• 제목/요약/키워드: River slope

검색결과 435건 처리시간 0.026초

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

  • 박재현;강민정;김기대
    • 한국산림과학회지
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    • 제104권3호
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    • pp.403-410
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    • 2015
  • 이 연구는 토석류 위험지역 총 272개소에서 토석류 유출에 영향을 미치는 20개의 산림환경인자에 대하여 산림환경 특성을 분석하였다. 입지환경인자 중 토심은 하(30 미만), 방위는 서쪽사면, 표고는 200~300 m, 산지평균경사는 $25{\sim}30^{\circ}$, 토질은 사양토, 모암은 화성암, 사면형은 복합사면이 토석류 위험이 높은 것으로 나타났다. 강우환경인자 중 최대시우량은 50~100 mm, 1일최대강우량은 300 m 이상이 토석류 위험이 높은 것으로 나타났다. 또한 유역환경인자 중 계상평균경사는 $10{\sim}20^{\circ}$, 계상평균폭은 10 m 미만, 계상에 있는 토석의 양은 적음(계상구성물 중 20% 미만), 수계밀도는 $1km/km^2$이내, 산사태 발생 가능성이 있는 경사 $20^{\circ}$ 이상의 분포비율은 40~60%, 산사태 위험도 2등급 이상 비율은 40~60%, 유목이 있는 상태, 사방공작물 시설이 있는 경우, 임상환경인자 중 영급은 3영급, 소밀도는 밀, 임상은 혼효림 등의 인자가 토석류 위험이 높은 것으로 나타났다.

한강유역의 중소하천에 대한 계획하폭 산정 (Determination of Design Width for Medium Streams in the Han River Basin)

  • 전세진;안태진;박정응
    • 한국수자원학회논문집
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    • 제31권6호
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    • pp.675-684
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    • 1998
  • 본 연구는 한강유역 중소하천 계획하폭 산정공식을 결정하기 위하여 216개 구간의 중소하천에서의 계획홍수량, 유역면적, 하상경사, 실제하폭을 수집한 후, 1) 최소자승법(least squares, LS), 2) 최소중간치자승법(least median squares, LMS) 및 3) 재가중최소자승법(reweighted least squares, RLS)을 이용하여 경험적인 계획 하폭 공식을 결정하였다. 한강유역에서의 기존하폭 산정공식과 비교하기 위하여 계획하폭 산정공식의 형식은 6가지 형으로 고려하였다. 기존하폭공식과 6가지 형의 공식을 평가하기 위하여 평균제곱근오차, 절대평균오차 및 평균오차를 계산하여 비교 검토한 결과, 하폭공식의 형식으로는 본 연구의 하폭-계획홍수량-하상경사로 표현된 공식이 적합한 것으로 나타났다. 본 연구에서 추정된 계획하폭 산정공식은 한강유역 중소하천 설계시 계획하폭 결정의 지표로 적용될 수 있으리라 기대된다.

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수치해석을 이용한 하천제방의 건전도 평가 (River Embankment Integrity Evaluation using Numerical Analysis)

  • 변요셉;정혁상;김진만;최봉혁;김경민;천병식
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2009년도 세계 도시지반공학 심포지엄
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    • pp.524-528
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    • 2009
  • An influence factors for soundness evaluation of river levee include resistibility and embankment for piping of ground consisting embankment in case piping, permeability coefficient of ground, height of embankment, the width of crest, material characteristics of embankment and foundation ground, shape of embankment slope, an influence for penetration of rainfall or river water in case slope stability. In this study, it was operated a feasibility investigation of existing design result, stability evaluation for permeability coefficient use and permeability coefficient change of foundation ground to investigate an influence in line with permeability coefficient change for result of river levee penetration analysis. The evaluation results of influence factors, the permeability coefficient used in design and it was evaluated influence in safety factor of piping. After the evaluation of influence factors, the permeability coefficient used in the design appears with the fact that differs in a design report about same soil, Accordingly, the stability investigation of embankment by application of literature data can affect stability evaluation results by change factors like a permeability coefficient, void ratio. It should be certainly used material properties by a test in soundness evaluation of river levee.

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자연하천에서 하도의 물리적 특성과 하상재료의 상관관계분석 (Analysis of Correlation on Physical Characteristics and Bed Materials in Natural Rivers)

  • 김기흥
    • 한국환경복원기술학회지
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    • 제13권2호
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    • pp.95-104
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    • 2010
  • The purpose of this study is to analyze the correlation between physical stream characteristics and bed materials in natural rivers. Accordingly, four natural rivers were selected reference streams, they were Nam river, Sumjin River, Naesung River and Han River. Grain size distributions of bed materials were gravels, cobbles and boulders in Han river and Nam river, were sand, gravels, cobbles and boulders in Sumjin river and were sand in Naesung river. Four reference streams were divided into each two reference reaches (straight and bend) by plan and profile characteristics of naturally meandering stream. Therefore various reference reaches were chosen in the aspect of physical stream characteristics and grain size distributions. The results investigated and analyzed are as follows. The streams that grain sizes distributions of river bed materials were coarse were stable because they had variety of bed slope without sediment deposition, and then the riffles frequency and the physical characteristics were various. Also, velocitydepth regime were various in four kinds, and the response parts for water level change were small, so that channel flow status were stable and excellent condition. On the other hand, sand river that grain sizes distributions of river bed materials were fine had not the variety of parameters as velocity-depth regimes, sediment deposition, channel flow status and riffles frequency, so that the physical stream characteristics were not various.

The Effects of DEM Resolution on Hydrological Simulation in BASINS-HSPF Modeling

  • Jeon, Ji-Hong;Yoon, Chun-Gyung
    • 한국농공학회:학술대회논문집
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    • 한국농공학회 2002년도 학술발표회 발표논문집
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    • pp.453-456
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    • 2002
  • In this study, the effect of DEM resolution (15m, 30m, 50m, 70m, 100m, 200m, 300m) on the hydrological simulation was examined using BASINS (Better Assessment Science Integrating point and Nonpoint Source) for Heukcheon watershed (303.3km2) data from 1998 to 1999. Generally, as the cell size of DEM increased, topographical changes were observed as the original range of elevation decreased. The processing time of watershed delineation and river network needed more time and effort on smaller cell size of DEM. The larger DEM demonstrated had some errors in the junction of river network which might effects on the simulation of water quantity and quality. The area weighted average watershed slope became lower but the length weighted average channel slope became higher as the DEM size increased. DEM resolution affected substantially on the topographical parameter but less on the hydrological simulation. Considering processing time and accuracy on hydrological simulation DEM mesh size of 100m is recommended for this watershed.

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MAPPING SOIL ORGANIC MATTER CONTENT IN FLOODPLAINS USING A DIGITAL SOIL DATABASE AND GIS TECHNIQUES: A CASE STUDY WITH A TOPOGRAPHIC FACTOR IN NORTHEAST KANSAS

  • Park, Sunyurp
    • Spatial Information Research
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    • 제10권4호
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    • pp.533-550
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    • 2002
  • Soil organic matter (SOM) content and other physical soil properties were extracted from a digital soil database, the Soil Survey Geographic (SSURGO) database, to map the amount of SOM and determine its relationship with topographic positions in floodplain areas along a river basin in Douglas County, Kansas. In the floodplains, results showed that slope and SOM content had a significant negative relationship. Soils near river channels were deep and nearly level, and they had the greatest SOM content in the floodplain areas. For the whole county, SOM content was influenced primarily by soil depth and percent SOM by weight. Among different slope areas, soils on mid-range slopes (10-15%) and ridgetops had the highest SOM content because they had relatively high percent SOM content by weight and very deep soils, respectively. SOM content was also significantly variable among different land cover types. Forest/woodland had significantly higher SOM content than others, followed by cropland, grassland, and urban areas.

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인공강우기에 의한 시험포장 토양유실량 모의 - 강우강도, 지표면 및 경사조건 변화 - (Simulation of Field Soil Loss by Artificial Rainfall Simulator - By Varing Rainfall Intensity, Surface Condition and Slope -)

  • 신민환;원철희;최용훈;서지연;이재운;임경재;최중대
    • 한국물환경학회지
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    • 제25권5호
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    • pp.785-791
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    • 2009
  • Using artificial rainfall simulator, the soil loss, which is deemed as the most cause of muddy water problem among Non-point source (NPS) pollutant, was studied by the analysis of direct runoff, groundwater discharge, and soil water storage properties concerned with rainfall intensity, slope of area, and land cover. The direct runoff showed increasing tendency in both straw covered and bared soil as slope increases from 5% to 20%. The direct runoff volume from straw covered surface were much lower than bared surface. The infiltration capacity of straw covered surface increased, because the surface sealing by fine material of soil surface didn't occur due to the straw covering. Under the same rainfall intensity and slope condition, 2.4~8.2 times of sediment yield were occurred from bared surface more than straw covered surface. The volume of infiltration increased due to straw cover and the direct runoff flow decreased with decrease of tractive force in surface. To understand the relationship of the rate of direct runoff, groundwater discharge, and soil water storage by the rainfall intensity, slope, and land cover, the statistical test was performed. It shows good relationship between most of factors, except between the rate of groundwater storage and rainfall intensity.

우리 나라 沖積河川 河床傾斜의 水理機何 特性에 관한 연구 (A preliminary study of the hydraulic-geometrical relations of bed slope in some selected alluvial rivers)

  • 우효섭;유권규;박종관
    • 대한지리학회지
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    • 제29권3호
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    • pp.253-265
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    • 1994
  • 본 연구에서는 하상이 주로 모래로 이루어진 우리 나라 충적하천에서 종단 하상경 사와 하천수리량과의 관계를 조사하였다. 조사대상 하천들은 주로 대하천의 1차 지류 중에 서 평형상태에 있다고 보여지는 하천들이다. 평형상태를 검토하기 위해서 Richards의 평형 하천의 조건을 참고하였다. 본 연구에서 채택된 방법은 Leopold와 Maddock식 형태와 Garde식 형태 두 가지이며, 이를 위하여 유역면적 100-2,000$ extrm{km}^2$ 까지의 18개 하천에 대해 상 류로부터 하천거리에 따른 하상경사, 유역면적, 하상재료 크기의 변화 등을 조사하였다. 조 사대상 충적하천에서 하상경사와 유역면적 및 하상재료의 크기 변화를 7개 하천자료를 이용 하여 Garde식 형태로 표시한 결과는 하상재료 크기의 변화에 대한 신뢰성 있는 자료의 부 족으로 현단계로서는 객관성이 부족한 것으로 보여진다. 14개 하천자료를 이용하여 얻어진 Leopold와 Maddock식 형태로 표시한 하상경사 S는 유역면적 A와 유역면적의 변화계수 0.0063 0.0063 $eta$를 이용하면 S = $S_{0}$ $A_{0}$$^{-------- +0.51}$A-$^{-------- -0.51}$$\beta$ $\beta$ 표시할 수 있다. 이 식에 의하면 조사대상 충적하천의 종단하상경사는 개략 적으로 유역면적의 -0.6승 정도에 비례하는 것으로 나타났다.

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하천환경에서의 그라스콘크리트의 적용성 연구 (Hydraulic Application of Grass Concrete In River Environment)

  • 장석환;남용혁;김서영;박성범;박웅서;박상우
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2006년도 학술발표회 논문집
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    • pp.472-477
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    • 2006
  • This study aims at investigating the failure cases of the pre-cast block system in river environments which widely used nowadays and reviewing the effect and flow resistance for grass concrete structure through the physical experiments by hydraulic model test and developing application method in river slope or levee which has rigid flood resistance. Grass concrete structure has been independently tested under high velocity flow under the super critical condition, it survived the 8 m/sec maximum flow velocity. This results shows grass concrete system is also suited to use in aggressive river environments such as repairing a flood damaged embankment that had placed at risk the adjacent drainage channel with vegetation.

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