• 한국방재학회 논문집
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• 제8권1호
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• pp.117-123
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• 2008

본 연구에서는 하천의 유지유량을 결정함에 있어서 어류의 서식처를 고려한 최적의 유량을 산정하기 위하여 한강수계의 주요지천에 1차원 물리서식처 모의 모형인 PHABSIM과 2차원 물리서식처 모의 모형인 River2D를 적용하였다. 또한 대상어종의 성장단계별(성어기 산란기) 두 모형의 가중가용면적(WUA)에 대하여 비교검토하였으며 어류서식조건을 고려한 최적유량 값을 산정하였다. 모의결과 1차원 모형과 2차원 모형에서 가중가용면적(WUA)의 상관분석 결과 $0.87{\sim}0.99$로 분석되었고 어류서식조건을 고려한 최적유량 역시 문막 지점의 성어기와 달천지점의 산란기를 제외하고 $3m^3/s{\sim}5m^3/s$의 차이로 큰 차이를 보이지 않았다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2008년도 학술발표회 논문집
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• pp.395-399
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• 2008

하천은 물을 활용하기 위한 이수기능과 홍수방어를 위한 치수기능, 그리고 자연생태계를 유지하기 위한 환경기능 등 크게 3대 기능으로 나뉜다. 그러나 이러한 기능을 수행하기 위해서 물이 흐르지 않는다면 불가능 하다. 따라서 이러한 기능을 충분히 수행하기 위해서는 얼마나 많은 물이 흘러야 하는 가에 대하여 조사 분석을 통하여 하천유지유량이라는 것을 제안하고 이를 법으로 고시하고 있다. 이러한 하천유지유량은 각 나라의 기후나 지형학적 특성 때문에 나라별로 다양한 방법을 적용하고 있으며 또한 지형학적, 생태학적, 신미적인 기능 등 각자의 필요하고 중요하게 생각하는 인자들을 기준으로한 유량 계산의 틀을 제안하고 있다. 우리나라에서도 최근 하천법 개정에 따라서 하천유지유량의 개념을 재 정립하고 그 유량을 산정방안 및 지침 등에 대하여 제안하였다. 그러나 이렇게 방안에 의해 제안되는 유량의 경우 근본적으로 상류로부터 흐러 내려오지 않는다면 아무리 좋은 방법에 의해 산정되고 고시되는 하천유지유량은 무용지물이 된다. 따라서, 본 연구에서는 하천유지유량을 충분히 흘려보내 줄 수 있는지를 분석한 하천유지가능유하량의 개념을 제안하고 산정방법을 제안하고자 한다.

• 한국관개배수논문집
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• 제18권1호
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• pp.68-80
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• 2011

To provide a operation rule curve for reservoir with low ratio of watershed area to paddy field area, Duckyong reservoir with watershed area of $15.8km^2$ and paddy field area of 1,071ha was selected, in which 4 meters are being heightened and full water levels will be increased from EL.26.0m to EL.30.0m, total water storages from 365.6M $m^3$ to 708.0M $m^3$. There was no operation rule curve that satisfied over 90% reliability of water supply in reservoir with watershed area of 1.48 times of paddy field area. The differences between observed and simulated reservoir daily water storages were minimized to determine parameters for simulating reservoir inflow in case of paddy field area of 550ha from 1991 to 2010. A operation rule curve was drawn to have a maximum storage with total water storage, which was in paddy field area of 700ha with ratio of 2.3 between watershed area and paddy field area. This case showed that annual irrigation water supply was 668M $m^3$ and instream flow of 57M $m^3$, water supply reliability of 55.6% in normal operation, and annual irrigation water supply was 605M $m^3$ and instream flow of 38M $m^3$, water supply reliability of 95.6% in withdrawal limited operation. Water supply reliabilities showed 35.6% without flood regulation and 17.8% with flood regulation in existing reservoir before heightening.

• 농업과학연구
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• 제37권2호
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• pp.285-293
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• 2010

To secure instream flow at the Yudeung urban stream reach of Daejeon city in South Korea, Yudeung upstream diversion was designed with total water storage of $59{\times}10^4m^3$, and the upstream Seongol reservoir was planned to raise the bank with various sizes. Downstream streamflows were simulated by considering outflows from upstream diversion and reservoir, and after then flow durations were analyzed and compared with flows of no reservoir condition. In case of no diversion or reservoir upstream, flow durations were $1^{st}$ flow of $84.72m^3/s$, $95^{th}$ flow of $2.10m^3/s$, $185^{th}$ flow of $0.92m^3/s$, $275^{th}$ flow of $0.42m^3/s$, and $355^{th}$ flow of $0.31m^3/s$. In case of upstream diversion, flow durations were $1^{st}$ flow of $94.38m^3/s$, $95^{th}$ flow of $2.96m^3/s$, $185^{th}$ flow of $1.22m^3/s$, $275^{th}$ flow of $0.50m^3/s$, and $355^{th}$ flow of $0.35m^3/s$. The increase flow rates were $0.04m^3/s$ in $355^{th}$ flow, $0.08m^3/s$ in $275^{th}$, and $0.30m^3/s$ in 185th. In case of Seongol reservoir with effective storage capacities of $365{\times}10^4m^3$, $544{\times}10^4m^3$, $750{\times}10^4m^3$, and $992{\times}10^4m^3$, flow durations were $85.5{\sim}83.9m^3/s$ on $1^{st}$ flow, $2.85{\sim}2.57m^3/s$ on $95^{th}$ flow, $1.16{\sim}1.27m^3/s$ on $185^{th}$ flow, $0.64{\sim}0.99m^3/s$ on $275^{th}$ flow, and $0.56{\sim}0.94m^3/s$ on $355^{th}$ flow. The increase flow rates were $0.25{\sim}0.63m^3/s$ in $355^{th}$ flow, $0.22{\sim}0.57m^3/s$ in $275^{th}$, and $0.24{\sim}0.35m^3/s$ in $185^{th}$. The more the sizes of upstream reservoirs increased, the $1^{st}$ and $95^{th}$ flows decreased in which coefficients of determination were 0.92, 0.99, respectively and the $185^{th}$, $275^{th}$, and $355^{th}$ flows increased in which coefficients of determination were 0.93 to 0.99.

• 한국환경과학회지
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• 제16권8호
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• pp.973-983
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• 2007

The eco-hydrologic effects of maintenance water supply on Oncheon stream are studied using hydrologic, hydraulic and ecologic models. SWMM (Storm Water Management Model) is used for long-term simulation of runoff quantity and water quality from Oncheon stream watershed. Using the output hydrologic variables from SWMM, HEC-RAS (River Analysis System) is then used to simulate the hydraulics of water flow through Oncheon stream channels. Such hydrologic, hydraulic and water quality output variables from SWMM and HEC-RAS are served as input data to execute PHABSIM (Physical Habitat Simulation) for the purpose of predicting the micro-habitat conditions in rivers as a function of stream flow and the relative suitability of those conditions to aquatic life. It is observed from the PHABSIM results that the weighted usable area for target fishes has the maximum value at $2m^3/s$ of instream flow. However, mid and down stream areas that have concrete river bed and covered region are unsuitable for fish habitat regardless of instream flow increment. The simulation results indicate that the simple maintenance water supply is limited in its effect to improve the ecological environment in Oncheon stream. Therefore, it is imperative to improve water quality and to recover habitat conditions simultaneously.

• 생태와환경
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• 제46권1호
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• pp.10-17
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• 2013

History of Instream Flow Incremental Methodology (IFIM) Following the large reservoir and water development era of the mid-twentieth century in North America, resource agencies became concerned over the loss of many miles of riverine fish and wildlife resources in the arid western United States. Consequently, several western states began issuing rules for protecting existing stream resources from future depletions caused by accelerated water development. Many assessment methods appeared during the 1960's and early 1970's. These techniques were based on hydrologic analysis of the water supply and hydraulic considerations of critical stream channel segments, coupled with empirical observations of habitat quality and an understanding of riverine fish ecology. Following enactment of the National Environmental Policy Act (NEPA) of 1970, attention was shifted from minimum flows to the evaluation of alternative designs and operations of federally funded water projects. Methods capable of quantifying the effect of incremental changes in stream flow to evaluate a series of possible alternative development schemes were needed. This need led to the development of habitat versus discharge functions developed from life stage-specific relations for selected species, that is, fish passage, spawning, and rearing habitat versus flow for trout or salmon. During the late 1970's and early 1980's, an era of small hydropower development began. Hundreds of proposed hydropower sites in the Pacific Northwest and New England regions of the United States came under intensive examination by state and federal fishery management interests. During this transition period from evaluating large federal reservoirs to evaluating license applications for small hydropower, the Instream Flow Incremental Methodology (IFIM) was developed under the guidance of the U.S. Fish and Wildlife Service (USFWS).

• 토지주택연구
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• 제2권3호
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• pp.299-305
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• 2011

하천과 강은 지구상에서 가장 현란하고 복잡한 생태계를 가지고 있는 지구상의 생태 중 하나이다. 최근, 전국적으로 생태하천에 대한 관심이 높아져가고 있는 현실에서 각 지역마다 생태하천 구성을 위한 계획들이 수립되어 시행되고 있다. 생태하천 조성을 위해서는 수질과 연계한 생태하천의 유지용수 확보가 가장 큰 문제임에도 불구하고 너무 많은 변수들로 최적의 의사결정을 도출하기가 쉽지 않다. 본 연구에서는 의사결정자가 주민인식조사와 연계하여 생태하천조성을 위한 의사결정을 지원할 수 있도록 시스템을 개발하였다. 의사결정지원시스템은 수리 수질 생태하천 모의모형과 최적의 생태하천유량 산정방안과 수질개선방안을 제시할 수 있도록 구성하였다.

• 한국관개배수논문집
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• 제17권2호
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• pp.57-70
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• 2010

This study was performed to analyze the affect of water supply capacity followed by allocating flood control volume in heightening reservoir, of which Baekgog reservoir was selected as a case study in here. Baekgog reservoir is located in Jincheon county, Chungbuk province, of which full water level will be heightened from EL. 100. 1m to EL. 102.1m, and total storage from 21.75M $m^3$ to 26.67M $m^3$. Flood inflow with 200year frequency was estimated to 997 $m^3$/s in peak flow and 22.54M $m^3$ in total volume. Reservoir flood routing was conducted to determine flood limited water levels, which was determined to have scenarios such as EL 97-98-99m in periods of 6.21.-7.20., 7.21.-8.20., and 8.21.-9.20., respectively, EL 97-97-97m, EL 98-98-98m in present reservoir, and EL 99-100-101m, EL 99-99-99m, and EL 100-100-100m in heightened reservoir. Reservoir inflow was simulated by DAWAST model. Annual paddy irrigation requirement was estimated to 33.19M $m^3$ to 2,975ha. Instream flow was allocated to 0.14mm/d from October to April. Operation rule curve was drawn using inflow, irrigation and instream flow requirements data. In case of withdrawal limit reservoir operation using operation rule curve, reduction rates of annual irrigation supply before and after flood control by reservoir were 2.0~4.3% in present size and 1.5~3.6% in heightened size. Reliability on water supply was decreased from 77.3% to 63.6~68.2% in present size and from 81.6% to 72.7~79.5% in heightened size. And reduction rates of water storage at the end of year before and after flood control by reservoir were 7.3~16.5% in present size and 7.7~16.9% in heightened size. But water supplies were done without any water deficiency through withdrawal limit reservoir operation in spite of low flood regulating water level.

• 한국수자원학회논문집
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• 제38권9호
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• pp.771-778
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• 2005

금번 연구에서는 금호강의 금호 수위관측소 지점에서 영천댐 건설에 따른 유황분석을 하였다. 분석 결과, 영천댐 건설 전에는 갈수랑 $10.49\;m^3/s$, 저수량 $13.30\;m^3/s$, 평수랑 $15.65\;m^3/s$, 풍수량 $25.00\;m^3/s$ 이었으나, 건설 후에는 갈수량이 $2.07\;m^3/s$, 저수랑 $2.89\;m^3/s$, 평수량 $4.0\;m^3/s$, 풍수량 $9.36\;m^3/s$ 으로 유황이 상당히 열악해 진 것으로 분석되었다. 유지유량 증분법의 물리적 서식처모의 모형을 적용하여 피라미의 성장단계별 가중된 가용면적-유량 관계곡선을 작성하였다. 이 관계곡선으로 유지 가능일 수를 초과확률로 가중된 가용면적의 서식처 현황곡선을 작성하고, 영천댐건설에 따른 하천의 유황변화가 어류 서식환경에 미치는 영향을 평가하였다. 평가결과, 산란기와 성어기 모두 영천댐건설에 따라 가중된 가용면적이 감소하여 어류 서식환경이 저하되었다. 그러나 산란기중 유량의 초과확률 $90\;\%$ 이상에서는 영천댐에서 하류지역의 관개용수를 공급함으로써 유황이 개선되고 가중된 가용면적도 증가하여 어류서식환경이 개선된 것으로 평가되었다.

• 한국수자원학회논문집
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• 제38권7호
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• pp.545-554
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• 2005

금번 연구는 낙동강 유역의 영강, 위천, 회천, 거창위천, 청도천, 단장천에서 산란기와 성어기에 어류의 서식과 수심, 유속, 하상재료 등 수리학적 특성에 관한 자연과학과 공학의 학제간 상호 연계조사를 시행하였으며, 어종별(피라미와 갈겨니), 성장단계별(산란기와 성어기), 서식처조건별(수심, 유속과 하상재료) 어류 서식 적합도 기준을 작성하였다. 유지유량 증분법 개념의 물리적 서식처 모의시스템을 적용하여, 낙동강 유역의 주요 하천에서 어류서식에 적합한 유량을 산정하고, 그 중 가장 큰 유량값을 생태학적 추천유량으로 결정하였다. 금번 결정한 생태학적 추천유량은 내성천 $6.5\;m^3/s$ 등 $5.0\;m^3/s{\sim}10.0\;m^3/s$ 이었다. 또한 생태학적 추천유량과 기존에 산정된 생태계 필요유량 및 유황분석 결과를 비교${\cdot}$검토 하였다.