• 지질공학
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• 제2권1호
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• pp.19-35
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• 1992

화강편마암을 지반으로 하는 지역의 Fill Dam 코어기초에 3-12m 폭의 단층대와 40여m 폭의 단층파쇄대가 신선한 암반사이에 분포하며, 이들 각각의 암반의 탄성특성은 현저한 차이를 보인다. 평판재하시험 및 시추공내 변형시험 등의 현장 원위치 시험결가 신선한 암반의 변형계수는 $42,000~168,000kg/\textrm{cm}^2$의 범위를 보이나 단층대의 변형계수는 $963~2,204kg/\textrm{cm}^2$, 파쇄대에서는 $1,238~2,098kg/\textrm{cm}^2$의 범위를 나타낸다. 이와 같이 큰 차이의 변형계수값을 갖는 단층대 및 단층파쇄대와 신선한 암반 사이에는 댐 성토 후 부등침하가 예상된다. 따라서 이에 대한 보강을 위하여 증분식 유한요소 프로그램인 FEADAM 84를 이용한 지반과 보강에 따른 변위 등을 검토하였다. 이때 구성된 유한요소망은 지표조사 및 시추조사에서 확인된 불연속면이 기하학적 분포특성을 고려하였다. 유한요소 해석을 통하여 계산된 단층대와 신선한 암반 사이의 보강 전 부등침하량은 약 6cm에 달하며, 콘크리트 치환 보강 후에는 0.5cm 이내로 나타났다.

• Journal of Microbiology and Biotechnology
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• 제18권1호
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• pp.5-14
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• 2008

The deep subseafloor rock in oil reservoirs represents a unique environment in which a high oil contamination and a very low biomass can be observed. Sampling this environment has been a challenge owing to the techniques used for drilling and coring. In this study, the facilities developed by the Brazilian oil company PETROBRAS for accessing deep subsurface oil reservoirs were used to obtain rock samples at 2,822-2,828 m below the ocean floor surface from a virgin field located in the Atlantic Ocean, Rio de Janeiro. To address the bacterial diversity of these rock samples, PCR amplicons were obtained using the DNA from four core sections and universal primers for 16S rRNA and for APS reductase (aps) genes. Clone libraries were generated from these PCR fragments and 87 clones were sequenced. The phylogenetic analyses of the 16S rDNA clone libraries showed a wide distribution of types in the domain bacteria in the four core samples, and the majority of the clones were identified as belonging to Betaproteobacteria. The sulfate-reducing bacteria community could only be amplified by PCR in one sample, and all clones were identified as belonging to Gammaproteobacteria. For the first time, the bacterial community was assessed in such a deep subsurface environment.

• 한국암반공학회:학술대회논문집
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• 한국암반공학회 2003년도 춘계학술발표회 논문집
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• pp.13-30
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• 2003

본 고에서는 터널 굴착전 대상지반의 지질상태 및 암반거동을 암반예측시스템(RPS)을 통해 사전에 예측하고, 시공중 취약구간에 대해 적절한 대응을 하는 새로운 종합적인 방법을 소개하고자 한다. 암반예측시스템(RPS)은 선진보링(LIM), 선진수평시추, 탄성파탐사(TSP/HSP)로 구성되어 있다. 암반예측시스템에서 탄성파탐사(TSP/HSP)는 주요 단층과 공동등 연약대의 위치에 대한 개략적인 정보를 제공하며, 선진수평시추는 탄성파탐사(TSP/HSP)에 의해 예측된 연약대 전방에서 단층 또는 공동의 위치와 폭을 확인하는 데 활용된다. 선진보링(LIM)은 암반의 연경도와 굴착면 부근의 작은 연약대를 발견하는 데 활용된다. 암반예측시스템(RPS)은 영동선 철도현장의 솔안터널에 성공적으로 적용되어 그 효용성이 입증되었다.

• 자원환경지질
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• 제45권4호
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• pp.365-375
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• 2012

이 연구는 캐나다 Core Research Center (CRC) 시추코어 Saleski 03-34-88-20w4와 Saleski 08-01-88-20w4를 이용하여 비투멘을 함유한 캐나다 앨버타주 데본기 탄산염암의 무기 지화학적 특징을 규명하고, 탄산염 저류층에 대한 지화학적 기초자료를 구축하는데 목적이 있다. 대부분이 0.2 mm 이하 크기의 돌로마이트 입자로 구성된 탄산염암은 소량의 석영과 방해석을 포함한다. 두 CRC 코어 탄산염암의 퇴적환경과 돌로마이트화 과정이 유사하나 Saleski 03-34-88-20w4 코어 탄산염암이 Saleski 08-01-88-20w4 코어 탄산염암보다는 쇄설성 퇴적물 유입이 상대적으로 많은 환경에서 형성되었다. 동위원소 분석결과 두 CRC 코어 돌로마이트 생성온도는 약 40~$55^{\circ}C$이고, 돌로마이트 생성 속성수는 데본기 해수이다. 캐나다 앨버타 데본기 Cairn층과 비교한 결과 돌로마이트 생성온도는 같으나, Cairn층은 약간의 대륙기원 암석과 반응한 속성수가 해수에 혼합되었을 가능성이 있다.

• 지구물리와물리탐사
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• 제20권4호
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• pp.207-215
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• 2017

비전통 에너지 자원의 하나인 셰일가스를 개발하기 위해서는 수평시추와 수압파쇄가 필요하고 이 작업들은 수평응력차비가 낮은 곳에서 실시한다. 수평응력차비는 일반적으로 최대 수평응력과 최소 수평응력을 측정하여 구하지만 동탄성계수와 이방성변수를 활용하여 구하기도 한다. 본 연구에서는 단양 석회암 암석코어 시료실험을 통해 이방성 특성을 살펴보고 수평응력차비를 구하였다. 단양 석회암체에서 퇴적 층리면에 수직, 45도, 수평방향으로 된 암석코어 시료를 성형하고 P파 속도, S파 속도, 밀도를 측정한 후 동탄성계수, 컴플라이언스계수를 구하여 수평응력차비를 계산하였다. 시료분석결과 수평응력차비는 약 0.185로 제시하였다. 단양 석회암은 층리 대칭축에 따라서 P파, S파의 속도가 변화하여 Thomsen 매개변수 값도 이와 같은 특징을 잘 반영하고 있으며 수평응력차비는 포아송 비보다 컴플라이언스 값에 영향을 많이 받고 있다. 향후 SH파 속도를 측정할 경우 좀 더 정확한 암석물리 물성을 구할 수 있을 것으로 판단된다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2000년도 봄 학술발표회 논문집
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• pp.199-206
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• 2000

The grout-effect evaluation of the ground reinforcement technique, which has been widely applied to civil engineering and construction fields, is not established for the guidelines of choosing the efficient evaluation method, and in fact the experts have little effort to determine the reinforcement effect quantitatively. The evaluation of the grout was carried out by experiments on core specimen and drilling, which is impossible to evaluate grout-reinforcement effect quantitatively. This paper presents an example on verification of FRP grout-effect using geophysical prospecting on ground surface, which is 2D resistivity survey that easily visualize survey results with color graphics and seismic refraction method that interprets the subsurface seismic velocity structure.

• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2005년도 춘계학술대회
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• pp.693-696
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• 2005

KIGAM (Korea Institute of Geoscience and Mineral Resources) launched a new project to develop the low-temperature geothermal water in the area showing high geothermal anomaly, north of Pohang city, for large-scale space heating. Surface geologic and geophysical surveys including Landsat 1M image analysis, gravity, magnetic, Magnetotelluric (MT) and controlled-source audio-frequency MT (CSAMT), and self-potential (SP) methods have been conducted and the possible fracture zone was found that would serve as deeply connected geothermal water conduit. In 2004, two test wells of 1.1km and 1.5km depths have been drilled and various kinds of borehole survey including geophysical logging, pumping test, SP monitoring, core logging and sample analysis have followed. Temperature of geothermal water at the bottom of 1.5km borehole reached over $70^{\circ}C$ and the pumping test showed that the reservoir contained huge amount of geothermal water. Drilling for the production well of 2 km depth is on going. After test utilization and the feasibility study, geothermal water developed from the production well is going to be provided to nearby apartments.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2006년도 춘계 학술발표회 논문집
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• pp.1-11
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• 2006

To be design the slope, the area distributed the shale or mica schist which was metamorphosed by shale must carefully consider the stability. The shale has the detrital materials of which the grain size are 1/256mm and fissility. As the reason the slope of shale is always unstable by bedding slip and fissility but also the joint and fault. Mica schist is also another unstable rock for slope by schistosity, cleavage, axial plane of a fold etc. In general shale and mica schist contain the swelling clay minerals such as smectite, vermiculite and montmorillonite. These minerals make the slope unstable. At OO tunnel construction area for the rail way of the Kyungbu high speed train, the slope of mica schist is very unstable by the distribution phenomena of the discontinuous plane such as joints which are 1-5cm spacing and thrust and strike-slip fault. By the drilling core of this area, most RQD have 0-20%.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2004년도 춘계학술발표회
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• pp.11-19
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• 2004

When pile foundation constructed by driving method, it is desirable to perform monitoring and estimation of pile drivability and bearing capacity using some suitable tools. Dynamic Pile Monitoring yields information regarding the hammer, driving system, and pile and soil behaviour that can be used to confirm the assumptions of wave equation analysis. Dynamic Pile Monitoring is performed with the Pile Driving Analyser. The Pile Driving Analyser (PDA) uses wave propagation theory to compute numerous variables that fully describe the condition of the hammer-pile-soil system in real time, following each hammer impact. This approach allows immediate field verification of hammer performance, driving efficiency, and an estimate of pile capacity. The PDA has been used widely as a most effective control method of pile installations. A set of PDA test was performed at the site of Donghea-1 Gas Platform Jacket which is located east of Ulsan. The drilling core sediments of location of jacket subsoil are composed of mud and sand, silt. In this case study, the results of PDA test which was applied to measurement and estimation of large diameter open ended steel pipe pile driven by underwater hydraulic hammer, MHU-800S, at the marine sediments were summarized.

• Ocean and Polar Research
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• 제25권spc3호
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• pp.373-384
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• 2003

When pile foundation is constructed by dynamic method, it is desirable to perform monitoring of drivability with pile penetration. Dynamic pile monitoring yields information regarding driving hammer, cushion, pile and soil behaviour that can be used to confirm the assumptions of wave equation analysis. In this study, dynamic monitoring of the steel pipe pile was performed with Pile Driving Analyser (PDA). The PDA utilizes the wave propagation theory to compute numerous variables which describe the conditions of the hammer-pile-soil system in real-time and following each hammer impact. This approach allows immediate field verification of hammer performance, driving efficiency, and estimation of pile bearing capacity. A series of PDA test were performed at the Ieodo Ocean Research Station (IORS) located in southeast of Marado, a southernmost small island south of Jeju Island. The drilling core sediments of Ieodo subsoil are composed of mud and sand, showing lamination and wavy or lenticular bedding, which were often bioturbated. This paper summarizes the results of PDA tests which were applied in measurement and estimation of large diameter open ended steel pipe pile driven by steam hammer, Vulcan-560 and MRBS-4600, at the marine sediments.