• Journal of Korea Water Resources Association
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• v.30 no.6
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• pp.709-720
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• 1997

When flood control storage lacks for the reservoir operation of multipurpose dams during flood period, the additional flood control storage should be considered for the flexible use of limited storage capacity. Flood period is divided by meteorological characteristics in this study and the water levels for water demand and flood control are investigated for the divided flood period. Based on the investigations, we suggest the variable restricted water level(VRWL) from the considerations of water conservation and flood control which can determine dam operating water level during flood period. This paper presents an application of the methodology to determination of the VRWL during flood period at the Taechong Dam and the results are discussed.

• Water for future
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• v.28 no.6
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• pp.217-228
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• 1995

For optimal reservoir operation during flood period, a general and systematic policy is suggested to make balance of the conflicting purposes between water conservation and flood control. The purpose of this study is to decide the restricted water level of the reservoir during flood period specially to meet water demand in non-flood period. The optimal policy is derived by reallocation of storage capacity through the application of variable restricted water level(VRWL) and minimum required water level(MRWL) for shorter intervals. This study also suggests water level dconditions to secure conservation storage capacity at the end of the flood period estimated by reservoir operation study. This paper illustrates an application of the Daecheong Dam and Chungju Dam respectively during flood and the results are reviewed.

• KSCE Journal of Civil and Environmental Engineering Research
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• v.32 no.2B
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• pp.93-101
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• 2012

HEC-ResSim, reservoir operation model, is applied to Seomjin river dam in order to establish a rational method for water supply and flood control by dam operation. In order to minimize downstream flood damage for Seomjin river basin and adjacent regions, reservoir routing is applied to several frequency flood events within the framework of rainy seasonal operation rule and then the characteristics change of hydrological behavior for the downstream of study area is investigated in depth. Its quantitative efficiency and estimation method is evaluated on the basis of the adjustment scheme of conservation water surface elevation for flood control and water secure; reservoir routing considering preliminary release and variable restricted water level; and its effect to water supply; and downstream flood-duration analysis.

• Proceedings of the Korea Water Resources Association Conference
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• 2017.05a
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• pp.369-369
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• 2017

농업용저수지는 이수 목적으로 비홍수기 농업용수 공급을 위한 용수 확보를 주요 목적으로 하고 있다. 한편, 농업용저수지가 홍수조절능력 또한 지니고 있음이 다수의 연구를 통해 제기되고 있으며, 이에 치수 목적으로 홍수기 홍수피해 저감을 위한 치수 대책 또한 수립할 필요가 있다. 현재 우리나라 농업용저수지의 홍수기 운영은 제한수위 방식을 기준으로 하되 필요에 따라 예비방류를 허용하는 조합 형태를 취하고 있다. 이러한 운영 방식은 홍수기 이후 상시만수위로 복귀하지 못하면 해당 년도 잔여 비홍수기 혹은 다음 년도 영농 시작 시기의 농업용수 공급에 차질이 생길 수 있다는 문제점이 있다. 따라서 홍수기 농업용저수지의 운영은 홍수조절과 함께 상시만수 위로의 복귀를 동시에 고려하여 이루어질 필요가 있다. 가변 홍수기 제한수위 (Variable Restricted Water Level, VRWL) 방식은 홍수 발생빈도와 규모를 고려하여 단위기간별 (일별 혹은 순별) 제한수위를 차등 부여하는 방식으로, 한정된 저수공간의 효율적 재할당에 따라 이수와 치수의 효율을 증대시키는 방안이 될 수 있다. 따라서 본 연구에서는 농업용저수지를 대상으로 저수지 유입량 빈도해석을 수행하고 순별 가변 홍수기 제한수위를 산정한 후 가변 홍수기 제한수위 적용에 따른 홍수조절효과를 평가하고자 한다. 연구대상지는 전국 110개 둑높이기 농업용저수지 중 가능최대홍수량 대상저수지 (유역면적 2,500 ha 이상, 총 저수량 500만 톤 이상) 12개소로 선정하였고, 저수지별 기상자료와 지형자료를 구축하였다. 저수지 유입량 모의를 위하여 장기유출량 산정 모형인 TANK를 이용하였으며, 구축된 저수지 유입량 자료를 토대로 순별 유입량 빈도해석을 수행하고 홍수기 저수지 유입량의 이론적 확률분포형을 선정하였다. 선정된 확률분포형을 토대로 초과확률 10%에 따른 순별 저수지 수위로서 가변 홍수기 제한수위를 산정하였다. 산정된 가변홍수기 제한수위 적용 효과를 분석하기 위하여 홍수조절용량을 산정하였고, 유역비 홍수량을 지표로 하여 홍수조절능력을 평가하였다. 향후 본 연구의 결과는 둑높이기 농업용저수지의 홍수기 제한수위 설정 및 관리, 운영 지침 개선에 있어 기초자료로 활용할 수 있을 것으로 사료된다.

• Water for future
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• v.29 no.1
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• pp.235-248
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• 1996

Apreliminary release scheme (PRS) is suggested for the operating rules during flood period to deal with conflicts between flood control and water conservation purposes. PRS can be used to decide the optimum releases, based on the forecast of an oncoming flood and flow rate at the control point downstream when comparing the variable restricted water level (VRWL) for flood control with the minimum required water level (MRWL) for conservation use. The model is applied to Chungju and Daechung reservoirs through simulations of the technique. This study illustrates the procedure to decide the time and size for preliminary releases. Also, effects of duration and magnitude of preliminary release are reviewed based on historicqal flood records. The simulation results indicate that the proposed PRS is effective for the managers to find optimal operating policies during flood period. The proposed scheme can be used with main release scheme using real-time operation on hour-to-hour basis to decide the release for a flood.

• Smart Structures and Systems
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• v.23 no.6
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• pp.627-639
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• 2019

Passive control may not provide enough damping for a stay cable since the control devices are often restricted to a low location level. In order to enhance control performance of conventional passive dampers, a new type of damper integrated with a rotary electromagnetic damper providing variable damping force and a flywheel serving as an inertial mass, called the rotary electromagnetic inertial mass damper (REIMD), is presented for suppressing the cable vibrations in this paper. The mechanical model of the REIMD is theoretically derived according to generation mechanisms of the damping force and the inertial force, and further validated by performance tests. General dynamic characteristics of an idealized taut cable with a REIMD installed close to the cable end are theoretically investigated, and parametric analysis are then conducted to investigate the effects of inertial mass and damping coefficient on vibration control performance. Finally, vibration control tests on a scaled cable model with a REIMD are performed to further verify mitigation performance through the first two modal additional damping ratios of the cable. Both the theoretical and experimental results show that control performance of the cable with the REIMD are much better than those of conventional passive viscous dampers, which mainly attributes to the increment of the damper displacement due to the inertial mass induced negative stiffness effects of the REIMD. Moreover, it is concluded that both inertial mass and damping coefficient of an optimum REIMD will decrease with the increase of the mode order of the cable, and oversize inertial mass may lead to negative effect on the control performance.

• Economic and Environmental Geology
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• v.40 no.5
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• pp.517-535
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• 2007

Two distinctive Mesozoic hydrothermal systems occurred in South Korea: the Jurassic/Early Cretaceous(ca. $200{\sim}130$ Ma) deep-level ones during the Daebo orogeny and the Late Cretaceous/Tertiary(ca. $110{\sim}45$ Ma) shallow hydrothermal ones during the Bulgugsa event. The Mesozoic hydrothermal system and the metallic mineralization in the Korean Peninsula document a close spatial and temporal relationship with syn- to post-tectonic magmatism. The calculated ${\delta}^{18}O_{H2O}$ values of the ore-forming fluids from the Mesozoic metallic mineral deposits show limited range for the Jurassic ones but variable range for the Late Cretaceous ones. The orogenic mineral deposits were formed at relatively high temperatures and deep-crustal levels. The mineralizing fluids that were responsible for the formation of theses deposits are characterized by the reasonably homogeneous and similar ranges of ${\delta}^{18}O_{H2O}$ values. This implies that the ore-forming fluids were principally derived from spatially associated Jurassic granitoids and related pegmatite. On the contrary, the Late Cretaceous ferroalloy, base-metal and precious-metal deposits in the Taebaeksan, Okcheon and Gyeongsang basins occurred as vein, replacement, breccia-pipe, porphyry-style and skarn deposits. Diverse mineralization styles represent a spatial and temporal distinction between the proximal environment of subvolcanic activity and the distal to transitional condition derived from volcanic environments. The Cu(-Au) or Fe-Mo-W deposits are proximal to a magmatic source, whereas the polymetallic or the precious-metal deposits are more distal to transitional. On the basis of the overall ${\delta}^{18}O_{H2O}$ values of various ore deposits in these areas, it can be briefed that the ore fluids show very extensive oxygen isotope exchange with country rocks, though the ${\delta}D_{H2O}$ values are relatively homogeneous and similarly restricted.