• Title/Summary/Keyword: Geological Structure

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Analysis of Reservoir Vulnerability Based on Geological Structure Around Pohang Earthquake (포항지진 발생 주변지역 지질특성에 따른 저수지 취약성 해석)

  • Lim, Sung Keun;Song, Sung-Ho;Yu, Jaehyung
    • Journal of the Earthquake Engineering Society of Korea
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    • v.22 no.3
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    • pp.169-174
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    • 2018
  • A total of 594 reservoirs (17%), which are managed by KRC, equipped with earthquake-resistant facilities whereas remaining ones did not. In addition, reservoirs were placed without the effect of geological structures (i.e., fault and lineament). Therefore, development on technique for alleviating the potential hazards by natural disasters along faults and lineaments has required. In addition, an effective reinforcement guideline related to the geological vulnerabilities around reservoirs has required. The final goal of this study is to suggest the effective maintenance for the safety of earth fill dams. A radius 2 km, based on the center of the reservoir in the study area was set as the range of vulnerability impacts of each reservoir. Seismic design, precise safety diagnosis, seismic influence and geological structure were analyzed for the influence range of each reservoir. To classify the vulnerability of geological disasters according to the fault distribution around the reservoir, evaluation index of seismic performance, precise safety diagnosis, seismic influence and geological structure were also developed for each reservoir, which were a component of the vulnerability assessment of geological disasters. As a result, the reservoir with the highest vulnerability to geological disasters in the pilot district was analyzed as Kidong reservoir with an evaluation index of 0.364. Within the radius of 100km from the epicenter of the Pohang earthquake, the number of agricultural infrastructure facilities subject to urgent inspections were 1,180 including reservoirs, pumping stations and intakes. Four reservoirs were directly damaged by earthquake among 724 agricultural reservoirs. As a result of the precise inspection and electrical resistivity survey of the reservoir after the earthquake, it was reported that cracks on the crest of reservoirs were not a cause of concern. However, we are constantly monitoring the safety of agricultural facilities by Pohang aftershocks.

Geology and Geological Structure around Harar, NE Ethiopia (에티오피아 북동부 하라르 일대의 지질과 지질구조)

  • Ryoo, Chung-Ryul;Heo, Cheol-Ho;Yang, Seok-Jun;Alemu, Tadesse
    • The Journal of the Petrological Society of Korea
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    • v.24 no.2
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    • pp.65-75
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    • 2015
  • Around Harar in the northeastern part of the Ethiopia, the Precambrian granitic gneiss and gabbro bodies are developed with several pegmatites. The rock bodies in this area have been deformed by ductile and brittle deformations developing fold and ductile shear structure, and thrust and fault.

Subsurface Geological Structure of the Southwestern Part of Ogcheon Zone by Gravity Survey (1) (중력탐사에 의한 옥천대 남서부의 지하지질구조(1))

  • Kim, Sung Kyun;Ahn, Kun Sang;Oh, Jinyong
    • Economic and Environmental Geology
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    • v.30 no.4
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    • pp.363-369
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    • 1997
  • As a part of the study to know the deep geological structure of the Ogcheon Zone. gravity survey is performed along the survey line of which direction is roughly perpendicular to major faults of the Zone. Recent studies for petrology. geochemistry. and structural geology in south-western Ogcheon Zone are outlined. Raw gravity data are corrected to obtain Bouguer anomalies and the anomalies are interpreted to obtain subsurface structures along the survey line. The subterranean density discontinuities determined from the power spectrum method are appeared at depths of 15.4 km and 2.8 km. It is considered that the depth of 15.4 km indicates the boundary between upper and lower crust. Probably the depth of 2.8 km represents the boundary between upper volcanic formations and granites. Alternatively. the observed Bouguer anomalies are interpreted in terms of lateral density variation model. Finally. the subterranean geological structure to satisfy the Bouguer anomalies is presented through the iterative forward method in which results obtained from surface geological informations and from the inverse method are adopted as an initial model.

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Application of Self-Supported Diaphragm Wall Method Using Counterfort Technique (부벽식 기법을 사용한 자립식 지하연속벽 공법의 적용)

  • Jeong, Gyeong-Hwan;Jeong, Dong-Yeong;Park, Hun-Kook;Han, Kyoung-Tae;Ryu, Ji-Young
    • Proceedings of the Korean Geotechical Society Conference
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    • 2004.03b
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    • pp.775-782
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    • 2004
  • Recently, the cases which are constructed close by neighboring structure or underground structure are on the increase to get the utmost out of the land exploitation of underground space in the downtown area. As the building becomes larger, the excavation depth is getting deep, and the excavation area is getting, wide too. These are frequent occasions that the application of Strut or Anchor method is difficult, because of site boundary, civil application and the ground condition. Therefore, to solve these problem, we analyze and compare design with measuring data, change the design factor and show the improvement of course through the application of self-supported diaphragm wall using counterfort technique which is a new method. It is expected to be a contribution to the suitable exploitation method of construction.

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The Latest Progress on the Development of Technologies for $CO_2$ Storage in Marine Geological Structure and its Application in Republic of Korea (해저 지질구조내 $CO_2$ 저장기술의 연구개발 동향 및 향후 국내 실용화 방안)

  • Kang, Seong-Gil;Huh, Cheol
    • Journal of the Korean Society for Marine Environment & Energy
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    • v.11 no.1
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    • pp.24-34
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    • 2008
  • To mitigate the climate change and global warming, various technologies have been internationally proposed for reducing greenhouse gas emissions. Especially, in recent, carbon dioxide capture and storage (CCS) technology is regarded as one of the most promising emission reduction options that $CO_2$ be captured from major point sources (eg., power plant) and transported for storage into the marine geological structure such as deep sea saline aquifer. The purpose of this paper is to review the latest progress on the development of technologies for $CO_2$ storage in marine geological structure and its perspective in republic of Korea. To develop the technologies for $CO_2$ storage in marine geological structure, we carried out relevant R&D project, which cover the initial survey of potentially suitable marine geological structure fur $CO_2$ storage site and monitoring of the stored $CO_2$ behavior, basic design for $CO_2$ transport and storage process including onshore/offshore plant and assessment of potential environmental risk related to $CO_2$ storage in geological structure in republic of Korea. By using the results of the present researches, we can contribute to understanding not only how commercial scale (about 1 $MtCO_2$) deployment of $CO_2$ storage in the marine geological structure of East Sea, Korea, is realized but also how more reliable and safe CCS is achieved. The present study also suggests that it is possible to reduce environmental cost (about 2 trillion Won per year) with developed technology for $CO_2$ storage in marine geological structure until 2050.

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Traditional Medicine Resources and Traditional Medicine Information Shown on The Chosun Dynasty Geological Document (조선시대(朝鮮時代) '지리지(地理志)' 류(類)에 나타난 한약자원(韓藥資源) 및 고전의학(古傳醫學) 정보(情報))

  • Lee, Jeong-Hwa;Kim, Seong-Su
    • Korean Journal of Oriental Medicine
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    • v.13 no.3
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    • pp.69-78
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    • 2007
  • King Se-Jong, who had put much effort into maintaining the national structure, published geological documents to reinforce his authority and through these documents could see the nationwide distribution of medicinal resources. Since then the regional geological documents published in each region included information on the local medical environment of those times. This study is one that focuses on how to specifically understand oriental medicine resources and the contents of ancient medicine by applying the appropriate geological information.

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Geophysical Prospecting for Geothermal Resources at Northern Part of Kumseongsan, Euiseong (의성 금성산 북부지역의 지열자원 지구물리탐사)

  • Lee, Gidong;Han, Kihwan;Kim, Kibeom;Lee, Jongmoon
    • Journal of the Korean GEO-environmental Society
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    • v.7 no.6
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    • pp.35-44
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    • 2006
  • Various geophysical methods and geological survey were applied for prospecting of geothermal resources and the attitude of volcanic body at northern part of Kumseongsan, Euiseong. They include magnetic, self-potential, radioactive and resistivity methods, temperature logging near the earth's surface and geological survey. The results of this study are summarized as follows. Various geophysical anomalies is related to the geologically Cretaceous conduit. Anomalies of resistivity and temperature logging seem to be related to the geological structure and terrestrial heat. Small radioactive and self-potential anomalies seem to be associated with chemical character of rocks. The sedimentary rocks dip steeply toward the volcanic rocks, aquifuge. Ideal geological structure for bearing ground water and geothermal resources was founded in the study area. The study area and the adjacent two hot springs area consist of Cretaceous sedimentary and volcanic rocks, and have similar geology.

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Geophysical Investigation for Detecting a Bedrock and Geological Characterization in Natural Slope (자연사면에서 기반암 및 지질특성을 탐지하기 위한 지구물리 조사)

  • Park, Jong-Oh
    • The Journal of Engineering Geology
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    • v.19 no.1
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    • pp.1-8
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    • 2009
  • Geophysical surveys were conducted on an upper part of a natural slope located at Daejeon University. Electrical resistivity and seismic refraction measurements were carried out to obtain information on a weathered zone and internal structure at shallow depth, while AMT measurement a bed rock and geological structure at deep depth. With all the techniques applied, these results show a good correlation between electrical resistivity images and refraction velocity distributions for the characterization of a weathering and geological structure at depth. In particular, AMT survey seems to be the powerful tool for detecting a distribution of a bed rock with deep depth. The combined geophysical investigation produced a detailed image of a subsurface structure and improved well in the interpretation.

Development and Application of Landslide Analysis Technique Using Geological Structure (지질구조자료를 이용한 산사태 취약성 분석 기법 개발 및 적용 연구)

  • 이사로;최위찬;장범수
    • Spatial Information Research
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    • v.10 no.2
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    • pp.247-261
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    • 2002
  • There are much damage of people and property because of heavy rain every year. Especially, there are problem to major facility such as dam, bridge, road, tunnel, and industrial complex in the ground stability. So the counter plan for landslide or ground failure must be necessary In the study, the technique of regional landslide susceptibility assessment near the Ulsan petrochemical complex and Kumgang railway bridge was developed and applied using GIS. For the assessment, the geological structures such as bedding and fault were surveyed and the geological structure, topographic, soil, forest, and land use spatial database were constructed using CIS. Using the spatial database, the factors that influence landslide occurrence, such as slope, aspect, curvature and type of topography, texture, material, drainage and effective thickness of soil, type, age, diameter and density of forest, and land use were calculated or extracted from the spatial database. For application of geological structure, the geological structure line and fault density were calculated. Landslide susceptibility was analyzed using the landslide-occurrence factors by probability method that is summation of landslide occurrence probability values per each factors range or type. The landslide susceptibility map can be used to assess ground stability to protect major facility.

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Case Histories of Rock Slope Failure and Restoration (암반사면의 붕괴와 극복사례)

  • Ro, Byung-Don;Park, Wan-Seo
    • 한국방재학회:학술대회논문집
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    • 2007.02a
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    • pp.505-508
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    • 2007
  • Usually, cut-slope is the term that call rock slope. Therefore, the cause of instability of cut-slope is influenced generally in lithological and structure geological qualities including weathering disintegration. Through the several case studies, we could confirm that stabilization countermeasure also should be based in geological properties.

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