• 제목/요약/키워드: Runoff ratio

검색결과 319건 처리시간 0.029초

산지 소규모 유역의 유출 특성 평가-용담 구량천 (Assessment of Small Mountainous Catchment Runoff at Yongdam-dam Guryang)

  • 김성구;장형준;이효상
    • 한국산학기술학회논문지
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    • 제19권4호
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    • pp.633-641
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    • 2018
  • 최근 들어 홍수와 가뭄과 같은 자연 재해의 위험이 증가하고 있다. 이러한 위험을 저감하기 위하여 신뢰할 수 있는 수문자료는 수자원 분석 및 수공구조물 설계에 있어 매우 중요하다. 한국의 중부에 위치한 용담 구량천 유역은 K-water와 UNESCO IHP의 연구유역으로써 신뢰 할 수 있는 강수량, 유출량, 증발산량 등의 수문자료를 제공하고 있다. 본 연구는 실측된 수문자료를 바탕으로 우리나라의 산지 유역의 유출 특성을 분석하기 위하여 용담 구량천 유역에서의 유출특성을 Probability Distributed Model을 적용하여 분석하였다. 분석 결과, 유역 유축을 홍수기(6월-9월), 평수기(10-5월)로 기간 분리하여 분석하는 것이 필요함을 확인하였다. 유역 유출비가 홍수기에는 0.27~0.41, 평수기에는 0.30~0.45의 분포를 나타내고 있다. Probability Distributed Model은 적용기간에 따라 차별화된 검정 매개변수를 제시하고 있다. 또한, 2015년 평수기를 제외하고 다른 기간은 유역의 유출을 모두 적합(Nash Surcliffe Efficiency >0.7)하게 모의하고 있어 모형의 적용성을 확인하였다. 본 연구는 Probability Distributed Model을 활용한 기간분리를 통한 소규모 산지 유역의 유출특성방법을 제시한다.

제수원공 설계를 위한 장기간 연속수수량 추정모형의 개발 - 중심유역을 중심으로 (A Developmont of Numerical Mo del on the Estimation of the Log-term Run-off for the Design of Riverheads Works -With Special Reference to Small and Medium Sijed Catchment Areas-)

  • 엄병현
    • 한국농공학회지
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    • 제29권4호
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    • pp.59-72
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    • 1987
  • Although long-term runoff analysis is important as much as flood analysis in the design of water works, the technological level of the former is relatively lower than that of the latter. In this respect, the precise estimation model for the volume of successive runoff should he developed as soon as possible. Up to now, in Korea, Gajiyama's formula has been widely used in long-term runoff analysis, which has many problems in applying in real situation. On the other hand, in flood analysis, unit hydrograph method has been exclusively used. Therefore, this study aims at trying to apply unit hydrograph method in long-term runoff analysis for the betterment of its estimation. Four test catchment areas were selected ; Maesan area in Namlum river as a representative area of Han river system, Cheongju area in Musim river as one of Geum river system, Hwasun area in Hwasun river as one of Yongsan river system, and Supyung area in Geum river as one of Nakdong river system. In the analysis of unit hydrograph, seperation of effective rainfall was carried out firstly. Considering that effective rainfall and moisture condition of catchrnent area are inside and outside of a phenomenon respectively and the latter is not considered in the analysis, Initial base flow(qb)was selected as an index of moisture condition. At the same time, basic equation(Eq.7) was established, in which qb can take a role as a parameter in relating between cumulative rainfall(P) and cumulative loss of rainfall(Ld). Based on the above equation, computer program for estimation model of qbwas seperately developed according to the range of qb, Developed model was applied to measured hydrographs and hyetographs for total 10 years in 4 test areas and effective rainfall was estimated. Estimation precision of model was checked as shown in Tab- 6 and Fig.8. In the next stage, based on the estimated effective rainfall(R) and runoff(Qd), a runoff distribution ratio was calculated for each teat area using by computerised least square method and used in making unit hydrographs in each test area. Significance of induced hydrographs was tested by checking the relative errors between estimated and measured runoff volume(Tab-9, 10). According to the results, runoff estimation error by unit hydrograph itself was merely 2 or 3 %, but other 2 or 3 % of error proved to be transferred error in the seperation of effective rainfall. In this study, special attentioning point is that, in spite of different river systems and forest conditions of test areas, standardized unit hydrographs for them have very similar curve shape, which can be explained by having similar catchinent characteristics such as stream length, catchinent area, slope, and vegetation intensity. That fact should be treated as important factor ingeneralization of unit hydrograph method.

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미래토지이용 및 기후변화에 따른 하천유역의 유출특성 분석 (Analysis of Future Land Use and Climate Change Impact on Stream Discharge)

  • 안소라;이용준;박근애;김성준
    • 대한토목학회논문집
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    • 제28권2B호
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    • pp.215-224
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    • 2008
  • SLURP 준 분포형 수문모형을 이용하여 예측된 토지이용 자료와 미래 기후변화 시나리오에 의한 기상자료 및 식생지수 정보를 고려한 상태에서 하천유역의 유출에 미치는 영향을 분석하였다. 경안천 경안수위관측소 상류유역($260.4km^2$)을 대상으로 4개년(1999-2002) 동안의 일별 유출량 자료를 바탕으로 모형의 보정(1999-2000)과 검증(2001-2002)을 실시하였다. 토지이용 예측은 1996년, 2000년, 2004년의 Landsat TM 및 ETM+ 위성영상을 이용하여 CA-Markov 기법으로 검증(2004)을 실시한 후, 미래의 토지이용(2030, 2060, 2090)을 예측하였다. 예측된 토지이용은 시간이 경과할수록 산림과 논은 지속적으로 감소하고 도시, 초지, 나지 등은 증가하는 경향을 보였다. 미래의 식생정보 예측을 위하여 NOAA/AVHRR 위성영상으로부터 추출된 월별 NDVI(1998-2002)와 월평균기온간의 선형 회귀식을 도출하여 미래의 식생지수 정보(2030, 2060, 2090)를 추정하였다. IPCC SRES A2, B2 기후변화 시나리오에 대한 CCCma CGCM2 모의결과 값(2030s, 2060s, 2090s)을 Stochastic Spatio-Temporal Random Cascade Model(SST-RCM) 기법을 이용하여 downscaling 한 뒤 하천유출의 변화를 분석한 결과, 기후변화에 따른 하천유출율은 1999-2002년의 59%에 비해 미래에는 13%~34%로 감소하는 것으로 모의되었고, 반면에 토지이용의 변화에 대한 유출율은 0.1%~1% 증가하였다.

Determination of flood-inducing rainfall and runoff for highly urbanized area based on high-resolution radar-gauge composite rainfall data and flooded area GIS Data

  • Anh, Dao Duc;Kim, Dongkyun;Kim, Soohyun;Park, Jeongha
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2019년도 학술발표회
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    • pp.157-157
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    • 2019
  • This study derived the Flood-Inducing-Rainfall (FIR) and the Flood-Inducing-Runoff (FIRO) from the radar-gage composite data to be used as the basis of the flood warning initiation for the urban area of Seoul. For this, we derived the rainfall depth-duration relationship for the 261 flood events at 239 watersheds during the years 2010 and 2011 based on the 10-minute 1km-1km radar-gauge composite rainfall field. The relationship was further refined by the discrete ranges of the proportion of the flooded area in the watershed (FP) and the coefficient variation of the rainfall time series (CV). Then, the slope of the straight line that contains all data points in the depth-duration relationship plot was determined as the FIR for the specified range of the FP and the CV. Similar methodology was applied to derive the FIRO, which used the runoff depths that were estimated using the NRCS Curve Number method. We found that FIR and FIRO vary at the range of 37mm/hr-63mm/hr and the range of 10mm/hr-42mm/hr, respectively. The large variability was well explained by the FP and the CV: As the FP increases, FIR and FIRO increased too, suggesting that the greater rainfall causes larger flooded area; as the rainfall CV increases, FIR and FIRO decreased, which suggests that the temporally concentrated rainfall requires less total of rainfall to cause the flood in the area. We verified our result against the 21 flood events that occurred for the period of 2012 through 2015 for the same study area. When the 5 percent of the flooded area was tolerated, the ratio of hit-and-miss of the warning system based on the rainfall was 44.2 percent and 9.5 percent, respectively. The ratio of hit-and-miss of the warning system based on the runoff was 67 percent and 4.7 percent, respectively. Lastly, we showed the importance of considering the radar-gauge composite rainfall data as well as rainfall and runoff temporal variability in flood warning system by comparing our results to the ones based on the gauge-only or radar-only rainfall data and to the one that does not account for the temporal variability.

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강우시 및 건기시 축산지역에서 배출되는 오염물질의 유출특성 비교 (Characteristics of Pollutant Concentration from Livestock Wastewater Effluent Combined with Stormwater Runoff)

  • ;;이유화;김이형
    • 한국물환경학회지
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    • 제28권6호
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    • pp.896-901
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    • 2012
  • 축사지역은 가축분뇨처리장으로부터의 오염물질 배출농도가 높아 인근 하천의 수질 및 수생태계에 큰 영향을 끼친다. 또한 강우시에는 축사주위에 축적되어 있던 각종 비점오염물질들이 강우유출수와 함께 유출되어 처리장 방류수와 함께 인근 하천의 주요 오염원으로 작용한다. 그러나 점오염원으로 배출되는 처리장의 배출수와 비점오염원 형태로 배출되는 강우유출수의 오염물질 유출특성이 달라 관리에 어려움을 겪고 있다. 본 연구에서는 축사지역의 점및 비점오염원의 특성을 분석하여 향후 가축분뇨 관리대책 수립에 필요한 기본자료를 제공하고자 한다. 연구대상지역은 10ha의 돈사 지역이며 모니터링은 2008년 10월부터 2011년 11월까지 3년동안 수행되었다. 입자상 물질 및 인의 배출농도는 비점오염원에서 높게 나타났으며, 유기물질 및 질소의 배출농도는 점오염원에서 높게 나타났다. 또한 비점오염원이 섞인 유출수에서는 TN/TP 비에 비해 낮은 BOD 농도를 보였다. 축사지역의 가축분뇨관리는 비점오염원에서의 입자상 물질 관리와 유기물질에 비해 높게 배출되는 점오염원의 영양염류 관리가 필요한 것으로 나타났다.

고속도로 노면 청소에 따른 강우시 유출오염부하 저감 효과 분석 (Effect of Road Sweeping on the Abatement of Runoff Pollution Loads from in the Highway)

  • 강희만;이두진;윤현식
    • 상하수도학회지
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    • 제26권6호
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    • pp.851-860
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    • 2012
  • In this study, to evaluate the abatement of runoff pollution loads by the road sweeping(cleaning), various investigations are implemented at the sample area of the highway. As the results of evaluating the removal efficiency of pollutants along road cleaning, TSS showed about 78 % of the removal efficiency and COD showed 49 % of removal efficiency through the operation of cleaning vehicle of vacuum suction method. In case of TN and TP, they showed the relatively-lower removal efficiency by 30~35 %. TSS removal efficiency along the number of cleaning appeared about 60 % in case of one time of cleaning and the additional removal effect did not appear though the number of cleaning increased to two times. With running speed of cleaning vehicle, TSS removal ratio is lessened from 60 % to 20 % when cleaning vehicle speed up to 20 km/hr from 6 km/hr. It seems that the reasons why the removal efficiencies are inversely proportional to its speed are related to the lower vacuum efficiencies and the disturbed particles on the road. In the pollutant build-up analysis, it is showed that it takes more time to the critical pollutant build-up in the shoulder than the center of the road. It is also showed that the proper cleaning cycle is recommended as 4~6 dry weather days without rainfall events.

교량 강우유출수내 비점오염물질의 유출특성 및 상관성 (Washoff Characteristics and Correlation of Nonpoint pollutants in a Bridge Storm Runoff)

  • 위승경;김이형;정용준;길경익
    • 한국물환경학회지
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    • 제24권3호
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    • pp.378-382
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    • 2008
  • During the dry periods, many types of pollutants are being accumulated on the paved surface by vehicle activities and the accumulated various pollutants are inflowing into the near watershed areas for the rainfall periods. Particularly, bridges are the centralized region to be the surface runoff of the stromwater due to the high ratio of the impermeable area. Also, the metals, toxic chemicals and sediments originated from bridges could be strongly influenced to the watershed areas during the runoff. Therefore, the present study is achieved to provide washoff characteristics and correlation from the bridge during rainfall periods. The result shows that the EMC ranges for 95% confidence intervals in a bridge land use are 10.12~128.09 mg/L for TSS, 6.07~21.15 mg/L for BOD, 2.10~6.70 mg/L for TN and 0.06~0.85 mg/L for TP.

도시 소유역 유효불투수율의 민감도 분석 (Sensitivity analysis of effective imperviousness estimation for small urban watersheds)

  • 김대근;고영찬
    • 상하수도학회지
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    • 제23권2호
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    • pp.181-187
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    • 2009
  • In this study, a runoff hydrograph and runoff volume were calculated by using the kinetic wave theory for small urban watersheds based on the concept of low impact development(LID), and the effective imperviousness was estimated based on these calculations. The degree of sensitivity of the effective imperviousness of small watersheds to the impervious to pervious area ratio, infiltration capability, watershed slope, roughness coefficient and surface storage depth was then analyzed. From this analysis, the following conclusions were obtained: The effective imperviousness and paved area reduction factor decreased as the infiltration capability of pervious area increased. As the slope of watersheds becomes sharper, the effective imperviousness and the paved area reduction factor display an increasing trend. As the roughness coefficient of impervious areas increases, the effective imperviousness and the paved area reduction factor tend to increase. As the storage depth increases, the effective imperviousness and the paved area reduction factor show an upward trend, but the increase is minimal. Under the conditions of this study, it was found that the effective imperviousness is most sensitive to watershed slope, followed by infiltration capability and roughness coefficient, which affect the sensitivity of the effective imperviousness at a similar level, and the storage depth was found to have little influence on the effective imperviousness.

Global Assessment of Current Water Resources using Total Runoff Integrating Pathways and Global GIS

  • Taikan Oki;Takao Saruhashi;Yasushi Agata;Shinjiro Kanae;Katumi Musiake
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2001년도 학술발표회 논문집(I)
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    • pp.67-75
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    • 2001
  • Anticipated water scarcity in the first half of this century is one of the most concerned international issues. However, even though the issue has an international impact and world wide monitoring is critical, there are limited number of global estimates at present. In this study, annual water availability was derived from annual runoff estimated by land surface models using Total Runoff Integrating Pathways (TRIP) with 0.5 degree by 0.5 degree longitude/latitude resolution globally. Global distribution of water withdrawal for each sector in the same horizontal spatial resolution was estimated based on country-base statistics of municipal water use, industrial water use, and agricultural intake, using global geographical information system with global distributions of population and irrigated crop land area. The total population under water stress estimated for 1995 corresponded very well with former estimates, however, the number is highly depend on how to assume the ratio how much water from outside of the region can be used for water resources within the region. It suggests the importance of regional studies evaluating the possibility of water intake as well as the validity of the investment for water resources withdrawal facilities.

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시설재배지 토양의 유거수에 의한 염류의 이동 (Salt Movement of Soils by Runoff in Green House Area)

  • 강보구;김현주;이경자;김재정;홍순달
    • 한국환경농학회지
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    • 제20권2호
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    • pp.112-115
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    • 2001
  • 염류가 집적된 시설재배지 토양에 대한 유거수에 의한 염류의 이동을 조사하여 농업환경보전자료로 활용하고자 충북 청주지역 시설재배농가 포장에 유거수를 수거할 수 있는 lysimeter를 설치하여 시험을 수행한 결과 다음과 같다. 본 시험중에 내린 강우량의 유거수율은 $38{\sim}77%$의 범위로 평균 58% 이었고 유거수중의 양이온 평균 함량은 $Ca^{2+}(27.12\;mg/L)$ > $K^-(9.18\;mg/L)$ > $Mg^{2+}(2.53\;mg/L)$ > $Na^+(1.89\;mg/L)$의 순이었으며 음이온들의 평균 함량은 $SO_4\;^{2-}(63.38\;mg/L)$ > $NO_3\;^-(25.40\;mg/L)$ > $Cl^-(4.19\;mg/L)$ > $PO_4\;^{3-}(3.18\;mg/L)$의 순이었다. 조사기간중에 내린 강우량의 유거수에 의한 용탈량은 농도가 가장 높았던 $SO_4\;^{2-}$가 140.1 kg/ha 로 가장 많았으며 그 다음은 $Ca^{2+}:$ 59.9 kg/ha, $NO_3\;^-:$ 56.1 kg/ha, $K^+:$ 20.3 kg/ha, $Cl^-:$ 9.3 kg/ha, $PO_4\;^{3-}:$ 7.0 kg/ha, $Mg^{2+}:$ 5.6 kg/ha, $Na^+:$ 4.2 kg/ha 순이었다. 유거수의 $PO_4\;^{3-}$의 함량 및 용탈량은 토양에 집적된 함량에 비하여 낮았다.

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