• 제목/요약/키워드: Drainage basin

검색결과 324건 처리시간 0.025초

하계망패턴의 특색으로 구분한 중국의 자연지역 (The Physical Region of China Divided by the Characteristics of Drainage Patterns.)

  • 황상일
    • 한국지역지리학회지
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    • 제2권1호
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    • pp.151-164
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    • 1996
  • 하계망은 유역분지의 지질, 지형, 기후 등의 영향을 예민하게 반영하면서 발달하므로, 하계망 패턴의 특징에 따른 지역구분은 자연환경을 종합적으로 이해하는데 중요한 의의를 갖는다. 본연구는 자연환경이 매우 다양한 중국을 대상으로 하계망특색을 통하여 자연지역구분을 시도하였다. 중국의 하계망은 크게 내륙하천유역분지와 의류하천유역분지로 나누어 지며, 내륙하천유역분지는 (1)난맥상(亂脈狀) 하폐망(deranged pattern)과 (2)구심상 하계 망으로, 의류하천유역분지는 (1)수지상 하재망, (2)평행상 하계망, (3)선상 하재망, (4)망상 하계망으로 나누어 진다. 내륙하천유역분지의 하계망형성에는 지형과 기후가 함께 영향을 미치고, 의류하천유역분지에서 나타나는 평행상 하계망은 주로 지반운동에 결과된 지질구조선, 선상 하계망은 황하의 범람으로 인한 유로변경, 망상 하계망은 인간의 활동 등과 같은 요인에 의한 것이다. 이들의 지역적 분포는 난맥상 하계망은 짱베이(장북(藏北))고원지역, 구심상 하계망은 건조분지지역, 평행상 하계망은 양쯔대지와 인도판 사이의 구조운동의 영향을 강하게 받고 있는 횡단산맥지역, 양쯔강 상류지역, 칭짱(청장(靑藏))고원 이남의 갠지즈(Ganges River)강 상류유역분지지역이며, 선상 하계망은 황하하류 선상지지역인 하이허(해하(海河)) 화이허(회하(淮河)강 유역분지지역이고, 망상 하계망은 양쯔강삼각주, 장쑤성북부해안 및 주장강(주강(珠江)) 삼각주지역이다. 이들 지역을 제외한 나머지 지역은 가장 일반적으로 볼 수 있는 수지상 하계망을 하고 있다.

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도시하수도망에 대한 유출모형의 남용과 유출해석 (Runoff Analysis and Application of Runoff Model of Urban Storm Drainage Network)

  • 박성천;이관수
    • 한국환경보건학회지
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    • 제22권4호
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    • pp.33-42
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    • 1996
  • This research is to show the application of runoff model and runoff analysis of urban storm drainage network. the runoff models that were used for this research were RRL, ILLUDAS, and SWMM applicative object basin were Geucknak-chun and Sangmu drainage basin located in Seo-Gu, Kwangju. The runoff analysis employed the design storm that distributed the rainfall intensity according to the return period after the huff's method. The result from the comparative analysis of the three runoff models was as follows The difference of peak runoff by return period was 20-30% at Sangmu drainage area of $3.17 Km^2$, while less than 10% at Geucknak-chun drainage area of $12.7 Km^2$. The peak runoff were similar to all models. At the runoff hydrograph the times between rising and descending points were in the sequence of RRL, ILLUDAS and SWMM, but the peak times were similar to all models. The conveyance coefficient to examine the conveyance of the existing drainage network was 0.94-1.37, which means insecure, in Geucknak-chun drainage basin and 0.69-1.16, which means secure, in sangmu drainage basin.

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Comparative Study on the Runoff Process of Granite Drainage Basins in Korea and Mongolia

  • Tanaka, Yukiya;Matsukura, Yukinori
    • 한국제4기학회지
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    • 제17권2호
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    • pp.79-84
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    • 2003
  • This study revealed the differences in runoff processes of granite drainage basins in Korea and Mongolia by hydrological measurements in the field. The experimental drainage basins are chosen in Korea (K-basin) and Mongolia (M-basin). Occurrence of intermittent flow in K-basin possibly implies that very quick discharge dominates. The very high runoff coefficient implies that most of effective rainfall quickly discharge by throughflow or pipeflow. The Hortonian overlandflow is thought to almost not occur because of high infiltration capacity originated by coarse grain sized soils of K- basin. Very little baseflow and high runoff coefficient also suggest that rainfall almost does not infiltrate into bedrocks in K-basin. Flood runoff coefficient in M-basin shows less than 1 %. This means that most of rainfall infiltrates or evaporates in M-basin. Runoff characteristics of constant and gradually increasing discharge imply that most of rainfall infiltrates into joint planes of bedrock and flow out from spring very slowly. The hydrograph peaks are sharp and their recession limbs steep. Very short time flood with less than 1-hour lag time in M-basin means that overland flow occurs only associating with rainfall intensity of more than 10 mm/hr. When peak lag time shows less than 1 hour for the size of drainage area of 1 to 10 km2, Hortonian overland flow causes peak discharge (Jones, 1997). The results of electric conductivity suggest that residence time in soils or weathered mantles of M-basin is longer than that of K-basin. Qucik discharge caused by throughflow and pipeflow occurs dominantly in K-basin, whereas baseflow more dominantly occur than quick discharge in M-basin. Quick discharge caused by Hortonian overlandflow only associating with rainfall intensity of more than 10 mm/hr in M-basin.

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도시유역의 내수배제시스템 설계를 위한 유출특성분석 -SWMM의 적용- (Runoff Characteristics Analysis for Interior Drainage Systems in Urban Basin -Application of SWMM-)

  • 최윤영;이영화
    • 한국환경과학회지
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    • 제9권3호
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    • pp.193-199
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    • 2000
  • This study is carried out the analysis of the runoff characteristics for the design of the interior drainage systems by SWMM in urbanization basin. The basin analyzed in this study is Bumuh-chun basin which is located in Susung-gu of Taegu city. Huff method is used for rainfall distribution analysis. The optimal rainfall duration in Bumuh-chun basin is analyzed as about 90 minutes decided from comparison of arrival time and critical duration. Flood flow variation pattern is proposed through the comparison of the results of peak flow and peak time analyzed by SWMM about pre-urbanization and post-urbanization of Bumuh-chun basin. It is known that the variation of arrival time caused by the rapid increase of pavement rate in the upper area shows about 20∼25 minutes faster than pre- urbanization. Therefore, the management of surface water for design of water supply and drainage, and channel alteration has to considered the variation of geological factors according to urbanization.

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Fractal 나무의 개념을 기반으로 한 설마천 시험유역의 Fractal 차원 추정 (Estimation of fractal dimension for Seolma creek experimental basin on the basis of fractal tree concept)

  • 김주철;정관수
    • 한국수자원학회논문집
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    • 제54권1호
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    • pp.49-60
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    • 2021
  • 본 연구에서는 Fractal 나무의 개념을 이용하여 자연유역의 두 가지 개별적 Fractal 차원을 추정하는 방법을 제시하고자 한다. 이를 위하여 Fractal 나무의 성장 과정을 기반으로 유역 내부에서 발생 가능한 모든 배수 경로를 추출하여 완전한 배수망을 구성하고 이에 해당하는 Fractal 특성을 분석해 보고자 한다. 유역 내부에서 Fractal 나무의 성장 과정은 하천 유동의 특성을 가지는 배수 경로에서만 제한적으로 나타날 수 있다. 소규모 유역의 경우 Fractal 나무의 성장 단계에 따라 망상 구조의 분기 특성이 단일 하천 구간의 사행 특성에 비하여 민감하게 변화하여 단일한 망상 구조 속에서도 다양한 분기 구조가 생성될 수 있다. 따라서 소규모 유역을 대상으로 한 망상 구조에 대한 Fractal 차원은 단일한 수치의 고정된 형태보다는 범위의 형태로 취급되어야 하는 것이 타당한 것으로 판단된다. 또한, 소규모 유역의 배수 구조에 대한 분석에는 지형도나 수치지도로부터 추출한 하천망보다 본 연구에서 제시한 Fractal 나무의 성장에 따른 망상 구조와 같은 정보가 더 유용할 수 있을 것으로 판단된다.

배수밀도와 수원유역의 기하학적 특성을 기반으로 한 배수구조에 대한 해석 (Analysis of Drainage Structure Based on the Geometric Characteristics of Drainage Density and Source-Basin)

  • 김주철;김재한
    • 한국수자원학회논문집
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    • 제40권5호
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    • pp.373-382
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    • 2007
  • 수로가 시작되는 지점의 정확한 위치를 찾는 것은 구릉지 사면상의 물의 동적거동으로 인하여 매우 어렵다. 이러한 목적을 위하여, 김주철과 김재한(2007)은 DEM을 이용한 경사와 면적 사이의 규모에 따른 거동특성에 따라 실제 유역내 수로망을 제시한 바 있다. 본 연구는 이들의 연구 성과의 연장으로서, 배수밀도와 수원유역의 기하학적 특성을 기반으로 하여 DEM으로부터 동정된 가설수로망의 신뢰성을 평가하여 보았다. 그 결과 경사-면적한계기준에 의한 가설수로망이 자연유역의 배수구조를 매우 잘 묘사하고 있음을 확인할 수 있었다. 또한 지형학적 동질성을 가진 지역내 수원유역의 형상들 사이에는 훌륭한 기하학적 상사성이 존재함을 추론할 수 있었다. 면적한계기준은 수원유역의 형상을 구속하여 왜곡된 배수구조를 야기할 수도 있었다. 그럼에도 불구하고 DEM으로부터 동정된 가설수로망들이 공간 채움 구조를 잘 표현하고 있는 점이 특히 주목된다.

고속도로 현장별 비점오염 저감시설 선정방안 연구 (A Study for selecting the Highway Sites' Best Management Practice for Nonpoint Source Pollution)

  • 이용복;최상일;박계수;성일종;정선국
    • 환경영향평가
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    • 제20권6호
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    • pp.857-866
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    • 2011
  • This research categorized EIA target highways into following three types in order to minimize non-point source pollution from highway runoff. 1. Big drainage basin. 2. Small drainage basin. 3. Bridge section. The Natural, Filter and Swirl-Type devices were evaluated in terms of removal efficiency of TSS, BOD, COD, T-N, T-P, compatibility of site selection, economic feasibility, and maintenance convenience through which the final BMP was selected. According to the removal efficiency result, the area of Big and Small Drainage basin and bridge section had higher removal efficiency with natural facility than that of the Filter or Swirl-Type device. To make appropriate selection of highways'BMP for non-point source pollution, this study will aim to contribute to building more environmentally friendly highways by proposing the selection process that is made of 5 stages. 1. Selecting the target drainage basin. 2. Selecting the land for the mitigation facility. 3. Analysing the ease of maintenance. 4. Technically evaluating each installation. 5. Evaluating the effective implementation methods.

하계망으로 본 영산강 유역 옹관묘의 입지특성 (Location Characteristics of the Jar Coffins in the Yeongsan River Basin on the Drainage Network)

  • 이애진;박지훈;이찬희
    • 한국지형학회지
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    • 제23권3호
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    • pp.57-66
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    • 2016
  • The objective of this study is to find out geomorphological characteristics of historical ruins where people produced and consumed large jar coffins excavated in the Yeongsan river basin using the map of old drainage network to restore distribution network. For this purpose, we chose the 21 consumption sites. The results are as follows. First of all, large jar coffins(relics, 47.6% of total) in the Yeongsan River basin were located in Sampo stream basin, almost all of them were located within the Yeongsan River main stream basin and Sampo stream basin. Also, distance from all consumption site to river was within about 2km. Therefore, it is thought that the all consumption sites are located at the place of the gift of nature that was very favorable to water transport of jar coffins. The results of this study may be used as basic data for research of cultural relics in the Yeongsan river basin.

도시 하수도망의 수문학적인 평가와 설계확률유량의 점대화 성향에 관한 연구(제1보) (A Study on Hydrologic Analysis and Some Effects of Urbanization on Design Flow of Urban Storm Drainage Systems (1))

  • 강관원;서병하;윤용남
    • 물과 미래
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    • 제14권4호
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    • pp.27-34
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    • 1981
  • The design flow of the urban strom drainage systems has been assessed largely on a basis of empirical relations between rainfall and runoff, and the rational formula has been widely used for the cities in our country. In order to estimate it more accurately, the urban runoff simulation model based on the RRl method has been developed and applied to the sample basin in this study. The rainfall hyetograph of the design stromfor the design flow has been obtained by the determination of the total rainfall and the temporal distributions of that rainfall. The total rainfall has been assessed from the empirical formula of rainfall intensity and the temporal distribution of that rainfall determined on the basis of Huff's method from the historical rainfall data of the basin. The virtual inflow hydrograph to each inlet of the basin has been constructed by computing the series of discharges in each time increment, using design strom hyetograph and time-area diagram. The actual runoff hydrograph at the basin outlet has been computed from the virtual inflow hydrographs by developing a relations between discharge and storage for the watershed. The discharge data for verification of the simulated runoff hydrograph are not available in the sample basin and so the sensitivity analysis of the simulation model has not been possible. The peak discharge for the design of drainage systems has been estimated from the computed runoff hydrograph at the basin outlet and compared to thatl obtained form the rational formula.

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부착성장 조류 제어를 위한 침전지 배수로의 재질개선에 관한 연구 (Improvement of Drainage Material for Attached Algae Growth Control in Sedimentation Basin)

  • 전대영;임병란;유현선;조진우;황종혁;안규홍
    • 상하수도학회지
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    • 제19권2호
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    • pp.193-199
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    • 2005
  • The objective of this study was to investigate the characteristics of adhesion and detachment of algae on various materials of drainage canal in the sedimentation basin. The influence of surface washability, surface roughness, phosphorous concentration was studied using stainless steel, cement block and ceramic panel. The algae attached content of cement block was higher than that of the ceramic coating panel. The attachment varied significantly with respect to exposure time and different materials. the attachment was higher on rough surface (cement block) when compared to smooth surfaces. The content of attached algae increased with increasing phosphorous concentration in water. The detachment efficient of algae was higher on ceramic panel.