• Title/Summary/Keyword: 전기비저항 배열

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A Study on the Leachate Distribution of the Mooreung Landfill Site with Electrical Resistivity Surveys (전기비저항 탐사를 이용한 충주 무릉매립장 침출수 분포에 관한 연구)

  • Kim, Jun-Kyoung
    • The Journal of Engineering Geology
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    • v.16 no.4 s.50
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    • pp.455-463
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    • 2006
  • The electrical resistivity prospecting method with dipole-dipole array was applied to the Mooreung landfill site in order to survey the existence of leachate around the landfill site. Moreover, if there is leachate within Mooreung landfill site, the analysis of potential pathways to exterior environments was tried. Within the landfill site, the over-all characteristics of the electrical resistivity anomalies suggest that the leachate induced from the landfill materials has infiltrated the basement rock and fill the pores of basement rock in some parts of the landfill site. The consistency of the anomaly locations (left part of each survey line), anomaly geometries, and absolute resistivity value of anomaly through the 3 survey lines suggests that the resistivity anomaly be connected from the upstream to the downstream and correspond to the leachate material. Finally, the result from the electrical resistivity survey line near the gateway of the landfill site suggests that some of the leachate induced from landfill material leaks to the exterior groundwater system. It is necessary that more surveys using both geochemical and geophysical methods should be performed to find out potential pathways and depths of the leachate more precisely.

Application of Gold Exploration Using Three-dimensional Resistivity Inversion in Sambo mine (3차원 전기비저항 역산 방법을 이용한 삼보 광산에서 금광 탐사)

  • Park Jong-Oh;Kim Hee-Joon;Song Moo-Young;You Young-June
    • The Journal of Engineering Geology
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    • v.15 no.1
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    • pp.19-27
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    • 2005
  • The Sambo mine is located in Hae-je Myeon, Moo-an Gun, Chollanamdo, which consists of host gneiss and rhyolite possessing quartzite veins with other compositions such as gold, silver, and sublimated sulfur. The ore grade estimated from the core was 0.05~10.9g/t or less in gold and 0.05~389g/t or less in silver, indicating a partial mineralization. The purpose of this paper is to understand the subsurface structures and the distribution of mineralized bodies in the Sambo mine using a combined method of Schlumberger, Wenner, and Dipole-di-pole resistivity surveys on the surface and the resistivity tomography survey in boreholes. The result of three-dimensional resistivity inversion showed that the mineralized body is extended to 240m long in the N10°~20°E direction, with 30m wide and 80 m thick from the surface. The low resistivity zones (<1,000ohm-m) determined from the resistivity image were in good agreement with the mineralized bodies and weak zones identified from the logged cores.

Distribution of Resistivity Zones Near Nari Caldera, Ulleung-do, Korea, Inferred from Modified Dipole Arrays (변형 쌍극자배열법을 적용한 울릉도 나리 칼데라 주변 조면안산암 지역의 비저항분포 특성 분석)

  • Kim, Ki-Beom;Kim, Man-Il
    • The Journal of Engineering Geology
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    • v.29 no.3
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    • pp.223-236
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    • 2019
  • Resistivity surveys can identify the distribution of geological units and structures (including fragmented fault zones), the extent of weathered and modified geological strata, and the characteristics of groundwater. This study aims to analyze the underground sedimentary layers and geological structures near the Nari and Albong Basins of Ulleung-do, Korea, focusing on six survey lines to identify the spatial trends in subsurface resistivity. A modified dipole array method (D method) was employed, combining resistivity results obtained by existing dipole array methods (A and C methods). The modified method provides optimal analysis of the cross-section of underground resistivity, and shows a clear boundary between a low-resistivity zone (${\leq}500{\Omega}{\cdot}m$) of sedimentary layers and weak zones, and a high-resistivity zone (${\geq}5,000{\Omega}{\cdot}m$) of volcanic rock (trachyandesite). The estimated average thickness of the sedimentary layers is 50~100 m for the Albong Basin and 100~200 m for the Nari Basin. An anomaly zone, different from the weak zone in the bedrock, is identified as a caldera fault, and the low-resistivity zone extends from the surface down to the lowest survey depths.

Mortar Characterization using Electrical Resistivity Method (모르타르의 전기비저항 특성)

  • Farooq, Muhammad;Park, Sam-Gyu;Song, Young-Soo;Kim, Jung-Ho
    • Geophysics and Geophysical Exploration
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    • v.12 no.2
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    • pp.215-220
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    • 2009
  • Cement based mortars are widely used to improve the soft ground of a dam site, highway construction, and karst voids. The mechanical properties of the mortar are well documented in literature, however very limited work is done on their physical properties such as electrical resistivity which is considered as one of the most important physical property known while improving the soft grounds. In this paper, electrical resistivity of the Portland cement mortars is examined by employing the Wenner technique. Cylindrical specimens with various water/cement ratios (w/c) ranges from 0.35, 0.45, 0.50 and 0.65 were cast and tested. The test results showed that the electrical resistivity of the mortar increases with increasing curing time and decreases with increasing water content and w/c. A reasonable, good relation was found between electrical resistivity and compressive strength of mortar.

Effectiveness of the Electrode Arrays for Delineating 2-D Subsurface Structure (2차원 지하구조 규명을 위한 전극배열의 효율성)

  • Yoon, Jong-Ryeol;Lee, Kiehwa
    • Economic and Environmental Geology
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    • v.29 no.3
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    • pp.345-355
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    • 1996
  • The effectiveness of various electrode configurations in horizontal mappings and 1-D inversions of vertical sounding data for delineating 2-D structures was studied. Apparent resistivity values of three point, dipole-dipole, Wenner, and Schlumberger mappings were simulated for such structures as vertical dyke, tabular prism, buried vertical fault, ramp and complex structure by finite difference method (FDM) and they were compared with each other. Also 2-D cross sections for three structures obtained by interpolation of 1-D inverted sounding data in terms of three layers were compared for Schlumberger and Wenner arrays. On these cross sections, horizontal and vertical resistivity interfaces of the 2-D structures are revealed relatively clearly. Apparent resistivity curves of Schlumberger mapping show vertical resistivity discontinuities very well. On the whole, Schlumberger array is superior to the other arrays in electric sounding as well as mapping. This study clearly indicates that interpretations of 2-D structures based on 1-D inversion are possible.

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A Study on Application of Electrical Resistivity Survey to Detect the Leakage of Embankment with Weak Zone (취약대가 존재하는 제방의 누수 탐지를 위한 전기비저항 탐사의 적용성 연구)

  • Park, Samgyu;Kim, Jaehong
    • Journal of the Korean GEO-environmental Society
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    • v.14 no.4
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    • pp.5-13
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    • 2013
  • The water leakage of reservoir embankment usually occurs around channelling pipes, which gives little influence on the embankment in a normal state. However, the embankment can be destroyed when the water level of reservoir increases with heavy rain and the rainy season in summer. Investigating the water vein and its path is therefore very important from the viewpoint of disaster prevention and embankment maintenance. The water leakage in dams and levees where the channelling pipes are working as weak zone was analyzed by using both numerical simulation and experimental method in this study. To detect the water leakage, an electrical resistivity survey was used and investigated for its' usability. The numerical results show the size and location of weak zone increases the importance of selection of electrode spacing. The leakage experiments of model embankment present the best result is obtained under the conditions of electrode spacing of 0.3m and dipole-dipole array. By studying the water leakage in dams and levees, the electrical resistivity survey is observed it is a very useful method to predict the leakage.

Sediments Characteristics at the Bottom of Shallow Reservoir using Streamer Resistivity Survey (스트리머 전기비저항탐사를 이용한 담수호 바닥 퇴적물 특성 분석)

  • Song, Sung-Ho;Lee, Gyu-Sang;Kang, Mi-Kyung;Kim, Young-In;Kim, Yang-Bin;Cho, In-Ky
    • 한국지구물리탐사학회:학술대회논문집
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    • 2008.10a
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    • pp.47-50
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    • 2008
  • Streamer resistivity surveys in shallow marine environments were carried out to analyze sediment characteristics at the bottom of reservoir. Because the resistivity values of reservoir water are very low and those of sediment are relatively high, apparent resistivity values increase with depth. And it is necessary to eliminate the apparent resistivity data decreased highly when the number of separation increases. According to the repeated data processing, we proposed the resistivity ratio of upper-to-lower layer is $0.6{\sim}0.8$ because the RMS error of inversion leads to the minimum in these range. As a result of the inversion for two- and three-layer model, the inversion including water depth is proved to be more effective than conventional method.

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Distribution of Alluvium Depth by the Ordinary Kriging of Vertical Electrical Sounding Data (전기비저항 수직탐사 자료의 정규크리깅을 통한 충적층 분포도의 작성)

  • Jung, Yeon-Ho;Byun, Joong-Moo
    • Geophysics and Geophysical Exploration
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    • v.10 no.3
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    • pp.211-218
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    • 2007
  • In this study, vertical electrical sounding (VES) data and ordinary kriging are used to identify the alluvial depth of each area that Korea Resources Corporation (KORES) conducted groundwater survey at Miryang area in Gyeongsangnam-do and Pocheon area in Gyeonggi-do from 2003 to 2004. To verify the applicability of VES data to ordianry kriging, regression analysis of VES data versus drillhole data is conducted. Comparing the alluvial depth distributions using ordinary kriging with existing drillhole data, the result shows that the depth distributions are reasonably depicted along with the topography and the basin. So, the ordinary kriging of VES data is useful to identify the alluvial depth distributions.

Subsurface Imaging by a Small-loop EM Survey (소형루프 전자탐사법에 의한 지하 영상화)

  • Lim Jin-Taik;Cho In-Ky
    • Geophysics and Geophysical Exploration
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    • v.6 no.4
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    • pp.187-194
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    • 2003
  • A small-loop electromagnetic (EM) system using multiple frequencies has advantages in survey speed and cost despite of limitation on its depth of investigation. Therefore, small-loop EM surveys have been frequently used on various site investigations involving engineering and environmental problems. We have developed a subsurface imaging technique using small loop EM data. We used a one-dimensional (ID) inversion method to reconstruct a subsurface image from frequency EM sounding data. Tests using simulated data show that the method can reasonably recover the subsurface resistivity structure. Also, the method was tested on field data obtained with multiple frequency small loop EM system at a farm in Chunchon, Korea. The resistivity image obtained form field data compares favorably with the image from the dipole-dipole resistivity survey.

빛을 이용한 저항 변화 메모리 제어

  • Park, Jin-Ju;Lee, Seung-Hyeop;Yong, Gi-Jung
    • Proceedings of the Korean Vacuum Society Conference
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    • 2013.02a
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    • pp.607-607
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    • 2013
  • 차세대 비휘발성 메모리 소자로서 각광받고 있는 저항 변화 메모리(resistive switching random access memory; ReRAM) 소자는 속도가 빠르고, 에너지 소모가 적으며, 고집적화를 이루기 용이하다는 강점을 보유하고 있다. 지금까지 저항변화 물질의 최적화를 위해 매우 다양한 물질들이 연구되고 있으며, 그 물질에 따라 스위칭 메커니즘 및 동작 방법이 다르게 보고되어 왔다. 하지만 저항변화 메모리의 스위칭 거동은 전형적인 전기적 제어 조건으로부터 구현되었기 때문에 한정된 소자 특성을 나타낼 수밖에 없었다. 본 연구에서는 새로운 메모리 제어 조건으로 빛을 이용함으로써 한정된 소자 특성으로부터 벗어나고자 하였다. 저항 변화 물질로 잘 알려진 ZnO를 표면적이 넓은 형태로 합성하기 위하여 hydrothermal 방법으로 FTO 기판 위에 수직하게 배열된 ZnO 나노와이어를 형성하고 그 위에 Au 상부 전극을 형성하여 금속-절연체-금속 소자 구조를 제작하였다. 본 연구에서는 전형적인 전기적 제어 조건에 더불어 빛의 입사 유무 조건을 바꿔가면서 Au/ZnO 나노와이어/FTO 소자의 저항 변화 특성을 평가 하였을 뿐만 아니라 전기적 인가 없이 오직 빛만으로 두 가지 안정한 저항 상태를 반복적으로 전환하는 특성을 유도하였다. 본 결과를 바탕으로 필라멘트 이론에 기초한 저항 변화 메커니즘을 설명하는 모델이 제시되었다.

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