Distribution Of Phytoplankton Pigments In Yeongil Bay Water Of Korea, Late October

가을철 영일만해수중의 식물성플랭크톤 색소량과 그 분포

Chlorophyll concentrations of phytoplankton were determined by 5 meters interval from surface to bottom layers in Yeongil Bay water of Korea, late October 1973. The contents of phytoplankton chlorophyll decreased outward from the inner part to the entrance of the Bay. It seemed to be caused by incoming land waters which are rich in nutrients. And vertical distribution pattern of the chlorophyll showed three layer zones in the middle and outer parts, and two layers in the inner part of the Bay. These phenomena suggest that there are two different water masses, the one is bottom cold water originated from offshore, the other is surface warm water. And they are mixed together in the middle layer The correlationship between the contents of chlorophyll a and chlorophyll c represented perfect positive relation with coefficient of r 0.999 from the extracted data. In general, chlorophyll a percent-content of total chlorophyll varied in the range of 14.64∼19.83% (mean value; 18.74%) and chlorophyll c content was about as much as four times compared with chlorophyll a content.

무기물에서 유기물을 생산하는 곳으로서 뿐만 아니라 인류의 마지막 식량공급처로서의 해양에 대한 기초생산의 중요성이 날로 높아져 국제인도양조사때나 Kuroshio해역조사때 생산력이 측정되었고 북서태평양(Sorokin and Koblentz-Miskke; 1958, Ichimura and Saijo; 1959, Saijo and Ichimura; 1960, Aruga and Monsi; 1962, 천촌;1963), 인도네시아 주변해역(Doty et al;1963)등에서도 기초생산이 측정된 바 있다. 일본의 주요 9개만에서는 월별측정(송평 등;1964)이 되었다. 우리 나라 연안에서는 최와 정(1966)이 $C^{14}$를 이용하여 광합성량을 측청하였고 Kang(1967) 은 수영만에서 계절별로 산소소모에 의한 광합성량을 측정했다.다.