• Journal of Environmental Science International
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• v.29 no.1
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• pp.25-32
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• 2020

The determination of soil parameters is important in predicting the simulated surface runoff using either a distributed or a lumped rainfall-runoff model. Soil characteristics can be collected using remote sensing techniques and represented as a digital map. There is no universal agreement with respect to the determination of a representative parameter from a gridded digital map. Two representative methods, i.e., arithmetic and predominant, are introduced and applied to both FLO-2D and HEC-HMS to improve the model's accuracy. Both methods are implemented in the Yongdam catchment, and the results show that the former seems to be more accurate than the latter in the test site. This is attributed to the high conductivity of the dominant soil class, which is A type.

• Proceedings of the KSRS Conference
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• v.2
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• pp.602-605
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• 2006

This study is to apply QuickBird satellite image for the simulation of storm runoff in a small rural watershed. For a 1.05 $km^2$ watershed located in Goesan-Gun of Chungbuk Province, the land use from the QuickBird image was produced by on-screening digitising after ortho-rectifying using 2 m DEM. For 3 cases of land use, soil and elevation scale (1:5,000, 1:25,000 and 1:50,000), SCS (Soil Conservation Service)-CN (Curve Number) and the watershed physical parameters were prepared for the storm runoff model, HEC-HMS (Hydrological Modelling System). The model was evaluated for each case and compared the simulated results with couple of selected storm events.

• Proceedings of the Korea Water Resources Association Conference
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• 2016.05a
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• pp.168-168
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• 2016

도시화는 수문학적으로 산림이나 농경지와 같은 투수지역을 건물, 도로 등의 불투수 지역으로 변화시키는 것이며, 이로 인하여 홍수파의 도달시간이 줄어들고 첨두유량이 증가하는 등의 수문변화를 수반하게 된다. 도로나 건물 등이 대부분을 차지하고 있는 도시지역에서는 지표면이나 식생으로부터 대기 중으로 방출되는 증발산량이 농촌이나 산림지역보다 상대적으로 적으며, 강우시 토양중의 침투량과 지표면의 저류량도 도시지역에서는 매우 적게 나타난다. 도시화 전 후의 물순환특성을 평가하기 위해서는 도시 개발 전 후의 장단기 수문 관측 결과를 기초로 물순환계를 구성하는 인자간의 관계를 정량적으로 분석하고 물순환계 구성요소의 일부 변화가 다른 부분에 미치는 영향을 평가할 필요가 있다. 즉, 도시화가 물순환 구조 변동에 미치는 영향을 정량적으로 평가함으로써 유역 전체의 건전한 물순환 체계를 유지할 수 있는 대책 수립이 가능하다. 본 연구에서는 판교신도시 개발에 따른 유역에서의 홍수 및 유출특성 변화의 정량적 규명을 목적으로 두고 집중형 모형인 HEC-HMS모형과 물리적 기반의 준분포형 모형인 CAT을 이용하여 판교신도시 개발전의 정량적 물순환 특성을 평가하였다. 대상유역은 지방 2급 하천 탄천의 지류인 운중천, 금토천이 포함된 판교유역이며, 유역면적은 약 $25km^2$이다. 이 중 유역면적의 38 %에 해당하는 지역이 개발되었으며 개발된 지역은 하류부근에 위치한다. 강우자료는 지상 강우관측소인 수원 관측소의 지점강우 자료를 이용하였다. 도시 개발 전 단계에 해당하는 2006년, 2007년 호우사상 중 누적강우량 50 mm 이상인 호우사상을 추출하여 모의를 수행하였다. 유출 특성 분석을 위해 12개의 소유역과 5개의 하도로 구성하였으며 HEC-HMS의 손실량 산정방법으로는 SCS Curve Number법을 사용하였고, 단위도는 Clark 단위 도법을 적용하였다. CAT모형에서 침투는 Rainfall Excess방법, 하도추적은 Muskingum 방법을 적용하였다. 관측치와 모의치의 적합도 검증을 위해 RMSE (Root Mean Square Error), NSE (Nash Sutcliffe Efficiency), $R^2$값을 산정하여 비교 분석하였다.

• Proceedings of the KSR Conference
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• 2001.10a
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• pp.562-567
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• 2001

In this study, performance of reinforced railroad roadbeds with the slag(HMS-25) and soil were investigated through the real scale railroad roadbed tests. Several real scale reinforced railroad roadbeds were constructed in the laboratory with different subgrade conditions and were tested with the estimated actual train loads including the impact loading of train. The affecting factors such as plastic ＆ elastic settlement roadbed layers as well as surface of rails were measured. The settlement at rail surface and roadbed surface of case of soil and slag roadbed comparative with good roadbed site were 2.3, 5.7 times and 1.9, 1.6 times, respectively.

• Proceedings of the Korean Geotechical Society Conference
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• 2001.03a
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• pp.223-230
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• 2001

Nine different types of the reinforced railroad roadbeds which . are located in between Suwon-Chunan station of Kyongbu line were constructed in order to increase the bearing capacity of railroad roadbed and to improve the ridability as a part of speed-up project of conventional railroad systems. Each three sections were composed of weathered granite soil, crushed stone and furnace slag(HMS25), and fully instrumented with earth pressure cells, settlement plates and geophones to monitor the behavior of roadbeds under actual train loads. Field measurement has continued since October 31, 2000 and presently with rather longer measurement interval. The measurement data such as settlement, earth pressure and vibration levels are currently under analysis process. In this paper, only cumulative measurement data of railroad roadbeds were introduced. In the near future, comprehensive measurement data and result of analysis will be presented and design technique for the reinforced railroad roadbed will be proposed as a final product of this study.

• Journal of the Korean GEO-environmental Society
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• v.25 no.9
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• pp.5-14
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• 2024

In Korea, torrential rain frequency and intensity have surged over the past five years (2019-2023), breaking rainfall records. Due to insufficient observation facilities for rainfall and runoff data in small mountainous catchments, preparing for unexpected floods is challenging. This study examines the Bidogyo catchment in Goesan-gun, Chungcheongbuk-do, comparing design flood discharge calculated with optimized parameters versus standard guidelines. Using HEC-HMS and Q-GIS for model construction, five rainfall events were analyzed with data from the National Water Resources Management Information System. The time of concentration (Tc) and storage constant (K) were calculated using the Seokyeongdae formula and model optimization. Results showed that optimized parameters produced higher objective function values for flood events. The design flood discharge varied by -10.7% to 17.3% from the standard guidelines when using optimized parameters. Moreover, optimized parameters yielded flood discharges closer to observed values, highlighting limitations of the Seokyeongdae formula for all catchments. Further research aims to develop suitable parameter estimation methods for small mountainous catchments in Korea.

• Journal of The Korean Society of Agricultural Engineers
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• v.62 no.6
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• pp.85-95
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• 2020

According to the standard guidelines of design flood (MLTM, 2012; MOE, 2019), the design flood is calculated based on past precipitation. However, due to climate change, the frequency of extreme rainfall events is increasing. Therefore, it is necessary to analyze future floods' volume by using climate change scenarios. Meanwhile, the standard guideline was revised by MOE (Ministry of Environment) recently. MOE proposed modified Huff distribution and new CN (Curve Number) value of forest and paddy. The objective of this study was to analyze the change of flood volume by applying the modified Huff and newly proposed CN to the probabilistic precipitation based on SSP and RCP scenarios. The probabilistic rainfall under climate change was calculated through RCP 4.5/8.5 scenarios and SSP 245/585 scenarios. HEC-HMS (Hydrologic Engineering Center - Hydrologic Modeling System) was simulated for evaluating the flood volume. When RCP 4.5/8.5 scenario was changed to SSP 245/585 scenario, the average flood volume increased by 627 ㎥/s (15%) and 523 ㎥/s (13%), respectively. By the modified Huff distribution, the flood volume increased by 139 ㎥/s (3.76%) on a 200-yr frequency and 171 ㎥/s (4.05%) on a 500-yr frequency. The newly proposed CN made the future flood value increase by 9.5 ㎥/s (0.30%) on a 200-yr frequency and 8.5 ㎥/s (0.25%) on a 500-yr frequency. The selection of climate change scenario was the biggest factor that made the flood volume to transform. Also, the impact of change in Huff was larger than that of CN about 13-16 times.

• Proceedings of the Korean Institute of Electrical and Electronic Material Engineers Conference
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• 2008.06a
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• pp.370-370
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• 2008

ITO 박막은 현재 차세대 디스플레이인 LCD, PDP, ELD 등의 평판 디스플레이의 화소전극 및 공통전극으로 가장 많이 적용되고 있는 소재이며, 최근에는 태양전지의 투명전극으로 그 용도가 더욱 증가되고 있다. 이러한 소자들의 투명 전도막으로 사용되기 위해서는 가시광선 영역에서 80% 이상의 높은 투과도와 낮은 면 저항을 가져야 한다. 광 투과도와 면 저항은 ITO 박막의 증착조건에 따라 변하게 되는데 본 연구에서는 DC 마그네트론 스퍼터링법을 이용하여 Indium-Tin Oxide (ITO) 박막을 제작하고, 제작된 ITO 박막의 전기적 특성과 광학적 특성을 측정하여 공정조건에 따른 박막의 특성 변화를 평가하였다. 증착 조건은 주로 기판 온도와 증착 시간을 변화시켰다. 본 실험에서는 $In_2O_3$ : $SnO_2$의 조성비가 9:1 비율의 순도 99.99% ITO 타겟을 사용하였으며, coming 1737 glass를 30$\times$30 mm 크기로 가공하여 기판온도와 증착시간을 변화시키면서 ITO 박막을 제조하였다. 예비실험을 통해 인가전력 50W, 초기 진공 $2\times10^{-6}$ Torr, 작업 진공 $3.5\times10^{-2}$ Torr, 기판과 타겟 사이의 거리를 10 cm로 고정하였다. 기판 온도는 히터를 가열하지 않은 상온 ($25^{\circ}C$)에서 $400^{\circ}C$까지의 범위에서 변화시켰고, 증착시간은 5분에서 30분까지의 범위에서 변화시켰다. 증착된 박막의 면 저항 촉정을 위해 4 point probe를 사용하였고, 홀 (hall) 계수 측정기 (HMS-300)를 이용하여 홀 계수를 측정하였으며, 또한 박막의 두께는 $\alpha$-step을 사용하여 측정하였다. ITO 박막의 상분석을 위해 XRD를 사용 하였고, SEM을 이용하여 미세구조를 관찰하였다. 실험 결과로는 기판온도 $400^{\circ}C$, 증착시간 15분 이상에서는 면 저항이 모두 $8\Omega$/$\Box$이하로 낮게 나왔으며, 투과율 또한 모두 80% 이상의 높은 투과도를 보였다. 또한 ITO박막의 전기 전도도는 캐리어 농도와 이동도의 측정을 통해 두 가지 인자들에 의해 비례되는 것을 확인하였다.

• 한국방재학회:학술대회논문집
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• 2011.02a
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• pp.172-172
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• 2011

The interaction between land surface and atmosphere is essentially affected by hydrometeorological variables including soil moisture. Accurate estimation of soil moisture at spatial and temporal scales is crucial to better understand its roles to the weather systems. The KLDAS(Korea Land Data Assimilation System) is a regional, specifically Korea peninsula land surface information systems. As other prior land data assimilation systems, this can provide initial soil field information which can be used in atmospheric simulations. For this study, as an enabling high-resolution tool, weather research and forecasting(WRF-ARW) model is applied to produce precipitation data using GFS(Global Forecast System) with GFS embedded and KLDAS soil moisture information as initialization data. WRF-ARW generates precipitation data for a specific region using different parameters in physics options. The produced precipitation data will be employed for simulations of Hydrological Models such as HEC(Hydrologic Engineering Center) - HMS(Hydrologic Modeling System) as predefined input data for selected regional water responses. The purpose of this study is to show the impact of a hydrometeorological variable such as soil moisture in KLDAS on hydrological consequences in Korea peninsula. The study region, Chongmi River Basin, is located in the center of Korea Peninsular. This has 60.8Km river length and 17.01% slope. This region mostly consists of farming field however the chosen study area placed in mountainous area. The length of river basin perimeter is 185Km and the average width of river is 9.53 meter with 676 meter highest elevation in this region. We have four different observation locations : Sulsung, Taepyung, Samjook, and Sangkeug observatoriesn, This watershed is selected as a tentative research location and continuously studied for getting hydrological effects from land surface information. Simulations for a real regional storm case(June 17~ June 25, 2006) are executed. WRF-ARW for this case study used WSM6 as a micro physics, Kain-Fritcsch Scheme for cumulus scheme, and YSU scheme for planetary boundary layer. The results of WRF simulations generate excellent precipitation data in terms of peak precipitation and date, and the pattern of daily precipitation for four locations. For Sankeug observatory, WRF overestimated precipitation approximately 100 mm/day on July 17, 2006. Taepyung and Samjook display that WRF produced either with KLDAS or with GFS embedded initial soil moisture data higher precipitation amounts compared to observation. Results and discussions in detail on accuracy of prediction using formerly mentioned manners are going to be presented in 2011 Annual Conference of the Korean Society of Hazard Mitigation.

• Journal of The Korean Society of Agricultural Engineers
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• v.59 no.1
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• pp.81-96
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• 2017

Along with climate change, it is reported that the scale and the frequency of extreme climate events (e.g. heavy rain, typhoon, etc.) show unstable tendency of increase. In case of Korea, also, the frequency of heavy rainfall shows increasing tendency, thus causing natural disaster damage in downtown and agricultural areas by rainfall that exceeds the design criteria of hydraulic structures. In order to minimize natural disaster damage, it is necessary to analyze how extreme precipitation event changes under climate change. Therefore a new design criteria based on non-stationarity frequency analysis is needed to consider a tendency of future extreme precipitation event and to prepare countermeasures to climate change. And a quantitative and objective characteristic analysis could be a key to preparing countermeasures to climate change impact. In this study, non-stationarity frequency analysis was performed and inundation risk indices developed by 4 inundation characteristics (e.g. inundation area, inundation depth, inundation duration, and inundation radius) were assessed. The study results showed that future probable rainfall could exceed the existing design criteria of hydraulic structures (rivers of state: 100yr-200yr, river banks: 50yr-100yr) reaching over 500yr frequency probable rainfall of the past. Inundation characteristics showed higher value in the future compared to the past, especially in sections with tributary stream inflow. Also, the inundation risk indices were estimated as 0.14 for the past period of 1973-2015, and 0.25, 0.29, 1.27 for the future period of 2016-2040, 2041-2070, 2071-2100, respectively. The study findings are expected to be used as a basis to analyze future inundation damage and to establish management solutions for rivers with inundation risks.