• Journal of the Korean Society of Hazard Mitigation
• /
• v.4 no.3 s.14
• /
• pp.9-17
• /
• 2004

In recent years slope failure due to heavy rainfalls or local downpours usually accompanied by typhoons has increasingly occurred in Korea. Also, the damages caused by slope failure have a tendency to be more disastrous than before. This study has been conducted to prepare an early warning system for slope failure by : (1) analyzing types and causes of slope failure, (2) examining the published evaluation criteria for slope stability, (3) estimating slope stability by considering the properties of slope-forming materials as well as the topographical and geological properties of slopes, and (4) determining the most important variables of affecting the stability of the slope under consideration. The data on the variations of slope conditions measured by an automatic in-situ measurement system and then transmitted to the central analysis system by using an internet. The most important variables can be back-calculated in the central system and compared with the values for the first and second management criteria. These management criteria should be modified and corrected continuously in the future by accumulated data and knowledge related to the early warning system for slope failure.

• The Journal of Engineering Geology
• /
• v.24 no.1
• /
• pp.137-146
• /
• 2014

The geology of the study area which is located in Samkoe-dong, Dong-gu, Daejeon city comprises black slate, limestone, and pebble-bearing phyllitic rock as meta-sedimentary rocks; and biotite granite and quartz porphyry intrusions. Face mapping revealed sliding in three or four sites of contained coaly slate, where the dip of the foliation and other discontinuities is parallel to the surface slope. The cause of the slope sliding is this parallelism as well as the swelling of the coaly slate when wet. In contrast, the slop on the opposite side of the road is relatively stable because the dip of the foliation and other discontinuities are oblique or normal to the surface slope. To ensure slope stability, a cut-and-cover tunnel was designed and constructed for the new road.

• The Journal of Engineering Geology
• /
• v.17 no.2 s.52
• /
• pp.253-261
• /
• 2007

The failure of the road cut-slope due to heavy rains brings about lots of injuries and damage on national properties. KICT has developed CSMS system by means of prevention to manage the dangerous cut slopes. In spite of the continuous management the frequency of cut-slopes failure is increasing the past due to changes of earth-environment. KICT has installed the "Real-Time Monitoring System" on dangerous slopes. The operation of Real-Time Monitoring System is used as a positive system to reduce injuries and damages. However, Although the slope manager is aware of the signs collapsed in advance, it has temporal and spatial limits until the slope manager performs the works which are preventing the accidents. When real time monitoring system finds out an indication of slope collapse, the Rock-fall Signal Lamp System makes road-users indicated the risk of cut slopes. It is a kind of prevention system that it will minimize the damages of the properties as suspension of traffic automatically or passively.

• Tunnel and Underground Space
• /
• v.24 no.4
• /
• pp.255-274
• /
• 2014

The target of this study is large scale rock slope collapsed by around 7 pm on August, 2012, which is located at ${\bigcirc}{\bigcirc}$ limestone quarries of Gangneung city, Gangwondo. The slope prior to the collapse is formed as the height of about 200 m and the average inclination of $45^{\circ}$. The estimated amount of the collapse is about $1,500,000m^3$ with respect to the slope after the collapse. Geotechnical and field investigations such as boring, geophysical prospecting, surface geological survey, geological lineaments, borehole imaging, metric 3D imaging, experimental and field test, mining work by year, and daily rainfall were performed to find the cause of rock slope failure. Various analyzes using slope mass rating, stereonet projection, limit equilibrium method, continuum and non-continuum model were conducted to check of the stability of the slope. It is expected that the cause of slope failure from the results of various analysis and survey is due to the combined factors such as topography, rainfall, rock type and quality, discontinuities, geo-structural characteristics as the limestone cavity and fault zones, but the failure of slope in case of the analysis without the limestone cavity is not occurred. Safe factor of 0.66 was obtained from continuum analysis of the slope considering the limestone cavity, so the ultimate causes of slope failure is considered to be due to the influence of limestone cavity developed along fault zone.

• Tunnel and Underground Space
• /
• v.28 no.6
• /
• pp.569-583
• /
• 2018

The purpose of this study is to identify the collapse characteristics by analyzing various factors causing collapse based on field survey and existing data on rock slopes occurring in the construction of roads and industrial complexes in Gyeongsangnam - do area. In the case of the slope where the slope has been directly surveyed, the analysis of the collapse characteristics can be used for the prediction and prevention of slope failure through the continuous collection of the slope data, database construction, management and analysis. The evaluation items used in the collapse characteristics of slope were selected among the items that can be regarded as objective evaluation items among the overlapping factors by comparing the evaluation items frequently used for the evaluation of the existing slope stability among various factors. The type of destruction of the rock slope depends on the type of carcass of the bedrock, such as planar fracture, wedge fracture, onho fracture, and conduction fracture, which are different from each other. And the slope stability analysis should be performed accordingly.

• The Journal of Engineering Geology
• /
• v.15 no.1
• /
• pp.57-66
• /
• 2005

The failure of cut slope and landslide sometimes come from a local downpour within a short duration in Korea. Especially, most of recent downpour converged upon a limited region and seemed the characteristics of guerilla. Characteristics of slopes failed due to local downpour are analyzed. failure mode is also analyzed with respect to the depth of soil layers and the change of groundwater level. To blow the influence factors of the slope stability during local downpour, the authors conducted field survey for failed slopes and tried to make a comparative study of 1,372 cut slope data distributed in the national road. FLAC-SLOPE(ITASCA Co.) is used to analyze slope stability with changing depth of soil layers and groundwater level. The result shows that the failed types of domestic slopes during local downpour are mainly shallow collapse and landslide. The change of soil depth and groundwater level have influenced on the stability of slopes.

• Economic and Environmental Geology
• /
• v.50 no.2
• /
• pp.129-143
• /
• 2017

The shallow sediments in the southwestern Ulleung Basin consist of mass flow deposits such as slide/slump and debris flow deposits (DFD), caused by slope failure. These sediments are proven to be important in studying geological disaster and stability of the seafloor. In this paper, we analysised the flow accumulation and slope failure susceptibility of the Ulleung Basin on the basis of multi-beam data, collected in this area. We also studied the distribution pattern and the seismic characteristics of the DFD in the uppermost layer of the Ulleung Basin on the basis of seismic data. The slope susceptibility was calculated as the frequency ratio of each factors including slope, aspect, curvature and stream power index (SPI), which causes the slope failure. These results indicate that the slope failure is frequently to occur in the southern and western continental slope of the Ulleung Basin. The sediment flow (mass flow) caused by the slope failure converges to the north and northwest of the Ulleung Basin. According to the seismic characteristics, the uppermost layer in study area can be divided into four sedimentary unit. These sedimentary units develop from the south and southwest to the north and northwest in association with slope susceptibility and flow accumulation.

• Proceedings of the Korean Geotechical Society Conference
• /
• 2007.09a
• /
• pp.588-595
• /
• 2007

기상이변과 관련되어 집중호우에 의한 사면 붕괴 및 산사태가 전세계적으로 많이 발생하고 있다. 국내에서도 사면 붕괴로 발생하는 재해에 대하여 사후 대책마련차원에서 벗어나 적극적인 방재관리차원의 체계를 마련코자 급경사지와 관련된 법률을 만들어 시행하게 되었다. 사면과 관련된 기술은 국내 기술도 선진국의 기술에 버금가는 좋은 기술을 가지고 있으나, 다소 미진한 부분에 대하여 해외의 사례와 동향을 파악하여 보다나은 기술개발 및 정책 결정에 도움이 되고자 자료를 수집하고 정리 하였다.

• Proceedings of the Korean Society for Rock Mechanics Conference
• /
• 2003.03a
• /
• pp.121-134
• /
• 2003

본 연구대상은 $\bigcirc$$\bigcirc$우회도로 Sta.3＋300~600 구간에 형성된 높이 약 50m의 대절토 암반사면으로 대부분 절취가 완료된 상태에서, 1차로 사면 좌측부의 발파암과 풍화암의 경계부를 따라 인장균열이 소규모로 형성되면서 Slip 등 사면파괴활동이 시작되었으며, 2차로 활동높이 35m, 활동폭 40m, 활동깊이 약 l0m 규모로 붕괴되었고, 주변에도 인장균열의 발생이 확인되는 등 추가 붕괴의 징후가 있어 사면의 안정성을 검토하였다. Rock Cleavages가 발달한 천매암으로 구성된 파괴활동사면을 대상으로 지표지질조사, 추가시추조사, 전기비저항탐사, 시추공 영상촬영(BIPS)을 실시하여 사면붕괴의 원인과 추후에 예상되는 붕괴의 양상을 파악하고, 연구지역에 가장 적합한 보강대책을 수립하고자 하였다.

• Proceedings of the Korean Geotechical Society Conference
• /
• 2006.10a
• /
• pp.35-45
• /
• 2006

강원도 홍천일대의 지역은 경기육괴의 편마암이 주암종으로 이루어진 지역으로 대규모의 홍천단층이 지나고 있다. 과거 이 단층대 부근에서 건설된 도로건설시에 발생된 많은 절토사면의 붕괴를 통해 그 원인 파악 및 차후 고려해야 할 사항을 파악하는 것이 매우 중요한 과제 중에 하나이다. 본 논문은 붕괴를 토대로 붕괴의 원인 및 대책방안을 파악하고자 한다. 홍천일대의 사면붕괴를 유발시키는 원인으로는 크게 두 가지 지질구조적인 요인을 들 수 있는데 하나는 사면방향으로 발달하는 편마암내에 발달하는 엽리면을 따라 붕괴가 발생되는 사례가 있고 둘째는 단층파쇄대 및 단층대를 따라 붕괴가 발생되는 원인으로 대별할 수 있다. 두 번째의 요인은 비교적 규모가 큰 사면붕괴를 유발하게 되고 막대한 복구비용이 수반되는 결과를 초래하게 된다. 이러한 단층의 수반에 의해 발생되는 절토사면은 대책방안으로 사면경사완화 방안, 앵커 및 억지말뚝과 같은 보강방법에 의해 안정화를 시키는 사례가 주를 이루었으며 차후 이 일대의 건설공사시에는 단층대의 방향 및 규모에 대한 조사를 세밀히 이루어져야 할 것이다.