• 한국환경복원기술학회지
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• 제21권2호
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• pp.1-11
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• 2018

As a result of climate change, mountain sediment disasters due to localized heavy rain and mountain development are occuring more frequently, thus, increasing social attention to and demand for soil erosion control projects. However, since 2011 Seoul Wumyeon Mountain landslide, the public is expressing increasing anxiety as well as negative perception regarding defective project results. Therefore, this study investigated promotional terms and information media related to soil erosion control projects according to the consumer in order to increase awareness of soil erosion control projects. In this study, the information consumers were divided into experts and the general public and conducted a survey related to promotional terms and media for communicating relevant information. In the result, the experts chose landslide prevention and recovery projects (41.8%) as an appropriate promotional term for soil erosion control projects. The general public, however, chose mountain sediment disaster prevention projects (32.5%) as the appropriate promotional term. However, the analysis showed that it would be necessary to develop an promotional term that can encompass the concept of 'disaster prevention' including forest and soil disaster as the word 'landslide' can suggest soil erosion control is limited to landslides only. In the survey regarding the media for communicating information related to soil erosion control projects according to the consumer type, the experts preferred radio and TV as media to communicate the relevant information, while, among the general public, the youths preferred social media such as Facebook and Twitter (22.22%) and adults radio and TV (34.07%), As for the most effective way to promote soil erosion control projects, the experts chose traditional promotinal media such as newspaper, radio, and TV (0.172) whereas the adults and youths preferred the internet and Facebook (0.089). It appears that using the preferred media for communicating information related to soil erosion control projects according to the consumer type will be effective way to promote soil erosion control projects.

• 한국습지학회지
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• 제16권2호
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• pp.221-233
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• 2014

유수에 의한 하천 유역과 하천의 토양의 침식, 유송, 퇴적 현상은 빈번하게 발생한다. 이러한 과도한 현상은 수공구조물의 안전위협, 홍수범람 등의 자연재해를 가중시킨다. 토양침식에 따른 토사재해를 방지하기 위해서는 가장 우선적으로 정확한 유사유출량을 예측할 필요가 있다. 이를 위해서는 유역특성에 적합한 모형의 선정, 관련인자의 정량적인 산출, 가용 수문자료의 확보는 매우 중요하다. 따라서, 본 연구의 목적은 실측자료를 확보하고 있는 설마천 시험유역의 강우량, 유출량, 유사량 자료를 이용하여 강우-유출거동에 따른 토양침식량과 유사유출량을 산정하는데 있다. 그리고 유사전달률 분석을 통하여 설마천 시험유역의 유사전달률을 제안하였다. 향후에는 타 유역에도 적용하여 다양한 조건에서의 토양침식량 및 유사유출량 산정방법의 정형화, 유역 특성별 유사전달률 산정 연구를 하고자 한다.

• 한국지하수토양환경학회지:지하수토양환경
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• 제22권6호
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• pp.66-73
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• 2017

Empirical erosion models like Universal Soil Loss Equation (USLE) models have been widely used to make spatially distributed soil erosion vulnerability maps. Even if the models detect vulnerable sites relatively well utilizing big data related to climate, geography, geology, land use, etc within study domains, they do not adequately describe the physical process of soil erosion on the ground surface caused by rainfall or overland flow. In other words, such models are still powerful tools to distinguish the erosion-prone areas at large scale, but physics-based models are necessary to better analyze soil erosion and deposition as well as the eroded particle transport. In this study a physics-based soil erosion modeling system was developed to produce both runoff and sediment yield time series at watershed scale and reflect them in the erosion and deposition maps. The developed modeling system consists of 3 sub-systems: rainfall pre-processor, geography pre-processor, and main modeling processor. For modeling system validation, we applied the system for various erosion cases, in particular, rainfall-runoff-sediment yield simulation and estimation of probable maximum sediment (PMS) correlated with probable maximum rainfall (PMP). The system provided acceptable performances of both applications.

• Journal of Forest and Environmental Science
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• 제29권3호
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• pp.237-248
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• 2013

The legal basis for the systematic prevention and response to landslide hazards, and the rehabilitation of landslide-hit areas, was established through the amendment of the Forest Protection Act in August 2012. The most noticeable amendment to the Act is the inclusion of clauses associated with the designation and management of landslide-prone zones (including debris flow-prone zones). In this paper, we (1) introduce the clauses related to the designation and management of landslide-prone zones that were included in the amended Forest Protection Act, (2) examine their significance by reviewing the present status of related domestic laws and structural countermeasures such as sediment check dams for sediment-related disaster prevention, and (3) suggest the future directions of the procedure for the designation and cancellation of such zones, and their maintenance and institutional aspects. The establishment of an institutional device for the designation and management of landslide-prone zones has great significance in the aspect of (1) the establishment of a comprehensive management and prevention system for potential landslide-prone zones in forested areas where the hazard risk has been poorly recognized as compared with the flood risks in lowlands, and (2) the establishment of the basis for overcoming the limits of structural countermeasures according to limited budgets. To develop the designation and management system for landslide-prone zones, not only must present problems be addressed, but a cooperation system between the administration and local residents must also be established.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2020년도 학술발표회
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• pp.172-172
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• 2020

In recent years, soil erosion has come to be regarded as an essential environmental problem in human life. Soil erosion causes various on- and off-site problems such as ecosystem destruction, decreased agricultural productivity, increased riverbed deposition, and deterioration of water quality in streams. To solve these problems caused by soil erosion, it is necessary to quantify where, when, how much soil erosion occurs. Empirical erosion models such as the Universal Soil Loss Equation (USLE) family models have been widely used to make spatially distributed soil erosion vulnerability maps. Even if the models detect vulnerable sites relatively well by utilizing big data related to climate, geography, geology, land use, etc. within study domains, they do not adequately describe the physical process of soil erosion on the ground surface caused by rainfall or overland flow. In other words, such models remain powerful tools to distinguish erosion-prone areas at the macro scale but physics-based models are necessary to better analyze soil erosion and deposition and eroded particle transport. In this study, the physics-based Surface Soil Erosion Model (SSEM) was upgraded based on field survey information to produce sediment yield at the watershed scale. The modified model (hereafter MoSE) adopted new algorithms on rainfall kinematic energy and surface flow transport capacity to simulate soil erosion more reliably. For model validation, we applied the model to the Doam dam watershed in Gangwon-do and compared the simulation results with the USLE outputs. The results showed that the revised physics-based soil erosion model provided more improved and reliable simulation results than the USLE in terms of the spatial distribution of soil erosion and deposition.

• 한국지형학회지
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• 제28권3호
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• pp.13-26
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• 2021

In mountain gully, channelized debris flow is an important phenomenon in the process of topographical change. Social infrastructure as roads may be damaged by channelized debris flows, but there has been little information about their occurrence and movement to prepare for the risk of the debris flow. Most of the channelized debris flows occur during heavy rains in mountainous valleys that are difficult to access, so there are not many field data. In this study, the topographical characteristics of the catchment, the rainfall and runoff related to the debris flow, the sedimentary pattern and the cross-sectional change of the channel bed, and the underflow velocity of the gravel bed have been investigated and analyzed in the Singi gully where the channelized debris flows occurred. In the catchment, there was almost no sediment runoff because the vegetation combine with the debris landforms and covered the surface. Therefore, the obvious cause of the channelized debris flows is the collapse of the slope and bed of the gully. Even if the gravel, cobbles, and boulders of the channel bed were lost by debris flow, the thalweg change due to debris flow may not be significant because they are supplied from the gully side slope normally. After the gabion structures were installed, the debris flow increased the thalweg change, bed erosion and side slope of the gully. Various sedimentary structures in the gully were classified according to the factors supporting the sedimentation. The hypsometric curve of the gully reflects the debris landforms and vegetation characteristics of the watershed and the sediment runoff due to debris flow, etc. The relationship between the flow velocity and the hydraulic gradient was non-linear under the condition that the porous medium with gully bed gravels is saturated with water. These results may be used as basic data for channelized debris flow research.

• 한국안전학회지
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• 제31권2호
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• pp.49-56
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• 2016

In Korea, there exist many mountains, and sudden storms occur during the summer season. When severe rainstorm events occur in steep slope topography, risk of debris flow is increased. Once debris flow occurs in urban area, it may cause casualties and physical damages due to rapid debris flow velocity along a steep slope. Accordingly, preventing method of sediment-related disaster for demage mitigation are essential. Recently, various studies on debris flow have been conducted. However, the prediction of the physical propagation of debris flow along the steep slope was not thoroughly investigated. Debris flow is characterized by various factors such as topography, properties of debris flow, amount of debris flow. In the study the numerical simulation was focused on the topographic factor. Fundamental analysis of the risk area was implemented with emphasis on the propagation length, thickness, and the development of maximum velocity. The proposed results and the methodology of estimating the structural vulnerability would be helpful in predicting the behavior and the risk assessment of debris flow in urban area. These results will be able to estimate the vulnerability of urban areas affected the most damage by debris flow.

• 한국산학기술학회논문지
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• 제19권11호
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• pp.481-487
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• 2018

땅밀림 피해지에서 피해지점 및 균열 탐지, 피해규모를 효율적으로 분석하기 위해서 무인기를 활용한 피해지 탐지 및 모니터링 방안에 대해 본 연구에서 제시하였다. 땅밀림 피해지에서 무인기를 촬영하고 분석한 결과, 정사영상을 구축하면 피해지의 균열 탐지 및 규모를 파악할 수 있기 때문에 현장조사 전에 조사자 안전을 확보하고, 조사계획 수립에 효율적 활용이 가능하였다. 또한, 정사영상에서 지형정보를 추출하면 땅밀림 피해지 균열에 대한 정량적 분석이 가능하였다. 본 연구에서 시범적으로 적용한 대상지에서는 전체 균열 면적 1.01ha, 길이 1.07km, 평균 폭 10m, 단차범위 1~10m로 땅밀림 피해가 발생한 것으로 나타났다. 땅밀림 피해지에서는 정기적인 무인기 촬영을 통하여 지형변위를 탐지하고 피해 확산 방향, 규모 등에 대한 모니터링이 가능하기 때문에 복구계획 수립에 효율적으로 활용할 수 있다. 무인기를 이용하여 땅밀림 피해지에 시험 적용한 결과, 지형이 험준하고 위험한 산지에서 빠르고 쉽게 정성적 정량적 결과를 획득할 수 있는 장점이 있었다. 산사태, 토석류, 땅밀림과 같은 산지토사재해 현장에서 무인기 활용가치가 높기 때문에 관련 산업분야 발전에 기여할 수 있을 것으로 기대된다.

• 대한공간정보학회지
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• 제22권4호
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• pp.165-173
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• 2014

노천채굴방식의 광산은 갱내채광에 비해 비교적 작업이 안전하고 채수율이 높으며 생산 원가가 저렴하여 대량생산과 공급이 가능하다는 장점이 있으나 산림훼손, 폐석 및 광재(鑛滓)의 퇴적, 광미(鑛尾)의 배출, 분진, 폐수, 소음, 지반침하, 토사유출, 산사태 등의 환경재해 유발요인들을 내재하고 있어 대표적 환경규제의 대상으로 흔히 지적되고 있다. 이에 본 연구에서는 노천광산에 대한 지형 및 환경 변화에 따른 문제에 대처하고, 친환경 생태학적 광간의 개발 및 복원을 위해서는 노천광산에 대한 주기적이고 정확한 모니터링 기법과 시스템을 개발하고자 하였다. 이에 본 연구에서는 노천광산에 대한 지형 및 환경 변화에 따른 문제에 대처하고, 친환경 생태학적 광간의 개발 및 복원을 위해서는 노천광산에 대한 주기적이고 정확한 모니터링 기법과 이를 이용한 시스템의 개발이 요구된다. 이에 기 개발되어있는 공간정보 오픈 플랫폼과 오픈소스 GIS툴을 이용하여 노천광산 모니터링 시스템 개발 환경 조성을 하고자 한다.

• 한국수자원학회논문집
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• 제48권2호
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• pp.115-126
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• 2015

최근 기후 변화에 따른 게릴라성 호우에 의한 전 세계 도심 속 산지 지역에서 토석류의 발생 빈도수가 증가하고 있으며, 이 결과 더 많은 인명피해와 주요 시설물 파괴 등의 피해가 사회적 큰 문제로 대두되고 있다. 현재까지는 도심지역 재해 관리 및 피난 계획 수립 시, 토석류 범람은 별도로 취급되어 피난 권고 시스템이 구축되고 있으나 피난계획 수립 시, 재해 발생 가능성을 고려한 여러 재해를 기반으로 통합적인 대책 수립이 필요하며 향후, 현재보다 더 큰 강우가 발생할 가능성이 굉장히 크며 이에 대한 대책 수립의 중요성 또한 강조되고 있다. 본 연구에서는 실제 지역에서의 토석류의 유동형태를 파악하고, 외력조건으로 DAD 분석을 통해 가능최대 강우량과 유출량을 산정하며 주거지 지역에서의 토석류 영향범위 파악을 목적으로 한다. 실제 지역에서의 토석류 특성을 분석하기 위해 토석류 흐름 패턴, 퇴적 깊이, 도달속도, 발생된 토사량 및 토석류 이동거리를 평가했다. DAD 해석 결과, 피크 시간 강우량은 국지성 호우에 의해 약 135mm, 24시간 누적 최대강우량은 태풍에 의한 호우로 약 544mm로 조사 되었다. 또한 토석류에 의한 영향범위를 파악 하였다.