Journal of Life Science (생명과학회지)

Korean Society of Life Science (한국생명과학회)
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Effect of Turbid Water on the Phytoplankton Community in Imha Reservoir

탁수가 임하호 식물플랑크톤에 미치는 영향

  • Park, Jung-Won (National Park Research Institute) ;
  • Yu, Sam-Hwan (Department of Biological Science, Andong National University) ;
  • Kim, Soon-Young (Department of Biological Science, Andong National University) ;
  • Lee, Jong-Eun (Department of Biological Science, Andong National University) ;
  • Seo, Eul-Won (Department of Biological Science, Andong National University)
  • 박정원 (국립공원연구원) ;
  • 유삼환 (안동대학교 자연과학대학 생명과학과) ;
  • 김순영 (안동대학교 자연과학대학 생명과학과) ;
  • 이종은 (안동대학교 자연과학대학 생명과학과) ;
  • 서을원 (안동대학교 자연과학대학 생명과학과)
  • Published : 2008.12.30
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Abstract

We investigated the effect of the turbid water on the phytoplankton community in the 4 sites of Imha reservoir. The turbidity of water was proportional to the concentrations of $SiO_2$-Si. Therefore, as the turbidity of water grow, the concentration of $SiO_2$-Si increased. And the both the turbidity of water and the concentrations of $SiO_2$-Si were increased as the water run deep. The concentration of chlorophyll-a decreased as the depth of water increased. Seventy phytoplankton taxa were identified and the most abundant group was Chlorophyceae consisting of 32 taxa (46%), and Cyanophyceae and Bacillariophyceae consisted of 12 taxa (17%). And Euglenophyceae, Synulophyceae, Cryptophyceae and Dinophyceae consisted of 6 taxa (9%), 4 taxa (6%), 3 taxa (4%) and 1 taxon (1%), respectively in Imha reservoir. The concentrations of phytoplankton were increased according to the turbidity of water because of the high amount of organic nutrition which is presented with turbid water. And especially, the concentrations of nitrogen increased easily because of the weak binding to the soil particle. In conclusion, total nitrogen and $SiO_2$-Si flowed into the Imha reservoir with soil particle, and these inorganic nutritions affect the growth of algae.

본 연구에서는 탁수 발생이 식물플랑크톤 군집에 어떠한 변화를 미치는가에 대해 이해하는 연구의 일환으로 임하호의 네 지점(중평리, 댐축, 도수로, 지례리)에서 9회에 걸쳐 시료 채취 및 조사를 한 결과는 다음과 같다. 임하호의 수질의 경우 탁도와 $SiO_2$-Si의 농도는 그 수치가 비례하여 탁도가 높으면 $SiO_2$-Si의 농도도 증가하고 수심이 깊어질수록 탁도와 $SiO_2$-Si의 농도가 증가하는 것을 알 수 있다. Chl-a는 수심이 깊어질수록 농도가 낮아지고 있어 수심에 따라 수질의 상태가 변하는 것으로 조사되었다. 임하호에서 출현한 식물플랑크톤은 모두 70종류였고, 녹조강이 32종류(46%) 남조강과 규조강이 12종류(17%), 유글레나강이 6종류(9%), 시누라조강이 4종류(6%), 은편모조강이 3종류(4%), 그리고 와편모조강이 1종류(1%)로 구성되었다. 탁수와 조류의 상관관계에서 식물플랑크톤의 현존량이 매우 높게 나타난 것은 탁수와 함께 유입된 영양물질등이 식물플랑크톤의 증가에 영향을 준 것으로 판단된다. 즉, 탁수와 TN 및 $SiO_2$-Si 등과 높은 상관관계가 나타난 것은 TN과 $SiO_2$-Si가 탁수와 함께 임하댐 내로 유입된 것으로 짐작할 수 있다. 질소의 경우 토양 미립자에 단단하게 부착하지 않고 느슨하게 결합되어 있기 때문에 적은 강우라도 쉽게 유출된다. 그리고 $SiO_2$-Si는 탁수의 성분으로 고려해 볼 때 TN과 $SiO_2$-Si는 탁수와 함께 임하댐내로 유입되었음을 알 수 있다. 따라서 탁수 유입 후 그리고 탁수 소멸 이후에는 오히려 식물플랑크톤 현존량이 더욱 증가된 것으로 판단된다.

Keywords

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