산 대리석을 재료로 120$\times$60$\times$25 mm크기의 시료에 균열각도 $\alpha$, 브릿지각도 $\beta$, 균열길이 2c, 브릿지길이 2b를 변화시키면서 2개의 인공균열을 제작하였다. 하중을 가하면서 날개형 균열개시응력, 날개형 균열 전파각도, 균열결합 응력을 측정하였으며 균열결합 유형을 정리하였다. 또한, 정규화된 최대강도(normalized peak strength)를 구하여 Ashby & Hallam 모형 (1986)의 이론해와 비교, 분석 하였다.