• Title/Summary/Keyword: runoff depth

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Risk assessment for inland flooding in a small urban catchment : Focusing on the temporal distribution of rainfall and dual drainage model (도시 소유역 내 내수침수 위험도 평가 : 강우 시간분포 및 이중배수체계 모형을 중심으로)

  • Lee, Jaehyun;Park, Kihong;Jun, Changhyun;Oh, Jeill
    • Journal of Korean Society of Water and Wastewater
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    • v.35 no.6
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    • pp.389-403
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    • 2021
  • In this study, dual drainage system based runoff model was established for W-drainage area in G-si, and considering the various rainfall characteristics determined using Huff and Mononobe methods, the degree of flooding in the target area was analyzed and the risk was compared and analyzed through the risk matrix method. As a result, the Monobe method compared to the Huff method was analyzed to be suitable analysis for flooding of recent heavy rain, and the validity of the dynamic risk assessment considering the weight of the occurrence probability as the return period was verified through the risk matrix-based analysis. However, since the definition and estimating criteria of the flood risk matrix proposed in this study are based on the return period for extreme rainfall and the depth of flooding according to the results of applying the dual drainage model, there is a limitation in that it is difficult to consider the main factors which are direct impact on inland flooding such as city maintenance and life protection functions. In the future, if various factors affecting inland flood damage are reflected in addition to the amount of flood damage, the flood risk matrix concept proposed in this study can be used as basic information for preparation and prevention of inland flooding, as well as it is judged that it can be considered as a major evaluation item in the selection of the priority management area for sewage maintenance for countermeasures against inland flooding.

Analysis of the Effectiveness of Runoff Reduction Facilities through the Analysis of Inundation Depth Distribution by Grid (격자별 침수심 분포 분석을 통한 우수저류시설 효과분석)

  • Lee Woo Jin;Park Jong Pyo;Kim Kwang Hyun;Jun Hwan Don
    • Proceedings of the Korea Water Resources Association Conference
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    • 2023.05a
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    • pp.504-504
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    • 2023
  • 최근 세계적인 기후변화로 인한 홍수의 빈도 및 규모가 커지게 되면서 최초 구조물의 설계시의 설계용량을 초과하는 국지적 집중호우가 발생하고 있다. 이는 도시방재를 위하여 기계획하였던 내수배제 시스템의 설계성능을 넘어 도시지역에 침수를 유발하게 된다. 이에 대한 해결책으로 도시의 내수배제 시스템을 개선하기 위한 우수저류조, 우수관거개선 등이 이루어지고 있지만 설치 이후 구체적인 효과분석이 이루어지지 않고 있다. 본 연구에서는 우수저류시설의 설치 여부에 따른 침수발생 양상을 분석하고 우수저류시설 침수저감효과를 정량적으로 분석할 수 있는 방안을 제시하였다. 이를 위하여 XP-SWMM을 이용하여 2차원 침수해석 모의를 실시하였고 다양한 조건에서의 모의를 위하여 2차원 침수해석 모의조건을 설정하였다. 기계획된 우수저류시설의 설계시의 임계지속기간을 기준으로 IDF Curve를 통하여 설계강우량, 확률강우량 및 방재성능목표량을 재산정하였고 Huff4분위법을 이용하여 강우분포를 시켜 XP-SWMM에 적용하였다. 또한, 유역 최종 방류구에서 기점수위 조건과 자유방류 조건을 분리하여 모의하였으며 최종적으로 우수저류시설의 설치여부에 따른 2차원 침수해석을 실시하였다. 2차원 침수모의 결과를 이용하여 월류량의 저감율과 격자별 침수심 분포 분석을 진행하였다. 월류량은 총량적인 지표를 가지고 있지만 격자별 침수심 분포 분석은 격자의 최대 침수심을 0.1m 간격으로 나누어 각 단계별 침수심 격자의 발생빈도를 산정하였다. 제안된 방법을 사용하여 분석을 진행한결과 우수저류조를 설치한 후에 격자의 최대침수심이 더 낮은 침수심 단계로 이동한 현상을 확인하였다. 이는 구조물의 설치 후에도 침수가 일어난다는 양적인 면이 아닌 격자의 침수심 분포 양상을 통해 도시침수에 직접적으로 저감이 나타나 효과를 기여할 수 있다는 지표라고 판단된다.

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Biological soil crusts impress vegetation patches and fertile islands over an arid pediment, Iran

  • Sepehr, Adel;Hosseini, Asma;Naseri, Kamal;Gholamhosseinian, Atoosa
    • Journal of Ecology and Environment
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    • v.46 no.1
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    • pp.31-40
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    • 2022
  • Background: Plant vegetation appears in heterogeneous and patchy forms in arid and semi-arid regions. In these regions, underneath the plant patches and the empty spaces between them are covered by biological soil crusts (moss, lichen, cyanobacteria, and fungi). Biological soil crusts lead to the formation and development of fertile islands in between vegetation patches via nitrogen and carbon fixation and the permeation of runoff water and nutrients in the soil. Results: The present study has investigated the association of biological soil crusts, the development of fertile islands, and the formation of plant patches in part of the Takht-e Soltan protected area, located in Khorasan Razavi Province, Iran. Three sites were randomly selected as the working units and differentiated based on their geomorphological characteristics to the alluvial fan, hillslope, and fluvial terrace landforms. Two-step systematic random sampling was conducted along a 100-meter transect using a 5 m2 plot at a 0-5 cm depth in three repetitions. Fifteen samplings were carried out at each site with a total of 45 samples taken. The results showed that the difference in altitude has a significant relationship with species diversity and decreases with decreasing altitude. Results have revealed that the moisture content of the site, with biocrust has had a considerable increase compared to the other sites, helping to form vegetation patterns and fertile islands. Conclusions: The findings indicated that biological crusts had impacted the allocation of soil parameters. They affect the formation of plant patches by increasing the soil's organic carbon, nitrogen, moisture and nutrient content provide a suitable space for plant growth by increasing the soil fertility in the inter-patch space.

Evaluation of Function of Upland Farming for Preventing Flood and Fostering Water Resources (밭농사의 수자원 함양과 홍수조절 기능에 대한 계량화 평가)

  • Hyun, Byung-Keun;Kim, Moo-Sung;Eom, Ki-Cheol;Kang, Ki-Kyung;Yun, Hong-Bae;Seo, Myung-Cheol
    • Korean Journal of Soil Science and Fertilizer
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    • v.36 no.3
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    • pp.163-179
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    • 2003
  • Multifunctionality of agriculture which is not traded on the market now has been an important international issue in that it environmental and public benefits. We carried out to modify and to update the function of upland farming on flood prevention and fostering water resources. Economic values of environmental benefits were evaluated by replacement cost methods. Models to evaluate the function of preventing flood were selected as: (1)precipitation(flood-inducing) - runoff(A), (2) soil depth ${\times}$ soil air phase, (3) precipitation (flood-inducing) - runoff(B), (4) soil depth ${\times}$ effective porosity of soil. Models to estimate the function of fostering water resources were (1) saturated hydraulic conductivity (Ks) ${\times}$ duration of saturation(days) ${\times}$ (1-ratio of water flow directly into river), (2) precipitation ${\times}$ ratio of water fostered by rain resources ${\times}$ (area of upland/total land area), and (3) soil water retention quantity(under standing crop or tree) - SWRQ(in bare soil). Function of preventing flood was $883Mg\;ha^{-1}$ of water per year and 645 million Mg for the whole upland area. Function of fostering water resources was $94.1Mg\;ha^{-1}$ of water per year and 69 million Mg for the whole upland area. The value of flood-preventing function evaluated by replacement cost methods was estimated 1,428 billion won per year as compared to the cost for dam construction. The value of water resource fostering were estimated 8.6 billion won in the price of living water.

Sewer overflow simulation evaluation of urban runoff model according to detailed terrain scale (상세지형스케일에 따른 도시유출모형의 관거월류 모의성능평가)

  • Tak, Yong Hun;Kim, Young Do;Kang, Boosik;Park, Mun Hyun
    • Journal of Korea Water Resources Association
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    • v.49 no.6
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    • pp.519-528
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    • 2016
  • Frequently torrential rain is occurred by climate change and urbanization. Urban is formed with road, residential and underground area. Without detailed topographic flooded analysis consideration can take a result which are wrong flooded depth and flooded area. Especially, flood analysis error of population and assets in dense downtown is causing a big problem for establishments and disaster response of flood measures. It can lead to casualties and property damage. Urban flood analysis is divided into sewer flow analysis and surface inundation analysis. Accuracy is very important point of these analysis. In this study, to confirm the effects of the elevation data precision in the process of flooded analysis were studied using 10m DEM, LiDAR data and 1:1,000 digital map. Study area is Dorim-stream basin in the Darim drainage basin, Sinrim 3 drainage basin, Sinrim 4 drainage basin. Flooding simulation through 2010's heavy rain by using XP-SWMM. Result, from 10m DEM, shows wrong flood depth which is more than 1m. In particular, some of the overflow manhole is not seen occurrence. Accordingly, detailed surface data is very important factor and it should be very careful when using the 10m DEM.

Application of Snowmelt Parameters and the Impact Assessment in the SLURP Semi-Distributed Hydrological Model (준 분포형 수문모형 SLURP에서 융설매개변수 적용 및 영향 평가)

  • Shin, Hyung-Jin;Kim, Seong-Joon
    • Journal of Korea Water Resources Association
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    • v.40 no.8
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    • pp.617-628
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    • 2007
  • The purpose of this paper is to prepare snowmelt parameters using RS and GIS and to assess the snowmelt impact in SLURP (Semi-distributed Land Use-based Runoff Process) model for Chungju-Dam watershed $(6,661.5km^2)$. Three sets of NOAA AVHRR images (1998-1999, 2000-2001, 2001-2002) were analyzed to prepare snow-related data of the model during winter period. Snow cover areas were extracted using 1, 3 and 4 channels, and the snow depth was spatially interpolated using snowfall data of ground meteorological stations. With the snowmelt parameters, DEM (Digital Elevation Model), land cover, NDVI (Normalized Difference Vegetation Index) and weather data, the model was calibrated for 3 years (1998, 2000, 2001), and verified for 1 year (1999) using the calibrated parameters. The average Nash-Sutcliffe efficiencies for 4 years (1998-2001) discharge comparison with and without snowmelt parameters were 0.76 and 0.73 for the full period, and 0.57 and 0.19 for the period of January to May. The results showed that the spatially prepared snow-related data reduced the calibration effort and enhanced the model results.

Urban Flood Simulation Considering Buildings Resistance Coefficient Based on GIS: Focused on Samcheok City (건물 저항계수에 따른 GIS기반의 밀집 시가지 침수모의 -삼척시가지를 중심으로-)

  • Ji, Juong-Hwan;Kang, Sang-Hyeok
    • Journal of Korea Water Resources Association
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    • v.43 no.2
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    • pp.211-220
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    • 2010
  • The objective of this paper presents the application of an "integrated urban flood modeling-runoff model, urban flood model and sewer system model-" in a highly urbanized area of Samcheok where is seriously inundated in 2002 and 2003. For this, we demonstrate how couple a 1-D hydrodynamic model of the river, a 2-D hydrodynamic model of the overland (surface) flow, and a sewer network model including each boundary conditions. In order to make data file for the model, topographic information like elevation and share rate of buildings are directly extracted from DEM or topographical source data without data exchange to avoid uncertainty errors. Furthermore, the research is to assess the impacts of Manning n and buildings influences to inundated depth by changing its share ratio from 10 % to 30 % in low-land urban area. As a results, we found out that the urban inundated depth was decreased by Manning n but increased by buildings ratio. The calculated results of inundation was similar with observed one in 2002 and 2003 flooding. Furthermore, the area was also inundated under not riverbank break case in 2002 flooding.

Comparison of Soil Chemistry and Environmental Characteristics of Organic Paddy and Conventional Paddy Before Basal Fertilizer Application (기비전 유기논과 관행논의 토양 화학 및 환경 특성 비교)

  • Park, Jeong-Soo;Wang, Long;Kang, Ku;Gu, Bon-Wun;Kim, Han-Joong;Hong, Seong-Gu;Hong, Seung-Gil;Park, Seong-Jik
    • Journal of The Korean Society of Agricultural Engineers
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    • v.57 no.6
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    • pp.47-57
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    • 2015
  • Organic farming system has been considered environmental friendly and sustainable agricultural practice. However, the influence of organic farming on soil quality and environment is not well informed and controversial. We sampled and analyzed 0~15 cm and 15~30 cm depth soils of organic and conventional paddy fields in Yongin and Anseong. The electric conductivity and organic matter content of organic paddy soil were significantly less (p = 0.0097, 0.0067, respectively) than those of conventional paddy soil. Available phosphate and total phosphorus in 0~15 cm depth of organic paddy soil were $211.1{\pm}135.3$, $872.4{\pm}286.3mg/kg$, respectively, less than those of conventional paddy soil. Available phosphate amount in conventional paddy was $358.8{\pm}246.7mg/kg$, which is higher than 300 mg/kg that can cause secondary environmental contamination by runoff. The amount of total nitrogen in organic paddy soil was less than that in conventional paddy while their difference was not significant. The concentration of the heavy metals in organic paddy soil was also lower than that in conventional paddy soil but their difference was not statistically significant. Our findings demonstrate that electric conductivity, organic matter, nutrients, and heavy metals in organic paddy soil were less than those in conventional paddy soil. However, additional monitoring of soil properties for longer period is necessary to certify such a conclusion.

Estimation of Magnitude of Debris Flow and Correlation Analysis Between Influencing Factors (토석류 규모 산정과 영향인자와의 상관성 분석)

  • Choi, Young-Nam;Hwan, Hui-Seok;Lee, Hyung-Ho;Yoo, Nam-Jae
    • Journal of the Korean Geosynthetics Society
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    • v.16 no.2
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    • pp.79-87
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    • 2017
  • In this paper, for 43 sites neighboring to western area of Gangwondo where disaster of debris flow occurred from 2006 to 2013, magnitude of debris flow was estimated from results of site investigation and correlation analysis between influencing factors to its magnitude was performed. Magnitude of channelized debris flow was found greater by 6.5 times of that of hill slope debris flow and approximately 5% of total volume was occurred at initiation part of channelized debris flow. As results of analyzing yield rate of debris flow, for channelized debris flow, yield rate values of $19m^3/m$ and $8m^3/m$ were obtained for total volume being over $10,000m^3/m$ as the large scale of debris flow and less than $10,000m^3/m$ respectively, and value of $5m^3/m$ was estimated for hill slope debris flow. As results of correlation analysis of influencing factors to magnitude of debris flow, runoff distance and erosion width were very highly correlated to its magnitude whereas average slope of basin and erosion depth showed relatively low correlation. In particular, value of erosion depth was in the range of 0.5-2.6 m, being similar range to the value proposed by Ikeya (1981). Triggering rainfall to debris flow such as continuous rainfall and maximum intensity of hour rainfall were analyzed to have low correlation with magnitude of debris flow.

Statistical Analyses of Soil Moisture Data from Polarimetric Scanning Radiometer and In-situ (Polarimetric Scanning Radiometer 와 In-situ를 이용한 토양수분 자료의 통계분석)

  • Jang, Sun Woo;Jeon, Myeon Ho;Choi, Minha;Kim, Tae-Woong
    • KSCE Journal of Civil and Environmental Engineering Research
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    • v.30 no.5B
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    • pp.487-495
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    • 2010
  • Soil moisture is a crucial factor in hydrological system which influences runoff, energy balance, evaporation, and atmosphere. United States National Aeronautic and Space Administration (NASA) and Department of Agriculture (USDA) have established Soil Moisture Experiment (SMEX) since 2002 for the global observations. SMEX provides useful data for the hydrological science including soil moisture and hydrometeorological variables. The purpose of this study is to investigate the relationship between remotely sensed soil moisture data from aircraft and satellite and ground based experiment. C-band of Polarimetric Scanning Radiometer (PSR) that observed the brightness temperature provides soil moisture data using a retrieval algorithm. It was compared with the In-situ data for 2-30 cm depth at four sites. The most significant depth is 2-10 cm from the correlation analysis. Most of the sites, two data are similar to the mean of data at 10 cm and the median at 7 cm and 10 cm at the 10% significant level using the Rank Sum test and t-test. In general, soil moisture data using the C-band of the PSR was established to fit the Normal, Log-normal and Gumbel distribution. Soil moisture data using the aircraft and satellites will be used in hydrological science as fundamental data. Especially, the C-band of PSR will be used to prove soil moisture at 7-10 cm depths.