• 생태와환경
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• 제45권1호
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• pp.34-41
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• 2012

The variation of dissolved oxygen (DO) was monitored with high frequency by an automatic data-logging sensor in a eutrophic urban stream (the Anyang Stream) located in a metropolitan area of Seoul, South Korea. In general, DO showed the diel variation of increase in daytime and decrease at night, implying that primary production is a major mechanism of oxygen supply in this ecosystem. The fluctuation of oxygen was determined by rainfall. DO depletion was most obvious after a rainfall resulting in an anoxic condition for a day, which is thought to be caused by scouring of periphyton and organic ooze at the stream bottom. Seasonally DO was higher in winter and frequently depleted in warm seasons. DO depletion was often at a dangerous level for fish survival. Fish survey showed that little fish was living at the study site and oxygen depletion may be the major stress factor for aquatic animals. From the results it can be suggested that a high frequency monitoring of oxygen should be established for the proper assessment of aquatic habitats and better management strategy.

• 한국지하수토양환경학회지:지하수토양환경
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• 제21권1호
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• pp.61-71
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• 2016

Visual MODFLOW was used for quantifying stream-aquifer interactions caused by seasonal groundwater pumping. A hypothetical conceptual model was assumed to represent a stream-aquifer system commonly found in Korea. The model considered a two-layered aquifer with the upper alluvium and the lower bedrock and a stream showing seasonal water level fluctuations. Our results show that seasonal variation of the stream depletion rate (SDR) as well as the groundwater depletion depends on the stream depletion factor (SDF), which is determined by aquifer parameters and the distance from the pumping well to the stream. For pumping wells with large SDF, groundwater was considerably depleted for a long time of years and the streamflow decreased throughout the whole year. The impacts of return flow were also examined by recalculating SDR with an assumed ratio of immediate irrigation return flow to the stream. Return flow over 50% of pumping rate could increase the streamflow during the period of seasonal pumping. The model also showed that SDR was affected by both the conductance between the aquifer and the stream bed and screen depths of the pumping well. Our results can be used for preliminary assessment of water budget analysis aimed to plan an integrated management of water resources in riparian areas threatened by heavy pumping.

• 한국농공학회논문집
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• 제47권6호
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• pp.15-24
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• 2005

The normalization on the characteristics of water level change at the upstream gauging station was attempted according to the operation of drainage sluice gate of the Geumgang estuary dam. The characteristics were normalized by the analysis of water level change and by the linear-regression of the water level data measured at the inner station of Geumgang estuary dam and upstream gauging station. The results of normalization may be referred to the management of Geumgang estuary lake, the operation of pumping and drainage stations in the shore of the lake. The mean response time of water level change on Ibpo, Ganggyeong and Gyuam water level station were 39,81 and 160 minutes, when sluice gate was opened respectively. The mean velocity of surface wave, the mean displacement of water level change, the mean time of water level change and the mean rate of water level change varied largely depending on the location of gauging station and the characteristics of stream section of the water level gauging station.

• 한국해안·해양공학회논문집
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• 제20권6호
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• pp.589-601
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• 2008

한강 하구역에 존재하는 신곡수중보의 철거 유무에 따른 지하수위 변동을 MODFLOW 모형을 이용하여 분석, 예측하였다. 토양의 비균질성을 반영하기 위하여 유효투수계수를 산정하였으며, 그 값은 지표면과 수평방향의 경우 0.313 m/day, 지표면과 수직 방향의 경우 0.0423 m/day이며, 이방성비는 7.19이다. 수중보 철거로 인한 하천 수위 하강은 지하수위 하강을 초래하며, 새로운 평형에 도달하는 시간은 약 3개월이 소요된다. 또한, 수중보 철거전에는 한강 본류에서 굴포천 쪽으로 지하수 함양이 되지만, 수중보 철거후에는 그 반대의 방향으로 기저유출이 진행된다. 수중보 철거로 인해서 수중보 상류 한강 본류의 영향을 받는 인접 지역에서는 최대 30 cm의 지하수위 감소가 발생한다. 그러나 수중보 하류의 수위를 배수 기점 수위로 하는 굴포천의 영향을 받는 굴포천 인근 지역에서는 약 10 cm의 지하수 하강이 발생한다. 한편, 대상 지역 부근의 단위면적당($km^2$) 지하수 이용량은 $52m^3/day$이며, 이러한 지하수 이용량은 신곡 수중보 철거 전후를 망라하여 최대 1 m의 지하수위 하강을 유발한다. 즉, 수중보의 철거로 인하여 유발되는 지하수위의 변동은 상시의 지하수의 이용량에 의한 지하수위 변동에 미치지 못한다.

• 대한기계학회논문집B
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• 제21권3호
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• pp.427-435
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• 1997

Conditional sampling techniques are utilized to investigate the relation between the wall skin-friction and stream wise velocity fluctuations in a turbulent boundary layer. Conditionally averaged results using a peak detection and the VITA (variable-interval time-averaging) technique show that a high skin friction is associated with high frequency components of the wall skin-friction fluctuations. The conditionally averaged wall skin-friction fluctuations obtained by using the VITA technique have a positively-skewed characteristics compared with the conditionally averaged stream wise velocity fluctuations. It is confirmed that there exists a phase shift between the wall skin-friction and stream wise velocity fluctuations, which was also found from the long-time averaged space-time correlations. The amount of phase shift between the wall skin-friction and stream wise velocity fluctuations is the same as that from the long-time averaged space-time correlations and does not change despite the variation of the detection threshold.

• 한국환경과학회지
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• 제22권5호
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• pp.515-522
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• 2013

To investigate groundwater variation characteristics in the Hancheon watershed, Jeju Island, an integrated hydrologic component analysis was carried out. For this purpose, SWAT-MODFLOW which is an integrated surface-groundwater model was applied to the watershed for continuous watershed hydrologic analysis as well as groundwater modeling. First, ephemeral stream characteristics of Hancheon watershed can be clearly simulated which is unlikely to be shown by a general watershed hydrologic model. Second, the temporally varied groundwater recharge can be properly obtained from SWAT and then spatially distributed groundwater recharge can be made by MODFLOW. Finally, the groundwater level variation was simulated with distributed groundwater pumping data. Since accurate recharge as well as abstraction can be reflected into the groundwater modeling, more realistic hydrologic component analysis and groundwater modeling could be possible.

• 한국환경생태학회지
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• 제34권4호
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• pp.282-293
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• 2020

본 연구에서는 2009-2019년 기간 동안 대전시 외곽의 도심개발에 따른 인근 하천(관평천)의 상류, 중류, 하류의 구간에서 4회 조사(2009, 2010, 2016, 2019)를 통해 이화학적 수질, 어류 종 조성, 생태 건강성 특성에 대해 장기간 변화추이를 분석하였다. 본 하천지역에서 도심개발은 2008년에 이루어졌고, 2012년에는 하천복원사업이 수행되어 하천복원 전과 후의 특성변화 추이를 모니터링 하였다. 하천 생태건강도 평가를 위해 군집수준의 어류평가지수(Fish Assessment Index, FAI)를 이용하였고, 어류의 기관(Organ) 수준에서 해부학적 건강도(Necropsy-based Health Assessment Index, HAI) 분석을 실시하였다. 이화학적 수질 분석에서는 중류(St. 2)에서 가장 낮은 탁도와 엽록소(Chl-a)가 측정되었다. 이는 빠른 유속에 의한 물리적 요인 때문으로 나타났다. 어류 조사에서는 총 18종이 채집되었고, 피라미(Zacco platypus)가 가장 우점 하는 종(40.6%)으로 나타났다. 하천복원 직후(2016)에는 민감종(Sensitive species)과 충식종(Insectivore species)이 우점, 종 다양도 및 종 풍부도 지수 상승, 생태건강도 지수(FAI)가 상승하여 생태 건강도는 "최상상태(A: 87.5)"로 나타났으나 가장 최근 조사인 2019년에는 전 기간에 비해 악화되는 것으로 나타났다. 기관(Organ) 분석에 의거한 해부학적 건강도 지수(HAI) 분석에 따르면, 피부손상(Skin)은 상류에서, 신장 손상(Kidney)은 하류 역에서 나타났고, 간(Liver)과 아가미(Gill)의 손상은 모든 지점에서 나타나 해부학적 측면의 건강도에서도 영향을 받는 것으로 나타났다.

• 한국조경학회지
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• 제30권6호
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• pp.17-25
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• 2003

The physical components of a river, such as water surface width/river width ratio, water level, and flow velocity vary according to different flowrates. Moreover, the riverside landscapes are greatly affected by the change of physical components of the stream or river. This paper provides an analysis of the influence of changing physical components of a river on the riverside landscape using a survey-based quantification method. The questionnaire was developed based on current literature, and was submitted to 326 people who each visited a representative station along the riverside.This survey was implemented three times at each representative station during periods of different flowrates. The results of this analysis and survey have Produced an understanding of the relationship between the variation of physical components and riverside landscapes. Survey results about the flow comparison are summarized as follows. Viewing riverside landscapes, most respondents are sensitive to the change of the flow velocity and prefer high water levels to low water levels. As a whole, respondents prefer abundant stream flows and moderate flow velocity in which they can perceive the flow of water. The minimum instream flows for riverside landscapes is estimated at each representative station by using a survey-based quantification method, and the estimated results of some representative stations were greater than the mean monthly flow at each station. The result of this analysis shows that establishing minimum instream flows for riverside landscapes is not only a technical problem, but also a legal problem. Therefore, in the to establish the instream flows in a river, the estimated results have to be considered as a relative standard. Regarding the survey results, respondents' satisfaction level didn't show any clear inclination according to the variation of various hydraulic properties. In determining the minimum instream flow using such an inquiry method, the structure of riverside scenery may vary according to the change of seasons or months. Therefore, to determine a consistent general inclination about the flow rate, it is necessary to have more detailed flow rates for each season or month combined with more inquiries.

• 한국수자원학회논문집
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• 제56권spc1호
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• pp.1037-1048
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• 2023

하천에 설치된 댐, 보 등과 같은 횡단구조물은 수생태계에 영향을 미치며 종적 연결성을 단절하기 때문에 어류의 이동을 확보하기 위하여 어도가 설치된다. 그러나 어도 내부의 흐름 특성 및 어종에 따라 어류의 통과효율의 차이가 발생한다. 본 연구에서는 3차원 RANS 모형과 자유수면 해석을 위한 VOF (volume of fluid)기법을 적용한 수치모형을 활용하여 계단식 어도에서 발생하는 난류흐름을 수치모의 하였다. 계단식 어도의 pool의 길이 변화 및 상류 수위 변동을 고려하였으며 이들의 변화에 따라 평균유속 및 난류운동에너지 분포를 분석하였다. 표면류 및 잠입류 특성을 잘 재현하였으며 pool의 길이가 증가하면서 표면류에서 잠입류로 변화하였고 상류 수위가 증가함에 따라 표면류 특성이 명확하게 나타났다. 어도 내 어류의 이동과 관련된 수리학적 인자는 유속 및 난류운동에너지 등이 있으며 이를 바탕으로 어류의 소상 가능성을 검토하였다.

• 대한지리학회지
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• 제44권4호
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• pp.429-446
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• 2009

본 연구는 일본 시가현(자하현(滋賀懸)) 기류(동생(桐生))수문시험지의 1차곡 소유역인 마쯔자와 유역에서 유역 내 수문과정과 토양수, 지하수, 계류수의 수질 등의 관측을 실시, 산림유역 내 황(黃) 플럭스를 수문지형학적 관점에서 해석하여 온대 산림유역 내의 황 순환 과정을 밝히고자 실시하였다. 유역 상부 교란 구역의 토양은 ${SO_4}^{2-}$의 공급원으로 작용하고 있었으며, 사면 수문과정을 통해 유역 중부와 하부의 심층토양 및 지하수대에 ${SO_4}^{2-}$가 저장되고 있었다. 계류수의 ${SO_4}^{2-}$ 농도는 지하수위 변동과 음의 상관을 나타내고 있는 바, 이는 심층지하수에 저장된 ${SO_4}^{2-}$가 가뭄 등의 저수위시 혹은 평수위시에 유출되고 있음을 의미한다. 본 연구의 결과로부터 산림유역 내 각 수문과정이 ${SO_4}^{2-}$의 저장과 유출에 중요한 역할을 하고 있다는 것이 정량적으로 밝혀졌다.