• 한국원자력학회:학술대회논문집
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• 한국원자력학회 2002년도 춘계공동학술발표회요약집
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• pp.277.1-277
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• 2002

• 한국지반환경공학회 논문집
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• 제4권2호
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• pp.5-13
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• 2003

국내의 경우 암반에 근입된 현장타설말뚝의 지지력을 계산하는데 있어 일축압축강도를 이용하는 경험적인 방법으로 설계를 수행하고 있다. 이러한 경험적인 설계방법들은 설계시 상당한 불확실성을 내포하는 것으로 나타났다. 최근에는 암반에 근입된 현장타설말뚝의 주면저항에 영향을 주는 모든 인자를 고려하는 설계법도 제안되었다. 암반에 근입된 현장타설말뚝의 지지력에 영향을 미치는 인자에는 여러 가지가 있는데 이중 굴착면의 거칠기는 암반에 근입된 말뚝의 전단거동에 중요한 역할을 하는 것으로 알려졌다. 따라서 본 연구에서는 국내 현장타설말뚝의 암반부 굴착벽면의 거칠기 특성을 조사, 분석하여 설계에 적용할 수 있는 거칠기 정수를 제안하였다.

• 문화기술의 융합
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• 제6권2호
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• pp.467-472
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• 2020

일반적인 보통 등급의 지반(ground) 상 구조물의 안정성 확보를 위한 설계입력정수(input-parameters) 도출방법들은 보편적으로 잘 알려져 있다. 연구지역과 같은 습곡된(folded) 변성암(metamorphic rocks) 지반은 엽리가(foliation) 촘촘히 발달해 있고, 엽리에 평행한 소규모 단층들(faults)이 분포하고 있어 설계입력정수 도출을 위한 특별한 조사방법 및 시험, 등이 요구된다. 수 mm 간격의 엽리가 발달한 변성암 지반은 엽리면 직접전단강도시험(direct shear test), 엽리의 배향(strike/dip)과 맵핑(mapping), 엽리의 지하 연속성 파악을 위한 시추조사, 변성암반의 암반분류(rock mass rating), 등이 필요하다. 특정 엽리면을 따라 발달한 소규모의 엽리평행단층(foliation-parallel faults)이 다수 발달한 지반은 선구조선 분석, 단층 추적을 위한 지표지질맵핑, 단층면 직접전단강도시험, 등이 필수적이다. 습곡지반은 지질구조구(structural domain) 분석, 불연속면의 평사투영(stereonet)해석, 습곡축을 따른 전기비저항탐사, 등의 추가조사로 설계입력정수 도출이 합리적이다.

• 한국측량학회지
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• 제22권3호
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• pp.233-244
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• 2004

최근 건설 분야를 비롯한 여러 산업분야에서 대상물에 대한 사실적인 표현이 가능한 3차원 수치영상에 대한 관심이 크게 증가하고 있다. 본 연구에서는 수치사진측량기법을 기반으로 3차원 수치영상 생성시스템을 개발하고 이를 이용하여 대상물에 대한 3차원 수치영상을 시범적으로 생성하였다. 그리고 3차원 수치정보의 획득을 위해 최근에 많이 활용되는 수치사진측량시스템에 의한 처리결과와 비교 분석을 통해 3차원 수치영상의 활용 가능성을 도출하고자 하였다. 또한 3차원 수치영상의 적용가능성을 점검하기 위해 암반사면의 불연속면 조사에 적용하였다. 연구결과, 본 연구에서 개발한 3차원 수치영상생성 시스템을 이용하여 대상물에 대한 3차원 수치영상을 효율적으로 생성할 수 있었으며, 암반사면에 대한 지표정보를 효과적으로 획득할 수 있었다.

• Geomechanics and Engineering
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• 제36권2호
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• pp.131-143
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• 2024

Shield tunneling construction commonly crosses underground pipelines in urban areas, resulting in soil loss and followed deformation of grounds and pipelines nearby, which may threaten the safe operation of shield tunneling. This paper investigated the pipeline deformation caused by double curved shield tunnels in soil-rock composite stratum in Nanjing, China. The stratum settlement equation was modified to consider the double shield tunneling. Moreover, a three dimensional finite element model was established to explore the effects of hard-layer ratio, tunnel curvature radius, pipeline buried depth and other influencing factors. The results indicate the subsequent shield tunnel would cause secondary disturbance to the soil around the preceding tunnel, resulting in increased pipeline and ground surface settlement above the preceding tunnel. The settlement and stress of the pipeline increased gradually as buried depth of the pipeline increased or the hard-layer ratio (the ratio of hard-rock layer thickness to shield tunnel diameter within the range of the tunnel face) decreased. The modified settlement calculation equation was consistent with the measured data, which can be applied to the settlement calculation of ground surface and pipeline settlement. The modified coefficients a and b ranged from 0.45 to 0.95 and 0.90 to 1.25, respectively. Moreover, the hard-layer ratio had the most significant influence on the pipeline settlement, but the tunnel curvature radius and the included angle between pipeline and tunnel axis played a dominant role in the scope of the pipeline settlement deformation.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 1999년도 봄 학술발표회 논문집
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• pp.277-284
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• 1999

This study describes the influence factors related to slope failure pattern and dimension in the southern Kyounggi area. Intrusive and metamorphic rocks are distributed in the study area. Geological condition, rainfall property and slope geometry are influence on slope failure characteristics in the study we& Geological factors related to slope failure are rock type, geological structure and weathering condition. Because of deep soil (RS-CW) depth of granite region, circular failure type is major failure pattern in granite region. Almost granite slopes with circular or surface failure pattern are failed during heavy rainfall season. But typical wedge failure type related to geological structure factor is a main failure pattern of metamorphic rock slope. Additionally failure dimension is influenced by geological factors and several factors, i.e. natural slope condition, failure type, rainfall intensity and etc. failure height/width ratio and thickness/length ratio of granite slope are 0.88 and 0.23. But the ratios of metamorphic rock slope are 1.36 and 0.19.

• 터널과지하공간
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• 제7권3호
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• pp.208-220
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• 1997

To asses the stability of structure around shaft during the excavation of -300 ml hopper room at 2nd shaft in Jangsung mine, some measurements were made with blast monitoring, stressmeter, extensometer and inclinometers. Instrumentations proved to be reliable and data were montiored over six month period. Stressmeters were set at the points of wall and arch of inset gang(level). Induced stresses were measured with the magnitude of 2.81 kgf/$\textrm{cm}^2$(tensile stress) and -4.45kgf/$\textrm{cm}^2$(compressive stress) respectively. These values were converged after two months. The magnitude of axial force in rock bolt was measured with 1.98 ton between the points of M2(2.25m) and M3(1.5 m) but this value was assumed within allowable level. Maximum displacement was also measured with 2 mm at the dephs of 12m from surface. But this value belongs within guide level.

• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2006년도 추계학술대회
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• pp.28-31
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• 2006

It is require to construct geothermal database to develop geothermal energy as renewable energy policy. It must be consist of geologic data, borehole data and geophysical data for geothermal database. In aspect of geology, there are included the distribution of geology, structural geology, geological time, rock name, density of rock, porosity, thermal diffusivity, specific capacity and thermal conductivity In order to calculate the heat general ion, it is needed to analysis the radioactivity elements as U, Th and K of rock. In aspect of borehole data, there are included temperature of depth, surface temperature and geothermal gradient And also there is geotherrnornetry using chemical components of groundwater as Na Ca, K and $SiO_2$. In aspect of geophysical data, there are some thematic map as booger gravity anomaly data and magnetic survey data and etc. In addition, it is important to descript the distribution of hot spring and water temperature.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2008년도 춘계 학술발표회 초청강연 및 논문집
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• pp.1344-1350
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• 2008

The slope surface at a linking road construction from a geological stratum situation and a spot investigation weathering about the base rock. We became formation the slope to very disadvantageous base rock. A stability review result confirmed report of the slope were difficult and presented the stability countermeasure. We executed the slope to the purpose to augment safely.

• Applied Microscopy
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• 제17권1호
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• pp.1-15
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• 1987

Testes from the allied rock wallaby(Petrogale assimilus) have been examined by the electron microscopy in thin sections in order to examine spermiogenesis and structure of spermatozoa. The spermiogenesis can be divided into nine stages: early Golgi, late Golgi, collapsing, nuclear protrusion, condensation and flattening, nuclear shaping, rotation, nuclear ring contraction, and maturation. The acrosome has been abruptly formed following the collapse of expanded acrosomal vesicle without the cap stage described in the eutheria. The flatly condensed nucleus rotates obliquely to the axis of the axial filament complex and the folded acrosome covers the anterior third of the dorsal nuclear surface forming a wide subacrosormal space as the nuclear ring has contracted. The Sertoli cell reaction and spur are prominent during the nuclear protrusion and rotation stages. A mature spermatozoon has S-shape head which has an extended part reaching to the vicinity of the middle piece.