• 한국지구과학회:학술대회논문집
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• 한국지구과학회 2003년도 추계학술발표회 및 정기총회
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• pp.149-150
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• 2003

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2005년도 총회 및 춘계학술발표회
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• pp.352-358
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• 2005

This study aims to separate hydrograph into baseflow and event water to calculate baseflow rate during a rainfall in small catchments, Yuseong, Daejeon, The hydrograph of stream during a period with no excess rainfall will decay. The discharge is composed entirely of groundwater contributions. During the period, the Cl concentration of the stream water can be regarded as being in equilibrium with that of the groundwater. Using Cl as a conservative tracer, two-component hydrograph separations were performed from end point of the period to next end point. The required data were obtained by monitoring of the surface water table, along with discharge rate of stream. Cl concentration of rainfall, surface water were measured and recorded. Hydrograph separation, a mixing model using chemical tracer is applied to chemical hydrograph separation technique. These results show that baseflow rates are 31.6% of rainfall in the catchments during study period.

• 한국산림과학회지
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• 제95권5호
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• pp.556-561
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• 2006

This study was conducted to choose end-members and tracers for application of End Member Mixing Analysis (EMMA) model for the coniferous forest catchment, Gwangneung Gyeongi-do near Seoul metropolitan of South Korea (N $37^{\circ}$ 45', E $127^{\circ}$ 09'). This coniferous forest of Pinus Korainensis and Abies holophylla was planted at stocking rate of $3.0stems\;ha^{-1}$ in 1976. Thinning and pruning were carried out two times in the spring of 1996 and 2004 respectively. We monitored two successive rainfall events during ten days from June 26, 205 to July 5, 2005. Two storm events were selected to determine the end members and natural traces for hydrograph separation. The event 1 amounts to 161.9 m for two days from June 26 to 27, 2005. The event 2 precipitates to 139.2 mm for one day of July 1, 205. Throughfall, groundwater, soil water and stream water of the two events above were sampled through the bulk and automatic sampler. Their chemical properties were analyzed for prediction of the main tracer. The end members that contribute to the stream runoff were identified from the three components including groundwater, soil water and throughfall. Each component and stream water in the two events formed the suitable mixing diagram in case of chloride-nitrate ion and sulfate-potassium ion. Especially, chloride-nitrate ion was found to be the most suitable tracers for EMMA model in the two events.

• 대한토목학회논문집
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• 제13권2호
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• pp.161-171
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• 1993

유역순간단위도를 수로기하학적 특성과 사면을 고려하여 유도하였다. 수로기하학적 특성은 Width function으로 정량화되며, 이것은 출구로부터 임의 흐름거리의 유량 분포를 나타낸다. 유역순간단위도의 유도에 사용된 모형은 간단한 확산함수에 의해 수로에 분포된 초기유량을 추적하는 추적요소와 사변에서의 체류시간 밀도함수인 지수분포로 나타내지는 사면요소로 구성하였다. 본 방법의 적용성을 검토하기 위하여 보청천유역, 위천유역에 대해 4개사상의 실측수문량을 이용하여 유역순간단위유량도를 산정하였으며, 산정 결과, 본 연구에서 제안한 방법 을 이용해 유역순간단위유량도를 유도할 수 있음을 확인하였다.

• 한국산림과학회지
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• 제96권5호
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• pp.561-566
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• 2007

This study was conducted to clarify runoff production processes in forested catchment through hydrograph separation using three-component mixing model based on the End Member Mixing Analysis (EMMA) model. The study area is located in the coniferous-forested experimental catchment, Gwangneung Gyeonggido near Seoul, Korea (N 37 45', E 127 09'). This catchment is covered by Pinus Korainensis and Abies holophylla planted at stocking rate of 3,000 trees $ha^{-1}$ in 1976. Thinning and pruning were carried out two times in the spring of 1996 and 2004 respectively. We monitored 8 successive events during the periods from June 15 to September 15, 2005. Throughfall, soil water and groundwater were sampled by the bulk sampler. Stream water was sampled every 2-hour through ISCO automatic sampler for 48 hours. The geochemical tracers were determined in the result of principal components analysis. The concentrations of $SO_4{^{2-}$ and $Na^+$ for stream water almost were distributed within the bivariate plot of the end members; throughfall, soil water and groundwater. Average contributions of throughfall, soil water and groundwater on producing stream flow for 8 events were 17%, 25% and 58% respectively. The amount of antecedent precipitation (AAP) plays an important role in determining which end members prevail during the event. It was found that ground water contributed more to produce storm runoff in the event of a small AAP compared with the event of a large AAP. On the other hand, rain water showed opposite tendency to ground water. Rain water in storm runoff may be produced by saturation overland flow occurring in the areas where soil moisture content is near saturation. AAP controls the producing mechanism for storm runoff whether surface or subsurface flow prevails.

• 한국지반환경공학회 논문집
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• 제11권9호
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• pp.15-25
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• 2010

본 연구는 중앙심벽형 필댐인 주암댐과 임하댐을 대상으로 자동계측에 의해 연속적으로 생산되는 침투수량 계측자료에 대하여 분석을 통하여 필댐 고유의 특성에 따른 장기 침투특성과 댐의 안전관리 방법을 검토하고자 하였다. 필댐의 침투수량 계측값에는 내재 하는 강우 성분 등의 외부 요인의 영향으로 직접적으로 이상 누수의 발생을 검출하는 것은 어렵다. 이 때문에, 종래 저수위와 강우량을 고려하는 중회귀분석 등에 의해 누수량을 추정하는 방법이 적용되어 왔으나, 강우 성분의 추정 오차가 상대적으로 크고 정밀도가 불량한 것으로 알려졌다. 본 논문에서는 강우 성분의 분리해석을 통해 직접적으로 강우 성분에 영향을 받지 않는 저수지 수위에 연동하는 댐별 침투거동을 평가함과 아울러 분석대상 댐의 지형적, 수리지질학적 특성을 반영한 3차원 수치해석을 실시하여 계측 침투수량 자료와 비교하였다. 2개 대상댐의 침투거동은 각각의 고유한 특징을 가지고 있으며, 장기적으로 침투수량의 감소를 보여주고 있어 안정적인 상태로 나타났다. 또한, 수문곡선분리법은 침투수 안전관리 방법으로 적용가능한 것으로 판단되었다.

• 한국지하수토양환경학회지:지하수토양환경
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• 제20권5호
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• pp.34-40
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• 2015

It is reported that the intensity of rainfall will likely increase, on average, over the world on 2000. For water resources security, many studies for flow paths from rainfall or snowmelt to subsurface have been conducted. In Korea, few isotopic studies for characterizations of flow path have been undertaken. For a better understanding of how water derived from atmosphere moves to subsurface and from subsurface to stream, an analysis of precipitation and stream water using oxygen-18 and deuterium isotopes in a small watershed, Dorim-cheon, Seoul, was conducted with high resolution data. Variations of oxygen-18 in precipitation greater than 10‰ (δ¹⁸O_max = −1.21‰, δ¹⁸O_min = −11.23) were observed. Isotopic compositions of old water (groundwater) assumed as the stream water collected in advance were −8.98‰ and −61.85‰ for oxygen and hydrogen, respectively. Using a two-component mixing model, hydrograph separation of the stream water in Dorim-cheon was conducted based on weighted mean value of δ¹⁸O. As a result, except of instant dominance of rainfall, contribution of old water was dominant during the study period. On average, 71.3% of the old water and 28.7% of rainfall contributed to the stream water. The results show that even in the small watershed, which is covered with thin soil layer in granite mountain region, the stream water is considerably influenced by old water inflow rather than rainfall.

• 한국수자원학회논문집
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• 제34권4호
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• pp.403-411
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• 2001

본 연구에서는 지표하층과 암반층 사이의 지표하흐름을 기존 TOPMODEL의 구조에 연계시킨 수정 TOPMODEL의 국내 유역 적용성을 검증하였다. 지표하층에 존재하고 있는 대공극은 신속한 유출발생을 위한 수문경로를 제공하고 있으며, 수문감쇠곡선 분석을 위한 이중저류체계의 필요성을 의미한다. 설마천 유역을 대상으로 2개월간의 연속적인 유역수문거동을 모의한 결과 수정 TOPMODEL은 기존 TOPMODEL에 비해 유출발생과정을 모다 포괄적이고, 현실적으로 재현할 수 있는 것으로 밝혀졌다. Monte-Carlo 방법을 도입한 매개변수 산정결과도 수정 TOPMODEL의 경우가 물리적으로 타당한 것으로 밝혀졌다.