논문 상세보기
pp.481-494
Groundwater level hydrographs from observation wells in Jeju island clearly illustrate distinctive features of recharge showing the time-delaying and dispersive process, mainly affected by the thickness and hydrogeologic properties of the unsaturated zone. Most groundwater flow models have limitations on delineating temporal variation of recharge, although it is a major component of the groundwater flow system. Recently, a convolution model was suggested as a mathematical technique to generate time series of recharge that incorporated the time-delaying and dispersive process. A groundwater flow model was developed to simulate transient groundwater level fluctuations in Pyoseon area of Jeju island. The model used the convolution technique to simulate temporal variations of groundwater levels. By making a series of trial-and-error adjustments, transient model calibration was conducted for various input parameters of both the groundwater flow model and the convolution model. The calibrated model could simulate water level fluctuations closely coinciding with measurements from 8 observation wells in the model area. Consequently, it is expected that, in transient groundwater flow models, the convolution technique can be effectively used to generate a time series of recharge.
1. 서 론
2. 컨벌루션 기법
3. 제주도 표선유역 정류 지하수 흐름 모델
3.1. 연구지역 개요
3.2. 모델영역 및 경계조건
3.3. 지하수 이용량 및 지하수위
3.4. 대수층 수리전도도 및 지하수 함양량
3.5. 정류 모사 결과
3.6. 모델 보정
4. 컨벌루션 기법이 연동된 부정류 지하수 흐름 모델
4.1. 부정류 모델 입력 자료
4.2. 부정류 모델 보정
5. 결론
REFERENCE
