Tidal variations of Nutrient Concentration in Hampyeong Bay, West coast of Korea

서해 함평만에서 조위변화에 따른 영양염 변동

  • 강미란 (한국해양연구원 남해특성연구부) ;
  • 임동일 (한국해양연구원 남해특성연구부) ;
  • 장풍국 (한국해양연구원 남해특성연구부) ;
  • 김기범 (경상대학교 해양과학대학 해양환경공학과) ;
  • 강영실 (국립수산과학원 해양환경연구본부)
  • Received : 2009.07.06
  • Accepted : 2009.08.07
  • Published : 2009.08.25

Abstract

In order to understand the circulation of nutrient between muddy tidal flat and the surrounding coastal area, tidal time-scale variations in nutrient concentrations were seasonally investigated at the entrance of Hampyeong Bay. The results show that the temperature was higher in ebb tide and lower in flood tide during the summer, but it was lower in ebb tide and higher in flood tide during the autumn/winter. The salinity was higher in flood tide and lower in ebb tide during the summer/winter because of the inflow of external sea water resulting from the increase in the tide level. By contrast, the salinity was lower in flood tide and higher in ebb tide during the autumn. Salinity difference was lower than 0.3 psu between flood tide and ebb tide during survey period. Meanwhile, all nutrient concentrations observed in Hampyeong Bay was lower in flood tide and higher in ebb tide during the summer, and by contrast, it was higher in flood tide and lower in ebb tide during the winter. Characteristically, no clear variation of concentrations was found depending on the tide level during the autumn. This tidal variations imply that the muddy tidal flat of Hampyeong Bay supplies nutrients to the seawater in summer and removes nutrient from the seawater in winter. During tidal cycle, seasonal variation of nutrient concentration in seawater is considered as the result of complex interactions between the mud flat and external sea water.

갯벌과 주변 연안역 사이의 물질순환, 특히 영양염 순환에 있어서의 갯벌의 역할을 이해하기 위해 서해 남부 해역의 대표적 갯벌인 함평만 입구에서 4차례(2008년 8월 5일과 18일, 2008년 10월 28일, 2009년 2월 9일)에 걸쳐 조위변화에 따른 영양염 변동을 조사하였다. 연구 결과에 의하면 수온은 조위변화에 따라 여름철 간조시 높고 만조시 낮은 반면, 가을과 겨울철은 간조시 낮고 만조시 높아 여름과 대조적인 경향을 보인다. 염분은 조위가 상승함에 따라 외해수가 유입되어 여름/겨울철에 만조시 높고, 간조시 낮은 일반적인 경향을 보이는 반면, 가을철에는 만조시 낮고 간조시 높은 반대의 경향을 보인다. 모든 계절에서 만조와 간조시 염분의 차는 0.3 psu미만이였다. 한편 함평만에서 관측된 모든 영양염은 조위변화에 따라 여름철 만조시 낮고 간조시 높은 반면, 겨울철은 만조시 높고 간조시 낮아 여름철과 반대의 패턴을 보인다. 특징적으로 가을철은 조위변화에 따른 뚜렷한 농도변동을 보이지 않았다. 이러한 결과는 함평만 갯벌이 여름철에는 영양염의 공급원으로 겨울철에는 영양염의 제거원으로 작용하고 있음을 보여준다. 이와 같은 영양염 계절별 조위변동은 외해수와 갯벌에서의 영양염 농도 차이를 반영하는 것으로 갯벌과 외해수 사이의 상호 복합적인 요인에 의해 나타나는 것으로 사료된다.

Keywords

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