• 한국지반신소재학회논문집
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• 제12권2호
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• pp.35-42
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• 2013

흙 구조물의 안정성은 물과 직접적인 관련이 있고, 강우나 침투수에 대한 충분한 대책을 세우지 않는다면 구조물에 큰 피해를 입을 수 있다. 최근 이상기후로 인한 집중호우의 횟수가 잦아짐에 따라 흙 구조물의 안정성에 대한 관심이 커지고 있으며, 구조물의 배수에 대한 여러 가지 방법이 제시되고 있다. 본 연구에서는 연직 배수공법에 사용되는 PBD(Plastic Board Drain)를 보강토 옹벽의 수평 배수재로 이용했을 시 적용성 여부에 대해 평가 하였다. 특히 전면벽을 콘크리트 블록이 아닌 토낭으로 하여 시공성과 경제성을 높이고, 토낭과 연결재, PBD를 일체화 시켜 안정성을 확보하였다. PBD를 활용한 배면수의 투수능 시험결과 보강토체 사이에 자갈층을 포설한 것과 유사한 효과를 나타내었으며, 실제 현장에서의 수평배수재로 활용이 가능한 것으로 판단된다.

• 한국환경복원기술학회지
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• 제19권3호
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• pp.103-119
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• 2016

This study aims to assess habitat feature on the large-scale spawning ground of the Boreal Digging Frog Kaloula borealis in Daemyung retarding basin of Daegu, and to analyze the relationships between species abundance and meteorological factors for each habitat. Fifty-seven(57) pitfalls were installed to collect species abundance of 4 survey regions, and high-resolution satellite image, soil sampling equipment, digital topographic map, and GPS were used to develop habitat features such as terrain, soil, vegetation, human disturbance. The analysis shows that the frog is most abundant in sloped region with densely herbaceous cover in southern part of the retarding basin. In the breeding season, lowland regions, where Phragmites communis and P. japonica dominant wetlands and temporary ponds distributed, are heavily concentrated by the species for spawning and foraging. Located in between legally protected Dalsung wetands and lowland regions of the retarding basin, riverine natural levee is ecologically important area as core habitat for Kaloula borealis, and high number of individuals were detected both breeding and non-breeding seasons. Temperate- and pressure-related meteorological elements are selected as statistically significant variables in species abundance of non-breeding season in lowland and highland regions. However, in sloped regions, only a few variables are statistically significant during non-breeding season. Moreover, breeding activities in sloped regions are statistically significant with minimum temperature, grass minimum temperature, dew point temperature, and vapor pressure. Significant meteorological factors with habitat features are effectively applied to establish species conservation strategy of the retarding basin and to construct for avoiding massive road-kills on neighboring roads of the study sites, particularly post-breeding movements from spawning to burrowing areas.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2003년도 Proceedings of ACRS 2003 ISRS
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• pp.962-964
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• 2003

In 2002 Thailand was faced with severe flooding in the North, Northeast and Central parts of the country caused by heavy rainfall of the monsoonal depression which brought about significant damages. According to the report by the Ministry of Interior and the Ministry of Agricultural and Co-operatives, the total damages were estimated to be about 6 billion bath. More than 850,000 farmers and 10 million livestock were effected. An area of 1,450,000 ha of farmland in 59 Provinces were put under water for a prolonged period. Satellite imageries were employed for mapping and monitoring the flood-inundated areas, flood damage assessment, flood hazard zoning and post-flood survey of river configuration and protection works. By integrating satellite data with other updated spatial and non-spatial data, likely flood zones can be predicted beforehand. Some examples of satellite data application to flood dis aster mitigation in Thailand during 2002 using mostly Radarsat-1 data and Landsat-7 data were illustrated and discussed in the paper. The results showed that satellite data can clearly identify and give information on the status, flooding period, boundary and damage of flooding. For comprehensive flood mitigation planning, other geo-informatic data, such as the elevation of topography, hydrological data need to be integrated. Ground truth data of the watershed area, including the water level, velocity, drainage pattern and direction were also useful for flood forecasting in the future.

• 한국약용작물학회지
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• 제17권3호
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• pp.204-209
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• 2009

This study was conducted to assess water movement in paddy-upland rotation soil scheduled for ginseng cultivation through the measurement of infiltration and permeability of soil water. Soil sample was divided with four soil layers. The first soil layer (to 30cm from top soil) was loamy sand, the second and the third soil layers (30$\sim$70 ㎝) were sand, and the fourth (< 120 ㎝) was sandy loam. The soil below 130 ㎝ of fourth soil layer was submerged under water. The shear strength, which represents the resisting power of soil against external force, was 3.1 kPa in the first soil layer. This corresponded to 1/8 of those of another soil layer and this value could result in soil erosion by small amount of rainfall. The rates of infiltration and permeability depending on soil layers were 39.86 cm $hr^{-1}$ in top soil, 2.34 cm $hr^{-1}$ in 30$\sim$70 ㎝ soil layer, 5.23 cm $hr^{-1}$ and 0.18 cm $hr^{-1}$ in 70$\sim$120 ㎝ soil layer, with drain tile, and without drain tile, respectively. We consider that ground water pooled in paddy soil and artificial formation of soil layer could interrupt water canal within soil and affect negatively on water movement. Therefore, we suggest that to drain at 5 m intervals be preferable when it makes soil dressing or soil accumulation to cultivate ginseng in paddy-upland rotation soil to reduce failure risk of ginseng cultivation.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2015년도 학술발표회
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• pp.396-396
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• 2015

Frequent urban floods affect the human safety and economic properties due to a lack of the capacity of drainage system and the increased frequency of torrential rainfall. The drainage system has played an important role in flooding control, so it is necessary to establish the effective countermeasures considering the connection between drainage system and surface flow. To consider the connection, we selected SWMM5 model for analyzing transportation capacity of drainage system and FLUMEN model for calculating inundation depth and time variation of inundation area. First, Thiessen method is used to delineate the sub-catchments effectively base on drainage network data in SWMM5. Then, the output data of SWMM5, hydrograph of each manhole, were used to simulate FLUMEN to obtain inundation depth and time variation of inundation area. The proposed method is applied to Sadang area for the event occurred in $27^{th}$ of July, 2011. A total of 11 manholes, we could check the overflow from the manholes during that event as a result of the SWMM5 simulation. After that, FLUMEN was utilized to simulate overland flow using the overflow discharge to calculate inundation depth and area on ground surface. The simulated results showed reasonable agreements with observed data. Through the simulations, we confirmed that the main reason of the inundation was the insufficient transportation capacities of drainage system. Therefore cooperation of both models can be used for not only estimating inundation damages in urban areas but also for providing the theoretical supports of the urban network reconstruction. As a future works, it is recommended to decide optimized pipe diameters for efficient urban inundation simulations.

• 한국지반환경공학회 논문집
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• 제24권5호
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• pp.21-28
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• 2023

본 논문에서는 시험적 연구를 통해 초속경 복합매트의 물성을 제시하고, 수치해석적 연구를 통해 지반조건, 강우량, 비탈면 기울기, 성토 높이 등에 따른 초속경 복합매트의 비탈면 보호효과를 분석한 연구를 다루었다. 그 결과 모든 조건에서 초속경 복합매트를 적용할 경우 비탈면 안전율은 증가하였으며, 안전율 증가율은 건기 시와 우기 시 모두 평균 40%의 증가율을 보였다. 이러한 연구결과를 통해 초속경 복합매트의 비탈면 보호효과를 입증하였으며, 초속경 복합매트는 비탈면 유실 및 붕괴가 예상되는 구간에 적용하기 적합할 것으로 사료된다.

• 한국지반공학회논문집
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• 제25권1호
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• pp.31-40
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• 2009

본 연구는 보강된 기존사면에 대한 새로운 사면 위험도 평가방법에 대한 연구로서 기존의 사면 안정성 및 위험도 평가방법들에서 주요 위험도 영향요소로 구분되는 강우, 암종, 배수상태 항목들에 대하여 검토하고 분석하였다. 분석 결과 사면 위험도에 영향을 미치는 19개의 주요요소를 선정하였으며 이를 Hudson(1991)이 제안한 Interaction matrix 개념의 위험도 분석 모델에 적용하였다. 적용결과 기존사면 위험도 평가방법인 SRI(Slope Risk Index)를 제시하였으며 국내 15개소 사면을 대상으로 검증을 실시하였다. 검증 결과 제시한 기존보강사면의 위험도 평가방법의 신뢰성을 확인할 수 있었다.

• Geomechanics and Engineering
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• 제34권3호
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• pp.267-284
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• 2023

Landslides are one of the most dangerous phenomena and natural disasters. Landslides cause many human and financial losses in most parts of the world, especially in mountainous areas. Due to the climatic conditions and topography, people in the northern and western regions of Iran live with the risk of landslides. One of the measures that can effectively reduce the possible risks of landslides and their crisis management is to identify potential areas prone to landslides through multi-criteria modeling approach. This research aims to model landslide potential area in the Oshvand watershed using a support vector machine algorithm. For this purpose, evidence maps of seven effective factors in the occurrence of landslides namely slope, slope direction, height, distance from the fault, the density of waterways, rainfall, and geology, were prepared. The maps were generated and weighted using the continuous fuzzification method and logistic functions, resulting values in zero and one range as weights. The weighted maps were then combined using the support vector machine algorithm. For the training and testing of the machine, 81 slippery ground points and 81 non-sliding points were used. Modeling procedure was done using four linear, polynomial, Gaussian, and sigmoid kernels. The efficiency of each model was compared using the area under the receiver operating characteristic curve; the root means square error, and the correlation coefficient . Finally, the landslide potential model that was obtained using Gaussian's kernel was selected as the best one for susceptibility of landslides in the Oshvand watershed.

• 대한원격탐사학회지
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• 제40권2호
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• pp.179-190
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• 2024

This study aims to compare supervised classification methods with phenology-based approaches, specifically pixel-based and segment-based methods, for accurate crop mapping in agricultural landscapes. We utilized Sentinel-2A imagery, which provides multispectral data for accurate crop mapping. 31 normalized difference vegetation index (NDVI) images were calculated from the Sentinel-2A data. Next, we employed phenology-based approaches to extract valuable information from the NDVI time series. A set of 10 phenology metrics was extracted from the NDVI data. For the supervised classification, we employed the maximum likelihood (MaxLike) algorithm. For the phenology-based approaches, we implemented both pixel-based and segment-based methods. The results indicate that phenology-based approaches outperformed the MaxLike algorithm in regions with frequent rainfall and cloudy conditions. The segment-based phenology approach demonstrated the highest kappa coefficient of 0.85, indicating a high level of agreement with the ground truth data. The pixel-based phenology approach also achieved a commendable kappa coefficient of 0.81, indicating its effectiveness in accurately classifying the crop types. On the other hand, the supervised classification method (MaxLike) yielded a lower kappa coefficient of 0.74. Our study suggests that segment-based phenology mapping is a suitable approach for regions like South Korea, where continuous cloud-free satellite images are scarce. However, establishing precise classification thresholds remains challenging due to the lack of adequately sampled NDVI data. Despite this limitation, the phenology-based approach demonstrates its potential in crop classification, particularly in regions with varying weather patterns.

• 대한지하수환경학회지
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• 제4권2호
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• pp.85-94
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• 1997

연구 지역은 제주도의 해안 용천수를 수원지로 하고 있는 삼양 3수원지로서 1996년 1월부터 원수의 염소이온농도가 먹는 물 수질기준치인 150 mg/ι를 훨씬 초과하여 그 원인을 수리지질학적으로 규명하기 위하여 연구를 수행하였다. 연구결과 그 원인은 다음과 같은 매우 복잡한 자연 및 인위적인 현상에 의해 발생하였다. 1996년 1월~9월 동안 내린 강수량은 그 이전 36년간 제주시에서 발생한 연평균 강수량의 41.7%에 해당하는 극심한 한발기로서 이러한 강수량의 감소는 결국 용천 유출량의 감소와 용천수위 강하의 원인이 되었고, 이로 인해 만조시 매 주기 별로 2~3.8시간 동안 해수면이 수원지내 지하수위보다 4.4~12.4cm 높게 되어 기존 차수벽 하부의 투수대 구간을 통해 해수가 역동수구배를 따라 수원지내 유입되어 지하수의 염소이온농도 증가원인이 되었다. 또한 주기적인 조석간만의 영향으로 인해 발생한 두께가 얇아진 담수체의 수축 팽창현상이 점이대의 확장을 촉진시켜 염소이온농도를 증가시켰으며, 뿐만 아니라 강수량 감소에 따른 지하함양량 감소로 점이대에서 지하수 흐름의 역전현상이 발생하였고, 이에 부가하여 강우누적결핍시기 동안 해안지하수체의 수축현상이 가장 심하게 발생한 간조시에 일평균 2790$\pm$450 ㎥의 지하수를 반복채수함으로 인해 추가적인 지하수위의 하강을 초래하여 점이대의 확장과 염수의 역상승 현상을 유발하였다. 수원지 주변 용천에서 염소이온농도가 150 mg/l이하로 유출되는 순수지하수 유출지속 시간은 하루 약 2시간 정도였으며 유출량은 532 ㎥/일 이였고 만조시 C $l^{－}$ 이온의 농도는 1900 mg/1 이상이다.