• 한국신재생에너지학회:학술대회논문집
• /
• 2009.11a
• /
• pp.572-575
• /
• 2009

지층 내에 발달한 고투수성 단층은 유체, 에너지, 그리고 용질이 이동하는데 있어서 중요한 역할을 하는 지질구조이다. 따라서 고투수성 단층 주변부에서는 온천, 지열 이상대, 그리고 금속 광상 등이 형성될 가능성이 크다. 이 연구에서는 열-수리적 거동 모델링을 통하여 단층에 의한 온천 또는 지열 이상대의 형성 원인을 확인하였다. 단층의 구조에 따른 지하수 유동과 이에 따른 지층 내 열적 상태를 확인하기 위해서 단층 구조가 다른 3가지의 경우에 대해서 2차원 열-수리적 거동 정류 모델링을 수행하였다. 모델링 결과 단층 구조가 다른 3가지의 모든 경우에서 단층의 투수율이 커지면 단층대에서의 용출 온도가 초기 온도 보다 높아지는 경향을 확인 할 수 있고, 경우에 따라서 모암의 투수율 역시 용출온도에 영향을 미치는 것을 확인 하였다. 따라서 심부지열 개발을 위한 연구지역에 대해 보다 정확한 예측 모델링을 수행하기 위해서는 단층의 구조, 단층과 모암의 투수율, 그리고 수리지질학적 정보 등이 매우 중요하다고 할 수 있다.

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
• /
• 2006.04a
• /
• pp.87-91
• /
• 2006

본 연구의 대상 지역은 전라북도 부안군 변산면 격포리 일대이다. 이 지역의 해안 대수층 내에서 발생하고 있는 해수 침투 현상을 효과적으로 모사하고 지하수 양수정의 설치 및 운영의 영향을 정량적으로 평가하기 위하여 지형과 지층의 구성 등의 수리지질학적 특성을 종합적으로 고려한 지하수 유동 및 염분 이동 삼차원 수치 모델링을 수행하였다. 지하수 양수 전의 정상 상태 수치 모델링 결과에서는 지하수 유동 및 염분 이동의 측면에서 대상지역의 수리지질학적 특성이 잘 반영되어 나타났다. 또한 지하수 양수 시의 비정상 상태 수치 모델링 결과에서는 지형과 지층의 특성에 따라서 염분 이동의 양상이 특징적으로 나타났으며 양수정의 위치에 따른 염분 농도의 시간적 공간적 분포의 변화를 효과적으로 예측할 수 있었다. 이러한 결과들은 향후 연구지역 뿐만 아니라 국내의 다른 해안 지역에서 지하수 자원의 개발 시에 해수 침투의 양상을 파악하고 예측하는데 효과적으로 활용될 수 있을 것으로 기대된다.

• Economic and Environmental Geology
• /
• v.40 no.6
• /
• pp.739-749
• /
• 2007

The seismic velocity at the formation varies widely with physical properties in the layers. These features on seismic shot gathers are not capable of reproducing normally by numerical modeling of homogeneous medium, so that we need that of random inhomogeneous medium instead. In this study, we conducted Gaussian autocorrelation function (ACF), exponential autocorrelation function and von Karman autocorrelation function for getting inhomogeneous velocity model and applied a simple geological model. According to the results, von Karman autocorrelation function showed short wavelength to the inhomogeneous velocity medium. For numerical modeling for a gas hydrate, we determined a geological model based on field data set gathered in the East sea. The numerical modeling results showed that the von Karman autocorrelation function could properly describe scattering phenomena in the gas hydrate velocity model which contains an inhomogeneous layer. Besides, bottom-simulating-reflectors and scattered waves which appear at seismic shot gather of the field data showed properly in the inhomogeneous numerical modeling.

• Journal of the Korean earth science society
• /
• v.37 no.4
• /
• pp.200-210
• /
• 2016

Geoacoustic modeling is used to predict sound transmission through submarine bottom layers of sedimentary strata and acoustic basement. This study reconstructed four geoacoustic models for sediments of 50 m thick at the Jeongdongjin area in the western continental margin of the East Sea. Bottom models were based on the data of the highresolution air-gun seismic and subbottom profiles (SBP) with sediment cores. P-wave speed was measured by the pulse transmission technique, and the resonance frequency of piezoelectric transducers was maintained at 1MHz. Measurements of 42 P-wave speeds and 41 attenuations were fulfilled in three core sediments. For actual modeling, the P-wave speeds of the models were compensated to in situ depth below the sea floor using the Hamilton method. These geoacoustic models of coastal bottom strata will be used for geoacoustic and underwater acoustic experiments reflecting vertical and lateral variability of geoacoustic properties in the Jeongdongjin area of the East Sea.

• Geophysics and Geophysical Exploration
• /
• v.13 no.1
• /
• pp.118-127
• /
• 2010

Resistivity logging instruments are designed to measure the electrical resistivity of a formation, and this can be directly interpreted to provide a water-saturation profile. However, resistivity logs are sensitive to borehole and shoulder-bed effects, which often result in misinterpretation of the results. These effects are emphasised more in the presence of tool eccentricity. For precise interpretation of short- and long-normal logging measurements in the presence of tool eccentricity, we simulate and analyse eccentricity effects by combining the use of a Fourier series expansion in a new system of coordinates with a 2D goal-oriented high-order self-adaptive hp finite-element refinement strategy, where h denotes the element size and p the polynomial order of approximation within each element. The algorithm automatically performs local mesh refinement to construct an optimal grid for the problem under consideration. In addition, the proper combination of h and p refinements produces highly accurate simulations even in the presence of high electrical resistivity contrasts. Numerical results demonstrate that our algorithm provides highly accurate and reliable simulation results. Eccentricity effects are more noticeable when the borehole is large or resistive, or when the formation is highly conductive.

• Journal of the Korean earth science society
• /
• v.39 no.2
• /
• pp.154-163
• /
• 2018

Geoacoustic model comprises physical and acoustic properties of submarine bottom layers influencing sound transmission through sea water and underwater. This study suggested for the first time that we made a geoacoustic model of long-coring bottom layers at the SSDP-105 drilling site of the Ulsan coastal area, which is located in the southwestern inner shelf of the East Sea. The geoacoustic model of 52 m depth below seafloor with three-layer geoacoustic units was reconstructed in the coastal sedimentary strata at 79 m in water depth. The geoacoustic model was based on the data of a deep-drilled sediment core of SSDP-105 and sparker seismic profiles in the study area. For actual modeling, the geoacoustic property values of the models were compensated to in situ depth values below the sea floor using the Hamilton modeling method. We suggest that the geoacoustic model be used for geoacoustic and underwater acoustic experiments of mid- and low-frequency reflecting on the deep bottom layers in the Ulsan coastal area of the East Sea.

• Journal of the Korean Geotechnical Society
• /
• v.17 no.6
• /
• pp.85-98
• /
• 2001

Cone penetration was analyzed by arbitrary Lagangian-Eulerian(ALE) method. In order to simulate full penetration, steady state analyses were performed using ABAQUS/Explicit, which models upward flow of soil layers. In the analysis of homogeneous layer it was found that the paths and the strain of soil particles were consistent with the result of the strain path method and that the ultimate resistance were reasonably evaluated. The cone penetration through different soil layers was also analyzed and that showed the transfer of cone resistance. The steady state ALE analysis could perform full penetration through the layered soils.

• Journal of Korea Water Resources Association
• /
• v.49 no.9
• /
• pp.741-748
• /
• 2016

Laboratory scale model was constructed for open-cut riverbed infiltration experiment and four kinds of media were selected, medium sand, sand, volcanic rock, and gravel, for the experiment. Hydraulic conductivity for each medium and flow rate from the collecting pipe with functional screen were estimated from the experiment. Modified hydraulic conductivity scenarios considering turbid water (30~50 NTU) were applied in Visual MODFLOW modeling to analyze the effects of turbid water on the flow rate. Twenty-two scenarios were generated considering prticles in turbid water and applied to each medium cases in MODFLOW modeling. The minimum error was occurred when the gravel medium had 20% less hydraulic conductivities for the third layer-depth from the top and clay particles in turbid water might play a role in adsorption process to the surface of volcanic rock (2~5 mm). For medium sand case the error was also quite small when the mediumhas 5% less hydraulic conductivities for the second layer-depth from the top.

• Proceedings of the KIEE Conference
• /
• 2009.04a
• /
• pp.80-83
• /
• 2009

현장 대지구조의 측정과 분석은 정확하고 신뢰성 있는 접지시스템의 설계와 시공에 매우 중요하며, 특히 대지 구조의 분석은 접지방식의 선정과 시공에 있어 절대적인 요소이다. 현장 측정 대지저항률의 실제적 분석을 통해 더 정확한 접지설계와 접지의 효율성을 높일 수 있으며, 시공 후 접지성능의 설계 오차를 최소화할 수 있게 된다. 대지는 다양한 형태의 지층과 구조로 이루어져 있으며, 접지설계의 신뢰성과 정확성은 대지 조건을 얼마나 현장 지질 조건에 가깝게 모델링 하는가에 달려있다. 현장 대지구조 및 지질 특성에 가깝게 분석하여 적용된 접지 설계는 시공 오류의 최소화, 성능의 안정화 그리고 비용의 절감은 물론 운용 설비의 운용 품질을 높여 주게 된다. 본 연구에서는 현장에서 측정된 대지저항률을 수직 지층와 수평지층 구조로 분석하여 그 결과를 비교하였고, 분석된 각각의 구조 대지저항률을 적용하여 접지시스템을 설계 비교하였다. 또한 설계된 접지시스템을 현장에 시공하여 측정된 결과값을 수직구조의 접지 설계치와 수평구조의 접지 설계치를 비교하므로써, 이를 통해 대지구조의 유형분석에 따른 접지설계의 신뢰성과 오류를 최소화하기 분석방안을 제시하였다.

• Journal of the Korean Geotechnical Society
• /
• v.18 no.6
• /
• pp.117-127
• /
• 2002

A deterministic approach of slope stability, which is generally corresponding to the model of a simple non-linear function for slopes, is problematic in that it does not account the versatile characteristics of ground layers in an effective way. To resolve this problem, this study proposes a new way of analyzing slope stability, so-called “genetic algorithm method, ” so as to reflect some particular conditions pertaining to the grounds under concern. Similarities and differences in slope stability that may exist between homogeneous and multiple ground layers are examined in a competitive manner, Overall, though similarities deemed a little bit salient, the algorithm method turned out to be very applicable to estimating the validity of slope stability. Furthermore, an additional effort to consider long-standing sequential and dynamic changes in both the amount of rainfall and the underground water level is made in order to improve the results.