This study intends to estimate the best model parameters for predicting the water quality and discharge of the study area, and provide the basic data necessary for predicting the water quality and discharge and examining changes in water quality on the basis of the changes hydraulic and hydrological changes and pollutional load of the study area. Nakdong River was selected for analysis, and the water quality survey data necessary for parameter estimation was based on the monthly water quality data (discharge, BOD, T-N and T-P) between December 1, 2002 ~ November 31, 2002. The topographical characteristics factors of the study area were based on the 1/25,000 numerical map published by the National Geographic Information Institute and satellite photographs. The presumed course: It measured the most suitable parameter that could imitate surveyed water quality and discharge using the method of trial and error, in this part the first numerical value was the model parameter presented SWAT. The result of analisys showed that a relative error between surveyed value and the result of water quality imitation about BOD, T-N, T-P that examined by this study, discharge correction : R2=0.912, discharge verification : R2=0.838, correction and verification of BOD : R2=0.847, correction and verification of T-N : R2=0.712 and, correction and verification of T-P : R2=0.726 and, BOD : RK1, RK3, T-N : RS3, RS4, T-P : RS2, RS5, GWSOLP, discharge : ALPAHA_BF, GWQMN, CH_N(2), CN2, SOL_AWC have been considered as the factors of the water quality performed in this water quality simulation, that is, the most effective parameters on BOD, T-N and T-P. It is considered that it will be possible to apply the most optimal parameter to an analysis of the water quality and discharge simulation at study area in the goal year by examining the interaction of the parameters through the parameters sampling which are able to applicable to prediction of the water quality and discharge in the future, also the analysis on the basis of the hydrological conditions: an outflow or the character of a flow will be needed.

The applied model for this study area is WINFLOW using finite element method, It is thought that the simulation result by WINFLOW model under the steady flow state reflects well the ground water distribution within the reliability level which shows the error range of 1.1% to 8.0% from the comparison between the computed values and the observed, and analyzed that the constant head distribution is shown along the east-west direction and gentle and stable head gradient along the north-south direction. Ground water of the study area shows stable movement from the south to the stream area, and the particle trace for each location shows relatively linear shape from the upstream to the pumping location while the radius of influence according to the pumping amount shows a significant difference at the down stream area from the pumping location. The simultaneous pumping from P and P1 shows more complicated appearance, not the increase of the radius of influence than pumping from a single well P or P1, and it is analyzed that the particle path takes nearly linear form. It is known that the flow direction of the ground water and the velocity of the flow affect on the magnitude of the radius of influence of the wells from the fact that the more decreasing pattern of the ground water head is observed at the side of the well and the down stream area than the upstream area when the ground water moves from south to north regarding the radius of influence according to the pumping amount. Satisfactory results in analyses of ground water movement are obtained through the significant reduction of the physical uncertainties in the flow system as well as the relatively convenient model application using WINFLOW model which is proposed in this study.

본 연구에서는 제주도 서귀포유역의 지하수 유동시스템 해석을 위해 MODFLOW 모델을 이용하였으며 양수량 측정자료를 통한 투수량계수 및 저류계수를 초기치로 선정하여 시행착오법을 통한 대상유역의 최종 매개변수를 얻을 수 있었고 모델의 모의 발생을 한 결과 지하수유동시스템에 대한 적용성이 잘 반영됨을 알 수 있었다. 서귀포 유역은 지형지질을 고려한 관측치 해석, 이(1996)의 연구결과 및 모의발생을 통한 결과로 볼 때 지하수두 분포는 표고 400m이내에서

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.

In the rainfall-runoff relation, consideration of the spatial movement of storms is very important in designing a hydraulic structure or evaluating an environmental influence for land usage. Because of this reason, this study has suggested the finite element model which consider the spatial movement of a stome and it was applied on a small river basin(Wi stream basin). In the application of the model the basin was treated as a pivot point and the storms are simulated with movement in each directions. As a result, it shows that the storms moving from north to south have bigger peak discharge and faster peak time than the storms moving in other directions. So these characteristics have to be considered in the designation of a hydraulic structure or evaluation of an environmental influence.