• 제목/요약/키워드: geophysical logging

검색결과 120건 처리시간 0.024초

An integrated studies for salt-water intrusion in Yeonggwang-gun, Korea

  • Hwang Seho;Chi Sejung;Lee Won-suk;Shin Jehyun;Park Inhwa;Huh Dae-Gee;Lee Sang-kyu
    • 한국지구물리탐사학회:학술대회논문집
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    • 한국지구물리탐사학회 2003년도 Proceedings of the international symposium on the fusion technology
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    • pp.455-458
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    • 2003
  • A combination of drilling, hydrogeochemical survey, geophysical survey and the numerical modelling for the flow and transport of groundwater was performed to evaluate the seawater intrusion in Baeksu-eup, Yeonggwang-gun, Korea. The survey area extends to over 24 $km^2$. Twelve wells were also drilled for the collection of geologic, geochemical, hydrologic, and geophysical logging data to delineate the degree and vertical extent of seawater intrusion. To evaluate and map the salinity in a coastal aquifer, geophysical data and hydrogeochemical results were used. Layer parameters derived from VES data, various in situ physical properties from geophysical well loggings, and the estimated equivalent NaCl concentration were used as the useful input parameters for the numerical simulation with density-dependent flow. Our multidisciplinary approach for evaluating the seawater intrusion can be considered as a valuable attempt to enhancing the utilization of various data and the reliability of numerical ground modelling.

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천부 지반 환경에서 속도검층 난제들에 대한 고찰 (Considerations on the Difficulties in Velocity Logging in the Near Surface Environments)

  • 조철현;변중무;황세호
    • 지구물리와물리탐사
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    • 제9권3호
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    • pp.185-192
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    • 2006
  • 토목이나 환경분야에 적용되는 시추공을 이용한 P파와 S파 속도검층 수행 시 여러 고려해야 할 사항이 있다. 토양이나 풍화암 등 연약층에 설치한 케이싱이 탄성파 측정에 미치는 영향, 사용되는 주파수에 따라 측정되는 탄성파 속도의 변화 등이 그것이다. 또한 속도검층으로부터 구한 탄성계수는 동적특성을 반영한다. 이러한 과제를 극복하기 위해서는 탄성파시험이 설정된 시추공에서는 가급적 케이싱을 설치하지 않고 공벽을 유지하는 시추 기술을 개발, 적용하도록 하고, 속도검층의 목적에 맞는 주파수 대역의 시험법을 적용하도록 해야 하겠다. 또한 내진설계자들이 속도검층에서 구한 동탄성계수와 실내역학시험에서 구한 정탄성계수와의 차이점을 인식하고 적절히 사용할 수 있도록 조언하는 것도 필요하다.

물리탐사에 의한 터널구간의 암반등급 산정 (A Case Study for Rock Mass Classification using Geophysical Exploration)

  • 김기석;권형석;김종훈
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2003년도 암반역학위원회 학술세미나 논문집
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    • pp.119-137
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    • 2003
  • Electrical resistivity is one of physical property of the earth and measured by electrical resistivity survey, electrical resistivity logging and laboratory test. Recently, electrical resistivity Is widely used In determination of rock quality in road and railway tunnel design. To get more reliable rock quality data from electrical resistivity, it needs a lot of test and study on correlation of resistivity and rock quality. Firstly, we did rock property test In laboratory, such as uniaxial compressive strength(UCS), P wave velocity, Young's modulus and electrical resistivity. We correlate each test results and we found out that electrical resistivity has exponentially related to UCS and P wave velocity and linearly related to Young's modulus. And we accomplished electrical resistivity survey in field site and carried out electrical resistivity togging at In-situ area. Also we performed rock classification, such as RQD, RMR and Q-system and we correlate electrical resistivity to rock classification results. We found out that electrical resistivity logging data are highly correlate to RQD, Q and RMR. Also we found out that electrical resistivity survey data are lower than electrical resistivity logging data when there are faults or fractures. And it cause electrical resistivity survey data to lowly correlate to RQD, Q and RMR.

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물리탐사자료의 GIS 복합처리에 의한 천부지질구조 해석 (Interpretation of shallow geological structure by applying GIS to geophysical data)

  • 송성호;정형재
    • 한국지하수토양환경학회:학술대회논문집
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    • 한국지하수토양환경학회 1998년도 공동 심포지엄 및 추계학술발표회
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    • pp.123-126
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    • 1998
  • We have conducted surface electrical resistivity surveys along with the electrical logging at Bookil-Myun, Chungwon-Goon, Choongchungbuk-Do to determine the depths of basement and water table, and for the purpose of preparing the basic input data for hydrogeologic model combined with GIS. A twenty lines of dipole-dipole array survey and a twenty-five stations of resistivity sounding were performed and ten holes were employed for electrical logging to cross check the surface data. A combined interpretation gave the quantitative information of the shallow geologic structure over the area and we constructed layers using the grid analysis of Arc/info. The constructed layers were turned out to be similar to the geologic structure confirmed from the drilling data and we concluded that the methodology adopted in this study would be applicable to hydrogeologic model setup as a tool of providing the basic input data.

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제주도 동부해안 한동리지역의 수문지질학적 연구

  • 김기표;윤정수;박원배
    • 한국지하수토양환경학회:학술대회논문집
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    • 한국지하수토양환경학회 2002년도 추계학술발표회
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    • pp.9-12
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    • 2002
  • The purpose of this study is to understand the high saline water phenomenon of Handong-ri area in the eastern coast of Jeju Island, were investigate the tidal effect of groundwater level, variation of electric conductivity and temperature, geological logging on the monitoring wells, chemical water quality, and ratios of oxygen istope of groundwater and seawater Results in investigating variation of interface zone of freshwater and saline water represented that the hyaloclastites formed at below groundwater table is developing toward the coast; this area consisted of stratum of good permeability. Hyaloclastites is presumed the main path of the high salinity water There are a lot of movement by the tide at upper layer. Salinity of lower layer spreads to upper up step in proportion to tidal energy. Because of hydrogeological characteristics, Interface zone of freshwater and saline water is made, High salinity of groundwater occur in east coastal area of Jeju Island. Therefore, I think that high saline groundwater phenomenon is natural condition by simple mixing.

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Permeability imaging in granitic rocks based on surface resistivity profiling

  • Sudo Hiroshi;Tanaka Toshikazu;Kobayashi Tsuyoshi;Kondo Tatsutoshi;Takahashi Toru;Miyamoto Masaharu;Amagai Mitsuru
    • 지구물리와물리탐사
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    • 제7권1호
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    • pp.56-61
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    • 2004
  • In order to image the distribution of permeability in granitic rocks, we carried out two-dimensional (2D) resistivity profiling, together with in-situ permeability tests, electrical logging of boreholes, and resistivity measurements of rock core samples in a laboratory. Based on the electrical logging and in-situ permeability data from boreholes, we obtained empirical equations which relate resistivity and permeability of the granitic rocks in the area studied. We then applied the empirical equation to a 2D resistivity section, to produce a 2D permeability section of the granitic rocks. In this paper, we present details of the field data and of the procedure for conversion from the resistivity section to a permeability section. The observed relationship between resistivity and permeability of the rocks is also discussed.

캐나다 아타바스카 분지 부정합형 우라늄광상 물리탐사 사례 (Geophysical Exploration on Unconformity-type Uranium Deposit in Athabaska Basin, Canada)

  • 유영준;김재철
    • 한국지구물리탐사학회:학술대회논문집
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    • 한국지구물리탐사학회 2009년도 특별 심포지엄
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    • pp.73-87
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    • 2009
  • Geophysical survey for unconformity-type uranium deposit applied to this study area in Athabaska Basin, Canada were carried out airborne TEM and magnetic, resistivity-induced polarization (DC-IP), puser seismic reflection and well-logging method. The results of airborne survey interpreted the lithological boundary, geological structures, and conductors. Also, these results decided to main targets for ground DC-IP survey. The Low resistivity and the high chargeability slices of 3D modeling interpreted from DC-IP survey response for conductors related to hydrothermal alteration zones and fault-controlled graphitic zones occurring at the unconformity-type uranium deposit, and they confirmed by diamond drilling. Seismic results interpreted to lake bottom surface, alluvium layer and intra-sandstone faults. We suggest the resonable field data acquisition of DC-IP method on the land or the lake in Athabaska Basin.

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지표 물리탐사법을 이용한 염/담수 영역의 고분해능 영상화

  • 박권규;신제현;박윤성;황세호
    • 한국지하수토양환경학회:학술대회논문집
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    • 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
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    • pp.446-449
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    • 2004
  • High resolution geophysical imaging to delineate costal aquifer and seawater- freshwater interface has been applied in Baesu-eup, Yeonggwang-gun, Jeolla province Electrical resistivity information from vertical electrical sounding and 2-D electrical resistivity survey is key parameter to map equivalent Nacl concentration map over the survey area. Seismic velocity from refraction tomographic survey, on the other hand, gives more reliable information on the subsurface stratagraphy than electrical resistivity methods which frequently suffer from low resolution due to masking effect. We imaged high-resolution 3-D structure of costal aquifer by correlating the electrical resistivity with seismic velocity, and mapped equivalent NaCl concentration map using resistivity and hydro-geological information from well logging.

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포항지역 신생대 제3기 미고결 퇴적층의 암반분류 (Rock Mass Classification of Tertiary Unconsolidated Sedimentary Rocks In Pohang Area)

  • 김성욱;최은경;이융희
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2009년도 춘계 학술발표회
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    • pp.999-1008
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    • 2009
  • A series of sedimentary rocks which are formed in the Tertiary are distributed around Samcheok(Samcheok-Pukpyoung basin), Younghae(Younghae basin), Pohang(Pohang basin), Gyeongju(Yangnam basin), Ulsan(Ulsan basin), Jeju(Seogyuipo formation) in the southern region of the Korean Peninsula. This study concerned with geological, geophysical, geotechnical properties of the unconsolidated rocks in the Pohang area. A consolidated rocks are classified as hard rock - soft rock - weathered rock - residual soil follows in degree of weathering. But unconsolidated rocks has soil properties as well as rock's at the same time. The results of field excursion, boring, borehole-logging, rock testing, geophysical survey, laboratory test are soft rock range, but the durability of the rock until the residual soil from the weathered rock. We accomplished the rock mass classification of the unconsolidated rocks.

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풍암퇴적분지 내 시추공 PABH1에서의 물리검층에 의한 암상의 판정 (Lithology Determination by Log Analysis from a Borehole-PABH1 in the Pungam Sedimentary Basin)

  • 김영화;장승익
    • 지질공학
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    • 제8권2호
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    • pp.163-173
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    • 1998
  • 강원도 홍천군 서석면 일대에 발달하고 있는 풍암퇴적분지 내에 위치한 시험시추공 PABH1에서 실시된 시추결과에 대한 암상판정과 동 퇴적분지의 구성암에 대한 물성반응의 특성을 확인하기 위하여 코어관찰과 코어의 물성측정, 그리고 지구물리검층을 실시하고 그 결과를 종합분석하였다. 시추공의 64미터와 124미터 구간에 걸쳐 정밀 코어관찰을 실시하고 11개 암상군으로 분류하였다. 코어 관찰결과 구분된 11개 그룹의 코어시료에 대하여 비저항, 자연감마 및 밀도를 측정하고 그 결과를 분석하였다. 지구물리검층 또한 비저항과 밀도, 자연감마곡선을 중점적으로 분석하여 암상판정을 시도하였다. 지구물리검층과 코어물성측정의 결 과에서 각 암상별로 특징적인 물성분포가 얻어졌으며 검층곡선만의 분석에 의해서도 암상의 구분이 충분히 가능할 수 있음을 보였다. 특히 이 지역에서의 조립질퇴적암과 세립질퇴적암, 그리고 퇴적기반인 화강편마암의 물성반응이 가장 현저하여 검층 해석에서 좋은 열쇄층의 역할을 할 수 있는 것으로 나타났다.

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