• Title/Summary/Keyword: geological region

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Case Study on the Mitigation of Dangerous Slope Considering the Value of Geoheritage (지질유산 가치를 고려한 위험비탈면 보존 방안 사례 연구)

  • Jeong, Jun-Ho;Kim, Seung-Hyun;Park, Byung-suk;Woo, Yong-Hoon;Kang, Yun-seok;Koo, Ho-bon;Son, Moon
    • The Journal of Engineering Geology
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    • v.30 no.1
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    • pp.71-84
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    • 2020
  • Various geological structures are found on the slope of Bangnim district in Pyeongchang, Gangwon-do, based on the Paleozoic Joseon Supergroup Limestone. The recumbent fold observed on the slope is a very rare geological structure that has not been found in Korea, and has important academic value in exploring the formation process of the Paleozoic geological structures in the Gangwon region. In this study, discussed the geological value of the geological structure observed on the slope of the road, and studied the management method of rockfall problem slopes. The state of development of recumbent folds has conservation value in geological scarcity and specificity. Preservation management measures should be prepared through the protection of slopes and measures to reduce of rockfall risks as geoheritage with an important value in geology science and education. Furthermore, it is expected to be preserved and utilized as a geopark.

The Distribution Characteristics of Topographical Relieves at Each Geological Area in Gyeongsangbuk-do Province using GIS (GIS를 이용한 경상북도 지질 지역별 지형 기복의 분포 특성)

  • KIM, Dae-Sik;LEE, Gwang-Ryul
    • Journal of The Geomorphological Association of Korea
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    • v.17 no.3
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    • pp.49-57
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    • 2010
  • The topographical rolling distribution characteristics of 10 geological areas in Gyeongsangbuk-do are analyzed using GIS. PEs, PEgrgn, Pp2, Kav·Kiv, and Khgr regions occupy the more than 60% that are a steep slope-a high elevation and a steep slope-a middle elevation region, and form high moutains in Gyeongsangbuk-do. Meanwhile, Ke1-9 and Te1-2 regions take possession of the more than 70% that are a low elevation region. Ke1-9 region form landward flatlands and hills around Nakdong river and tributaries of Nakdong river in Gyeongsangbuk-do. Then, Te1-2 region form coastal lowlands adjacent the East sea in Gyeongsangbuk-do. Also, Jgr region take possession of the more than 70% that are a middle elevation region, and form low moutains or flatlands in Gyeongsangbuk-do. Finally, Ols1 region take possession of the more than 50% that are a steep slope region, and form landward moutains in Gyeongsangbuk-do.

An Experimental Study on the Availability of Underground Air Energy Source in Non-Activity Volcanic Island (비활성 화산지역의 지중공기열원 에너지 이용에 관한 실험적 연구)

  • Kim, Yong-Hwan;Park, Sung-Seek;Kim, Woo-Jung;Kim, Nam-Jin;Hyun, Myung-Taek
    • Journal of the Korean Solar Energy Society
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    • v.34 no.5
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    • pp.73-80
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    • 2014
  • This study introduces and analyzes the geothermal energy availability in Non-active volcanic region. Jeju island in Korea is situated in non-active volcanic region. The island is composed of rock with high pore and clinker, scoria geological layer formed by volcanic activity about two million ago. Volcanic geological layers with porous characteristics have air, vapor, water and a underground structure through which air or water can move easily. For this reason, it is probable that the mechanism of energy acquisition is by convective heat transfer. For this presumption, the availability of underground air as energy source has been studied here through theoretical analysis and experimental data. The energy output of our system ranged from 2,485,076 kJ/day to 4,060,978 kJ/day monitored using variable velocity air flow controller. Our system has capability to be a reliable energy source irrespective of environmental changes. Consequently, underground air can be utilized for energy source and provide the optimal design of heating/cooling system.

Recent Observations of Micro-earthquakes and Its Implications for Seismic Risk in the Seoul Metropolitan Region, Korea (최근 관측된 수도권 지역 미소지진과 지진위험성)

  • Kim, Kwang-Hee;Han, Minhui;Kim, Myeongsu;Kyung, Jai-Bok
    • The Journal of the Petrological Society of Korea
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    • v.25 no.3
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    • pp.253-260
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    • 2016
  • A moment magnitude 3.1 earthquake occurred in the Seoul metropolitan region (SMR), Korea, on 9 February 2010. The unexpected shaking attracted much attention and raised concerns about the seismic hazards and risks in the SMR, which was regarded as an area safe from any earthquake hazard. The SMR has a population of 25 million and is one of the largest metropolitan areas in the world. A shakemap for a scenario earthquake with magnitude 6.5 and focal depth 12 km implies that the SMR will be exposed to serious risk because of its large population and the high vulnerability of its buildings. Although the instrumentally recorded earthquakes discussed in this article cannot be classified as major events, they should not be discounted as insignificant. Considering the low seismicity, micro-earthquakes below the magnitude of a conventional seismic network can achieve would be used to estimate background information in the evaluation of earthquake hazards and risks.

RADARSAT SAR Investigations of Lineament and Spring Water in Cheju Island (RADARSAT SAR 자료를 이용한 제주도 선구조 연구 및 용천 특성 연구)

  • 원중선;류주형;지광훈
    • Korean Journal of Remote Sensing
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    • v.14 no.4
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    • pp.325-342
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    • 1998
  • Two RADARSAT SAR images with different modes acquired by Canadian Space Agency to test the effectiveness of geological lineament extraction and spring water detection over the Cheju Island. Geological lineaments are poorly developed this basalt dominant volcanic island, but more linear features can be extracted when SAR and TM images are simultaneously analyzed than when TM image alone is used. This results mainly owe to the facts that RADARSAT SAR systems are able to provide data with different frequencies, azimuth, and incidence angles. Distribution of spring water along coast is poorly correlated with geological lineaments or drainage pattern, but those in middle range of mountain region are developed along geological lineaments. Detection of spring water using remotely sensed images are turned out to be very difficult to achieve. Radial shaped sea surface temperature anomaly derived from TM thermal band should be the best candidate for spring water, but the resolution is not high enough. We also investigate the normalized radar cross section (or sigma naught) converted from RADARSAT and ERS-1 SAR data but to discriminate the spring water effectively except where relatively large water mass is observed on land side. Speckle noise and irregularity in physical sea surface condition are the serious obstacles for this application. ERS-1 SAR image acquired in low incidence angle was more useful for geological lineament estimation and water body study than RADARSAT SAR images with high incidence angles. Therefore the selection of incidence angle is critical in geological and spring water applications of SAR images, and low incidence angles less than about 30$^{\circ}$ are recommended to monitor the Cheju volcanic island.

Building Information Modeling of Caves (CaveBIM) in Jeju Island at a Specific Site below a Road at Jaeamcheon Lava Tube and at a Broader Scale for Hallim Town (제주도 한림 재암천굴과 도로 교차구간의 CaveBIM 구축)

  • An, Joon-Sang;Kim, Wooram;Baek, Yong;Kim, Jin-Hwan;Lee, Jong-Hyun
    • The Journal of Engineering Geology
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    • v.32 no.4
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    • pp.449-466
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    • 2022
  • The establishment of a complete geological model that includes information about all the various components at a site (such as underground structures and the compositions of rock and soil underground space) is difficult, and geological modeling is a developing field. This study uses commercial software for the relatively easy composition of geological models. Our digital modeling process integrates a model of Jeju Island's 3D geological information, models of cave shapes, and information on the state of a road at the site's upper surface. Among the numerous natural caves that exist in Jeju Island, we studied the Jaeamcheon lava tube near Hallim town, and the selected site lies below a road. We developed a digital model by applying the principles of building information modeling (BIM) to the cave (CaveBIM). The digital model was compiled through gathering and integrating specific data: relevant processes include modeling the cave's shape using a laser scanner, 3D geological modeling using geological information and geophysical exploration data, and modeling the surrounding area using drones. This study developed a global-scale model of the Hallim region and a local-scale model of the Jaeamcheon cave. Cross-validation was performed when constructing the LSM, and the results were compared and analyzed.

InSAR Studies of Alaskan Volcanoes

  • Lu Zhong;Wicks Chuck;Dzurisin Dan;Power John
    • Proceedings of the KSRS Conference
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    • 2004.10a
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    • pp.47-52
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    • 2004
  • Interferometric synthetic aperture radar (InSAR) is a remote sensing technique capable of measuring ground surface deformation with sub-centimeter precision and spatial resolution in tens-of-meters over a large region. This paper highlights our on-going investigations of Aleutian volcanoes with SAR images acquired from European ERS-1 and ERS-2, Canadian Radarsat-l, and Japanese JERS-l satellites.

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Intensity-Magnitude Relation in the Sino-Korean Craton (중국-한국 육괴에서 진도-규모의 관계식 추정)

  • 이기화;이전희
    • Proceedings of the Earthquake Engineering Society of Korea Conference
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    • 2001.09a
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    • pp.3-10
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    • 2001
  • In order to establish the intensity-magnitude relation far the Korean earthquakes, those relations for the earthquakes in the Sino-Korean craton were estimated. In this process, earthquake data of northeastern China region whose geological environment is similar to Korea Peninsula were also utilized. These data were analyzed not only with linear fit, but also with non-linear fit. The fellowing relation, M=0.57 $\times$ 1$_{e}$ + 2.86, seems appropriate for the present, but its validity should be tested more in the future.e.

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InSAR Studies of Alaska Volcanoes

  • Lu Zhong;Wicks Chuck;Dzurisin Dan;Power John
    • Korean Journal of Remote Sensing
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    • v.21 no.1
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    • pp.59-72
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    • 2005
  • Interferometric synthetic aperture radar (InSAR) is a remote sensing technique capable of measuring ground surface deformation with sub-centimeter precision and spatial resolution in tens-of­meters over a large region. This paper describes basics of InSAR and highlights our studies of Alaskan volcanoes with InSAR images acquired from European ERS-l and ERS-2, Canadian Radarsat-l, and Japanese JERS-l satellites.

Effects of corner cuts and angles of attack on the Strouhal number of rectangular cylinders

  • Choi, Chang-Koon;Kwon, Dae-Kun
    • Wind and Structures
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    • v.6 no.2
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    • pp.127-140
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    • 2003
  • An investigation into the effect of corner cuts on the Strouhal number of rectangular cylinders with various dimensional ratios and various angles of attack is described. The Strouhal number given as a function of corner cut size is obtained directly from the aerodynamic behavior of the body in a uniform flow through a series of wind-induced vibration tests. For a quick verification of the validity of the Strouhal numbers obtained in this way, they are compared with the approximated the Strouhal numbers based on Shiraishi's early research. The test results show that the Strouhal number of the model with various corner cuts has a fluctuating trend as the angle of attack changes. For each cutting ratio as the angle of attack increases at each cutting ratio above $15^{\circ}$, the Strouhal number decreases gradually, and these trends are more evident for larger corner cut sizes. However, a certain corner cut size which is effective in reducing the wind-induced vibration can be identified by larger Strouhal numbers than those of other corner cut sizes. Three distinct characteristics of Strouhal number variation can be identified in three regions which are termed as Region I, II, and III based on the general trend of the test results. It is also found that the corner cut is effective in one region (Region-II) and less effective in another one (Region-III) when only the vortex-induced vibration occurs.