• Title/Summary/Keyword: weathered strata

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A Case Study on Reinforcement Method by Excavation Adjacent to the Subway Tunnel using Numerical Analysis (수치해석을 통한 지하철 구조물 인접 굴착에 따른 보강공법 적용사례연구)

  • Byun, Yo-Seph;Jung, Kyoung-Sik;Chun, Byung-Sik
    • Journal of the Korean GEO-environmental Society
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    • v.12 no.9
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    • pp.5-11
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    • 2011
  • Recently, large and deep excavations are increasing. The damage of adjacent structures due to excavation has steadily increased with increasing construction demand. Especially in urban development and poor conditions, the excavation adjacent to the subway structures has caused a lot of problems. This paper was reviewed that the underground excavation and reinforcement of the status process through a case study on the field. And stability analysis through the case study evaluates applicability for reasonable reinforcement method by numerical analysis. As a result, the strata distribution condition of all 16 sites consisted of landfill from the top and distributed in the order of deposits, weathered soils, weak rock from the bottom. Also, when proceeding the excavation adjacent to structures, the location of site and layer conditions have highly effect on the results of the construction. Therefore, this study was applied reinforcement method to protect damage by excavation. Displacement and settlement were within allowable criterion and hence, stability of structure was analyzed as safe.

Case Study of Friction Piles Driven into Clayey Soils on the Central Coast of Vietnam (베트남 중부 연안의 대심도 점토지반에 시공된 강관 마찰 말뚝의 항타시공관리)

  • Seol, Hoon-Il
    • Journal of the Korean Geotechnical Society
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    • v.40 no.3
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    • pp.19-31
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    • 2024
  • In Korea, driven piles are generally penetrated up to weathered rock or harder strata. Friction piles have been used to some extent in the southwest coastal area with deep soils; however, friction piles are not extensively due to uncertainties about construction quality. The embedded pile construction method is primarily used due to noise and vibration complaints. However, in Southeast Asian countries (e.g., Cambodia, Myanmar, and Vietnam), where soft sediments are deep, the driven pile method is commonly used due to its economic advantages. Construction companies are increasingly entering overseas construction markets, e.g., Southeast Asia; thus, it is necessary to understand the behavior of driven friction piles in the soil and improve on-site engineering management to gain market competitiveness in these countries. In this study, the bearing capacity of friction piles driven into clayey coastal soils in Vietnam with time-dependent characteristics was evaluated based on the dynamic and static pile load tests. Based on the results, a modified Danish formula is proposed for on-site quality management.

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.