• Animal cells and systems
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• 제16권1호
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• pp.69-76
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• 2012

This study was conducted to examine how a low-head dam removal (partial removal) could affect benthic macroinvertebrate communities in a stream. Benthic macroinvertebrates and substrates were seasonally sampled before and after dam removal (March 2006-April 2007). Benthic macroinvertebrates and substrates were quantitatively sampled from immediately upstream (upper: pool) and downstream (lower: riffle) sites, the location of the dam itself (middle), and immediately above the impoundment (control: riffle). After the removal, species richness and density of benthic macroinvertebrates as well as the EPT group (Ephemeroptera, Plecoptera and Trichoptera) increased to higher levels than those before the removal, while functional feeding groups and habitat orientation groups changed more heterogeneously at the upper site. At the lower site, species richness and density decreased somewhat immediately after dam removal, which was associated with an increase of silt and sand, but recovered after monsoon floods which helped to enhance substrate diversity at the upper site. Decreased dominance index and increased diversity index in both the upper and lower sites are evidence of positive effects from the dam removal. In conclusion, we suggest that even a partial removal of a dam, resulting in increased substrate diversity in the upper site, could sufficiently help rehabilitate lost ecological integrity of streams without major habitat changes.

• 한국수자원학회논문집
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• 제57권4호
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• pp.301-310
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• 2024

강수의 공간적·시간적 불균형이 물관리를 어렵게 하고 있다. 기후변화로 인해 강수의 불균형이 심화되고, 가뭄과 홍수가 빈번하게 발생하고 있다. 또한 가뭄과 홍수의 강도가 심화되어 기존의 물관리 시스템을 어렵게 만들고 있다. 2022년 6월부터 2023년 6월까지 영섬유역의 주요 수자원시설 저수율이 대부분 30% 이하였으며 유역 내 가장 용수 의존도가 높은 주암댐의 경우에 역대 최저 저수율인 20.3%까지 하락하였고 평림댐은 2023년 5월 4일 최저 저수율 27.3%를 기록하였다. 평림댐은 2022년 봄부터 강수량 부족으로 2022년 6월 19일 가뭄 관심 단계가 발령되었고 연이어 7월 2일 가뭄 주의 단계, 8월 21일 가뭄 심각 단계에 진입하였다. 수양제와 연계 운영이 가능한 평림댐은 관리기관이 다르다. 그럼에도 불구하고 가뭄 상황에서 유기적 연계 운영을 통해 평림댐에서 저수위에 도달하지 않고 3개군 급수인구 63,000명에게 안정적으로 용수를 공급할 수 있었다. 한정된 수자원 활용을 극대화할 수 있도록 유역간, 수원간 물이동을 원활하게 이동 가능 방안을 검토하여 수요자 중심의 물공급 시스템을 갖추어 기후변화로 인한 물부족 상황에 대비해야 한다.

• 신재생에너지
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• 제20권1호
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• pp.116-125
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• 2024

Ultra-low-head is an unexplored classification among the sites in which hydroelectric power can be produced. This is typically owing to the low power output and the economic value of the turbines available in this segment. A turbine capable of operating in an ultra-low-head condition without the need of a dam to produce electricity is developed in this study. A gate structure installed at a shallow water channel acting as a weir generates artificial head for the turbine mounted on the gate to produce power. The turbine and generator are designed to be compact and submersible for an efficient and silent operation. The gate angle is adjustable to operate the turbine at varying flow rates. The turbine is designed and tested using computational fluid dynamics tools prior to manufacturing and experimental studies. A parametric study of the runner blade parameters is conducted to obtain the most efficient blade design with minimal hydraulic losses. These parameters include the runner stagger and runner leading edge flow angles. The selected runner design showed improved hydraulic characteristics of the turbine to operate in an ultra-low-head site with minimal losses.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2019년도 학술발표회
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• pp.159-159
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• 2019

In this study, the simulation of sediment deposition at Sangju weir reservoir, South Korea, was carried out using artificial neural networks. The ANNs have typically been used in water resources engineering problems for their robustness and high degree of accuracy. Three basic variables namely turbid water inflow, outflow, and water stage have been used as input variables. It was found that ANNs were able to establish valid relationship between input variables and target variable of sedimentation. The R value was 0.9806, 0.9091, and 0.8758 for training, validation, and testing phase respectively. Comparative analysis was also performed to find optimum structure of ANN for sediment deposition prediction. 3-14-1 network architecture using BR algorithm outperformed all other combinations. It was concluded that ANN possess mapping capabilities for complex, non-linear phenomenon of reservoir sedimentation.

• 지질공학
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• 제28권2호
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• pp.277-295
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• 2018

10년 전부터 댐 건설에 대한 사회적 비판이 제기됨에 따라 댐 공사를 통해 새로운 수자원을 확보하기가 어려워졌기 때문에 기존 댐에 대한 검토가 필요하게 되었다. 이에 따라, 계획, 시공 및 관리 등의 접근 방식은 댐 보수 및 보강과 관련하여 이미 확보된 기술을 활용하여 실시되었다. 이러한 보수와 보강의 결과로, 다수의 댐에서 침투 그라우팅이 수행되었으나, 현재까지 기술의 정립이 미흡한 실정이고, 국내외적으로 발표된 논문도 극히 드문 편이다. 본 논문에서는 YC댐에 대한 저압 침투그라우팅 보강 기술을 상세하게 분석하였다. 결과적으로 침투그라우팅은 YC댐과 같이 코어형 필댐의 차수성 개선에 효과적으로 적용될 수 있음을 확인하였다. 그리고, 주입기준과 관련하여 경험적으로 증명된 침투그라우팅의 기술적 상세들을 제시하였다. 본 연구를 통한 필댐 침투그라우팅 기술의 구체적인 분석자료들은 향후 필댐 및 저수지 보수보강에 있어 유용한 자료로 활용 가능할 것으로 판단된다.

• 한국농공학회지
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• 제38권4호
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• pp.125-136
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• 1996

In order to investigate the characteristics of gravity drainage for geotextile, small-scale model tests for the geotextile chimney drain of earth dam which is a typical type of gravity drainage were carried out using 15 kinds of nonwoven and composite geotextiles. According to the results of this study, the drainage discharge of geotexgile drain generally increases with exponential function as hydraulic head increases and the increasing rate is greater in the coarser soil of dam material. It has a trend to increase when the construction slope of geotextile drain is steeper and the number of layers of geotextile is more. The relationship between the transmissivity of geotextile and the drainage discharge has positive correlation and the rate of increase is greater in the coarser soil. The geotextile products must be carefully selected in consideration of transmissivity of geotextile when the soil to be drained is coarser and the seepage flow is relatively high. Most of staple fiber nonwoven geotextile used in this study are found to be appropriate for drainage purpose. Among them, the composite geotextile the type of which geotextile is evaluated to be the most excellent material. But the geotextile of low permeability such as filament thermal bonded and filament spunbonded nowovens closely examined their transmissivity especially to be used for drainage function.

• 동의생리병리학회지
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• 제20권5호
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• pp.1089-1101
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• 2006

Following conclusions are drawn from study about Yukmigiwhangwon through referring to literatures and reviewing in the point of Hyungsang medicine. Yukmigiwhangwon was prescribed by Jeon Eul in order to cure five kinds of flaccidity of infants, but after since then it has been basically applied to symptoms which was caused by deficiency of the kidney not only infants but also adult. The deficiency of kidney is the lack of vital essence and body fluid stored in kidney, it happens because infants are born in the conditions of lack of receiving in the womb. And it happens because adults infringe the rules of life, especially the sexual life. Main symptoms of the poverty of renal functions are emptiness of the brain marrow, dizziness, forgetfulness, tinnitus, deafness, vertigo and dim eyesight, insomnia, the low back and knees aching and limping, heat on the legs, tibia aching, nocturnal emission, dry mouth, reddened tongue and little coating or non coating of the 'tongue, weak blood meridians. the treating method is nourishing Eum and supplementing kidney. In Dongeuibogam Yukmigiwhangwon is mentioned in the parts of vital essence, blood, voice, kidney, urine, eye, ear, the low back, hair, fire, exhaustion syndrome, cough, polydipsia, infant, etc. The shapes which Yukmigiwhangwon is applied to are the Dam Body Doing deficiency of Eum due to excess of Yang, man, infant, Jung type, Fish group, reverse triangular shape, big headed man, big eared man, big mouthed man, man having prominent cheekbones, man having long waist, man having big hips, man with thick hair or white hair, man with bald on the head, etc. In color it is applied to darkish complexion, flushed tip of the nose, or flushed cheek bones. Through inquiring into the clinical cases on the points of Hyungsang medicine Yukmigiwhangwon is efficacious cure to lumbago, symptoms of tendons and bones, symptoms of eyes and ears, symptoms of respiratory organs, dermatopathia, headache, polydipsia, urinary disorders, etc.

• 한국농공학회지
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• 제7권1호
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• pp.861-876
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• 1965

During my stay in the Netherlands, I have studied the following, primarily in relation to the Mokpo Yong-san project which had been studied by the NEDECO for a feasibility report. 1. Unit hydrograph at Naju There are many ways to make unit hydrograph, but I want explain here to make unit hydrograph from the- actual run of curve at Naju. A discharge curve made from one rain storm depends on rainfall intensity per houre After finriing hydrograph every two hours, we will get two-hour unit hydrograph to devide each ordinate of the two-hour hydrograph by the rainfall intensity. I have used one storm from June 24 to June 26, 1963, recording a rainfall intensity of average 9. 4 mm per hour for 12 hours. If several rain gage stations had already been established in the catchment area. above Naju prior to this storm, I could have gathered accurate data on rainfall intensity throughout the catchment area. As it was, I used I the automatic rain gage record of the Mokpo I moteorological station to determine the rainfall lntensity. In order. to develop the unit ~Ydrograph at Naju, I subtracted the basic flow from the total runoff flow. I also tried to keed the difference between the calculated discharge amount and the measured discharge less than 1O~ The discharge period. of an unit graph depends on the length of the catchment area. 2. Determination of sluice dimension Acoording to principles of design presently used in our country, a one-day storm with a frequency of 20 years must be discharged in 8 hours. These design criteria are not adequate, and several dams have washed out in the past years. The design of the spillway and sluice dimensions must be based on the maximun peak discharge flowing into the reservoir to avoid crop and structure damages. The total flow into the reservoir is the summation of flow described by the Mokpo hydrograph, the basic flow from all the catchment areas and the rainfall on the reservoir area. To calculate the amount of water discharged through the sluiceCper half hour), the average head during that interval must be known. This can be calculated from the known water level outside the sluiceCdetermined by the tide) and from an estimated water level inside the reservoir at the end of each time interval. The total amount of water discharged through the sluice can be calculated from this average head, the time interval and the cross-sectional area of' the sluice. From the inflow into the .reservoir and the outflow through the sluice gates I calculated the change in the volume of water stored in the reservoir at half-hour intervals. From the stored volume of water and the known storage capacity of the reservoir, I was able to calculate the water level in the reservoir. The Calculated water level in the reservoir must be the same as the estimated water level. Mean stand tide will be adequate to use for determining the sluice dimension because spring tide is worse case and neap tide is best condition for the I result of the calculatio 3. Tidal computation for determination of the closure curve. During the construction of a dam, whether by building up of a succession of horizontael layers or by building in from both sides, the velocity of the water flowinii through the closing gapwill increase, because of the gradual decrease in the cross sectional area of the gap. 1 calculated the . velocities in the closing gap during flood and ebb for the first mentioned method of construction until the cross-sectional area has been reduced to about 25% of the original area, the change in tidal movement within the reservoir being negligible. Up to that point, the increase of the velocity is more or less hyperbolic. During the closing of the last 25 % of the gap, less water can flow out of the reservoir. This causes a rise of the mean water level of the reservoir. The difference in hydraulic head is then no longer negligible and must be taken into account. When, during the course of construction. the submerged weir become a free weir the critical flow occurs. The critical flow is that point, during either ebb or flood, at which the velocity reaches a maximum. When the dam is raised further. the velocity decreases because of the decrease\ulcorner in the height of the water above the weir. The calculation of the currents and velocities for a stage in the closure of the final gap is done in the following manner; Using an average tide with a neglible daily quantity, I estimated the water level on the pustream side of. the dam (inner water level). I determined the current through the gap for each hour by multiplying the storage area by the increment of the rise in water level. The velocity at a given moment can be determined from the calcalated current in m3/sec, and the cross-sectional area at that moment. At the same time from the difference between inner water level and tidal level (outer water level) the velocity can be calculated with the formula $h= \frac{V^2}{2g}$ and must be equal to the velocity detertnined from the current. If there is a difference in velocity, a new estimate of the inner water level must be made and entire procedure should be repeated. When the higher water level is equal to or more than 2/3 times the difference between the lower water level and the crest of the dam, we speak of a "free weir." The flow over the weir is then dependent upon the higher water level and not on the difference between high and low water levels. When the weir is "submerged", that is, the higher water level is less than 2/3 times the difference between the lower water and the crest of the dam, the difference between the high and low levels being decisive. The free weir normally occurs first during ebb, and is due to. the fact that mean level in the estuary is higher than the mean level of . the tide in building dams with barges the maximum velocity in the closing gap may not be more than 3m/sec. As the maximum velocities are higher than this limit we must use other construction methods in closing the gap. This can be done by dump-cars from each side or by using a cable way.e or by using a cable way.

• 한국농공학회논문집
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• 제60권2호
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• pp.103-110
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• 2018

Most of the intake facilities of small agricultural reservoirs are conduits and they are regarded as serious defects due to the structural weakness that penetrates the body of the dam, and countermeasures are needed. This study suggests the application method of siphon type water intake facility by hydraulic model test and physical scale model test of siphon type water intake facility which has high safety and easy maintenance. Experimental results show that sufficient flow rate can be secured for the purpose of intaking water according to the differential head between the reservoir and the discharge part, and the flow rate can be controlled by the valve. The negative pressure was -31.5 kPa, and vibration and noise did not occur during the operation of the siphon. The maximum flow velocity in the discharge outlet was 1.11 m/s which meets the criterion for irrigation canals. Therefore, scour risk would be very low. As a result of the inflow distribution experiment, even if the inflow part is separated by only about 0.8 m, the flow velocity is remarkably decreased, so that the clogging by debris would not appear. When the pump was operated only once for the first time and the inside of the siphon was filled with water, continuous operation was possible by only valve operation. The results of this study are expected to be used for the design guidelines of the water intake facilities and improve safety and maintenance convenience of agricultural reservoirs.

• 한국작물학회지
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• 제34권s02호
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• pp.45-65
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• 1989

우리나라는 지형과 기후가 복잡다양한 데다가 하절기에는 필리핀 남양군도로부터 상습적으로 불어오는 태풍의 진로권내에 위치해 있고 년간 강우량의 대부분이 벼 재배기인 하절기에 집중적으로 내리는 관계로 이때 강우와 강풍이 단독 또는 동반하여 갖가지 풍수해양상을 일으킨다. 풍해는 조풍해, 건조풍해 및 강풍해로 구분하여 볼 때 조풍해(염풍해)는 1986년 8월 28~29일 태품 Vera호 내습시 남부 해안지방 일대에서는 강우가 그치면서 염분을 함유한 초속 6m정도의 강풍이 불어 해안으로부터 2.5km까지 도체 조기에 염분을 건물당 1.1~17.2mg 부착시켜 심한 조풍해를 일으켰다. 그리고 건조풍해는 '87년 이래로 내습한 대부분의 태풍들이 4.0~8.5m의 태풍이 남부 및 동해안에 불어 Foenhn 현상으로 건조풍이 되고 이때 출수기에 처한 벼 이삭은 심한 백수피해와 변색위피해를 받았다. 태풍해로서는 풀수기 이전의 벼 생육단계에서 경엽이 기계적으로 절상, 파열, 고사되고, 등숙기에는 도복과 탈입이 심하게 된다. 풍해경감은 태품 내습을 회피하도록 8월 15일까지 출수시키고 풍해저항성이 비교적 강한 상풍벼와 청청벼 재배가 효과적이다. 한편 수해로서는 농경지 유시, 이몰, 침관수 및 도복 등을 들 수 있으나 각종 Dam, 제방축조, 하구언공사 등으로 피해는 많이 줄었지만 국지적 집중호우나 강변유역 제방내의 내수로 인한 침관수나 도복피해는 상습적으로 일어난다. 핌관수해는 태풍과 다우가 주로 8월 말경에 내습하여 2~4일 정도 도체가 관수된다. 이따 남부 특수만식답의 벼생육단계는 생육초중기에 해당되므로 어린 생육단게일수록 피해가 크고 보통식세어는 생식생장기에 해당되므로 유수나 팬이삭은 불념이 되더라도 죽은 이삭을 갖는 경의 상위절로부터 재생경이 나와 정상이삭으로 되어 수량 감소가 가장 튼 감수분열기 피해에서도 66%의 수량보상력을 갖게 된다. 침관수피해 경감을 위해서는 사전적 조처로서 관수저항성 및 백엽고, 벼멸구, 도복저항성을 갖는 품종을 선택 재배하는 것이 효과적이다. 특히 통일형 품종은 일본형 품종에 비하여 관수시 모든 생육단게에서 관수저항성이 강한데 묘생존율이 높고, 엽신과 엽초의 이상신장력이 낮아 퇴수시 기술적 장해가 적으며 생식생장기에는 근활력, 광합성능력이 높아 피해회복이 빠르고 고위절분얼이삭에 의한 수량보상력이 높다. 이상을 종합하여 볼 때 풍수해를 최소화하기 위해서는 다음과 같은 연구가 금후 이루어져야 할 것이다. \circled1 기상예보, 풍수해 피해실태 및 그로 인한 작황 등의 원격탐사 및 전산화에 의한 분석 연구가 이루어져야 하고, \circled2 품수해와 관련된 불량환경에서 내성을 갖는 품종 육성 보급이 이루어져야 하고, \circled3 품수해 발생상습지에서는 벼 피해를 보상할 수 있는 타작물과의 함리적 작부체계 개선 연구가 이루어져야 하고, \circled4 피해도체의 활용도 증진 연구가 이루어져야 할 것이다.