• Geomechanics and Engineering
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• 제1권2호
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• pp.143-154
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• 2009

Many factors influence occurrences of rock burst in coal mines, such as mining methods, control methods of the coal roof, lithological characteristics of the roof and floor, tectonic stress, groundwater and so on. Among those factors, lithological characteristics in the roof are the intrinsic controlling factors that affect rock burst during coal mining. Tangshan colliery is one of the coal mines that have suffered seriously from rock bursts in China. In this paper, based on the investigating the lithological characteristics of coal roofs and occurrence of rock bursts in Tangshan colliery, a numerical method is used to study the influence of roof lithological characteristics on rock burst potential. The results show that the lithological characteristics in the roof have an important impact on the distributions of stresses and elastic strain energy in coal seams and their surrounding rocks. Occurrences of rock bursts in this colliery have a close correlation with the thick-bedded, medium- to fine-grained sandstones in the roof. Such strata can easily cause severe stress concentration and accumulate enough energy to trigger rock bursts in the working face during mining operations.

• 터널과지하공간
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• 제19권5호
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• pp.450-462
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• 2009

본 연구는 국내에서 출토되는 화성암, 변성암, 퇴적암 1,417개 블록의 일축압축강도를 간접방법으로 도출하는 과정에서 각 시험법에 따른 강도발현의 거동 특성을 분석하였다. 퇴적암은 간접시험법에 따라 암석군에 상관없이 동일거동을 보이며, 압열인장강도를 매개로 시행한 과정에서는 암석군끼리 동일 거동 특성을 나타내고 있다. 이는 간접시험법을 적용했을 때에는 지질학적 생성원인에 따라 상관성해석을 시행해야 신뢰성 높은 결과를 도출할 수 있음을 암시한다.

• 한국환경복원기술학회지
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• 제4권3호
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• pp.49-54
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• 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.

• The Korean Journal of Ecology
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• 제14권4호
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• pp.371-377
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• 1991

Some morphological characteristics were investigated on the leaves of quercus aliena, hypostomatous species, and lespedeza cyrtobotrya, amphistomatous species, that appeared dominantly on the rock faces in mt.pukhan, mt surak and mt. pulam near seoul. These characteristics were compared with those of normal sites rock faces. All two species growing on the rock faces had thickened leaves with well developed upper epidermis and palisade tissue. Quercus aliena growing on the rock faces showed the leaves with double layer of palisade cells and more regularly arranged spongy parenchyma cells to the lower epidermis. In the case of lespedeza cyrtobotrya, narrower and more lengthened palisade cells and smaller air gaps between the sponge parenchyma cells were observed on the rock faces than those growing in the normal sites. The stomater frequency of the lower epidermis of the tree leaves growing on the rock faces is higher thanthose of normal sites. However, the mean total stomata number of the tree leaves growing on the rock faces are fewer. Most of the morphological characteristics investigated indicate that the plants on the rock faces havesmaller coefficient of variation than those of the normal sites.

• 화약ㆍ발파
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• 제38권3호
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• pp.30-43
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• 2020

암석동역학은 동적하중조건하에서의 암반이나 암석의 역학적 거동에 대해 연구하는 학문으로, 자원개발이나 토목, 지진을 비롯한 재난재해, 국방과학 등 다양한 분야에 걸쳐 그 필요성이 증대되고 있다. 본 보고에서는 암석재료에 대한 동적 실험기법들과 동적 하중상태에서 암석이 보이는 역학적 거동 특성에 대한 최근의 연구결과들을 소개하고자 한다.

• Geomechanics and Engineering
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• 제29권4호
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• pp.377-390
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• 2022

The stability of the roof rock-coal pillar-floor rock composite structure is of great significance to coal mine safety production. The cracks existing in the composite structure seriously affect the stability of the roof rock-coal pillar-floor rock composite structure. The numerical simulation tests of rock-coal-rock composite structures with different crack characteristics were carried out to reveal the composite structures' mechanical properties and failure mechanisms. The test results show that the rock-coal-rock composite structure's peak stress and elastic modulus are directly proportional to the crack angle and inversely proportional to the crack length. The smaller the crack angle, the more branch cracks produced near the main control crack in the rock-coal-rock composite structure, and the larger the angle between the main control crack and the crack. The smaller the crack length, the larger the width of the crack zone. The impact energy index of the rock-coal-rock composite structure decreases first and then increases with the increase of crack length and increases with the increase of crack angle. The functional relationships between the different crack characteristics, peak stress, and impact energy index are determined based on the sensitivity analysis. The determination of the functional relationship can fully grasp the influence of the crack angle and the crack length on the peak stress and impact energy index of the coal-rock composite structure. The research results can provide a theoretical basis and guidance for preventing the instability and failure of the coal pillar-roof composite structure.

• 터널과지하공간
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• 제34권4호
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• pp.312-329
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• 2024

지하 심부를 대상으로 하는 에너지 저장 및 개발, 방사성폐기물 처분 등 여러 지하연구사업들에서 심부 암반대수층 내 지하수 흐름의 주요 통로가 되는 투수성 암반균열의 특성 정보들은 연구시설의 설계와 건설 그리고 운영에 있어 중요한 평가 요소로 고려된다. 국내에는 심도가 매우 깊은 암반시추공에서 투수성 암반균열의 위치와 수리특성, 균열 사이에 발생할 수 있는 지하수 유동 양상에 관한 연구와 데이터베이스가 매우 부족한 실정이다. 본 논문에서는 지온경사와 양수시험 자료분석을 통해 심부 암반대수층 내 투수성 암반균열의 수리특성을 평가하였다. 먼저 온도검층을 통해 심부 지온 분포를 확인하고, 심도별 온도자료를 이용하여 선형회귀분석을 통해 지온경사를 도출하였다. 또한 양수시험을 통한 용출온도를 이용해, 균열암반에 대한 수리특성을 분석하였다. 최종적으로 이러한 물리검층과 수리시험 자료를 통합 분석함으로써 투수성 암반균열의 잠재적 위치와 수리특성, 그리고 시추공 내 지하수 흐름을 평가하였다. 본 연구에서 제안된 심부 투수성 암반균열의 특성평가 과정과 결과들은 심부 암반대수층을 대상으로 하는 지하연구사업들의 성공적인 수행을 위한 기초 자료로 활용될 것으로 기대된다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 1999년도 봄 학술발표회 논문집
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• pp.339-346
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• 1999

The stability of rock slope is considered to have a deep relation with types of rocks because types of rocks have their own typical weathering profiles, geological structures and characteristics of failures. Therefore it is essential for the evaluation of rock slope stability to analyze geological and engineering characteristics in rock mass. The data which collected from investigated slopes in sedimentary rock of Kyengsang Basin along highways were analyzed. Primary factors affecting slope stability in rock mass are: dips and strikes of slopes and discontinuities, shear strength of discontinuities, slope geometry and geological structures etc.

• 터널과지하공간
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• 제21권1호
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• pp.50-65
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• 2011

이 연구에서는 퇴적암, 화성암, 변성암군의 10개 암종-1,417개의 시험자료를 이용하여 탄성파속도와 각종 역학적 parameter간의 상관성해석을 시행하였다. 해석 과정에서 나타나는 암종과 역학 parameter간의 거동특성이 상의함을 구명하였으며, 거동이 동일한 암종들을 모집단으로 상관성 해석을 하였다. 각종 시험자료는 표본의 규모 검정과 Chi-Square검정을 거친 후 해석에 임하였다. 도출된 추정식들은 95% 신뢰도가 확보됨을 확인할 수 있었다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2003년도 봄 학술발표회 논문집
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• pp.131-136
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• 2003

Landslide is a natural disaster frequently noticed In korea during monsoon season in flicting nationwise damages on human lives, properties, transportation networks, construction sites, etc. This study is about landslide characteristic in rainfall. This study selects seven sites that occured in 2001 and 2002. So elect areas divide and studied special quality by carcinoma by igneous rock, metamorphic rock, sedimentary rock. According to study finding, because igneous rock area is very thin into 1m interior and exterior soil layer, failures happened much rock and soil interface. There was place that depth of soil layer becomes about 2∼3m being area that receive serious weathering case of metamorphic rock. Therefore, at collapse much debriflow occurrence expect. Case that sedimentary rock area is broken through stratification looked. When see such results, it may become many helps to study characteristics of landslide occurrence area grasping collapse special quality by rock type.