• Proceedings of the Korea Society for Energy Engineering kosee Conference
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• 1995.05a
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• pp.230-235
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• 1995

염-암모니아계 화학열펌프기술의 핵심인 전도성 블록의 특성파악을 위한 기초단계 연구로서 전도성 블록의 제조 및 기초물성분석에 관한 연구를 수행하였다. 황산이 함유된 천연흑연을 열처리하여 팽창흑연을 준비하고 특성을 분석하였다. 이 팽창흑연을 압축, 성형하여 흑연지지체를 제조하였으며, 성형된 지지체에 진공기법을 이용하여 염을 함침하고 건조과정을 거쳐 전도성 블록을 제조하였다. 전도성 블록의 특성분석으로서 염의 입자내에 분산정도는 EPMA/EDS, 기공율 및 기공크기 분포는 헬륨침투법과 수은 침투법, 기체투과도는 Darcy's law를 적용하고, 열전도도 측정은 전이 일차원 열류기법을 이용하였다. 전도성 블록이 암모니아와 반응 했을때 부피팽창을 관찰하였으며, 반응기에서 전도성블록의 온도분포를 관찰하였다. 본 연구에서 제조된 블록은 염이 균일하게 분산되어 있었으며 기공율은 제조조건에 따라 0.4 ∼ 0.83, 기체투과도는 0.01 ∼ 10 Darcy, 열전도도는 흑연지지체의 겉보기 밀도가 110 kg/㎥ 인 경우, 반지름방향의 열전도도, λr은 20 W/mK, 축방향의 열전도도, λa는 17 W/mK 이였다. 겉보기밀도가 150 kg/㎥ 인 경우, λr은 22 W/wK, λa는 20 W/wK 이였다. 전도성 블록의 부피팽창은 비가역적이었으며 대부분이 반지름 방향보다 축방향에서 팽창이 일어났다. 온도분포는 초기 반응의 kinetics가 내부온도를 지배하였으나, 시간이 경과후 반응기 내부온도는 외부열전달에 의해 지배되었다.

• Journal of the Korean Geophysical Society
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• v.1 no.1
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• pp.51-58
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• 1998

A numerical program has been developed to model 2-D resistivity responses for a pole-pole array configuration in cross-hole resistivity measurements. Apparent resistivity and secondary potential were computed using the program for a cylindrical inhomogeneity in an uniform host medium excited by a point source of current in a borehole. Surprisingly apparent resistivity in the receiver hole turns out to be lower than the one of surrounding medium regardless of the conductivity of cylindrical inhomogeneity. Using only cross-hole data, therefore, it is impossible to interpret the conductivity of inhomogeneity. To overcome this problem, 3-D measurement and interpretation are necessary. If 3-D data acquisition is impossible, inline data should be used to get the information about the conductivity of inhomogeneity.

• The Journal of Engineering Geology
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• v.12 no.1
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• pp.63-73
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• 2002

To evaluate reinforced region of dike by cement grouting, we investigated both the electrical resistivity and the strength of cement grout having various water-cement ratio with curing time. These investigation results showed that the electric conductivity of grout is much higher than that of water and that the apparent resistivity of grouted region is much lower than that of unoccupied region by grout. It was founded that electrical resistivity survey might be quite effective to detect grout region in dike. As the results of electrical resistivity sounding at three dikes, apparent resistivities after grouting showed several tens to several hundreds of ohm-m which were lower than those of pre-grouting and showed stabilizing trend with curing time. From these results, we could estimate that this behavior of apparent resistivity is due to increasing strength with curing time.

• Geophysics and Geophysical Exploration
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• v.5 no.2
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• pp.108-117
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• 2002

We have introduced a new approach to obtain the conductivity information of subsurface using Cagniard impedance over two-dimensional (2-D) model in the presence of horizontal magnetic dipole source with the frequency range of $1\;kHz\~1\;MHz$. Firstly, we designed the method to calculate the apparent resistivity from the ratio between horizontal electric and magnetic fields, Cagniard impedance, considering the source effects when the plane wave assumption is failed in finite source EM problem, and applied it to several numerical models such as homogeneous half-space or layered-earth model. It successfully provided subsurface information even though it is still rough, while the one with plane wave assumption is hard to give useful information. Next, through analyzing Cagniard impedance and apparent resistivity considering source effect over 2-D models containing conductive- or resistive-block, we showed that the possibility of obtaining conductivities of background media and anomaly using this approach. In addition, the apparent resistivity considering source effect and phase pseudosections constructed from Cagniard impedance over the isolated conductive- and resistive block model well demonstrated outlines of anomalies and conductivity distribution even though there were some distortions came from sidelobes caused by 2-D body.

• 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.9 no.1
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• pp.114-120
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• 2006

The main purpose of this study is to apply spatial analysis using semivariograms to small-loop electromagnetic survey data to assess the extent of seawater intrusion in an experimental watershed. To indicate the extent of seawater intrusion over the study area, vertical electrical soundings at 33 points and electrical conductivity logging in two wells were conducted. From the correlation between resistivities obtained by inversion and the depth of the aquifer at the two wells, the region of seawater intrusion was identified and demonstrated by electrical conductivity logging results obtained over two years. To measure the variation of apparent conductivity with depth, an electromagnetic survey in six frequency bands was adopted. Apparent conductivity mapping with spatial analysis using semivariograms is an effective technique for identifying the region of seawater intrusion at shallow depth.

• Geophysics and Geophysical Exploration
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• v.6 no.3
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• pp.119-125
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• 2003

The small-loop electromagnetic (EM) technique has been used successfully for many geophysical investigations, particularly for shallow engineering and environmental surveys. In conventional small loop EM operating at small induction numbers, geometric sounding has been widely used because the depth of penetration of EM energy depends only on the source-receiver separation. Recently developed small loop EM system, however, measures the secondary magnetic field, $H^S$, at multiple frequencies with a fixed source-receiver separation and frequency sounding is tried actively. In this study, we analyzed the behavior of in-phase and quadrature components of ${H^S}_z$, for horizonal coplanar (HCP) configuration over two-layer models. Through this theoretical analysis, it was found that the in-phase component of ${H^S}_z$ is more suitable for frequency sounding than the quadrature component. But, the in-phase component of ${H^S}_z$ is too small to measure, especially in resistive and noisy environment like Korea. Using the fact that the quadrature component is much greater than the in-phase component and the difference of quadrature component of ${H^S}_z$ measured at two frequencies shows the same behavoir as the in-phase component, we suggested an alternative frequency sounding technique. Also, we defined an apparent conductivity, which reflects well the conductivity of subsurface layers.

• Journal of Energy Engineering
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• v.3 no.1
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• pp.44-53
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• 1994

STELF 기술의 핵심의 되는 IMPEX 블록의 잔류 공급률, 겉보기 밀도, 흑연의 혼합비 등 여러 가지 주요 변수가 블록의 특성에 미치는 영향을 조사하여 실제 반응기를 설계하는데 필요한 자료를 구하였다. 대표적인 염들에 대하여 물질전달 및 열전달 문제를 일으키지 않는 영역에서 최소의 부피를 갖는 값들을 계산하였고, 각각의 물질이 갖는 특정 전도도에서의 최대 냉방 및 난방 에너지 밀도를 계산하였다. 이로부터 얻은 값들을 8시간 동안 사용할 수 있는 6kW 냉방용 반응기 설계에 적용하여 본 결과 SrCL2-8/1 NH3가 최적의 염임을 확인하였다.

• 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.

• 한국지구물리탐사학회:학술대회논문집
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• 2006.06a
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• pp.83-86
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• 2006

From numerical modeling test $-{\rho}a$ by one steel casing borehole near resistivity survey line can be acquired. Negative apparent resistivities even in the flat area are surely subsurface information. Inversion technique for those need to be developed in the near future.