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Stability Analysis for Two Arch Excavation of a Tunnel Portal (터널 갱구 2 Arch 굴착에 따른 안정성 해석)

  • 이길재;유광호;박연준;채영수
    • Tunnel and Underground Space
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    • v.12 no.3
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    • pp.179-188
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    • 2002
  • This study is to understand the effect of the vibration and the stress changes due to the excavation of 2 arch parts of a tunnel, which is a Gyungbu Express Railway tunnel, on the tunnel itself and adjacent slopes in advance, and to analyze the stability. For the estimation of ground conditions, borehole tests, borehole camera logging and seismic logging were performed. Ground properties at a specific location were determined as input constants by performing 2 dimensional analyses with possible ranges of uncertain ground properties. Static and pseudo-static (due to blasting vibration) factors of safety were calculated. The behavior of the tunnel and its vicinity due to the tunnel excavation were predicted by 3 dimensional analyses. It was also tested whether the support system was proper.

Application of SP monitoring to the analysis of anisotropy of aquifer (대수층 이방성 분석을 위한 자연전위 모니터링의 적용)

  • 송성호;용환호
    • Economic and Environmental Geology
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    • v.36 no.1
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    • pp.49-58
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    • 2003
  • To analyze the anisotropic characteristics of fractured aquifer, variations of streaming potential were measured during and after pumping over several wells at the two test sites. Surface electrical resistivity survey, normal resistivity logging, and slug test were performed at the wells to identify the hydrogeological structure. Applying the results to the recently suggested model, the aquifer of the two test sites showed confined characteristics. Anisotropic direction appeared in using equi-potential maps from self-potential monitoring results matched well with the results of the hydrogeological test. The self-potential monitoring method adopted in this study would be useful for providing a more reliable information on the anisotropy of aquifer in the pumping test at single well.

매립장 주변 대수층 매질특성과 수질의 상관관계 연구

  • O In-Suk;Go Gyeong-Seok;Gu Min-Ho;An Ju-Seong
    • Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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    • 2006.04a
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    • pp.387-390
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    • 2006
  • 매립장주변의 대수층 특성과 수리지화학적 특성과의 상관관계 분석은 매립장 환경 위해 요인을 평가하는데 중요한 역할을 하며 이를 위해 생활쓰레기 매립장인 금산 매립장을 대상으로 연구를 수행하였다. 대수층 매질 특성을 파악하기 위해 토양시료를 채취하여 중금속 성분 및 pH, 전기전도도, 용존유기탄소, 양이온교환능력, 유기물함량, 토양 입도분석을 수행하였고, 수리지화학적 특성 파악을 위해 수질검층 및 지하수 시료를 분석하여 매립지역의 수직 및 수평적인 분포 특성을 파악하였다. 대수층의 토양특성과 지하수 수질특성의 비교분석 결과 침출수 집수정을 기점으로 침출수의 영향을 받은 관측정의 전기전도도(EC) 측정값이 배경 지하수에 비해 상대적으로 높은 값을 보여 주었다. 입도분석 결과 상부 표토에 가까운 50cm 이내의 토양은 농경의 영향으로 심부보다 상대적으로 실트질 토양이 많고 이보다. 심부의 토양은 사질 토양으로 되어 있었다. 이러한 투수성이 좋은 사질 토양은 지하수의 이동을 비교적 쉽게 유도하기 때문에 매립장으로부터 침출수가 누출되었을 때 지하수 흐름을 따라 빠르게 이동할 수 있는 통로로 작용될 것으로 판단된다.

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제주도 동부지역의 수문지질에 관한 연구(II)

  • 고기원;박윤석;박원배;문덕철
    • Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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    • 2003.04a
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    • pp.67-72
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    • 2003
  • 제주도 동부지역에 설치한 심부관측정과 지하수 개발공에 대한 시추코아 지질검층, EC 및 수온검층, 지하수위 관측, 수질조사 등의 자료를 기초로 이 지역의 지하지질 분포와 지하수 부존특성에 대해 해석을 실시하였다. 제주도 동부 해발 200m 이하지역은 평균 해수면 하 90~120m 깊이까지 투수성이 좋은 용암류 누층으로 이뤄져 있으며, 일부지역에서는 서귀포층 상부에 유리쇄 설성 각력암층(hyaloclastite breccia)이 두껍게 분포하고 있어 담수지하수의 확산과 해수의 유입이 잘 일어날 수 있는 지질상태를 이루고 있다. 특히 서귀포층은 G-H비에 의한 담.염수 경계면 분포 깊이보다 깊은 위치에 존재하고 있어 제주도 서부지역에서처럼 담수지하수를 저류 해주는 역할을 기대하기 어려운 것으로 판단된다. 제주도 동부지역 지하수체는 수직적으로 담수지하수, 저염지하수, 염수지하수로 구분할 수 있으며, Ghyben-Herzberg 원리가 적용되는 담수렌즈(기저지하수) 두께는 일반적인 G-H비 보다 훨씬 얇은 평균 1:20의 비율을 나타냈다. 담수렌즈는 대체로 해안으로부터 내륙쪽 8km 지역까지 광범위하게 발달하고 있으며, 담수렌즈 포장량은 822백만톤(공극율 5%)에서 1,970백만톤(공극율 12%)의 범위로 추정되었다.

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A Case Study on Geotechnical Properties and Weathering Degree of Weathered Granite Rock (화강 풍화암의 지반특성 및 풍화도 평가에 대한 사례 연구)

  • Lee, Seung-Hwan;Yoo, Byeong Soo;Chung, Choong-Ki
    • Journal of the Korean Geotechnical Society
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    • v.33 no.12
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    • pp.127-139
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    • 2017
  • Site investigation including boring and various in-situ borehole test (Pressuremeter test, Borehole shear test, Downhole test, Suspension PS logging, Density logging) and X-ray fluorescence analysis for rock core sample were performed to estimate geotechnical properties and weathering degree of weathered granite rock in Goyang. Deformation modulus, shear strength parameter and shear wave velocity estimated through in-situ borehole test had a tendency to increase with depth. And several chemical weathering indices evaluated by X-ray fluorescence analysis had a general tendency of reducing weathering degree in accordance with depth. Also, relationship between VR determined as a representative weathering index and the geotechnical properties was analyzed.

Automatic Interpretation of the Borehole Normal Resistivity Data by Using a Personal Computer (퍼스널 컴퓨터를 이용한 비저항 물리검층자료의 자동해석)

  • Kim, Jin-Hu
    • Journal of Ocean Engineering and Technology
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    • v.2 no.2
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    • pp.51-60
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    • 1988
  • A data transform is performed by using a point-electrode focusing method in order to obtain accurate and objective interpretation of the borehole normal resistivity data. Two new synthetic curves can be generated through the data transform. The one is an approximate apparent resistivity curve, which would be used to predict the true resistivity of the formation. The other one is a bed boundary coefficient curve, which would be used to distinguish bed boundaries. The accuracy of the normal data interpretation can be improved and this method takes much less computational time than a linear inversion technique. Moreover, this method does not require an initial guess model and limitation of number of unknown parameters. Since this algorithm can be run on a personal computer, an immediate interpretation would be possible at the field work site. If an additional set of electrodes(a=125cm)is attached to a normal resistivity tool which is being used (a=25cm, 50cm, 100cm), the apparent resistivity for the point-electrode focusing device can be calculated, and it would maximize the use of short and long normal resistivity data and promote the accuracy of the interpretation.

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Integrity Test of DCM Treated Soils with a Cross-hole Sonic Logging (시추공간 음파검층법을 이용한 심층혼합 개량지반의 건전도 조사)

  • 김진후;조성경
    • Journal of Ocean Engineering and Technology
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    • v.15 no.1
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    • pp.73-78
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    • 2001
  • Soundness evaluation of a structure being constructed under the sea is usually difficult. In this study, a cross-hole sonic logging(CSL) which have been used for non-destructive test of concrete piles is adopted for the integrity test and monitoring of DCM(deep cement mixing) treated soils. Chemical and physical characteristics of raw ground materials are analysed to delineate ground environmental effects on the strength of DCM treated soils. In order to convert cross-hole sonic logging data into compressive strength, correlations between compressive strengths and wave velocities of core samples have been obtained. It is found that there is little effect of ground environment on the strength of the DCM treated soils, and the density distribution of core samples and cross-hole logging data show that a defective zone may exist in the DCM treated soils. With the time lapse, however, the defective zone has been cured and consequently, compressive strength of the DCM treated soils increases and satisfies the design parameter. From this study it can be concluded that the cross-hole sonic logging can be used for the integrity test as well as monitoring the curing stage of the structures, successfully.

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Relationship between lithology and rock physical property using borehole prospecting (시추공 물리탐사를 통한 지반물성과 암상과의 상관성 분석)

  • 송무영;김환석;박종오
    • The Journal of Engineering Geology
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    • v.12 no.2
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    • pp.127-135
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    • 2002
  • The relationship between the seismic velocity and RQD was estimated using the RQD data obtained from the optical borehole image processing and drill core logs and the seismic velocity measured from the PS logging. The seismic velocity and crack aperture show a high correlation in the granite in Yuseong area and banded gneiss in Paldang area. However, such a relationship cannot be found in the sedimentary rock in Sabuk area. In the sedimentary rock of Sabbuk area, the seismic velocity shows widespread distribution especially in the 0∼20mm range of accumulated crack aperture probably because the wide distribution of fracture zone in coaly shale results in the inaccurate measurements of the crack aperture.