Korean Journal of Fisheries and Aquatic Sciences (한국수산과학회지)

The Korean Society of Fisheries and Aquatic Science (한국수산과학회)
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A Preliminary Study comparing the Growth of Phytoplankton according to the Ratio of Deep and Surface Seawater

해양심층수와 표층수의 혼합비율에 따른 식물플랑크톤의 증식 변화에 대한 기초연구

  • Kim, Ah-Ree (Deep Ocean water Application Research center, Korea Ocean Research and Development institute) ;
  • Lee, Seung-Won (Deep Ocean water Application Research center, Korea Ocean Research and Development institute) ;
  • Jung, Dong-Ho (Deep Ocean water Application Research center, Korea Ocean Research and Development institute) ;
  • Moon, Deok-Soo (Deep Ocean water Application Research center, Korea Ocean Research and Development institute) ;
  • Kim, Hyeon-Ju (Deep Ocean water Application Research center, Korea Ocean Research and Development institute)
  • 김아리 (한국해양연구원 해양심층수연구센터) ;
  • 이승원 (한국해양연구원 해양심층수연구센터) ;
  • 정동호 (한국해양연구원 해양심층수연구센터) ;
  • 문덕수 (한국해양연구원 해양심층수연구센터) ;
  • 김현주 (한국해양연구원 해양심층수연구센터)
  • Received : 2010.05.12
  • Accepted : 2010.08.13
  • Published : 2010.08.31
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Abstract

The artificial upwelling of deep seawater increases primary production. This study conducted a lab-scale experiment to investigate the growth of phytoplankton with the mixing ratio of deep and surface seawater. The chlorophyll content in the sample of pure deep seawater was highest, regardless of the phytoplankton groups. Nutrients contained in the deep seawater positively influenced the growth of phytoplankton. The optimum mixture to apply in an artificial upwelling system was a 1:1 ratio of deep and surface seawater. An experiment considering other environmental conditions, such as luminance and specific gravity, should be performed.

Keywords

References

  1. Arrigo KR, Ditullio RB, Lizotte MP, Robbison DH, Van Woert M and Worthen DL. 2000. Phytoplankton taxonomic variablilty and nutrient untilization and primary production in the Ross sea. J Geophys Res 105, 8827-8846. https://doi.org/10.1029/1998JC000289
  2. de Baar HJW, de jong JTM, Bakker DCE, Loscher BM, Veth C, Bathmaann U and Smetacek V. 1995. Importance of iron for plankton blooms and carbon dioxide drawn in the Southern Ocean. Nature 373, 412-145. https://doi.org/10.1038/373412a0
  3. Cho KD, Kim DS and Park SE. 2003. Characteristics of oceanographic conditions in an area suitable for the construction of artificial upwelling. J Fish Soc 36, 187-192. https://doi.org/10.5657/kfas.2003.36.2.187
  4. Chung CS, Shim JH, Park YC and Park SG. 1989. Primary productivity and nitrogenous nutrient dynamics in the East sea of Korea. J Oceanological Soc Kor, 24, 52-61.
  5. David T, Susan SK and Peter K. 1982. Phytoplankton community ecology: The role of limiting nutrients. Ann Rev Ecol Syst 13, 349-372. https://doi.org/10.1146/annurev.es.13.110182.002025
  6. Doosan EnCyber, 2010. Upewlling. Retrieved from http://100.naver.com
  7. Guillard RL and Ryther JH. 1962. Studies for marine planktonic diatioms Cyclotella nana Hustedt and Detomnule conferracea (cleve). Gram Can J Microbiol 8, 229-239. https://doi.org/10.1139/m62-029
  8. Hecky RE and Kilham P. 1988. Nutrient limitation of phytoplankton in freshwater and marine environments: A review of recent evidence on the effects of enrichment. Limnol Oceanogr 33, 796-822. https://doi.org/10.4319/lo.1988.33.4_part_2.0796
  9. Hong NS, Kang SW and Kim JY. 2002. Investigation of efficiency of artificial upwelling device in East sea. J Kor Soc Coastal & Ocean Engineers 13, 270-273.
  10. Kim DS, Shim JH, Kim KT and Kang YC. 2004a. Distribution of total $CO_{2}$, Nutrients, Chlorophyll a in the Scotia Sea during austral summer. Ocean and Polar Res 26, 401-414. https://doi.org/10.4217/OPR.2004.26.3.401
  11. Kim DS, Kim KH, Shim JH and Yoo SJ. 2007. The effect if anticyclonic eddy on nutrients and chlorophyll during spring and summer in the Ulleung Basin, East Sea. J Kor Soc Oceanograpy, 12, 280-286.
  12. Kim HJ, Moon DS, Jung DH and Yoon SJ. 2004b. Investigation and analysis of the characteristic stablilty of deep ocean water (I). J Kor Soc Marine Environmental Engineering 7, 30-34.
  13. Kim KW. 2008. Cultivation of marine microalgae from east sea and production of bioactive compounds by them using deep seawater. MSc. thesis, National university of Kangnung, Gangwon, Korea.
  14. Lee JB, Han MS and Yang HS. 1998. The Ecosystem the southern coastal waters of the East sea, Korea - 1. Phytoplankton community structure and productivity in september, 1994. 1998. J Kor fish Soc 31, 45-55.
  15. Lee TK, Park MW, Snin KS and Jang M. 2000. Comperision on growth and biochemical composition of Gymnodium sangvineum and Skeletonema costatum grown in different N, P concentrations. Kor J Environ Biol 18, 395-401.
  16. Ministry of maritime affairs and fisheries. 2006. III. Marine organism. In: Marine environment official test method. Korea ocean research and development institute, Jungin I&D, Seoul, Korea, 265-278.
  17. Moon SG and Choi CM. 2003. A list of important species and distribution of marine phytoplankton in Korea. J of the Environmental Sciences 12, 725-733. https://doi.org/10.5322/JES.2003.12.7.725
  18. Nakashima, T. 2005. What is deep ocean water; The utility of deep ocean water. In: Kaiyoushinsousui no riyou. Kim HJ, ed. Shingisul Korea 53-67; 147-157.
  19. Nicholas W, Atsuki K, Shigenao M, Masud B and Steve WA. 2009. Nutrient transport from an artificial upwelling of deep sea water. J Oceanography 65, 349-359. https://doi.org/10.1007/s10872-009-0032-x
  20. Ryther JH. 1969. Photosynthesis and fish production in the sea. Science 166, 72-76. https://doi.org/10.1126/science.166.3901.72
  21. Sim JH and Park YC. 1986. Primary productivity measurement using carbon-14 and nitrogenous nutrient dynamics in the southeastern sea of Korea. J Oceanological Soc Kor 21, 13-24.

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