• Title/Summary/Keyword: Landslide analysis

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Analysis of Characteristics using Geotechnical Investigation on the Slow-moving Landslides in the Pohang-si Area (포항지역 땅밀림지의 지반조사를 통한 땅밀림 특성 분석)

  • Lee, Moon-Se;Park, Jae-Hyeon;Park, Yunseong
    • Journal of Korean Society of Forest Science
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    • v.108 no.2
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    • pp.233-240
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    • 2019
  • The aim of this study was to provide basic data that could identify and help prevent a slow-moving landslide using an analysis of the relationship between below-ground characteristics and water from three slow-moving landslide areas in Pohang, Gyeongsangbuk-do, South Korea. Surface surveys, resistivity, seismic exploration, well logging, and boring surveys were conducted in the three areas. The main direction of discontinuous surface was matched with the slope direction of the three landslides. The results indicatedthat slow-moving landslides might occur in the direction of the slope. Underground water was distributed within the crush zones within the three landslide areas and flowed along the tensile cracks. There was a significant difference (p<0.01) between the mean angle of the tensile cracks and that of the underground waterflow (p=0.8019). These results indicated that the progress of a slow-moving landslide can be forecast by monitoring the location and flow of underground water within a known slow-moving landslide area.

Monitoring the Symptoms of Landslide Using the Non Prism Totalstation (무프리즘 토탈스테이션을 이용한 산사태 징후 모니터링)

  • Yang, In-Tae;Park, Jae-Kook;Park, Gun;Kim, Jun-Suk
    • Proceedings of the Korean Society of Surveying, Geodesy, Photogrammetry, and Cartography Conference
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    • 2007.04a
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    • pp.409-412
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    • 2007
  • To minimize damages caused by landslides due to severe rain falls and storms during the rainy season every year, it is necessary to carry out research to monitor the symptoms of landslide in advance and prevent them. If proper actions ate taken in advance by monitoring the symptoms of landslide, personal and property damages caused by landslides can be prevented or minimized. This study tries to measure the movement of model slopes after causing displacement to each model slope using no prism Total Station and examine the applicability of Total Station by displacement through the analysis of the data.

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Thresholds of Rainfall Duration and Intensity for Predicting Abrupt Landslide Occurrence (돌발 산사태 예·경보를 위한 강우기준 설정 연구)

  • Kim, Seong-Pil;Park, Jae-Sung;Bae, Seung-Jong;Heo, Joon
    • Journal of The Korean Society of Agricultural Engineers
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    • v.56 no.4
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    • pp.53-58
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    • 2014
  • The objective of this study is to suggest rainfall threshold for landslide forecasting and warning. For this study, we chose the research area where landslide have occurred. And we performed infiltration-stability analysis with rainfall intensity-duration. As the results of this study, slope stability variation chart with rainfall intensity-duration are established. This kind of chart is believed to be able to be used for forecasting and warning the landslide caused by rainfall.

Application of Fuzzy Information Representation Using Frequency Ratio and Non-parametric Density Estimation to Multi-source Spatial Data Fusion for Landslide Hazard Mapping

  • Park No-Wook;Chi Kwang-Hoon;Kwon Byung-Doo
    • Journal of the Korean earth science society
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    • v.26 no.2
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    • pp.114-128
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    • 2005
  • Fuzzy information representation of multi-source spatial data is applied to landslide hazard mapping. Information representation based on frequency ratio and non-parametric density estimation is used to construct fuzzy membership functions. Of particular interest is the representation of continuous data for preventing loss of information. The non-parametric density estimation method applied here is a Parzen window estimation that can directly use continuous data without any categorization procedure. The effect of the new continuous data representation method on the final integrated result is evaluated by a validation procedure. To illustrate the proposed scheme, a case study from Jangheung, Korea for landslide hazard mapping is presented. Analysis of the results indicates that the proposed methodology considerably improves prediction capabilities, as compared with the case in traditional continuous data representation.

THE EFFECTS OF UNCERTAIN TOPOGRAPHIC DATA ON SPATIAL PREDICTION OF LANDSLIDE HAZARD

  • Park, No-Wook;Kyriakidis, Phaedon C.
    • Proceedings of the KSRS Conference
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    • 2008.10a
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    • pp.259-261
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    • 2008
  • GIS-based spatial data integration tasks have used exhaustive thematic maps generated from sparsely sampled data or satellite-based exhaustive data. Due to a simplification of reality and error in mapping procedures, such spatial data are usually imperfect and of different accuracy. The objective of this study is to carry out a sensitivity analysis in connection with input topographic data for landslide hazard mapping. Two different types of elevation estimates, elevation spot heights and a DEM from ASTER stereo images are considered. The geostatistical framework of kriging is applied for generating more reliable elevation estimates from both sparse elevation spot heights and exhaustive ASTER-based elevation values. The effects of different accuracy arising from different terrain-related maps on the prediction performance of landslide hazard are illustrated from a case study of Boeun, Korea.

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Prediction of Potential Landslide Sites Using Determinitstic Model (결정론적 기법을 이용한 산사태 위험지 예측)

  • Cha, Kyung-Seob;Chang, Pyoung-Wuck;Woo, Chull-Woong;Kim, Seong-Pil
    • Journal of The Korean Society of Agricultural Engineers
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    • v.47 no.6
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    • pp.37-45
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    • 2005
  • Almost every year, Korea has been suffered from serious damages of lives and properties, due to landslides that are triggered by heavy rains in monsoon season. In this paper, we systematized the physically based landslide prediction model which consisted of 3 parts, infinite slope stability analysis model, groundwater flow model and soil depth model. To evaluate its applicability to the prediction of landslides, the data of actual landslides were plotted on the predicted areas on the GIS map. The matching rate of this model to the actual data was $84.8\%$. And the relation between hydrological and land form factors and potential landslide were analyzed.

Suggestion and Evaluation for Prediction Method of Landslide Occurrence using SWAT Model and Climate Change Data: Case Study of Jungsan-ri Region in Mt. Jiri National Park (SWAT model과 기후변화 자료를 이용한 산사태 예측 기법 제안과 평가: 지리산 국립공원 중산리 일대 사례연구)

  • Kim, Jisu;Kim, Minseok;Cho, Youngchan;Oh, Hyunjoo;Lee, Choonoh
    • Journal of Soil and Groundwater Environment
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    • v.26 no.6
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    • pp.106-117
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    • 2021
  • The purpose of this study is prediction of landslide occurrence reflecting the subsurface flow characteristics within the soil layer in the future due to climate change in a large scale watershed. To do this, we considered the infinite slope stability theory to evaluate the landslide occurrence with predicted soil moisture content by SWAT model based on monitored data (rainfall-soil moisture-discharge). The correlation between the SWAT model and the monitoring data was performed using the coefficient of determination (R2) and the model's efficiency index (Nash and Sutcliffe model efficiency; NSE) and, an accuracy analysis of landslide prediction was performed using auROC (area under Receiver Operating Curve) analysis. In results comparing with the calculated discharge-soil moisture content by SWAT model vs. actual observation data, R2 was 0.9 and NSE was 0.91 in discharge and, R2 was 0.7 and NSE was 0.79 in soil moisture, respectively. As a result of performing infinite slope stability analysis in the area where landslides occurred in the past based on simulated data (SWAT analysis result of 0.7~0.8), AuROC showed 0.98, indicating that the suggested prediction method was resonable. Based on this, as a result of predicting the characteristics of landslide occurrence by 2050 using climate change scenario (RCP 8.5) data, it was calculated that four landslides could occur with a soil moisture content of more than 75% and rainfall over 250 mm/day during simulation. Although this study needs to be evaluated in various regions because of a case study, it was possible to determine the possibility of prediction through modeling of subsurface flow mechanism, one of the most important attributes in landslide occurrence.

Strategy of Technology Development for Landslide Hazards by Patent Analysis (특허 분석을 통한 산사태재해 관련 기술개발 전략)

  • Bae, Khee Su;Sawng, Yeong-Wha;Chae, Byung-Gon;Choi, Junghae;Son, Jeong Keun
    • The Journal of Engineering Geology
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    • v.24 no.4
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    • pp.615-629
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    • 2014
  • This study analyzed existing patents related to real-time monitoring and detection technology for landslides on natural terrain. The purpose of patent analysis is to understand landslide hazard technology trends and to develop new advanced technology. This study searched patent data using key words related to landslide monitoring and detection in Korea, the USA, Japan, China (Hong Kong), Europe, and Taiwan. The patents were divided into five main categories and five to seven subcategories in each main category and analyzed by year, country, and applicants. The results were utilized to derive a portfolio of promising technologies for each country. The analysis results will also contribute to the development of more effective research strategies and to categorize research findings from previous studies on landslide hazards.

Developing Forecast Technique of Landslide Hazard Area by Integrating Meteorological Observation Data and Topographical Data -A Case Study of Uljin Area- (기상과 지형자료를 통합한 산사태 위험지 예측 기법 개발 -울진지역을 대상으로-)

  • Jo, Myung-Hee;Jo, Yun-Won
    • Journal of the Korean Association of Geographic Information Studies
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    • v.12 no.2
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    • pp.1-10
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    • 2009
  • Recently the large scale of forest disaster such as landslide and forest fire gives a very bad impact on not only forest ecosystem but also farm business so that it has became the main issue of environmental problems. In this study, the landslide hazard area forecast method was developed by considering not only the topographic thematic maps based on GIS and satellite images but also amount of rainfall data, which are very important factors of landslide. Uljin-gun was selected as the study area and the GIS weight score and overlay analysis were applied to topographical map and meteorological observation map. Finally the landslide area distribution map was constructed by considering the evaluation criteria. Also, the accuracy could be acquired by comparing the landslide hazard area forecast map and real damaged area extracted from satellite image.

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Study on Landslide using GIS and Remote Sensing at the Kangneung Area(II)-Landslide Susceptibility Mapping and Cross-Validation using the Probability Technique (GIS 및 원격탐사를 이용한 2002년 강릉지역 태풍 루사로 인한 산사태 연구(II)-확률기법을 이용한 강릉지역 산사태 취약성도 작성 및 교차 검증)

  • Lee Saro;Lee Moung-Jin;Won Joong-Sun
    • Economic and Environmental Geology
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    • v.37 no.5
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    • pp.521-532
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    • 2004
  • The aim of this study is to evaluate the susceptibility of landslides at Kangneung area, Korea, using a Geographic Information System (GIS) and remote sensing. Landslide locations were identified from interpretation of satellite image and field surveys. The topographic, soil, forest, geologic, lineament and land cover data were collected, processed and constructed into a spatial database using GIS and remote sensing data. Using frequency ratio model which is one of the probability model, the relationships between landslides and related factors such as slope, aspect, curvature and type of topography, texture, material, drainage and effective thickness of soil, type, age, diameter and density of wood, lithology, distance from lineament and land cover were calculated as frequency ratios. Then, the frequency ratio were summed to calculate a landslide susceptibility indexes and the landslide susceptibility maps were generated using the indexes. The results of the analysis were verified and cross-validated using actual landslide location data. The verification results showed satisfactory agreement between the susceptibility map and the existing data on landslide locations.