• Magazine of korean Tunnelling and Underground Space Association
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• v.13 no.2
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• pp.9-23
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• 2011

• The Journal of Engineering Geology
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• v.9 no.1
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• pp.17-29
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• 1999

There are three major processes to impact the groundwater flow near underground storage caverns in the coastal area; effect of topography, effect of sea water intrusion, and effect of excavation. In this paper, the effects of three items were numerically studied to identify the major cause for altering the flow pattern. It turned out that the excavation is the most significant effect on the groundwater flow system. The groundwater pressure distributions and consequent groundwater pathways were significantly altered near the openings. By increasing the groundwater pressures from water curtain holes, the potential leakage of storage cavern was properly prevented

• Magazine of korean Tunnelling and Underground Space Association
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• v.1 no.2
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• pp.8-38
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• 1999

• Proceedings of the Korean Society for Rock Mechanics Conference
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• 1996.03a
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• pp.11-24
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• 1996

최근 들어 지하공간 활용에 대한 필요성이 강하게 대두되면서 지하암반 굴착공사가 매우 활발하게 진행되고 있다. 오래 전부터 공사되었던 지하철 및 산악터널 뿐만 아니라 오늘날에는 지하암반의 특수성을 이용한 지하공간 사업 즉, 지하양수 발전소, 핵폐기물 저장소, 유류 비축기지 등이 건설 중에 있으며, 지하공간과 관련된 대형 프로젝트가 구상되고 있다. (중략)

• Proceedings of the Korean Society for Rock Mechanics Conference
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• 1996.03a
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• pp.43-54
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• 1996

장대 터널, 지하철, 양수발전소, 유류 비축기지, 핵폐기물 지하처분장 및 농축산물 지하 저장소 등 지하공간개발의 구상 및 그 건설이 활발한 가운데, 그 관련기술에 대한 관심이 고조되고 있다. 특히 지하공간개발을 위한 사전 설계단계 및 시공에 있어 국내ㆍ외적으로 현지암반 초기응력 측정은 중요한 요소로 대두되고 있다. (중략)

• Proceedings of the Korean Society for Rock Mechanics Conference
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• 2007.10a
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• pp.163-173
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• 2007

• Proceedings of the Korean Society for Rock Mechanics Conference
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• 1994.03a
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• pp.52-55
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• 1994

현대산업의 주요 에너지원인 석유는 매장량의 지역적 편중이 심하여 전량수입에 의존하는 우리나라의 경우 정부의 에너지 수급정책이 국제 정세 흐름에 크게 영향을 받음. 과거 우리는 1,2차 석유파동을 통하여 안정적 에너지 공급의 위협을 받아 국가 경제 및 국민생활에 막대한 혼란을 경험한 바 있음. (중략)

• Economic and Environmental Geology
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• v.43 no.2
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• pp.149-162
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• 2010

The most serious problem in oil stockpiles with artificial underground cavern is maintaining the stability of ground water system. In order to understand the ground water system around K-1 site, we determined the regional flow direction and level distribution of groundwater, and investigated the major geologic factors influencing their flow system. Reactivated surface along the contact between granite and gneiss, and fractures and faults along the long acidic dyke may contribute as important pathways for groundwater flow. Within K-1 site, groundwater level fluctuation is closely related to the rainfall events and injection from surface or influx water. In this project, the effect of groundwater pumping from the southern wells was examined. Based on equations relating water level drawdown to pumping rate at those wells, their pumped outflow of groundwater ranged from $80\;m^3$/day to less than $250\;m^3$/day. The modeling results with MODFLOW imply that the previous groundwater pumping at distance of 1.2 km may not affect the groundwater level variations of the K-1 site. However, continuous pumping work at quantity over $250\;m^3$/day in this area will be able to affect the groundwater system of the K-1 site, particularly along the acidic dyke.

• The Journal of Engineering Geology
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• v.20 no.2
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• pp.169-181
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• 2010

This study aimed at simulating several responses to stresses caused by the ground water level variations around the K-1 oil stockpile. For this simulation, we considered the characteristic hydrogeological condition including the special occurrence of long and thick acidic dyke, which is regarded as the main geological structure dominating the ground water flow system at this study area. We activated twenty-four imaginary wells which are located in northern and southern area around central K-1 site. Each neighboring distance is altogether 300 m and whole distance between K-1 site and remote wells is 1,200 m. Through the modeling, we operated the long-term and continuous pumping tests and finally categorized five zones based on maximum pumping rates for the imaginary wells; zone I within 300 meter distance from K-1 site with a pumping rate of 50 $m^3/day$; zone II between 300 to 600 meter distance from K-1 site with a pumping rate of 75 $m^3/day$; zone III between 600 to 900 meter distance from K-1 site with 150 $m^3/day$; zone IV between 900 to 1,200 meter distance from K-1 site with 300 $m^3/day$; and zone V of acidic dyke area. At zone V, especially because of their possibility of high transmissivity for groundwater flow, it is necessary to control and restrict groundwater discharge.

• Proceedings of the Korean Society for Rock Mechanics Conference
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• 1996.03a
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• pp.73-82
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• 1996

지하철, 지하유류비축기지와 같은 지하구조물의 건설이나, 대형 건축물의 건설을 위한 지반조사로서 시추조사는 가장 기본적이라 할 수 있으며, 서울 일대에서는 지하철 1∼8호선, 경부고속전철 등의 대규모 사업과 관련하여 많은 시추조사가 실시되었다. 그러나 이와 같은 대형 건설사업을 위한 시추공 자료들은 건설 당시에만 사용되었을 뿐 이후 자료의 보존 및 관리가 잘 되지 않았다. (중략)