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박재충,박정원,김대현,신재기,이희무 한국육수학회 2005 생태와 환경 Vol.38 No.1
안동호를 5~10km 구간으로 분할한 5개 지점에 대하여 2002년 6월부터 2003년 6월(13개월)가지 총 21회에 걸쳐 지점별 물리 화학적 수질특성과 TSI, TSIm, LTSI로 수체의 영양상태 평가 및 평가방법간의 상관성을 비교 분석하였다. TSI와 TSIm은 평가항목(TP, Chl-α, SD)에 따라 지점별로 빈영양-중영양-부영양상태로 다양한 결과를 보여 개별 항목으로 수역의 영양상태를 평가하는 것은 곤란하였으나 댐 저수지의 상류에서 하류로 진행하면서 영양도가 낮아지는 결과는 세 평가방법이 동일하였다. 평가방법 간의 상관성은 수심이 깊고 연중 안정된 수질상태를 보이는 하류보다 수심이 얕고 수질변동 폭이 큰 상류수역에서 상대적으로 높았으며, 영양지수의 평균값에 의한 상관은 r=0.9117~0.9909 범위로 조사되어 상호 보완적인 적용은 가능한 것으로 나타났다. LTSI는 TSI와 TSIm에 비해 댐 저수지의 구간별 수질특성을 잘 반영하였으며 영양상태 평가의 간편성과 주관적인 평가 오류의 최소화에 보다 효과적이라 사료된다. Using TSI, TSIm and LTSI, we compared physico-chemical water quality and trophic state of 5 stations in Lake Andong from June 2002 to June 2003 and examined the correlation of them. It is difficult to evaluate trophic state of waters by each parameter, TP, Chl-α and SD, because TSI and TSIm in each section show different results, oligo-, meso- and eutrophic state. But three methods, TSI, TSIm and LTSI, show the same result that trophic degree lows as it goes to a lower area of the lake. The correlation among them is closer in the upper shallow waters than in the lower deep waters. The reciprocal application of trophic state indices is possible because the coefficient of mean correlation ranges 0.9117 to 0.9909. In conclusion, it seems that LTSI reflects a characteristic of water quality in each section better than TSI, TSIm and is very effective to simplify trophic state evaluation and minimize researcher's subjectivity.
박재충,박정원,김종달,신재기,Park, Jae-Chung,Park, Jung-Won,Kim, Jong-Dal,Shin, Jae-Ki 한국조류학회(藻類) 2005 ALGAE Vol.20 No.4
Spatial and temporal variations of environmental factors and phytoplankton community were investigated in the three stations of Andong Reservoir in 1997 and 2003. The changes of physico-chemical water quality and phytoplanktonic biomass were higher in 2003 than that of 1997, due to rainfall difference. The concentration of total nitrogen (TN) and total phosphorus (TP) in the reservoir decreased, but total nitrogen fell relatively more between them. TN/TP ratio decreased from 109 to 90 showing no change at the downstream but a big decrease at the midand upstream. Predominant phylum of phytoplankton in Andong Reservoir were six genus that composed to Anabaena, Aphanizomenon and Microcystis of Cyanophyceae, Cosmarium and Scenedesmus of Chlorophyceae and Synedra of Bacillariophyceae, respectively. Among the observed phytoplankton, diatom Synedra occured as the maximum amount of 3,400 cells mL$^{-1}$ even at the above 30°C. Green algae Scenedesmus observed along with Microcystis. It seemed to be compete with Microcystis during the high water temperature period. Although trophic state of Andong Reservoir was decreased, the standing crops of phytoplankton were increased. Moreover bluegreen algae, Aphanizomenon and Microcystis in the region of upstream to midstream and diatom, Synedra in the region of midstream to downstream were increased until to reach the algal bloom, respectively. It seemed necessary to attention the changes of blue-green algae Aphanizomenon, that has an ability of nitrogen fixation.
인공호에서 몬순과 태풍 강우에 의한 고탁수층의 이동과 소멸특성
박재충,박정원,신재기,이희무 한국육수학회 2005 생태와 환경 Vol.38 No.1
낙동강 수계의 최대 인공호인 안동댐 저수지에서 2002~2004년 동안 홍수기의 수온성층 구조에 따른 고탁수의 유입특성과 시·공간적 변동을 조사하였다. 6월부터 수온성층이 형성되었으며 성층구조에 따라 유입 수괴의 이동경로가 결정되었고 고탁수의 유입에 의해 성층 구조가 변하였다. 고탁수는 유입 시기와 수량에 관계없이 저수지 상류부에서는 심층류로 유입되었고 중류부에서 바닥으로부터 분리되어 중층 밀도류의 형태로 하류까지 이동하였다 또한 중층 밀도류의 형성지점은 유입량과 시기에 따라 공간적으로 다소 차이가 있었다. 유입량에 의해 수온성층과 BO분포가 변하였고, 시기에 따라 변수층에는 2개의 수온 급감층과 저산소층이 각각 존재하였다. 최하류까지 이동한 홍수량의 고탁수층은 상승류를 형성하여 수심 15 m 아래에서 최대 20m 두께로 고탁수층을 형성하였다. 고탁수층은 저수지 바닥으로 침전되지 않았고 중층의 취수구를 통해 하류로 배출되었으며 가을 순환시기 이후 완전 소멸되었다. During the period of heavy rain from 2002 to 2004, the characteristics of the inflow, temporal and spatial fluctuations of high turbid water according to thermal stratification were studied on the Andong Reservoir which is the largest artificial lake in the Nakdong River basin, Korea. Thermal stratification was formed in June. Its structure determined to the pathway of inflowing turbid water and has affected by the transportation of high turbid water. Regardless of the time and amount of inflow, the high turbid water showed the shape of underflow at the riverine zone, separated from the bottom at the transition zone and moved to the lacustrine zone with the shape of density current. The plunging point depended on the time and amount of inflow. The distributions of thermal stratification and DO concentrations were changed by inflowing discharge. Two thermoclines and minimum DO layers were found out existing at metalimnion in a specific time, respectively. The layer of high turbid water which formed with the thickness of 20 m at the maximum below the depth of 15 m moved toward dam. Not settled to the bottom, the newly formed layer was discharged through the intake-outlet and dispersed into all layers by the circulation in the fall.
국내 6개 다목적댐 저수지의 담수 전,후 수질 비교평가
박재충 ( Jae Chung Park ),신재기 ( Jae Ki Shin ),송영일 ( Young Il Song ),정용문 ( Yong Moon Jeong ),송상진 ( Sang Jin Song ) 한국환경영향평가학회 2011 환경영향평가 Vol.20 No.1
This study was carried out to assess the variations of water quality caused by the dam construction on the river. Six dams-Yongdam, Miryang, Hoengseong, Boryeong, Jangheung and Buan-constructed recently in Korea were selected for the study. Chemical oxygen demand(COD) was increased in the initial stage of water storage at dams compared to the lotic(river) environment, but after 3 years it was maintained lower and stabilized concentrations. Five dams except for Jangheung Dam were maintained Ia~Ib grade conditions under the water quality criteria of Korea. The concentrations of total nitrogen(T-N) were decreased under the lentic(reservoir) environment compared to the river status. Total phosphorus(T-P) was decreased 13~63% at the reservoir condition. We concluded that increase of COD concentration was due to the debris organic materials of the land, but temporary phenomenon. T-N and T-P concentrations were decreased at the lentic condition compared to the lotic.