• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2006년도 총회 및 춘계학술발표회
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• pp.277-281
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• 2006

A study on stream-groundwater exchange was performed using head and temperature data of stream water, streambed, and groundwater. Groundwater level and temperature were obtained from multi-depth monitoring wells in small-scale watershed. In the summer time, time series of temperatrue data at streambed and groundwater were monitored for three months. In the winter time, we measured the temperature gradient between stream water and streambed. The observed data showed three typical types of temperature characteristics. First, the temperature of streambed was lower than that of stream water; second, the temperature of streambed and stream water was similar; and last, the temperature of streambed was higher than that of stream water. The interconnections between the stream and the streambed were not homogeneously distributed due to weakly developed sediments and heterogeneous bedrock exposed as bed of the stream. The temperature data may be used in formal solutions of the inverse problems to estimate groundwater flow and hydraulic conductivity.

• 한국지구과학회지
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• 제26권8호
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• pp.821-827
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• 2005

섬진강의 상류인 요천은 남원을 관통하며 흐른다. 요천의 수온은 상류에서 하류로 갈수록 높아지는 경향을 나타냈다. DO, 인, 총질소, 전기전도도, 총용존고형물은 정점 8에서 크게 상승하였다. 그러나 수소이온농도와 용존산소는 급져히 떨어졌다. 정점 8은 남원시의 중앙부를 지나는 작은 개천과 합류하는 지점이며, 주변에 남원위생사업소가 있다. 정점 8 이하의 하류에서, 갈수기인 4월과 6월의 COD양은 호소수질기준 3급수에 해당한다. 이러한 수질오염은 남원시에서 배출되는 생활하수 등으로 유입된 COD, 총인, 총질소가 원인일 것으로 추정된다. 별다른 오염원이 없는 정점 2와 3에서 높은 함량의 COD와 총질소는 농업활동에 의해 발생했을 가능성이 있다.

• 한국측량학회지
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• 제20권3호
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• pp.255-264
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• 2002

지형은 강우시 유역의 유출반응을 결정하는 중요한 인자이다. 유역분석에서 하천망은 중요한 지형 매개변수이다. DEM격자 크기와 배수누적 행렬의 흐름누적 임계값은 격자 DEM를 이용하여 추출된 하천망에 영향을 미친다. 따라서 DEM에 의해서 추출된 하천망의 배수 밀도는 선택된 DEM 격자크기와 흐름누적 임계값에 따라 다양하다. 일반적으로 작은 흐름누적 임계값은 높은 배수밀도를 가지는 아주 세부적인 하천망을 만들어 내고, 큰 임계값은 조잡한 하천망을 만들어 낸다. 이 연구에서는 연구대상지역에서 총 하천길이가 각각의 DEM 격자크기에 대해 흐름누적 임계값을 계산하는데 이용되었다. 하천망은 흐름누적 임계값을 적용하여 각각의 DEM 격자크기에 대해 추출되었으며, 흐름누적 임계값과 각각의 DEM 격자크기에 연관성이 회귀방정식으로 도출되었다.

• 한국농공학회:학술대회논문집
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• 한국농공학회 1998년도 학술발표회 발표논문집
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• pp.547-551
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• 1998

Reaeration coefficient is the physical absorption of oxygen from the atmosphere by water. It is the most important natural means by which a stream replaces the oxygen consumed in the biodegradation of organic wastes, and the rate constant describing this process is the reaeration coefficient, It. Reaeration coefficient is the dominant parameter affecting the use of water quality model. Therefore accurate estimation of the reaeration coefficient is essential for optimum water quality management. There is several method to estimate stream reaeration coefficient. In this study, it would be concluded that SI-peak method is of practical use when applied to small stream, and CRI method is adequate to large stream.

• Journal of Mechanical Science and Technology
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• 제17권1호
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• pp.122-128
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• 2003

This paper presents a thermodynamic analysis of heat pump system using water as a heat source and heat sink. The primary object in this study is the optimization of exergetic efficiency. Two different systems, 2-stream and 1-stream system, are analyzed in detail. Mass flow ratio (the ratio of mass flow rate of water through evaporator to that through condenser) is identified as the most important parameter to be optimized. It is shown that there exists an optimum mass flow ratio to maximize exergetic efficiency. The variation of optimum exergetic efficiency of 2-stream system is quite small and the value lies between 0.2∼0.23 for the range of investigation in this study. However, far better performance can be obtained from 1-stream system. This means considerable irreversibilities are generated through condenser of the 2-stream system. The effects of adiabatic efficiency of compressor-motor unit on the overall system performance are also examined in the analysis.

• 한국농공학회:학술대회논문집
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• 한국농공학회 2005년도 학술발표논문집
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• pp.330-335
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• 2005

This study was performed for the analysis of the variation characteristics on riverbed according to the arrangement of stream. It was monitored of the variation progress of riverbed dependent on the elapsed time after the arrangement and It was studied that the hydraulic adjustment of the riverbed caused by the variation of the riverbed. The large amount of deposit just after the construction in which the riverbed was arranged to natural form was come from the reduction of flow rate by the installed artificialities such as weirs and stone weirs and by the stones or the concrete blocks attached to the stream sides of riverbanks. This phenomenon was well consistent with the usual characteristics that the accumulation is induced on upper stream of hydraulic artificialities and the erosion is induced on down stream of hydraulic artificialities. The large reduction of the deposit 1 year later after the construction showed that the riverbed eroded considerably because of the recovery of flow amount and the rise of flow rate.

• 한국농공학회:학술대회논문집
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• 한국농공학회 2000년도 학술발표회 발표논문집
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• pp.570-577
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• 2000

In this study, using modified tracer method(Constant Rate Injection, CRI method), reaeration rates were measured in the territories of Bokha stream. In case of Kwanri stream, reaeration rates of a diversion were measured simultaneously. Propane gas and Rhodamine-WT were used as gas and dye tracer, respectively. The experimental results show that reaeration rates of the stream were ranged from 6.16 to 24.52 1/day and those of a diversion in Kwanri stream were ranged from 28.39 to 123.61 1/day. It is resulted that mean velocity of stream is a dominant factor in reaeration process and diversion significantly influence on reareation process.

• 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.

• 대한원격탐사학회지
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• 제40권1호
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• pp.9-18
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• 2024

Small streams, despite their rich ecosystems, face challenges in vegetation assessment due to the limitations of traditional, time-consuming methods. This study presents a groundbreaking approach, combining unmanned aerial vehicles(UAVs), convolutional neural networks(CNNs), and the vegetation differential vegetation index (VDVI), to revolutionize both assessment and management of stream vegetation. Focusing on Idong Stream in South Korea (2.7 km long, 2.34 km² basin area)with eight diverse revetment methods, we leveraged high-resolution RGB images captured by UAVs across five dates (July-December). These images trained a ResNeXt101 CNN model, achieving an impressive 89% accuracy in classifying vegetation cover(soil,water, and vegetation). This enabled detailed spatial and temporal analysis of vegetation distribution. Further, VDVI calculations on classified vegetation areas allowed assessment of vegetation vitality. Our key findings showcase the power of this approach:(a) TheCNN model generated highly accurate cover maps, facilitating precise monitoring of vegetation changes overtime and space. (b) August displayed the highest average VDVI(0.24), indicating peak vegetation growth crucial for stabilizing streambanks and resisting flow. (c) Different revetment methods impacted vegetation vitality. Fieldstone sections exhibited initial high vitality followed by decline due to leaf browning. Block-type sections and the control group showed a gradual decline after peak growth. Interestingly, the "H environment block" exhibited minimal change, suggesting potential benefits for specific ecological functions.(d) Despite initial differences, all sections converged in vegetation distribution trends after 15 years due to the influence of surrounding vegetation. This study demonstrates the immense potential of UAV-based remote sensing and CNNs for revolutionizing small-stream vegetation assessment and management. By providing high-resolution, temporally detailed data, this approach offers distinct advantages over traditional methods, ultimately benefiting both the environment and surrounding communities through informed decision-making for improved stream health and ecological conservation.

• 한국해양학회지:바다
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• 제22권1호
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• pp.1-17
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• 2017

본 연구는 소하천 하구의 영양염 분포를 조절하는 요인에 대해 알아보기 위하여 수행되었다. 남해안 당항포에 위치한 세 하천(닫힌 하구: 고성천, 열린 하구: 구만천, 마암천)에서 2010-12년까지 계절별로 영양염(질산염, 암모늄, 인산염) 농도를 측정하였다. 고성천의 댐은 담수의 희석을 막고 체류시간을 증가시켜 높은 영양염 농도의 원인이 되어 인위적인 요인이 소하천 하구의 영양염 분포에 중요함을 나타내었다. 그 외에 물리, 기후, 생지화학적 요인이 세 하천 영양염 분포에 영향을 주었다. 세 하천 모두에서 질산염은 상류에서 높고 하류로 갈수록 감소하였다. 이것은 상류 집수역에서 공급이 많고, 하류로 갈수록 희석 및 하구 내 생지화학적 과정에 의한 제거가 활발하기 때문으로 여겨진다. 특히 탈질소화 등 대표적인 생지화학적 질소영양염 제거과정은 상류에서 하류로 갈수록 감소하는 경향이 뚜렷하였다. 그러나 암모늄과 인산염은 하천에서 유입되는 농도가 높은 경우에만 상류에서 하류로 갈수록 농도가 낮아지는 경향이 뚜렷하게 나타났다. 영양염 농도의 계절 분포는 여름철에 낮고, 겨울철에 높은 경향을 보였다. 여름철 유량으로 인해 체류시간이 감소하였고, 희석 증가로 하천 내 영양염 농도를 감소시켰으며, 높은 수온으로 인한 생물 생산에 의한 영양염 제거 역시 낮은 영양염 농도에 영향을 주었다. 소하천 하구는 높은 질소제거율(-k) 을 가지는 등 대형하구와는 구별되는 영양염 거동을 보이며 향후 소하천 하구 관리를 위해서는 이러한 특성을 파악하는 것이 필수적이다.