• Proceedings of the KSEG Conference
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• 2002.04a
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• pp.155-160
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• 2002

지구물리검층기법을 이용하여 시추공 내에서 수리상수를 결정을 위한 예비연구의 하나로 모형시추공을 이용한 전기전도도 검층기법의 적용을 시도하였다. 실험은 모형 시추공 내에 전기전도도가 다른 지층수를 유입, 유출시키면서 공내수의 전기전도도 변화를 모니터링하는 방법으로 이루어졌다. 실험 결과, 전기전도도 분포의 변화 양상은 단위 시간당 유량과, 공내수와 지층수의 전기전도도 차, 밀도 차에 의하여 크게 영향받는 것으로 나타났으며 모형 시추공 내에서의 전기도도 변화는 매우 일정한 경향을 보였다. 모형 시추공 내에서의 전기도도 변화는 유량의 변화와 매우 좋은 상관이 얻어졌으며 이로부터 투수계수 유도를 위한 모델 방정식이 유도될 수 있었다. 전기전도도검층 기법은 시추공 내에서의 투수계수를 구하는데 있어서 매우 효과적일 방법이 될 수 있는 것으로 나타났다.

• Proceedings of the KSEEG Conference
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• 1999.04a
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• pp.80-85
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• 1999

본 연구에서는 토목분야에서 중요한 문제가 되는 기초 파일의 깊이 탐지와 관련하여 시추공 자력탐사의 적용성을 확인하기 위하여 시추공 자력탐사 모형 반응 계산 및 역산 알고리즘을 개발하였다. 모형 반응 계산은 시추공 자력탐사에 적합하고 삼성분 이상을 계산할 수 있도록 기존의 방법을 수정하였으며, 역산 알고리즘은 일반적인 자력탐사 자료 역산의 불안정성을 고려하여 광역적 최적화 기법의 하나임 ASA(Adaptive Simulated Annealing : Ingber, 1993)를 이용하였다. 개발된 모형 반응 및 역산 알고리즘을 간단한 모형 및 합성자료에 대해 적용한 결과 그 타당성을 검증할 수 있었다. 또한 실제 현장에서 부딪힐 수 있는 무작위 잡음을 첨가한 자료, 주변 파일의 영향 및 지표 구조물에 의한 영향을 고려한 복잡한 모형에 대해 기초 파일의 깊이를 탐지해 낼 수 있었으며, 이를 토대로 실제 현장 적용시 고려해야할 현장지침에 대해서도 고찰할 수 있었다. 마지막으로 실제 현장자료에 적용한 결과 실제 파일의 깊이를 역산해 낼 수 있음을 확인함으로써, 기초 파일의 깊이 탐지를 위한 시추공 자력탐사의 적용성 및 본 알고리즘의 현장 적용성을 확인할 수 있었다.

• 한국지구물리탐사학회:학술대회논문집
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• 2005.09a
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• pp.73-82
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• 2005

We constructed a series of calibration models in the campus of Kangwon National University. A series of experiment for calibrating sonde response as well as casing effect in field measurement. Here we explained the process of construction of calibrating facility which consists of three model holes of different density and three model holes of different diameter. It was discussed the calibration equations obtained from its sonde response calibration test. A density correction chart for different separation of detector from hole wall was suggested, and verified the possibility of determining true density from measurements in cased hole.

• The Journal of Engineering Geology
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• v.13 no.3
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• pp.281-292
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• 2003

We setup a continuous measurement system for electrical conductivity of fluid in a model borehole and verified the basic environments in electrical conductivity measurement for estimating hydraulic constants. The experiment was made by monitoring the conductivity change within the hole using NaCI solution of different salinities and incoming formation fluid using distilled water. The experiment was made under the state of constant flow rate by maintaining balance between inflow and outflow. Conductivity variation features were observed by controlling salinity contrasts and temperature differences between fluid within the hole and incoming formation fluid. flow rate and the location of inlet and outlet. The results of the experiment show well the role of each affecting factor on the conductivity distribution. and suggest appropriate environments for conductivity measurements. It is considered that the basis of the conductivity measurement for henceforward laboratory model and/or in-situ borehole experiment has been prepared.

• The Journal of Engineering Geology
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• v.30 no.1
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• pp.17-30
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• 2020

An optical televiewer is a geophysical logging device that produces continuous high-resolution full-azimuth images of a borehole wall using a light-emitting-diode and a complementary metal-oxide semiconductor image sensor to provide valuable information on subsurface discontinuities. Recently, borehole imaging logging has been applied in many fields, including ground subsidence monitoring, rock mass integrity evaluation, stress-induced fracture detection, and glacial annual-layer measurements in polar regions. Widely used commercial borehole imaging logging systems typically have limitations depending on equipment specifications, meaning that it is necessary to clearly verify the scope of applications while maintaining appropriate quality control for various borehole conditions. However, it is difficult to directly check the accuracy, implementation, and reliability for outcomes, as images derived from an optical televiewer constitute in situ data. In this study, we designed and constructed a modular fractured borehole model having similar conditions to a borehole environment to report unprecedented results regarding reliable data acquisition and processing. We investigate sonde magnetometer accuracy, color realization, and fracture resolution, and suggest data processing methods to obtain accurate aperture measurements. The experiment involving the fractured borehole model should enhance not only measurement quality but also interpretations of high-resolution and reliable optical imaging logs.

• Journal of Soil and Groundwater Environment
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• v.8 no.1
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• pp.48-56
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• 2003

A geophysical conductivity logging technique has been adopted to determine hydraulic constants using a simplified physical model that depicts the borehole condition. An experiment has been made by monitoring the conductivity change within the model hole using borehole environment water and incoming-outgoing water of different salinity, under the state of constant flow rate by maintaining balance between inflow and outflow. Conductivity variation features were observed that depended on flow rate, salinity contrasts between fluid within the hole and incoming-outgoing fluid, and density contrasts between fluid conductivity within the hole and incoming fluid. The results of the experiment show the uniform change of fluid conductivity within the hole with time, a fairly good correlation between the flow rate and the conductivity change rate. The geophysical conductivity logging technique can be an efficient tool for determining hydraulic constants if the model equation is verified by henceforward experiments.

• Proceedings of the Korean Society for Rock Mechanics Conference
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• 2011.09a
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• pp.47-65
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• 2011

• Proceedings of the KSEG Conference
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• 2003.04a
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• pp.101-106
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• 2003

• Tunnel and Underground Space
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• v.4 no.3
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• pp.250-255
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• 1994

복잡한 지하구조인 지하터널과 핵폐기물 저장소 부지조사에 관한 자료해석을 위하여 지오토모그래피를 이용하였다. 지하터널의 조사는 지하저장소, 자원개발 및 군사적인 측면에서 많은 연구와 응용이 요구된다. 본 연구에서는 미육군이 현장에서 얻은 자료를 처리하고 이를 이론모형의 결과와 비교하였다. 또한 핵폐기물 부지 조사는 미국의 핵폐기물 저장소의 후보로 지정된 Yucca Mountain의 지질구조에 대한 이론모형계산을 행하였으며, Jaramillio(1993)가 모형실험치를 image 방법에 의하여 계산한 결과와 비교하였다. 탐사방법으로는 탄성파 시추공-시추공 방법과 VSP 방법을 사용하였다. 지오토모그래피의 기본이론은 터널과 지하공간 제3권 1호(1993)에서 설명되었다.

• Geophysics and Geophysical Exploration
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• v.15 no.4
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• pp.227-234
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• 2012

In this study, we make simulation of density log using a Monte Carlo N-Particle (MCNP) algorithm to make an analysis on density logging under different borehole environments, since density logging is affected by various borehole conditions like borehole size, density of borehole fluid, thickness and type of casing, and so on. MCNP algorithm has been widely used for simulation of problems of nuclear particle transportation. In the simulation, we consider the specific configuration of a tool (Robertson Geologging Co. Ltd) that Korea institute of geoscience and mineral resources (KIGAM) has used. In order to measure accurate bulk density of a formation, it is essential to make a calibration and correction chart for the tool under considerations. Through numerical simulation, this study makes calibration plot of the density tool in material with several known bulk densities and with boreholes of several different diameters. In order to make correction charts for the density logging, we simulate and analyze measurements of density logging under different borehole conditions by considering borehole size, density of borehole fluid, and presence of casing.