• Title/Summary/Keyword: 산림사면

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Evaluation and Prediction of Failure Hazard Area by the Characteristics of Forest Watershed (산림유역 특성에 의한 붕괴 위험지역의 평가 및 예지)

  • Jeong, Won-Ok;Ma, Ho-Seop
    • Korean Journal of Environment and Ecology
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    • v.20 no.4
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    • pp.415-424
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    • 2006
  • This study was carried out to analyze the characteristics of forest watershed factors by using the quantification theory(I) for evaluation and prediction of the failure hazard area. Present $sediment(m^3/yr/ha)$ of erosion control dams were investigated in 95 sites of erosion control dam constructed during 1986 to 1999 in Gyeongnam province. The results obtained from this study were summarized as follows; General condition of class I(Very hazard area) were as follow; Igneous rock in parent rock, coniferous in forest type, below 20year in stand age, below 30cm in soil depth, SCL in soil texture, $31{\sim}40%$ in gravel contents, $S{\sim}E$ in aspect, $2,501{\sim}3,600m$ in length of main stream, $26{\sim}30$ in number of total streams, $6,601{\sim}10,000m$ in length of total streams, over 3 in stream order, over 16 in number of first streams order and over $31^{\circ}$ of slope gradient. General condition of class IIl(hazard area) were as follow; Metamorphic rock in parent rock, hardwood in forest type, over $21{\sim}24year$ in stand age, $31{\sim}40cm$ in soil depth, SiCL or SCL in soil texture, $11{\sim}20%$ in gravel contents, $S{\sim}W$ in aspect, $1,501{\sim}2,600m$ in length of main stream, $6{\sim}10$ in number of total streams, $3,501{\sim}5,500m$ in length of total streams, 2 in stream order, $6{\sim}10$ in number of first streams order and over $31^{\circ}$ of slope gradient. General condition of class III(Un hazard area) were as follow; Sedimentary rock in parent rock, mixed in forest type, over 25year in stand age, $41{\sim}50cm$ in soil depth, SiCL in soil texture, below 10% in gravel contents, $N{\sim}W$ in aspect, below 500m in length of main stream, below 5 in number of total streams, below 1,000m in length of total treams, below 1 in stream order, below 2 in number of first streams order and below $25^{\circ}$ of slope gradient. The prediction method of suitable for failure hazard area divided into class I, II, and III for the convenience of use. The score of class I evaluated as a very hazard area was over 4.8052. A score of class II was 4.8051 to 2.5602, it was evaluated as a hazard area, and class III was below 2.5601, it was evaluated as a un hazard area.

Forest Structure in Relation to Slope Aspect and Altitude in valley Forests at Hambaeksan Area (함백산지역 계곡부의 사면방향과 해발고에 따른 산림구조)

  • 박인협;최윤호;이석면;최영철;유석봉
    • Korean Journal of Environment and Ecology
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    • v.15 no.4
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    • pp.361-368
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    • 2002
  • The valley forests located at the east-facing slope and the west facing slope in Hambaeksan area were studied to investigate forest structure in relation to aspect and altitude of the slope. There was little difference in density. mean DBH and basal area of the tree layer between east-facing slope and west-facing slope. The importance percentages of Tilia amurensis and Betula costata in west-facing slope were higher than those in east-facing slope. However, the importance percentages of Quercus mongilica and Fraxinus rhynchophylla in the west facing slope were lower than those in east-facing slope. Species diversity of the west-facing slope was 1.415 and that of the east-facing slope was 1.328. Elevation trends were also found for forest structure. As elevation Increased basal area and mean height of the tree layer decreased in both of east-facing slope and west-facing slope. There was a tendency that number of species, species diversity and evenness decreased with increasing elevation. The importance percentage of Quercus mongolica increased with increasing elevation while those of Betula costata and Maackia amurensis decreased. The result of cluster analysis for the tree and subtree layer indicated that the studied forests were classified into the mixed forest community of broad-leaved tree species at west-facing slope and the low and middle elevation belts of east-facing slope and Quercus mongolica community at the high elevation belt of east-facing slope. Quercus mongolica was significantly and positively correlated with Symplocos chinensis for. pilosa, Acer tschonoskii var. rubripes and deutzia glabrata. Betula costata was significantly and negatively correlated with Quercus mongolica and Acer pseudo-sieboldianum.

The Effect of Pinus densiflora Root System on Stability of Damaged Slopes (소나무의 근계특성이 사면안정화에 미치는 영향)

  • Suh, Dong-Jun;Kim, Se-Geon;Kim, Dong-Geun
    • Journal of Forest and Environmental Science
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    • v.26 no.3
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    • pp.193-202
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    • 2010
  • To analyze the effects of tree roots on the stability of damage slope, distributional and physical properties of five-year Pinus densiflora roots were investigated. In the composition of roots, the proportion of main root to lateral root was 1 to 9 in slope condition. Root tensile force was increased in accordance with increased proportion to diameter of Pinus densiflora roots. However, tensile strength was decreased in proportion to diameter of roots. Root shear strength showed that soil containing Pinus densiflora roots was higher than that of non-treated soils. This result shows that Pinus densiflora roots significantly stabilize the surface-soil rather than sub-soil in damage slopes.

Influenced on Analysis of Characteristics of Forest Environmental Factors on Debris Flow Occurrence (토석류 위험지역에 영향하는 산림환경 특성 분석)

  • Park, Jae-hyeon;Kang, Min-Jeong;Kim, Ki-Dae
    • Journal of Korean Society of Forest Science
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    • v.104 no.3
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    • pp.403-410
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    • 2015
  • This study was conducted to analyze the forest environmental characteristics on a total of 20 forest environmental factors affecting the debris flow against 272 sites of risk areas. In the case of environmental factors, it showed the high risk of debris flow under the following conditions such as soil depth of less than 30cm, west slope, altitude of 200~300 m, mountain average slope of $25{\sim}30^{\circ}$, sandy loam, igneous rocks, and composite slope. Among the rainfall factors, 50~100 mm of maximum hourly rain fall and 300 mm of maximum rain fall per day have been shown the high risk of debris flow. Furthermore, the high risk of debris flow was related to the river-bed average slope of $10{\sim}20^{\circ}$, the river-bed average width of >10 m, the small amount of debris in river-bed (less than 20% of river-bed structure), the drainage density of >$1km/km^2$, the 40~60% of area with more than $20^{\circ}$ slope, and the 40~60% of areas with risk grade 2 of landslide. In addition, forest environmental factors including the driftwood, soil erosion control structures, age-class 3, crown density (density), and mixed forest were important factors causing the high risk of debris flow.

Effects on the Early Growth of Revegetation Plants by Microorganisms in Slope of Forest Road (임도사면에 있어서 미생물처리가 녹화식물의 초기생육에 미치는 영향)

  • Ma, Ho-Seop;Park, Jin-Won
    • Journal of Korean Society of Forest Science
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    • v.95 no.4
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    • pp.423-428
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    • 2006
  • This study was carried out to investigate the early growth of revegetation plants by microorganisms in slope of forest road in Jinju area. The results were summarized as follows; The chemical properties of forest soil were changed by microorganisms. Soil pH, organic mater content, concentrations of total nitrogen, available phosphorus, exchangeable cations and CEC in treated plot were increased more than those of controlled plot in the surface soil. It showed that the availability of nutrients including nitrogen and phosphorus was increased by an application of microorganisms in the soil. The coverage rates showed statistically significant differences between plots (p<0.05). The germination rates of woody plants were better in treated plot than in controlled plot. The results indicate that the application of microorganisms would be significantly contributed for the early growth of revegetation plants on slope of forest road.

On the Topographies and Recovery of Vegetation in the Hillside Erosion Control Districts (산복사방공사시공지(山腹砂防工事施工地)에 있어서 지형(地形)과 식생회복(植生回復))

  • Kang, Wi Pyung
    • Journal of Korean Society of Forest Science
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    • v.64 no.1
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    • pp.42-46
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    • 1984
  • This study was carried out to obtain the advanced basic data for hillside erosion control works. Recovery of vegetation in the hillside erosion control districts depends on various factors i.e., topographies, soil qualities, rain conditions and erosion control methods. The only relations between topographies and vegetation coverage were surveyed, since the other factors were equal in all those surveyed areas. The results obtained are summarized as follows; 1) Mean coverage values were decreased in order of 80%, 78.7%, 64.0% and 56.5%r in concave slope, uniform slope, compound slope and convex slope respectively. The mean coverage of all aspects was 69.8%. The slope pattern have a influence on formation of coverage. 2) Moisture ratio in soil and mean slope have an effect on the mean coverage value. 3) In the beginning of the hillside erosion control working, coverage (14.8%) by arbor species was too low comparing with that by herb. 4) It is more desirable to recover regetation by artificial planting or seed planting than by the natural vegetation in the barren hillside. In the beginning of the hillside erosion control working, it is difficult to expect vegetation recovery by natural species.

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A Study on Landslide in the Slope of the Forest Road (임도사면(林道斜面)의 붕괴(崩壞)에 관(關)한 연구(硏究))

  • Oh, Jae-Man;Chun, Kun-Woo
    • Journal of Forest and Environmental Science
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    • v.7 no.1
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    • pp.35-41
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    • 1990
  • This study was conducted to find out the suitable gradient and length of the slope from the landslide of banking slope and cutting slope caused by rainfall. The survey was carried out on forest road built in 1986. And the period of survey was from June, 1989 to August, 1989 after dividing the forest road into A and B. The survey plots consisted of the 12 banking slopes and 6 cutting slopes. The results obtained from the study were summarized as follows; 1. The rate of landslide appeared 75% in A forest road, 50% in B forest road, and then the average 67% in A and B forest road. But the value of landslide showed considerably low. 2. Because of landslide chiefly occuring on banking slope of $36^{\circ}{\sim}38^{\circ}$ and on cutting slope of $42^{\circ}{\sim}43^{\circ}$, it is suitable to decide the banking slope and cutting slope below each $36^{\circ}$ and $40^{\circ}$. 3. Landslide was the same on banking slopes through the length of slope. The best suitable length of slope is below 4m in cutting slope.

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A comparison of Induced Landslide of Factors and Landslide Hazard Assessment Using GIS (GIS을 이용한 자연사면 안정성 평가표 비교 및 산사태 유발 인자 고찰)

  • Lee, Min-Kyu;Kim, Gyu-Won
    • Proceedings of the Korean Association of Geographic Inforamtion Studies Conference
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    • 2010.06a
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    • pp.261-266
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    • 2010
  • 그 동안 산사태 연구는 강우에 의한 예측 연구나 결정론적 유한요소법 및 한계평형 연구가 많이 이루어 졌지만 자연의 요소 이외의 인간 활동적 요소에 대한 연구는 외국의 사례에 비해 선행연구가 많이 없는 실정이다. 이번 연구 논문에서는 산림청의 사면평가표를 GIS을 이용해 강우 조건과 사회적 인자(도로, 빌딩, 주택 등)에 따른 산사태 위험지역들을 GIS Map상에서 어떤 차이가 나는지 알아보았다. 또한 사면평가표의 항목에서 사회적 인자 항목이 산사태 발생에 있어 통계적으로 유의한지를 다변량 통계분석을 통해 알아보았다.

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Application of Drone Photogrammetry for Current State Analysis of Damage in Forest Damage Areas (드론 사진측량을 이용한 산림훼손지역의 훼손 현황 분석)

  • Lee, Young Seung;Lee, Dong Gook;Yu, Young Geol;Lee, Hyun Jik
    • Journal of Korean Society for Geospatial Information Science
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    • v.24 no.3
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    • pp.49-58
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    • 2016
  • Applications of drone in various fields have been increasing in recent years. Drone has great potential for forest management. Therefore this paper is using drone for forest damage areas. Forest damage areas is divided into caused by anthropogenic and occurs naturally, the possibility of disasters, such as slope sliding, slope failures and landslides, sediment runoff exists. Therefore, this research was to utilize the drone photogrammetry to perform the damage analysis of forest damage areas. Geometrical treatment processing results in Drone Photogrammetry, the plane position error RMSE was ${\pm}0.034m$, the elevation error RMSE was ${\pm}0.017m$. The plane position error of orthophoto RMSE was ${\pm}0.083m$, the elevation error of digital elevation model RMSE was ${\pm}0.085m$. In addition, It was possible to current state analysis of damage in forest damage areas of airborne LiDAR data of before forest damage and drone photogrammetry data of after forest damage. and application of drone photogrammetry for production base data for restoration and design in forest damage areas.

Stability Evaluation of Cut Slope in Forest Roads by Forest Environment Factors (산림환경인자에 의한 임도 절토비탈면의 안정성 평가)

  • Jeon, Kwon-Seok;Oh, Sung-Yoon;Ma, Ho-Seop
    • Journal of the Korean Society of Environmental Restoration Technology
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    • v.6 no.4
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    • pp.43-51
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    • 2003
  • The purpose of this study was evaluate to the stability on cut slope of forest roads by forest environmental factors. The total of 19 environmental factors on cut slope of forest roads were investigated in about 42.74km constructed during 1987 to 1993 in Gyeongnam and Jeonnam province. The evaluation of slope stability in forest roads were conducted by the discriment analysis. The main factors influencing the stability of cut slope were significant in order of coverage, soil hardness, degree of slope, altitude, silt loam, convex(凸) and compound(凹凸). The centroids value of discriminant function in the stability and unstability area estimated to -1.194 and 1.127, respectively. The boundary value between two groups related to slope stability was -0.072. The prediction rate of discriminant function for stability evaluation of was as high as 90.4%.