• Title/Summary/Keyword: Micro-phytoplankton

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Modeling the effect of nutrient enrichment on the plankton population: Validation using mesocosm experiment data (영양염 증가에 따른 부유생태계 반응 모의: FVCOM을 이용한 중형폐쇄생태계(Mesocosm) 자료 재현)

  • Song, Yong-Sik;Choi, Hee-Seon J.;Yoo, Sang-Cheol;Hong, Hyeon-Pyo;Seo, Ji-Ho;Lee, Hyo-Jin;Kim, Tae-In;Woo, Seung-Buhm;Choi, Jung-Ki
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.23 no.5
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    • pp.358-368
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    • 2011
  • Responses of plankton populations to nutrient enrichment in mesocosm experiments in Shihwa lake were simulated using FVCOM. Dissoloved oxygen module was added to the FVCOM to simulate impacts of its decreased levels. The ecological model included the major components of the pelagic ecosystem including nutrients, phytoplankton (pico-, nano-, micro-), zooplankton (two groups of protozoa, mesozooplankton), particulate organic matter, dissolved organic matter and bacteria, and was calibrated using trophodynamic data collected from Gyeonggi Bay and Shihwa Lake. The model was able to reproduce major responses of plankton populations to nutrient enrichment, including phytoplankton of different size groups, change of dominance of protozoa from < 20 ${\mu}m$ oligotrichs to scuticociliates, and reponses to bacteria and low levels of dissolved oxygen in water column of the mesocosms.

Spatio-temporal Fluctuation of Phytoplankton Size Fractionation in the Uljin Marine Ranching Area (UMRA), East Sea of Korea (동해 울진 바다목장해역의 크기별 식물플랑크톤 생물량의 시·공간적 분포 특성)

  • Yoon, Yang Ho
    • Korean Journal of Environmental Biology
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    • v.34 no.3
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    • pp.151-160
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    • 2016
  • To understand size fractioned chlorophyll a and material cycles of coastal ecosystem in Uljin marine ranching area (JMRA) of East Sea, 4 times of survey were conducted from April to November 2008. Picoplankton, nanoplankton and netplankton in the surface of UMRA fluctuated with an annual mean of $0.26{\mu}g\;L^{-1}$ between the lowest value of $0.03{\mu}g\;L^{-1}$ and the highest value of $0.87{\mu}g\;L^{-1}$, annual mean $1.32{\mu}g\;L^{-1}$ between $0.11{\mu}g\;L^{-1}$ and $5.60{\mu}g\;L^{-1}$, annual mean $0.45{\mu}g\;L^{-1}$ between no detected (nd) and $4.68{\mu}g\;L^{-1}$, respectively. And the relative ratio of picoplankton, nanoplankton and netplanktons on the phytoplankton biomass was on annual average 12.9%, 65.0% and 22.1%, respectively. The 10 m layer was similar to the surface. The relative ratio of pico- and nano-plankton was higher throughout the year. That is, the material cycle of UMRA consists of a microbial food web rather than traditional food chain at a lower trophic levels. Primary production is deemed to have a higher possibility of being adjusted by top-down dynamics, such as micro-zooplankton grazing pressure rather than nutrients supply.

Seasonal Variation of Picoplankton Community in Lake Juam (주암호에서 미세조류의 계절적 군집 변화)

  • Cheong, Cheong-Jo
    • Journal of Korean Society of Environmental Engineers
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    • v.32 no.3
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    • pp.271-277
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    • 2010
  • The purpose of this study is to investigate the seasonal variation of picoplankton community in Lake Juam depending on the change of physico-chemical factors such as rainfall, water depth, DO and pH. The concentration of chlorophyll-a was most high as 18.03 mg/$m^3$ in July when the rainfall and water temperature were highest. The concentration was gradually decreased in October, April and that of January was decreased most low as 1.86 mg/$m^3$. The highest concentration of the Chl-a was shown at 2 and 5 m of water depth than surface, and the concentration was gradually decreased when the water depth becomes deep. Overall, microplankton was the highest rate as 33.9~54.2%, nanoplankton was 24.3~30.5% and picoplankton was 21.6~41.2%. Picoplankton was included as considerable concentration in the water of Juam lake. Therefore it is necessary to remove thoroughly the picoplankton in the water treatment processes such coagulation·sedimentation and sand filtration. The protoplasm released from destruction of picoplankton by chlorine has high possibility to cause regrowth of bacteria and pathogenic microorganism in the distribution system by playing the role of the assimilable organic carbon.