• 자원환경지질
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• 제13권3호
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• pp.159-166
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• 1980

A model study was conducted for the investigation of apparent resistivity variation along with electric resistivity variation of host rock and dip variation of bed. Experiments were carried out for the cases of horizontal and dipping beds in a water tank by using Wenner and Schlumberger arrays and by changing salinity of water. The ratios of resistivity values of the bed to that of brine were 1 : 10, 1 : 50, 1 : 100 and 1 : 500. Natural coally-shale of $55cm{\times}35cm{\times}3.5cm$ was used as a bed for experimental model, and brine as a host rock. Equi-resistivity curves and characteristic curves were obtained for each case of the experiment. The equi-resistivity curve was drawn both on the cross section parallel to strike of bed and longitudinal section perpendicular to it. The characteristic curve was drawn on the cross section. In the case of dipping bed of different dips, the curves are parallel to the boundary of the bed in the upper part of the bed, and are inclined to the opposite direction with the same angle of the dip of bed in the lower part. We can deduce, from the equi-resistivity curves, the location, shape and dip of the bed. It is shown in the characteristic curves that when the ratio of resistivity value of bed to that of host rock increases, the slope of curves becomes steeper, location of low-resistivity zone lower, and the width of it narrower. The slope of curves also becomes steeper when dip of bed increases. We can deduce, from the characteristic curves, the ratio of resistivity values between adjacent beds. It was found out from the experiments that electric resistivity method could be applicable to prospecting for underground geology with an electric resistivity contrast of 1 : 10. This fact strongly suggests that distinction of coal from coally-shale could be possible in a certain field condition.

• 지질공학
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• 제12권1호
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• pp.23-34
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• 2002

시추공 영상조사는 지하 구조를 직접 확인함으로서 좀더 정확한 자료를 얻기 위하여 실시되고 있으나, 시추공 좁은 공간내에 국한된 정보이기 때문에 원하는 공간범위의 지하 구조물에 직접적으로 적용하기 어려운 실정이다. 이에 시추공 영상 자료를 처리하고, 방향에 따른 위경사를 고려하여, 2차원의 지하 불연속면을 원하는 단면의 방향에따라 가시화하는 프로그램을 개발하고, 지하 불연속면의 분포를 넓은 공간에 확장하여 현장에 적용함으로서 시추공 영상분석을 보완하였다. 이와 관련된 프로그림이 별도로 판매되어 일부에서 사용되고 있으나, 내용이 알려지지 않았고 일반인이 사용하는데에 제한이 있었으므로 이번 기회에 희망자들이 쉽게 사용할 수 있게 될 것이다. 지하 구조물이 계획된 지역의 지하단면을 작성하기 위하여 포트란과 비쥬얼배직 프로그래밍 언어를 사용하여 Window GUI(Graphic User Interface) 환경으로 프로그램을 제작하였고 이 프로그램을 이용하여 전라북도 장수군 계남면 장계리 지역 터널계획 구간의 불연속면 분포도를 작성하였다. 시추공내에 국한된 불연속면을 가시화 프로그램을 이용하여 공간적으로 확장함으로서 부근 전체의 지하구조를 파악하며, 다른 지점에서의 불연속면의 분포 형태를 추측할 수 있었다. 또한 터널에 영향을 미치는 불연속면의 절리간극의 크기 범위와 불연속면들의 출현 심도 및 영향 범위 등을 계획된 터널의 방향에 따라 가시화하여 설계와 시공에 쉽게 이용하게 하였다.

• 한국안전학회지
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• 제12권4호
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• pp.79-85
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• 1997

In order to improve the surface characteristics of polymethylmethacrylate(PMMA), oxide thin film coatings were applied using the sol-gel dip-coating technique. The $Si(OC_2H_5)_4$, tetra-ethyl-ortho-silicate(TEOS) was used as a starting material for $SiO_2$ coating. The hardness of the alkoxy-derived oxide-coated PMMA was increased from 190 MPa for non-coated PMMA with increasing film thickness. By optimizing the heating conditions and the hydrolysis conditions, a maximum apparent hardness obtained In the present study was achieved 310 MPa using the withdrawal velocity of 5cm/min and heat treatment at $90^{\circ}C$ for 5 hours, which is about 1.6 times larger than that of uncoated PMMA.

• 자원환경지질
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• 제13권3호
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• pp.141-158
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• 1980

A geologic structure could be formed through various processes, because there are a number of factors which control the deformation of the Earth's crust. In geology, we could call it geological epistemology to describe exactly a geologic structure, and call it geological logics to infer logically the deforming process through which the geologic structure had been formed. Degree of legitimacy of geological logics depends upon the degree of exactness of geological epistemology. This study described quantitatively 3-dimensional Hambaek Syncline through computer analysis, and examined qualitatively into its deforming mechanism based on the results of 3-dimensional analysis of the structure. Input data for the computer analysis are dips and dip directions of bedding planes of the structure. The Hambaek Syncline disclose a minor fold group of NE-SW or NNE-SSW trend and a large scale fold of E-W trend. The conclusions of this study are as follows: (1) The fold of E-W trend is primary fold $(F_1)$ and the minor fold group of NE-SW or NNE-SSW trend secondary fold $(F_2)$. (2) Hambaek Syncline is cylindrical type fold. (3) Apparent axial trace of Hambaek syncline does not coincide with true axial trace. The apparent axial trace is $N70^{\circ}-80^{\circ}W$ in Gohan and Sabuk area, and changes to $N70^{\circ}-80^{\circ}E$ in the westward of the area, while the true axial trace is $N40^{\circ}-70^{\circ}W$ in the former, and $N60^{\circ}-80^{\circ}E$ in the latter area. (4) Westward dipping of axial plane of the minor fold group of NE-SW or NNE-SSW trend can be attributed to simple shear movements along overthrusts. (5) Angle between axial trace and the directional trace of the maximum principal compressive stress $({\sigma}_1)$ may not be perpendicular each other. The angle between them is governed by the following factors; 1) the plunge of fold axis 2) the dip of axial surface 3) cylindrisity (6) The mean axial trace of Hambaek Syncline $(F_1)$ is $N45.6^{\circ}W$, and the directional trace of ${\sigma}_1$ is $N52.4^{\circ}E$ (7) The mean axial trace of the minor fold group of NE-SW or NNE-SSW trend $(F_2)$ is $N21^{\circ}E$, and the directional trace of ${\sigma}_1$ is $N22^{\circ}W$.

• 한국식물병리학회지
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• 제2권1호
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• pp.1-11
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• 1986

Dip-method에 의한 전자현미경적 관찰의 결과, 사철나무 이병엽에서 길이 230-280nm, 폭 70-80nm의 단간형(일단이 둥근 탄환형 : bullef-shaped, 양단이 둥근 간균형 : bacilliform)의 바이러스 입자가 다수 검출되었다. 이 바이러스 입자를 사철나무 엽맥황화 바이러스(Euonymus vein clear virus : EVCV)로 명명하였다. EVCV는 피막(두께 8-10nm)을 갖고 있고, 이 피막의 표면에는 5-6nm의 염주모양의 돌기가 있다. 핵단백(nucleocapsid)은 길이 200-220nm, 폭 50-55nm의 나선구조를 갖고 있다. 바이러스 입자는 절편시료의 각종세포의 세포질내 또는 핵내와 핵막간극내에 산재 혹은 집단으로 관찰되었다. 이들 바이러스 입자의 인체는 핵막으로 둘러싸여 있었다. 대부분의 절편상에서는 바이러스 입자의 집단이 핵막의 내막과 외막 사이의 간극에서 관찰되었는데, 이것은 바이러스 입자의 성숙장을 시사하고 있는 것으로 생각된다. 어떤 절편상에서는 바이러스 입자의 피막이 핵막의 내막과 연결되어 있는 것도 관찰되어, 이 피막이 핵막의 내막으로부터 유래된 것으로 시사되었다.

• 자원환경지질
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• 제21권2호
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• pp.131-137
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• 1988

Geological and electrical resistivity surveys were carried out to investigate subsurface geology and geologic structure of the Bonghwajae area in the Okchon zone. Pseudosections of the apparent electrical resistivity distribution along the three survey lines were obtained by using dipole-dipole electrode array method, and models of subsurface geology and geologic structure by using two dimensional finite difference method. The Bonghwajae fault zone exists around Bonghwajae area in the north-south direction, and is a boundary between Okchon Group and Choson Supper Group. Metabasite and hornblende gabbro intruded along the Bonghwajae fault zone remaining two fracture zones with low resistivity value of 20 ohm-m and widths of about 100m and 70-300m. They strike nearly N-S and dip westward with a high angle of $60-70^{\circ}$. Sochangri fault with a width of about 160m exists between Jisogori and Bonghwajae, by which Bonghwajae fault zone is displaced about 1km in the east-west direction. Hornblende gabbro whose electrical resistivity value is in the range of 5000-8000 ohm-m intruded the metabasite of 2000-4500 ohm-m after the Sochangri fault had formed. Great Limestone Group is widely distributed in the east of Bonghwajae fault zone, and interbeds so called Yongam formation of graphitic black slate with an extremely low electrical resistivity value of 2 ohm-m.

• 한국터널지하공간학회 논문집
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• 제3권2호
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• pp.3-12
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• 2001

본 논문은 절리암반 터널의 안정성 해석을 위한 2차원 개별요소모델링방법에 대한 개선방안을 제안하였다. 먼저, 절리군과 터널의 상대방위를 고려하여 터널단면상에서 불연속거동이 가능한 절리군을 구별하는 기준을 제시하였다. 이 기준에 따라 불연속거동이 가능한 절리군은 개별요소(암석블록)의 변이 되도록 하고 그 외 절리군은 암석블록의 탄성특성을 보정하는 방법을 제시하였다. 또한, 주어진 절리의 기하학적 특성에 대해서 절리의 방위편차와 유한길이를 고려한 복잡한 모델과 절리의 평균방위와 무한길이를 고려한 단순한 모델의 특성을 분석하였다. 그 결과, 후자의 모델이 일관성 있는 터널의 국부적 파괴양상과 명료한 암반의 불연속거동을 보여줌으로써 터널설계목적에 적절함을 확인하였다.

• Geomechanics and Engineering
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• 제27권6호
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• pp.605-614
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• 2021

Water inrush from fault is one of the most severe hazards during tunnel excavation. However, the traditional evaluation methods are deficient in both quantitative evaluation and uncertainty handling. In this paper, a comprehensive methodology method combined intuitionistic fuzzy AHP with a Bayesian network for the risk assessment of water inrush from fault in the subsea tunnel was proposed. Through the intuitionistic fuzzy analytic hierarchy process to replace the traditional expert scoring method to determine the prior probability of the node in the Bayesian network. After the field data is normalized, it is classified according to the data range. Then, using obtained results into the Bayesian network, conduct a risk assessment with field data which have processed of water inrush disaster on the tunnel. Simultaneously, a sensitivity analysis technique was utilized to investigate each factor's contribution rate to determine the most critical factor affecting tunnel water inrush risk. Taking Qingdao Kiaochow Bay Tunnel as an example, by predictive analysis of fifteen fault zones, thirteen of them are consistent with the actual situation which shows that the IFAHP-Bayesian Network method is feasible and applicable. Through sensitivity analysis, it is shown that the Fissure development and Apparent resistivity are more critical comparing than other factor especially the Permeability coefficient and Fault dip. The method can provide planners and engineers with adequate decision-making support, which is vital to prevent and control tunnel water inrush.