• Water for future
• /
• v.35 no.5
• /
• pp.21-30
• /
• 2002

The inflow into a multi-purpose dam reservoir contains many suspended solids from the upper stream during the rainy season. Concentrations of SS increased to 73.3 mg/l and the TP measurement increased to 0.09 mg/l during the rainy season in 1999. It was discovered that particles less than $10\;\mu\textrm{m}$ in size composed about 50% of the total amount. Some of these particles reduce the reservoir capacity and have an impact on water. In this study, the sediment depth at Daecheong multi-purpose dam was examined. Piston coring was performed at 9 locations At Hoenam 1 out of 9 locations examined showed maximum depth, which was 90 cm and at Muneui 3 showed the minimum depth, which was 35 cm. At Hoenam, the release rate of TN was found to be $62.14~84.72\;mg/\textrm{m}^2{\cdot}day$ in 1998. However, it was found to considerably reduced to $23.20\;mg/\textrm{m}^2{\cdot}day$ in 2001. The release rate of TP was measured at $13.02~14.38\;mg/\textrm{m}^2$.day at 1998, and it was reduced to $6.93mg/\;mg/\textrm{m}^2{\cdot}day$ in 2001.

• The Korean Journal of Ecology
• /
• v.13 no.4
• /
• pp.297-309
• /
• 1990

The distribution of aquatic macrophytes in TanChon basin, a stream of the Han River, were investigated in terms of environmental gradient from June 1989 to March 1990. In the basin, 12 species of aquatic macrophytes were listed and four communities of Potamogeton crispus community. $P. octandrus$ community, $Hydrilla verticillata$ community and $Vallisneria$ asiatica community were recongized by character species. $P. crispus, P. octandrus$ and $V. asiatica$ were found in rapids while $H. verticillata , Ceratophyllum demersum$ and $Trapa japonica$ were done in pools. The depth of sediment $TanCh\u{o}n$ was showed as a exponential function of water velocity, Bd=exp (-K Wv). The values of Biochemical Oxygen Demand(BOD), Chemical Oxygen Demand(COD) and Suspendid Solid(SS) were recorded as range of 3.2~121.0mg/1, 4.2~54.5mg/1 and 4.1~114.0mg/1, respectively. And the linear positive correlation between BOD(X) and COD(Y) were expressed as Y=3.904+0.4308 X with $R^2$=0.9808 and also the correlation between BOD value(X) and SS value(Y) were done as Y=5.333+0.9606X with $R^2$=0.9700. In two dimensional analysis of BOD and water velocity, their clusters were showed similar types matching to communities classified by character species. However, no aquatic macrophyes were found at the site with BOD$\geq$50mg/l or DO$\leq$0.2mg/l.

• KCID journal
• /
• v.14 no.2
• /
• pp.207-213
• /
• 2007

For sustainable development at a watershed, environment friendly site-specific management practices need to be developed and implemented. The soil and Water Assessment Tool(SWAT)model has been world-wide used to estimate stream flow, sediment, and nonpoint source pollutant loads, and effects on water quality of different management practices. In this study, the SWAT model was used to estimate the flow resources at Hwacheon areas using Digital Elevation Model(DEM),Land use, precipitation ,wind ,maximum and minimum temperature, solar radiation, humidity of watershed The R2 value and EI value for the comparison of SWAT estimated flow and measured flow were 0.87 and 0.67 respectively for calibration period, and the R2 value and E1 value for validation were 0.75 and 0.67 respectively. The comparison results show what the SWAT model is applicable to simulate hydrology behaviors at this study watershed.

• Proceedings of the Korea Water Resources Association Conference
• /
• 2007.05a
• /
• pp.253-257
• /
• 2007

Channel-aquifer interaction is one of the key hydrological processes that determine water flows in the stream/river channel. Field measurements of channel-aquifer interaction, however, is very difficult and costly, particularly when one intends to understand its variations across a catchment for a long period. Hydrological simulations using a catchment model are a relatively easier and cheaper alternative provided the model structure is appropriate for describing channel-aquifer interaction. In this study, a catchment model called CAMEL (Chemicals from Agricultural Management and Erosion Losses) is used for estimating channel-aquifer interaction over time and space. CAMEL is a distributed catchment model to simulate transformation and transport processes of sediment and pollutants as well as water flows at the catchment scale. In the model, a catchment is represented using a network of square columns each of which is comprised of various storages of water. CAMEL explicitly simulates both surface and subsurface processes including channel-aquifer interaction. This paper presents an application study results of CAMEL for the Tarland Burn Catchment, a small (catchment area $52\;km^2$) rural catchment in Scotland, UK, demonstrating some of the channel-aquifer interaction dynamics across the catchment during a 2-year period.

• Journal of Korean Society of Coastal and Ocean Engineers
• /
• v.13 no.1
• /
• pp.56-60
• /
• 2001

Tidal asymmetry which is generated at the mouth of an estuary tends to be more serious toward the upper stream due to the growth of shallow tides. Thus careful observations and applications for the shallow tides are needed if studies related to sediment or pollutant transport are carried on. An aim of the present study was to clarify the characteristics of generation and propagation of shallow tides by various numerical experiments including the effect of inter-tidal zone. The results of the present study will give a fundamental guide for the analysis of tidal envirorunental changes and for the design of a numerical model if coastal constructions are conducted.

• Journal of The Korean Society of Agricultural Engineers
• /
• v.57 no.1
• /
• pp.89-97
• /
• 2015

This study is to assess the effect of non-point source pollution discharge loads between tillage and no-tillage applications for upland crop areas using SWAT (Soil and Water Assessment Tool) watershed modeling. For Byulmi-cheon small rural catchment ($1.17km^2$) located in upstream of Gyeongan-cheon watershed, the rainfall, discharge and stream water quality have been monitored in the catchment outlet since 2011. The SWAT model was calibrated and validated in hourly basis using 19 rainfall events during 2011-2013. The average Nash-Sutcliffe model efficiency and $R^2$ (determination coefficient) for streamflow were 0.67 and 0.79 respectively. Using the 10 % surface runoff reduction from experiment results for no-tillage condition in field plots of 3 % and 8 % slopes under sesami cultivation, the soil saturated hydraulic conductivity for upland crop areas was adjusted from 0.001 mm/hr to 0.0025 mm/hr in average. Under the condition, the catchment sediment, T-N (total nitrogen, TN), and T-P (total phosphorus, TP) discharge loads were reduced by 6.9 %, 7.4 %, and 7.7 % respectively.

• Water for future
• /
• v.19 no.4
• /
• pp.321-328
• /
• 1986

Bottom sediment-river water samples were studied to determine the extent of biodegradable matter and to examine the reduction of COD, TKN and TOC by using of warburg and aerated batch reactor. Warburg studies were conducted to study the Oxygen Uptake Rates, Reaction Rate Constants and CBOD. Bacth reator studies were conducted to determine the reduction of COD, TKN and TOC. Results from the batch recator study indicate high concentration of COD in samples. Less than 10 precent of the Organic Carbon was found to be biodegradable in 48 hours of Warburg experiment. Appreciable Immediate Oxygen Demand of sediments suggests that dredging of the river bottom is likely to deplete dissolved significantly in the river water.

• Korean Journal of Remote Sensing
• /
• v.11 no.2
• /
• pp.59-73
• /
• 1995

The study is focused on the analysis of geomorphological environment changes of alluvial bar in lower Kum river using satellite-based multitemporal/multisensor data. Landsat datas for environment changes analysis consists of Landset MSS(2 scenes) and Landset TM(7 scenes) acquired from 1979 to 1994. This study is to develop the analysis techniques for the environment change detection of using ratio, classification, false color composite etc, of Landsat data especially useful to the geomorphological study of tidal flats and river channels. The results of this study can be summarized as follows : 1. The lower Kum River alluvial bar have had rapid geomorphological changes after the construction of the temporary dam to block the river flowing in 1983. The most alluvial bar located in the river has both bankway growth, especially the allurival bar in the Lower Kum River had grown between 1983 to 1990. 2. After construction of the estuarine barrage, no remarkable geomorphological changes have been found in Kum River area but the growth and formation of new underwater bar has continued. The enormous materials was needed for the growth and formations of new underwater barrier oslands and bar would be supplied from the sea bottom and river sediment to diminish of stream velocity after construction of the estuarine barrage.

• Proceedings of the Korea Water Resources Association Conference
• /
• 2023.05a
• /
• pp.220-220
• /
• 2023

단순한 하상 변동 모형은 단일한 입경으로 구성된 하상재료를 다루는 데에 비해, 실제 하천에서는 다양한 입경의 유사가 섞여있다. 이러한 혼합 입경의 유사 이송을 모의하고자 하면 퇴적층의 생성과 소멸을 어떻게 모의하는지에 대한 기법이 중요해진다. 과거 연구에서는 유수의 영향을 받는 하상 두께가 입도 분포에 따라 다르다고 생각하였다. 반면, 다른 연구들에서는 두께가 합리적인 범위 내에 있다면 모의 결과에 영향을 미치지 않는다고 보고 상수로 설정하였다. 퇴적층의 개수를 어떻게 고려하느냐에 따라서도 모의기법이 나누어진다. 단일한 입경을 모의하는 경우 단일 퇴적층을 고려하지만, 혼합 입경을 고려하는 모형은 크게 2개의 퇴적층(active layer와 non-active layer)으로 나누는 종류와 3개 이상의 퇴적층을 고려하는 모형으로도 나눌 수 있다. 이 연구에서는 혼합 입경의 유사 이송을 모의할 수 있는 전 지형 발달 모형을 활용하여 퇴적층 처리 기법의 차이가 얼마나 모의 결과에 영향을 주는지를 파악하였다. 모의 결과는 기법이 바뀜에 따라 매우 민감하게 변하는 것을 확인할 수 있었다. 또한 이 연구에서는 3개 이상의 퇴적층을 고려함에 있어서 기존 퇴적층에 새로운 물질이 퇴적되었을 때 경계면에서 입자가 섞이는 mixed layer를 고려하는 개념을 제시한다.

• Proceedings of the Korea Water Resources Association Conference
• /
• 2021.06a
• /
• pp.174-174
• /
• 2021

지표면에서 소규모의 요철로 이루어진 미세지형 (Micro Topography)은 자연 지형의 일반적인 특징이다. 지표면에서의 흐름해석 시 이러한 미세지형에 의한 효과를 정확히 고려하기 위해서는 고해상도의 지형격자를 사용하여야 하나, 대부분의 지표유출모델은 미세지형이 존재하지 않는 저해상도의 거친 표면으로 간주함으로써 바닥 마찰 효과를 증가시켜 미세지형에 의한 영향을 대략적으로만 반영한다. 본 연구에서는 보다 정확한 강우-유출 및 유사-유출 해석을 목적으로 고해상도의 지형격자를 사용하여 미세지형을 포함한 건조 및 반건조 지대에서의 흐름을 수치적으로 모의하였다. 미세지형의 형태는 마루와 골 사이가 직선으로 이루어진 파동의 형태로 이상화 하였으며, 파동의 진폭과 파장을 조절하여 다양한 형태의 미세지형을 고려하였다. 수치모형은 흐름의 움직임에 대한 Saint-Venant 방정식과 침식 및 유사이송에 대한 Hairsine-Rose 방정식을 함께 계산하는 통합모형인 tRIBS-FEaST를 사용하였다. 수치 모의 결과에서 나타난 미세지형의 핵심 영향은 최대 유량 및 유사량 도달시간의 지연, 유사 입자 크기별 유사-유출량 증감, 그리고 하천 유출(stream flow)의 생성이었다. 또한, 미세지형의 형태에 따라 미세지형과 강우-유출 및 유사-유출 사이에 비례 혹은 반비례 관계가 성립함을 보였다. 수치 모의 결과를 종합적으로 검토하여 미세지형이 강우-유출과 유사-유출에 미치는 영향에 대해 논의하였으며, 기존 Manning 거칠기 계수를 통한 해석 방법의 적부를 판단하였다.