• Proceedings of the Korea Water Resources Association Conference
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• 2016.05a
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• pp.256-256
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• 2016

우리나라는 산지가 국토의 64%이상으로 토석류 등 지반재해의 위험성에 노출되어 있다. 토석류에 의한 피해는 예측하기 매우 힘들고 외력도 한순간에 가옥을 파괴할 정도로 매우 거대하기 때문에 지진에 의한 피해를 제외하고는 매년 반복하여 막대한 재산 및 인적손실을 발생시키고 있는 재해이다. 도심지의 경우 토석류의 피해발생시 도로 및 건물 등 재산과 인적 피해가 크기 때문에 큰 이슈화가 되며 토석류가 산지 내에서 발생할 경우 해당 피해지역에 마을 민가나 교량 등이 위치하지 않으면 토석류의 피해를 인식하기 어려워 이에 따른 조치도 늦어지고 있다. 이에 국내 및 국외에서는 산지 및 도심지의 토석류 피해를 저감하기 위하여 토석류 유출저감시설(사방댐)의 설치를 통하여 토석류 흐름 및 인공구조물들을 보호하고 있다. 본 연구에서는 토석류 수치모형인 RAMMS모형과 Flo-2d모형을 이용하여 동일 매개변수를 적용 후 토석류 수치모델링을 실시하였다. 토석류 피해지에 토석류 유출저감시설의 존재 유 무에 따른 토석류 피해범위, 유출량 등을 산정하였으며 토석류 유출저감시설의 위치에 따른 피해저감 효과를 분석하였다.

• Proceedings of the Korea Water Resources Association Conference
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• 2009.05a
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• pp.1482-1488
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• 2009

최근 전 세계적인 기후변화로 인하여 홍수 해일 지진 등의 자연재해가 거대해지고 빈번하게 발생되고 있다. 이러한 점차 대형화되고 다양화되는 자연재해발생시 국민의 생명과 재산 피해를 최소화하기 위한 다양한 방안이 수립되고 있으며, 특히 풍수해에 대비하기 위한 방안으로써 비상대처계획(Emergency Action Plan, 이하 EAP)수립, 홍수위험지도 및 비상대피지도 등 재해지도 제작, 홍수재해관리시스템 개발 등이 이루어지고 있다. 특히 EAP는 이러한 점차 대형화되고 다양화되는 자연재해에 대비하기 위한 방안으로써, 재해 발생시 국민의 생명과 재산 피해를 최소화하기 위해 시설물 지역의 관리주체 및 유관기관이 발생 가능한 비상상황을 미리 예측하고 대응조치를 신속하고 효율적으로 집행할 수 있도록 구성되어 있으며, 이를 시스템화 한 것이 비상대처시스템(Emergency Action System, 이하 EAS)이라 할 수 있다. 현재 우리나라를 비롯하여 미국, 유럽, 일본 등 선진국을 중심으로 댐 저수지 붕괴에 대비한 EAP 수립을 의무화하고 그 대상 범위를 확장하는 단계에 있으며, 홍수위험지도 및 비상대피지도 제작 등에 있어서 일부 선진국의 경우 다양한 시나리오와 시민의 복합적인 요구를 반영하는 시도를 진행 중에 있다. 또한 일부 선진국의 경우 비상대처계획을 반영한 홍수재해통합관리시스템 구축이 진행중에 있으며, 일본의 경우 첨단기술의 접목을 통해 시민의 대피 시뮬레이션 모델을 개발하는 단계에 이르고 있다. 따라서 본 연구에서는 풍수해에 대비해 수립된 국내 외 EAP, 재해관련 지도, 홍수재해관리시스템 등에 대한 사례조사를 통하여 통합적인 비상대처 및 관리가 가능한 표준화된 EAS 모델의 정립 방향을 모색하고자 한다.

• Journal of Navigation and Port Research
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• v.29 no.8 s.104
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• pp.661-666
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• 2005

Recent warnings indicate that there is a potential risk of massive earthquake. These earthquakes could produce large-scale tsunamis. Consideration of the effect of Tsunami to the moored ship is very important bemuse it brings the loss of life and vast property damage in a viewpoint of ship operations within a harbor. If a tsunami occurs, a ship in a harbor may begin drifting in case of ship entering and departing harbor, and breakage of mooring rope and drifting of moored ship are happened. And extremely serious accident, such as stranding and collision to a quay, might occur. On the other hand, since the tsunami consists of approximately component waves of several minutes, there is a possibility of resonance with the long period motion of mooring vessel. As the speed of Tsunami is much faster than tidal current in a harbor, a strong resisting force might act on the moored ships. In this paper, the numerical simulation procedure in the matter of ship motions due to the attack of large-scale tsunamis are investigated and the effects on the ship motions and mooring loads are evaluated by numerical simulation.

• Journal of the Korea institute for structural maintenance and inspection
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• v.20 no.4
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• pp.1-8
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• 2016

Recently, buildings tend to be large size, complex shape and functional. As the size of buildings is becoming massive, the need for structural health monitoring(SHM) technique is ever-increasing. Various SHM techniques have been studied for buildings which have different dynamic characteristics and are influenced by various external loads. Generally, the visual inspection and non-destructive test for an accessible point of structures are performed by experts. But nowadays, the system is required which is online measurement and detect risk elements automatically without blind spots on structures. In this study, in order to consider the response of non-linear structures, proposed a signal feature extraction and the adaptive threshold setting algorithm utilized to determine the abnormal behavior by using statistical methods such as control chart, root mean square deviation, generalized extremely distribution. And the performance of that was validated by using the acceleration response of structures during earthquakes measuring system of forced vibration tests and actual operation.

• Economic and Environmental Geology
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• v.57 no.1
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• pp.1-15
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• 2024

The Melanesian region in the western Pacific is dominated by complex plate tectonics, with the largest oceanic plateau, the OntongJava plateau, and a hotspot, the Caroline Islands. To better understand the complex geodynamics of the region, we estimate P- and S-velocity models and 𝛿 (V_P/V_S) model by using relative teleseismic travel times measured at seismometers on land and the seafloor. Our results show high-velocity anomalies in the subduction zones of the Melanesian region to a depth of about 400 km, which is thought to be subducting Solomon Sea, Bismarck, and Australian plates along plate boundaries. Along subduction zones, positive 𝛿 (V_P/V_S) anomalies are found, which may be caused by partial melting due to dehydration. A broad high-velocity anomaly is observed at 600 km depth below the Ontong-Java plateau, with a negative 𝛿 (V_P/V_S) anomaly. This is thought to be a viscous and dry remnant of the Pacific plate that subducted at 45-25 Ma, with a low volume of fluids due to dehydration for a long period in the mantle transition zone. Beneath the Caroline Islands, a strong low-velocity anomaly is obseved to a depth of 800 km and appears to be connected to the underside of the remnant Pacific plate in the mantle transition zone. This suggests that the mantle plume originating in the lower mantle has been redirected due to the interaction with the remnant Pacific plate and has reached its current location. The mantle plume also has a positive 𝛿 (V_P/V_S) anomaly, which is thought to be due to the influence of embedded fluids or partial melting. A high-velocity anomaly, interpreted as an effect of the thick lithosphere beneath the Ontong-Java plateau, is observed down to 300 km depth with a negative 𝛿 (V_P/V_S) anomaly, which likely indicate that little fluid remains in the melt residue accumulated in the lithosphere.

• Geophysics and Geophysical Exploration
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• v.21 no.1
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• pp.26-32
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• 2018

The Northeast China is an important site geologically and geophysically because of a huge volcano called Mt. Baekdu, which is one of the largest volcanoes in the world. Signs of eruption have been recently observed and people are keen to its behavior. We carried out relative travel time tomography to investigate the velocity structure between 100 ~ 600 km depth beneath Northeast China. We used teleseismic data during 2009 ~ 2011 recorded in NecessArray provided by IRIS (Incorporated Research Institute for Seismology). The relative observations were obtained by using the multi-channel cross-correlation method. Based on the tomographic results, we observed that the locations beneath which low-velocity zones are observed coincide with the locations of several volcanic regions in Northeast China. A low-velocity anomaly is revealed beneath Mt. Baekdu down to 600 km depth, which is thought to the main origin of the magma supply for Mt. Baekdu. Another low velocity anomaly is observed beneath east of the Datong volcano down to around 300 km depth, which is inferred to be related to an upwelling from deep mantle. We observed a low velocity anomaly beneath the Wudalianchi volcano down to around 200 km depth, which may imply that this volcano has been formed by an upwelling from the asthenosphere.