• Tunnel and Underground Space
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• v.17 no.6
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• pp.493-502
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• 2007

Measurements of hydraulic conductivity are point or interval values, and are highly limited in their number. Meanwhile, results of geophysical prospecting can provide the information of spatial variation of geology, and abundant in number. In this study, it was aimed to develop a data integration tool for constructing a hydraulic conductivity map by integrating geophysical data and hydraulic conductivity measurements. The developed code employed a geostatistical optimization method, simulated annealing (SA), and consists of 4 distinct computation modules by which from exploratory data analysis to postprocessing of the simulation were processed. All these modules are equipped with Graphical User Interface (GUI). Validation of the developed code was evaluated in-situ in characterizing hydraulic characteristics of highly permeable fractured zone.

• 한국지구과학회:학술대회논문집
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• 2005.09a
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• pp.93-102
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• 2005

변산반도 서부 해안지역의 소규모 유역에 대하여 대수층을 통한 해수침투의 범위를 공간적으로 규명하기 위하여, 시추자료를 포함한 전기비저항 탐사와 지하수의 수질분석을 실시하였다. 전기비저항 탐사는 다층 구조로 되어있는 대수층 내 지하수의 수질변화 특성을 효과적으로 탐지해 낼 수 있는 수직탐사법을 이용하였으며, 탐사결과 겉보기비저항 곡선은 H type에 해당함을 알았다. 시추에 의해 3층 구조로 밝혀진 연구지역에 대하여 총 30 지점에 대한 H type 수직탐사 자료의 1차원 역산결과, 중간층과 상/하부층의 비저항 크기 차이가 크게 나타남에 따라 이 연구에서는 고전도도 지역, 중간지역, 저전도도지역 등 3가지의 영역으로 구분하였다. 15개 지점의 천부 지하수 관정에서 채취된 지하수 시료 분석결과를 TDS에 대한 HCO3/Cl과 Ca/Na 몰비로 도시하였는데, 그래프의 기울기에 따라 크게 2가지 그룹으로 구분되었다. 수직탐사의 3가지 영역과 지하수 수질 분석에 의한 2가지 그룹을 비교한 결과 낮은 농도의 HCO3/Cl과 Ca/Na를 나타내는 관정은 고전도도 지역에 위치하며, 높은 농도의 HCO3/Cl과 Ca/Na를 나타내는 관정은 저전도도 지역에 위치하는 것으로 나타났다. 따라서 이 연구에서 제시한 바와 같이 전기비저항 수직탐사 결과와 지하수 수질분석 결과를 복합 해석하는 경우 시추자료가 제한적인 해안지역 대수층을 통한 해수침투 범위를 효과적으로 규명할 수 있는 것으로 밝혀졌다.

• Geophysics and Geophysical Exploration
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• v.2 no.3
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• pp.142-148
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• 1999

Three-dimensional electromagnetic modeling algorithm in homogeneous half-space was developed using the extended Born approximation to an electric field integral equation. To examine the performance of the extended Born approximation algorithm, the results were compared with those of the full integral equation results. For a crosshole source-receiver configuration, the agreement between the integral equation and the extended Born approximation was remarkable when the source frequency is lower than 20 kHz and conductivity contrast lower than 1:10. Beyond this conductivity contrast, the simulated results by the extended Born approximation exhibit a difference with respect to those by the integral equation. Therefore, the limit of accuracy lies below contrast of 1:10 in the extended Born approximation. Since for the source frequency range from 20 kHz to 100 kHz, however, the difference is relatively small, the extended Born approximation could be used for a reasonable 3-D EM modeling algorithm.

• Composites Research
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• v.34 no.5
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• pp.290-295
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• 2021

The application of lightweight structural composites to automobiles as a solution in line with global fuel economy regulations to curb global warming is recognized as a megatrend. This study was conducted to provide a technical approach that can respond to the issue of replacing parts that require conductive properties to maximize the application of thermoplastic carbon fiber reinforced plastics (CFRPs), which are advantageous in terms of repair, disposal and recycling. By utilizing the properties of the low-viscosity polymerizable oligomer matrix, it was possible to prepare a thermoplastic CFRP exhibiting excellent impregnation properties while uniformly mixing the conductive filler. Various carbon-based conductive fillers such as carbon black, carbon nanotubes, graphene nanoplatelets, graphite, and pitch-based carbon fibers were filled up to the maximum content, and electrical and thermal conductive properties of the fabricated composites were compared and studied. It was confirmed that the maximum incorporation of filler was the most important factor to control the conductive properties of the composites rather than the type or shape of the conductive carbon filler. Experimental results were observed in which it might be advantageous to apply a one-dimensional conductive carbon filler to improve electrical conductivity, whereas it might be advantageous to apply a two-dimensional conductive carbon filler to improve thermal conductivity. The results of this study can provide potential insight into the optimization of structural design for controlling the conductive properties of thermoplastic CFRPs.

• Journal of the Korean earth science society
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• v.24 no.5
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• pp.440-448
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• 2003

We have performed 3-D geomagnetic induction Modeling considering with anomalous conductive structures to interpret the conductive anomaly proposed by previous studies on the Korean Peninsula. The results of modeling coincide well with the observed induction arrow. we confirm the fact that Imjin River Belt and Ogcheon Belt presumed in the model are reasonable. In the western-middle area of the peninsula (YIN, ICHN) the induction arrows seem to reflect the existence for the Imjin River Belt and the induction arrows in western-south area (HNS, CHY, DZN, MWN) is likely to reflect the effect of the Ogcheon Belt. The difference arrows, calculated by subtracting the sea effect from observed induction arrow in the western area of the peninsula at the period of 60-minutes, show little difference with the observed induction arrows. Especially, the difference arrows in YIN, ICHN also show a similar pattern to those at the periods longer than 10-minutes. These results strongly suggest that the Imjin River Belt and the Ogcheon Belt extend down to the deep part of the crust in spite of the limitation of our model.

• Geophysics and Geophysical Exploration
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• v.7 no.2
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• pp.136-147
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• 2004

In this study, the characteristics of magnetotelluric (MT) responses due to a three-dimensional (3-D) body are analyzed with 3-D numerical modeling. The first model for the analysis consists of a single isolated conductive body embedded in a resistive homogeneous half-space. The second model has an additional conductive overburden while the other conditions remain the same as the first one. The analysis of apparent resistivities shows well that the 3-D effects are dominant over some frequency range for the first model. Two mechanisms, current channeling and induction, for secondary electric fields due to the conductive body are analyzed at various frequencies: at high frequencies induction is more dominant than channeling, while at low frequencies channeling is more dominant than induction. Tippers have a strong relation to the position of anomalous body and the real and imaginary parts of induction vector also indicate the position of anomalous body. off-line conductive anomaly sometimes causes severe problem in 2-D interpretation. In such case, induction vector analysis can give information on the existence and location of the anomalous body. Each parameter of the second model shows similar responses as those of the first model. The only difference is that the magnitude of all parameters is decreased and that the domain showing the 3-D effects becomes narrower. As shown in this study, the analysis of 3-D effects provides a useful and effective means to understand the 3-D subsurface structure and to interpret MT survey data.

• Geophysics and Geophysical Exploration
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• v.5 no.4
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• pp.309-315
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• 2002

Conventional electromagnetic (EM) method using small loops as a source and receiver has been used in detection of conductive buried objects like a metal detector or in qualitative estimation of the subsurface conductivity variation. Recently, however, since detection of buried objects and imaging of the subsurface conductivity distribution in a relatively conductive area are in a high demand for environmental and engineering purposes, the quantitative interpretation technique of EM data is actively studied. In this regard, we introduce a brief principle of EM survey and show an example of the detection of buried conductive material and imaging of the subsurface conductivity distribution based on data measured at a test survey area. Through this study, we show that multi-frequency EM surveys using small loops may be a good solution to give quick and detail information of subsurface in a conductive survey area.

• Tunnel and Underground Space
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• v.15 no.2 s.55
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• pp.145-156
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• 2005

MODFLOW, 3-D finite difference code, is widely used to model groundwater flow and has been used to assess the effect of excavations on the groundwater system due to construction of subways and mountain tunnels. The results of numerical analysis depend on boundary conditions, initial conditions, conceptual models and hydrogeological properties. Therefore, its accuracy can only be enhanced using more realistic and field oriented input parameters. In this study, SA(simulated annealing) was used to integrate hydraulic conductivities from a few of injection tests with geophysical reference images. The realizations of hydraulic conductivity random field are obtained and then groundwater flows in each geostatistically equivalent media are analyzed with a numerical simulation. This approach can give probabilistic results of groundwater flow modeling considering the uncertainty of hydrogeological medium. In other words, this approach makes it possible to quantify the propagation of uncertainty of hydraulic conductivities into groundwater flow.

• Geophysics and Geophysical Exploration
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• v.10 no.1
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• pp.50-59
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• 2007

The advent of towed geo-electrical array surveying on water and land has resulted in datasets of magnitude approaching that of airborne electromagnetic surveying and most suited to 1D inversion. Robustness and complete automation is essential if processing and reliable interpretation of such data is to be viable. Sharp boundaries such as river beds and the top of saline aquifers must be resolved so use of smoothness constraints must be minimised. Suitable inversion algorithms must intelligently handle low signal-to-noise ratio data if conductive basement, that attenuates signal, is not to be misrepresented. A noise-level aware inversion algorithm that operates with one elastic thickness layer per electrode configuration has been coded. The noise-level aware inversion identifies if conductive basement has attenuated signal levels so that they are below noise level, and models conductive basement where appropriate. Layers in the initial models are distributed to span the effective depths of each of the geo-electric array quadrupoles. The algorithm works optimally on data collected using geo-electric arrays with an approximately exponential distribution of quadrupole effective depths. Inversion of data from arrays with linear electrodes, used to reduce contact resistance, and capacitive-line antennae is plausible. This paper demonstrates the effectiveness of the algorithm using theoretical examples and an example from a salt interception scheme on the Murray River, Australia.

• The Bulletin of The Korean Astronomical Society
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• v.37 no.2
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• pp.195.2-195.2
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• 2012

궤도상에서 지구의 대기는 태양의 복사에너지에 의하여 양이온과 음이온으로 이온화된 자유 전자로 존재하게 되는데 이러한 상태를 플라즈마 환경이라고 부른다. 인공위성이 궤도에서 운용될 때, 플라즈마 환경에서의 강한 에너지를 가진 전하들은 위성을 투과하여 위성 내부에 축적될 수 있다. 이러한 전하들은 고립되어 있는 전도체의 끝에 모이게 되고, 전하량이 breakdown 레벨에 이르게 되면 아크 방전이 일어나게 된다. 방전에 의한 전류가 민감한 회로에 들어가게 되면 오동작이나 기능손상을 일으킬 수 있다. 보통 저궤도 위성이 놓이게 되는 낮은 고도와 경사각에서 플라즈마는 밀도가 높고 낮은 에너지를 가지는 반면, 정지궤도 위성이 놓이게 되는 높은 고도의 플라즈마는 낮은 밀도와 지구자기 폭풍 등에 기인하여 높은 에너지를 갖는다. 따라서 정지궤도 인공위성의 경우 ESD의 영향을 좀 더 면밀하게 검토하고 검증할 필요가 있다. 본 논문에서는 정지궤도 위성용 ESD 시험장비의 개발결과에 대하여 논의한다. 시험장비는 ESD 건과 Spark gap, 몇몇의 저항 및 캐패시터로 구성된다. 정지궤도 상에서의 ESD 방전 전류를 모사하는 파형을 구현하기 위한 방법과 결과를 소개하였다.