• Title/Summary/Keyword: 액상화 재해지도

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Comparison of Liquefaction Probability Map Regarding with Geotechnical Information and Spatial Interpolation Target (공간보간 대상 및 지반정보에 따른 액상화 확률지도 비교)

  • Song, Seongwan;Hwang, Bumsik;Cho, Wanjei
    • Journal of the Korean GEO-environmental Society
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    • v.22 no.11
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    • pp.5-13
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    • 2021
  • The interest of expecting the liquefaction damage is increasing due to the liquefaction in Pohang in 2017. Liquefaction is defined as a phenomenon that the ground can not support the superstructure due to loss of the strength of the ground. As an alternative against this, many studies are being conducted to increase the precision and to compose a liquefaction hazard map for the purpose of identifying the scale of liquefaction damage using the liquefaction potential index (LPI). In this research, in order to analyze the degree of precision with regard to spatial interpolation objects such as LPI value and geotechnical information for LPI determination, liquefaction hazard map were made for the target area. Furthermore, based on the trend of precision, probability value was analyzed using probability maps prepared through qualitative characteristics. Based on the analysis results, the precision of the liquefaction hazard map setting the spatial interpolation object as geotechnical information is higher than that as LPI value. Furthermore, the precision of the liquefaction hazard map does not affect the distribution of the probability value.

Seismic Risk Assessment on Buried Electric Power Tunnels with the Use of Liquefaction Hazard Map in Metropolitan Areas (액상화 재해지도를 이용한 수도권 전력구 매설지반의 지진시 위험도 평가)

  • Baek, Woohyun;Choi, Jaesoon
    • Journal of Korean Society of Disaster and Security
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    • v.12 no.1
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    • pp.45-56
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    • 2019
  • In this study, the seismic risk has been evaluated by setting the bedrock acceleration to 0.154g which, was taking into consideration that the earthquake return period for the buried electric power tunnels in the metropolitan area to be 1,000 years. In this case, the risk assessment during the earthquake was carried out in three stages. In the first stage, the site classification was performed based on the site investigation data of the target area. Then, the LPI(Liquefaction Potential Index) was applied using the site amplification factor. After, candidates were selected using a hazard map. In the second stage, risk assessment analysis of seismic response are evaluated thoroughly after the recalculation of the LPI based on the site characteristics from the boring logs around the electric power area that are highly probable to be liquefied in the first stage. The third Stage visited the electric power tunnels that are highly probable of liquefaction in the second stage to compensate for the limitations based on the borehole data. At this time, the risk of liquefaction was finally evaluated based off of the reinforcement method used at the time of construction, the application of seismic design, and the condition of the site.

Correlations of Earthquake Accelerations and LPIs for Liquefaction Risk Mapping in Seoul & Gyeonggi-do Area based on Artificial Scenarios (서울, 경기지역의 시나리오별 액상화 위험지도 작성을 위한 지진가속도와 LPI 상관관계 분석)

  • Baek, Woohyun;Choi, Jaesoon
    • Journal of the Korean GEO-environmental Society
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    • v.20 no.5
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    • pp.5-12
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    • 2019
  • On November 15, 2017, a unpredictable liquefaction damage was occurred at the $M_L=5.4$ Pohang earthquake and after, many researches have been conducted in Korea. In Korea, where there were no cases of earthquake damage, it has been extremely neglectable in preparing earthquake risk maps and building earthquake systems that corresponded to prevention and preparation. Since it is almost impossible to observe signs and symptoms of drought, floods, and typhoons in advance, it is very effective to predict the impacts and magnitudes of seismic events. In this study, 14,040 borehole data were collected in the metropolitan area and liquefaction evaluation was performed using the amplification factor. Based on this data, liquefaction hazard maps were prepared for ground accelerations of 0.06 g, 0.14 g, 0.22 g, and 0.30 g, including 200years return period to 4,800years return period. Also, the correlation analysis between the earthquake acceleration and LPI was carried out to draw a real-time predictable liquefaction hazard map. As a result, 707 correlation equations in every cells in GIS map were proposed. Finally, the simulation for liquefaction risk mapping against artificial earthquake was performed in the metropolitan area using the proposed correlation equations.

Liquefaction Hazard Assessment according to Seismic Recurrence Intervals Using Simple Estimating Method in Busan City, Korea (간이평가법을 이용한 지진재현주기별 부산광역시 액상화 재해 평가)

  • Lim, Hyunjee;Jeong, Rae-yoon;Oh, Dongha;Kang, Hyejin;Son, Moon
    • The Journal of Engineering Geology
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    • v.30 no.4
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    • pp.589-602
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    • 2020
  • As can be seen in many earthquakes, liquefaction causes differential settlement, which sometimes produces serious damages such as building destruction and ground subsidence. There are many possible active faults near the Busan city and the Yangsan, Dongrae, and Ilgwang faults among them pass through the city. The Busan city is also located within the influence of recent earthquakes, which occurred in the Gyeongju, Pohang, and Kumamoto (Japan). Along the wide fault valleys in the city, the Quaternary unconsolidated alluvial sediments are thickly accumulated, and the reclaimed lands with beach sediments are widely distributed in the coastal area. A large earthquake near or in the Busan city is thus expected to cause major damage due to liquefaction in urban areas. This study conducted an assessment of the liquefaction hazard according to seismic recurrence intervals across the Busan city. As a result, although there are slight differences in degree depending on seismic recurrence intervals, it is predicted that the liquefaction potential is very high in the areas of the Nakdonggang Estuary, Busan Bay, Suyeong Bay, and Songjeong Station. In addition, it is shown that the shorter the seismic recurrence interval, the greater difference the liquefaction potential depending on site periods.

Developing Geologic Loss Estimation Factors : Effect of DEM Resolution in Site Classification (지질재해예측 입력인자 개발 : DEM 해상도가 지반분류에 미치는 영향)

  • Kang, Su Young;Kim, Kwang-Hee
    • 한국방재학회:학술대회논문집
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    • 2011.02a
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    • pp.161-161
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    • 2011
  • 지진, 산사태, 액상화 등의 지질재해 예측을 위한 지역적 지반특성을 규명하기 위해서 지질도 또는 지형도를 이용하여 간접적인 방법이 사용되기도 한다. DEM에서 추출한 경사도는 지반분류 시 하나의 기준으로 사용되어질 수 있고, 이때 DEM의 해상력에 따라 그 결과가 다르게 산출될 수도 있다. 이번 연구에서는 DEM의 해상력에 따라 우리나라 일부지역의 지반분류 결과에 어떤 영향을 미치는지 살펴보았다. 각기 다른 해상도의 DEM을 적용하여 우리나라 동남부 지형을 경사도 기준으로 지반분류한 후 그 면적차이를 해상도별로 비교한 결과, 지반분류 C 지역의 면적 변화가 가장 뚜렷하였다. $V_s30$ 범위로 분류한 결과에서는 180 m/sec 이하의 지역에서 해상도별로 가장 큰 변화가 있었다. 고해상도에서는 지반분류 B와 E의 지역에서 면적이 저해상도 보다 크게 산출되는 경향이 있었고, 저해상도에서는 지반분류 C와 D 지역의 면적이 고해상도 보다 크게 산출되는 경향이 있었다. 이는 DEM의 해상도가 낮아질수록 각기 다른 지반정보를 함유한 작은 셀이 큰 셀로 만들어지는 과정에서 평균화되는 지반정보가 과대평가 또는 저평가되었기 때문이다. 연구지역 내 시추지역의 지반과 지반분류 결과를 비교하면 해상도별로 78%~52%까지 일치하였고, 고해상도에서 일치율이 더 높았다. 지형의 변화가 심하고 인구나 산업시설이 밀집된 재해 고위험군 지역은 고해상도의 지도를 이용하고, 지형의 변화가 없거나 단단한 지반의 지역은 재해가 상대적으로 작아서 저해상도의 사용으로 자료처리 시간의 효율성을 증대시키는 방안도 생각할 수 있다.

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Effects of DEM Resolutions in Site Classification (DEM 해상도가 지반분류에 미치는 영향)

  • Kang, Su-Young;Kim, Kwang-Hee
    • Journal of Korean Society for Geospatial Information Science
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    • v.19 no.1
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    • pp.21-28
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    • 2011
  • Site conditions affect the magnitude of loss due to geologic hazards including, but not limited to, earthquakes, landslides and liquefaction. Reliable geologic loss estimation system requires site information which can be achieved by GIS-based method using geologic or topographic maps. Slope data derived from DEM can be an effective indicator for classifying the site conditions. We studied and discussed the effect of different DEM resolutions in the site classification. We limited the study area to the south-eastern Korea and used two different resolutions of DEMs to observe discrepancies in the site classification results. Largest discrepancy is observed in the areal coverage of site class C(very dense soil and soft rock) and E(soft soil). Comparison of results shows that more areas are classified as site class B(general rock) or E(soft soil) when we use higher resolution DEM. The comparison also shows that more areas are classified as site class C or D(stiff soil) using lower resolution DEM. The comparison of results using resampled DEMs with different resolutions shows that the areal coverage of site class B and E decreases with decreasing resolutions. On the contrary, areal coverage of site class C and D increase with decreasing resolutions. Loss estimation system can take advantage of higher-resolution DEMs in the area of rugged or populated to obtain precise local site information.