• 제목/요약/키워드: water-bloom

검색결과 441건 처리시간 0.031초

Influence of Rainfall on Cyanobacterial Bloom in Daechung Reservoir

  • 안치용;김희식;윤병대;오희목
    • 생태와환경
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    • 제36권4호통권105호
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    • pp.413-419
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    • 2003
  • 1999년과 2001턴, 여름부터 가을까지 대청호의 남조류 수화현상에 대한 강우영향을 조사하였다. 두 해의 6,7월 강수량은 매우 유사하였으나, 수화발생 시기인 8,9월의 강수량은 현저한 차이를 보였다. 1999년에는 8월 하순 이후 그전 2개월에 비해 약 70%의 강수량 증가가 있었으나, 2001년에는 같은 기간 동안 5분의 1수준으로 감소하였다. 더 높은 엽록소-a, 파이코시아닌, 남조류 농도가 2001년 측정되었으며, 이것은 극심한 수화의 발생으로 이어졌다. 또한 2001년에는 조사기간동안 남조류의 비율이 항상 80%를 상회하였으며, 남조류는 Microcystis spp.가 대부분을 차지하였다. 이와는 반대로 1999년에는 수화의 발생이 보고되지 않았다. 이러한 차이에도 불구하고 수화가 절정을 이루는 시기는 두 해 모두 8월 하순에서 9월 초순으로, 강수량에 관계없이 일정하였다. 수화 이전 시기의 적당한 강수와 이후의 충분한 일조 시기가 남조류의 수화 형성에 영향을 끼치는 중요인자들 중의 하나로 판단되었다.

Assessment of the Marine Environment in Masan-Jinhae Bay of Korea in Relation to Algal Blooms

  • 이문옥
    • 한국해양공학회지
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    • 제22권5호
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    • pp.7-24
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    • 2008
  • Masan-Jinhae Bay, in Korea, is known for its frequent algal bloom outbreaks. This study was conducted in order to examine the environmental characteristics of the area, with the aim of identifying indicators that could be used to speculate about future algal blooms. The water temperatures and salinities in Haengam Bay, one of the small inner bays within Jinhae, appeared to re relatively higher than those in Masan and Jinhae bays, across most seasons. Furthermore, stratification begins to develop in all three regions from spring to summer as a result of the local heating effects and an increase in the efficient from the surrounding land. As a result, anoxic conditions appear near the bottom layer of the bay, leading to the deterioration of water quality, which has been identified as one of the causes of bloom outbreaks. Compared to Haengam and Jinhae bays, concentrations of DIN and DIP were remarkably higher in Masan Bay. However, the mean ratio of DIN to DIP was 3.3$\sim$13.6 in all three regions throughout the year, suggesting that nitrogen can function as a growth-limiting factor for phytoplankton. The results of mathematical models showed that cumulative organic pollutants may be a trigger for direct algal bloom occurrences, since residual tidal currents appeared to be less than $3\;cm\;\cdot\;s^{-1}$. Furthermore, computed DO concentrations in the four small inner bays of Jinhae during the summer appeared to be $3\;cm\;\cdot\;l^{-1}$ indicating a hypoxic state. Likewise, computed Chl-a concentrations turned out to be more than $0.01\;mg\;\cdot\;l^{-1}$, indicating eutrophication across most seasons. Based on the overall results, Masan-Jinhae Bay appeared to possess a very high potential for algal bloom outbreaks at anytime during the year.

은이온 수용액의 Microcystis 생장 억제 효과 (Effect of Silver Ion Solution on the Inhibition of Microcystis Growth)

  • 최강국;이상훈;배기서;신재기;오희목
    • 환경생물
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    • 제26권3호
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    • pp.183-191
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    • 2008
  • The effect of silver ion solution on the growth of Microcystis aeruginosa UTEX 2388 (cyanobacterium) and Chlorella sp. KCTC AG20136 (green alga) was investigated using separated and mixed culture in filtered natural water and BG11 medium. In separated culture, M. aeruginosa UTEX 2388 and Chlorella sp. KCTC AG20136 were found to be sensitive to 0.01 and 0.1 mg L$^{-1}$ of silver ion, respectively. Also, the silver ion concentrations for the growth inhibition of M. aeruginosa UTEX 2388 and Chlorella sp. KCTC AG20136 in the mixed culture were same in separated culture. Cyanobacteria were more sensitive to the silver ion solution than green algae. In bloom sample, the minimal inhibition concentration of silver ion solution for the low Chl-${\alpha}$ sample (110$\sim$190 ${\mu}g$ L$^{-1}$) and high Chl-${\alpha}$ sample (1,500$\sim$1,900 ${\mu}g$ L$^{-1}$) was about 0.1 and 3.0 mg L$^{-1}$, respectively. The silver ion concentration for the inhibition of algal bloom sample was affected by the algal biomass. In order to use silver ion solution for the control of algal bloom, the silver ion concentration must be determined in consideration of a minimal effect on the environment.

담수수계에서 남조류 증식억제의 기술적, 전략적 접근 (Technical and Strategic Approach for the Control of Cyanobacterial Bloom in Fresh Waters)

  • 이창수;안치용;나현준;이상협;오희목
    • 환경생물
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    • 제31권4호
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    • pp.233-242
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    • 2013
  • Cyanobacteria (blue-green algae) are not only the first oxygenic organisms on earth but also the foremost primary producers in aquatic environment. Massive growth of cyanobacteria, in eutrophic waters, usually changes the water colour to green and is called as algal (cyanobacterial) bloom or green tide. Cyanobacterial blooms are a result of high levels of primary production by certain species such as Microcystis sp., Anabaena sp., Oscillatoria sp., Aphanizomenon sp. and Phormidium sp. These cyanobacterial species can produce hepatotoxins or neurotoxins as well as malodorous compounds like geosmin and 2-methylisoborneol (MIB). In order to solve the nationwide problem of hazardous cyanobacterial blooms in Korea, the following technically and strategically sound approaches need to be developed. 1) As a long-term strategy, reduction of the nutrients such as phosphorus and nitrogen in our water bodies to below permitted levels. 2) As a short term strategy, field application of combination of already established bloom remediation techniques. 3) Development of emerging convergence technologies based on information and communication technology (ICT), environmental technology (ET) and biotechnology (BT). 4) Finally, strengthening education and creating awareness among students, public and industry for effective reduction of pollution discharge. Considering their ecological roles, a complete elimination of cyanobacteria is not desirable. Hence a holistic approach mentioned above in combination to addressing the issue from a social perspective with cooperation from public, government, industry, academic and research institutions is more pragmatic and desirable management strategy.

영산강 다기능보 운영에 따른 플러싱 및 조류 배제 효과 모델링 (Modeling the Flushing Effect of Multi-purpose Weir Operation on Algae Removal in Yeongsan River)

  • 정선아;이혜숙;황현식;김호준
    • 대한환경공학회지
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    • 제37권10호
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    • pp.563-572
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    • 2015
  • 본 연구는 영산강 수계 승촌보에서 시행되었던 조류배제를 위한 다기능보 운영 사례를 대상으로, 3차원 모델링을 통한 효과 분석을 목적으로 수행되었다. 2013년 5월 영산강 승촌보 구간에서 녹조류 Eudorina sp.가 대량 발생하였으며, 집적된 녹조의 배제를 위하여 서로 다른 방법으로 두 차례에 걸쳐 플러싱 방류를 시행하였다. 조류 발생의 공간적 분포에 대한 상세분석과 이해를 위해 고해상도의 3차원 모형 ELCOM-CAEDYM을 적용하여 1개월 동안의 수질과 chl-a 분포를 모의하였다. 모델링 결과 ELCOM-CAEDYM 모형은 실제 조류의 발생 패턴을 우수하게 모의하였으며, 저비용으로 조류 발생에 대한 고해상도의 공간적인 데이터를 재생산 하는데 적합할 것으로 판단되었다. 모델링 결과를 이용하여 두 가지 방법의 플러싱 방류 CASE를 분석한 결과, 가동보를 이용하여 플러싱 방류를 실시한 CASE1의 경우 서창교~황룡강 합류지점에 발생하였던 조류는 가동보 운영에 의하여 빠르게 하류로 이동되었으나, 이후 방류량이 감소하면서 보 내에 잔류하였던 것으로 분석되었다. 반면, 소수력발전을 중단하고 고정보를 통한 월류를 실시한 CASE2는 비교적 배제 효과가 크게 나타나 대부분의 조류가 플러싱되어 감소된 것을 관측 자료와 모델링 결과로서 확인할 수 있었다.

대청호 수류차단막 설치 위치에 따른 녹조제어 효과 분석 (Analysis the Effects of Curtain Weir on the Control of Algal Bloom according to Installation Location in Daecheong Reservoir)

  • 이흥수;정세웅;정희영;민병환
    • 한국물환경학회지
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    • 제26권2호
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    • pp.231-242
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    • 2010
  • The objective of study was to determine an optimal location of a float-type curtain weir in Daecheong Reservoir and to assess its effectiveness for the control of algal blooms in the reservoir. CE-QUAL-W2, a laterally averaged two-dimensional hydrodynamic and eutrophication model, was modified to accommodate vertical displacement of the weir according to water surface fluctuation and applied to simulate the reservoir hydrodynamics and water quality changes for the reservoir. The model calibrated in a previous study was updated and validated for different hydrological conditions representing drought year (2008) and normal year (2006) for the study, and adequately simulated the temporal and spatial variations of water temperature, nutrients and algal (Chl-a) concentrations. The effectiveness of curtain weir on the control of algal bloom was evaluated by applying the validated model to 2001 and 2006 assuming 9 scenarios for different installation locations. The reduction rates of algal concentration were placed in the range of 11.2~40.3% and 20.3~56.7% for 2001 and 2006, respectively. Although, the performance of curtain weir was slightly varied for different locations and different hydrological years, overall, the performance was improved as the weir was installed further downstream.

NOAA 위성자료에 의한 해수표면 수온분포와 Cochlodinium polykrikoides 적조 발생의 상관성 (Relationship between Sea Surface Temperature derived from NOAA Satellites and Cochlodinium polykrikoides Red Tide occurrence in Korean Coastal Waters)

  • 서영상;김정희;김학균
    • 한국환경과학회지
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    • 제9권3호
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    • pp.215-221
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    • 2000
  • The relationship between the distribution of sea surface temperature(SST) and dinoflagellate(Cochlodinium polykrikoides) bloom areas were studied. The SST data were derived from the infrared channels of AVHRR(Advanced Very High Resolution Radiometer) sensor on NOAA(National Oceanic and Atmospheric Administration) 12 and 14 satellites during 1995-1998. The initial water temperature at C. polykrikoides bloom was about 21${\circ}C$ at the coastal areas of the South Sea and along the shore of the East Sea of Korea during the summer season of 1995. The northern limit of red tides was coincident with that of 21${\circ}C$ isothermal line in the East Sea. The red tides that initially bloomed at the coast of Pohang on September 21, 1995 moved to the coast of Uljin on September 26, 1995. The skipped appearance of the red tides in the areas between Pohang and Uljin was due to the East Korean Warm Current, which was moving offshore from Pohang to approach to Uljin. The cold water which was formed by tidal front in the western coast of the South Sea and by upwelling water from deep layer in the southeastern coast of the Korean peninsula played a role in blocking the spreading of red tides during summer season in 1997 and 1998. In conclusion, the distribution of red tides appeared to be dependent on the initial water temperature at red tides bloom. The SST at the red tides varied from 21${\circ}C$ to 25${\circ}C$; 21${\circ}C$, 23${\circ}C$, 24 and 24-25${\circ}C$ in 1995, 1996, 1997 and 1998, respectively.

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새만금 수역 식물플랑크톤 현존량의 경년(2001-2010) 변화 (Annual Variations(2001-2010) of Phytoplankton Standing Stocks in Saemangeum Water Region)

  • 여환구
    • 한국산학기술학회논문지
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    • 제13권9호
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    • pp.4326-4333
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    • 2012
  • 새만금 방조제 건설기간에 해당하는 2001년부터 2010년까지 10년간 새만금 수역에서 식물플랑크톤 현존량을 조사하였다. 식물플랑크톤 현존량은 조사 시기 및 조사 정점에 따라 57 - 85,219 cells/ml의 큰 변화를 보였다. 새만금호 내부 수역은 담수 및 해수의 유입량 변화와 계절변화에 기인하여 식물플랑크톤 현존량이 시공간적으로 변화하였다. 한편, 담수 정점들은 상시적으로 높은 현존량이 기록되어 녹조발생이 잦았으나 방조제 밖 해수역의 현존량은 보편적 범위에 있어왔다. 장기적 관점에서 방조제 물막이 공사 완공(2006년 4월)을 전후하여 비교할 때 식물플랑크톤 현존량의 큰 변화는 나타나지 않았다.

물리·화학적 방법을 이용한 Cyanobacteria와 식물 플랑크톤의 제어 (Control of Cyanobacteria and Phytoplankton Using Physico-chemical Methods)

  • 정원화;전은형;안태영
    • 한국환경복원기술학회지
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    • 제7권5호
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    • pp.75-84
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    • 2004
  • Loess, PAC, MACF and plants were applied to the control of the phytoplankton bloom in laboratory and in field, In field experiment using oil fence, 5ppm concentration of coagulant(PAC) was observed to be effective in controlling the cyanobacterial bloom, resulting in 90% removal of cyanobacteria and phytoplankton from the water column, hi case of Synedra sp., however, only 50% of biomass decreased with the same PAC concentration. MACF(micro-air bubble coagulation and floating), a kind of physicochemical method, was applied to the column of the Kyongan stream and resulted in over 80% chlorophyll a and 73.5% TP removal, Chlorophyll a and total phosphorus were effectively removed from water body when 2.0 g/L of loess with the particle radius of 125 ${\mu}m$ was inputted. In case of experiments involving plants, big cone pine, gingko, and pine needle were observed to be effective in restraining phytoplankton bloom at 0.5g/200ml level. During a field test done at Kyungan stream, where Microcystis heavily occurred, Pine needle and big cone pine were observed to be effective on suppressing algal growth.