• Journal of Biosystems Engineering
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• 제3권2호
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• pp.35-61
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• 1978

동력경운깅가 일반 경사지에서 견인주행하는 경우 견인주행성능과 주행특성을 구명하기 위하여 토양의 종류 및 상태는 일정하게 하고 지면의 기하학적 조건과 견인주행속도 및 견인하중을 변수로 하여 외부동력전달계의 시점인 좌우차륜과 토양간에 발생하는 차륜구동력 및 굴름정항과 Engine에서 구동륜까지 내부전달계를 통하여 전달된 동력의 이론치와 실험치와의 부합여부를 검정하고 부가적으로 동력경운기가 경사지기계화의 동력기로써의 가능성여부와 문제점을 찾으려한다.

• Journal of Biosystems Engineering
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• 제3권2호
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• pp.34-34
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• 1978

동력경운깅가 일반 경사지에서 견인주행하는 경우 견인주행성능과 주행특성을 구명하기 위하여 토양의 종류 및 상태는 일정하게 하고 지면의 기하학적 조건과 견인주행속도 및 견인하중을 변수로 하여 외부동력전달계의 시점인 좌우차륜과 토양간에 발생하는 차륜구동력 및 굴름정항과 Engine에서 구동륜까지 내부전달계를 통하여 전달된 동력의 이론치와 실험치와의 부합여부를 검정하고 부가적으로 동력경운기가 경사지기계화의 동력기로써의 가능성여부와 문제점을 찾으려한다.

• 대한공간정보학회지
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• 제24권3호
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• pp.85-92
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• 2016

토지 개발 인허가 기준에는 중요 요소로서 경사도가 포함되어 있다. 토지 적성 평가 지침, 산지전용허가기준 등에는 수치지형도상 평가대상 토지의 평균경사도를 측정하여 경사도로 사용하며, GIS를 적용할 수 있다고 규정되어 있다. 입력 자료로는 국토지리정보원의 1/5,000 수치지형도 외에 한국토지정보시스템 전산자료를 활용 가능한 자료로 예시하고 있다. 경사도 계산에는 수치지형도의 등고선을 이용한 방법, 이를 DEM으로 변환하여 이용하는 방법 등 다양한 방법이 제시되고 있으나 표준화된 경사도 계산 방법은 제시되지 못하고 있어 실무에서 혼란이 발생하고 있다. 이러한 혼란을 감소시키기 위하여 본 연구에서는 표준화된 경사도 계산 방법과 적정 해상도를 결정할 수 있는 방안을 제안하고자 하였다. 경사도 계산에 사용되는 여러 방법을 분석한 결과, 지형의 복잡성을 고려하여 결정된 해상도를 가진 DEM을 만들어 유한차분법을 이용하여 평균경사도를 계산하는 개선된 방안을 제시하였다.

• Journal of Biosystems Engineering
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• 제12권3호
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• pp.62-72
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• 1987

The necessity of using land on slopes for agricultural production has been recognized all arable land resources in plains are decreased. Mechanization is one of the main factors determining the extent of cultivating slope lands and it must be considered as a means of increasing labor productivity. This article discussed some relevent aspects of farm mechanization on slopes. It includes the potential slope land resources which can be tilled for food and forage productions, design characteristics of agricultural machines for use in slope lands, and possible solutions of the problems to be encountered in the mechanization process.

• 한국환경복원기술학회지
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• 제19권4호
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• pp.19-28
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• 2016

The objectives of this study were to establish the slope criteria and analyze the forest land restoration plan in North Korea. Reviewing the literature of the countries, the relationships among the climate, erosion controls, and slope criteria with forest restoration programmes, implemented were analyzed. Comparison of forest land management policies was conducted between South and North Korea. The soil erosion controls using biological barriers were at $15{\sim}20^{\circ}$slopes in arid climate regions and $25{\sim}30^{\circ}$ in humid climate regions. In the case of South Korea, an afforestation policy from the "Act on Clearance Project of Slash-and Burn Agriculture" of 1966 was enforced on mountains with slope greater than $20^{\circ}$, however, at present, the "Marginal Cropping Land Policy" recommends cropping lands with slope bigger than $8.5^{\circ}$ to forest land. In 1961, in "Land Reclamation of One Million Hectare", North Korea reclaimed additional cropping lands with slope bigger than $8.5^{\circ}$, and currently, the "Act on Forestry" states to enforce reforestation with slope bigger than $20^{\circ}$. This study recommends that South Korea aids for forest land restoration in North Korea based on the different stages of their development on reconciliation and cooperation between South and North Korea.

• 한국안전학회지
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• 제30권3호
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• pp.52-58
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• 2015

As sudden rainfall has happened, the debris flow has occurred in the mountain area. Recently sudden rainfall occurred so frequently caused by abnormal climate. Thus debris flow hazard had consecutively increased damage because of debris flow. Recently, Enormous damage due to debris flow have occurred in Korea. Various studies have been conducted to prevent search debris flow hazard. This study was carried out for debris flow behavior according to the land slope on propagation. It is the important one among factors that are related to the propagation over the city with respect to debris flow discharge and depth. For the numerical simulations in this study, the land slope was varied of 5, 0, $-5^{\circ}$ to investigate the debris flow behavior with the FLO-2D, often recommended by FEMA to simulate debris flow. To verify the performance of FLO-2D, comparison with the USGS experiments (Iverson et al, 2010) was conducted. From numerical results the propagation length of the debris flow was found the most sensitive one. Maximum of debris flow thickness and velocity and structural vulnerabilities were investigated to the effect of land slope. They was became smaller according to land slope of 5, -5, $0^{\circ}$ in the order. As a result, debris flow behavior analysis about the effect of the land slope could contribute to understand the vulnerability of city for debris flow hazards.

• Spatial Information Research
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• 제16권3호
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• pp.279-290
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• 2008

자연재해로 인한 수많은 피해 중 특히 산사태 등 사면붕괴로 인한 피해는 인간에게 많은 인적/물적 자원의 손실을 가져왔다. 이런 사면붕괴로 인한 피해를 줄이고자 사면붕괴 예방을 위해 다양한 계측장비를 이용하여 사면붕괴 예 경보 시스템을 구축하였다. 하지만 대상사면에 접근성 문제를 해결하고 위험 사면 전체에 대한 안전성 평가를 실시할 수 있는 효율적인 계측장비는 많지 않은 실정이다. 이에 사면붕괴예방을 위한 효율적인 계측장비로서 측량학적인 접근 방법으로 사면거동의 정확한 계측을 위해 지상라이다시스템을 이용하여 사면붕괴 예방을 위한 시스템의 활용가능성 판단을 위한 실험을 실시하였다. 본 연구에서는 인공으로 조성되어 사면안정화 공법이 적용된 토사사면에 사면상부에서 단계별로 실물 하중을 가하여 하중에 따른 사면의 거동을 Total Station과 지상라이다시스템을 이용하여 계측하였다. 두 시스템을 이용하여 계측한 성과의 정확한 비교 분석을 위해 두 시스템의 계측 결과를 동일한 좌표계로 일치시키는 3D Similarity Transformation을 통해 서로 다른 좌표계를 가지고 있는 두 좌표계를 하나의 좌표계로 통일시켜 사면이 실물하중에 어떤 거동이 일어나는지를 분석하였다. 타켓중심의 사면거동 분석결과, 지상라이다 시스템은 Total Station과 비교해 X축으로는 1cm이내의 차이가, Y축으로는 규칙적이지 않는 거동의 경향이 발생하고, Z축으로는 서로 유사한 경향을 보였다. 연속된 점에 대한 사면지동 분석결과, Y축의 위치에 따라 사면 하부에서 상부의 방향으로 사면거동의 경향이 다르게 나타나 Total Station에서 분석하기 어려웠던 사면의 연속적인 변화를 관찰할 수 있었다. 따라서 지상라이다 시스템은 Total Station에 버금가는 측량성과를 획득하여 효율적인 사면모니터링을 위한 계측장비로 판단되었으며 기존의 사면모니터링기법의 한계를 대체 할 수 있는 측량학적 분석방법으로 많은 활용이 기대된다.

• 한국환경복원기술학회지
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• 제17권2호
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• pp.49-60
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• 2014

This study was conducted to evaluate the effect of forest fire on natural distribution and regeneration of Pinus densiflora Sieb. & Zucc. in Goseong, Gangwon province, Korea. After 13 years of the last forest fire in 2000, five investigation plots ($10m{\times}10m$) in each of rocky land and ridge, the well-known location as a favorite site for natural distribution of P. densiflora, were set to investigate stand characteristic and soil environment including physico-chemical properties and moisture contents of soil. Also, five investigation plots in slope area were set and investigated as well. The concentration of organic matter, total nitrogen, and exchangeable nutrients ($K^+$, $Ca^{2+}$, $Mg^{2+}$) were highest in the slope while the soil in the rocky land showed the lowest concentration of organic matter, total nitrogen, available $P_2O_5$, and exchangeable nutrients ($K^+$, $Na^+$, $Ca^{2+}$, $Mg^{2+}$). The soil in the slope only showed higher concentration of total nitrogen, $K^+$ and $Ca^{2+}$ than the unburned area in Goseong. Mean soil moisture contents in the rocky land (5.77%) were lowest while the slope (15.78%) and the ridge (15.27%) showed almost three times as much than the rocky land. P. densiflora was dominant in the rocky land and Quercus spp. were dominant in the ridge and slope. The average proportion of P. densiflora was highest in rocky land (58.4%, 14.6 trees per plot) followed by the ridge (25.2%, 7.8 trees per plot) and the slope (11.3%, 3.4 trees per plot) while the average height of P. densiflora was highest in slope (277cm) followed by the ridge and the rocky land. The height and crown width of Quercus spp. were higher than P. densiflora in the every plot. The results suggest that P. densiflora may be able to naturally regenerate and survive in the rocky land after the fire while P. densiflora in the ridge and the slope are suppressed by Quercus spp.

• 환경영향평가
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• 제15권1호
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• pp.1-12
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• 2006

Changes in the soil physical property and the topographic condition derived from agricultural activities like as farming activities, land clearance and cutting down resulted in environmental and economic problems including the outflow of nutrient from farms and the water pollution. Several theories on the soil conservation have been developed and reviewed to protect soil erosion in the regions having a high risk of erosion. This study was done using the USLE model developed by Wischmeier and Smith (1978), and model for the slope length and steepness made by Desmet and Govers (1996), and Nearing (1997) to evaluate the potential of the soil erodibility. Therefore, several results were obtained as follows. First, factors affecting the soil erosion based on the USLE could be extracted to examine the erosion potential in farms. Soil erodibility (K), slope length (L), and slope steepness (S) were used as main factors in the USLE in consideration of the soil, not by the land use or land cover. Second, the soil erodibility increased in paddy soils where it is low in soil content, and the very fine sandy loam exists. Analysis of the slope length showed that the value of a flat ground was 1, and the maximum value was 9.17 appearing on the steep mountain. Soil erodibility showed positive relationship to a slope. Third, the potential soil erodibility index (PSEI) showed that it is high in the PSEI of the areas of steep upland and orchard on the slope of mountainous region around Dokjigol mountain, Dunji mountain, and Deummit mountain. And the PSEI in the same land cover was different depending on the slope rather than on the physical properties in soil. Forth, the analysis of land suitability in soil erosion explained that study area had 3,672.35ha showing the suitable land, 390.88ha for the proper land, and 216.54ha for the unsuitable land. For unsuitable land, 8.71ha and 6.29ha were shown in fallow uplands and single cropping uplands, respectively.

• 토지주택연구
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• 제9권2호
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• pp.51-57
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• 2018

The causes of landslides are dependant on rainfall events and the soil characteristics of a slope. For the conventional slope stability, the slope stability analysis has been carried out assuming the saturated soil theory. But, in order to clearly explain a proper soil slope condition by rainfall, the research should be performed using the unsaturated soil mechanism suitable for a soil slope in the field. In the study, by using two major categories of soils in Korea, such as granite and gneiss weathered soils, landslide model test and finite element method have been compared with the difference of seepage and soil stability analysis. The hydraulic conductivity of gneiss weathered soil is slower than that of granite weathered soil, and the gneiss weathered soil contains much finer soils than the granite weathered soil. It was confirmed that the instability of the slope was progressing slowly due to the slow rate of volumetric water content of the surface layer.