본 연구는 남해안 북만 해역을 대상으로 조류성장잠재력(AGP) 시험을 통하여 H. akashiwo의 성장제한요인을 평가하였다. 영양물질의 첨가 및 미생물과의 동시배양에 의하면 적조발생 단계별 H. akashiwo의 성장은 서로 다른 제한요인에 의하여 영향을 받는 것으로 나타났다. 적조발생 전의 H. akashiwo 성장은 질산질소 50μM과 연산인 5μM을 복합첨가하면 크게 증가하였지만 인산인을 단독 첨가하거나 미생물과 동시 배양하여도 전혀 영향이 없었다. 적조발생 전의 H. akashiwo 성장제한요인은 질산질소로 나타났다. 적조발생시기의 H. akashiwo 성장은 질산질소 50μM 또는 인산인 5μM을 단독첨가하면 증가하였지만 미량영양물질이나 vitamin B12을 첨가해도 전혀 영향이 없었다. 적조발생 시기의 H. akashiwo 성장제한요인은 질산질소와 인산인이 동시에 작용하는 것으로 나타났다. 반면에 적조소멸시기의 H. akashiwo 성장은 질산질소와 인산인을 첨가하면 약간 증가하였지만 미생물과 동시 배양하면 현저히 감소하였다. 그러므로 적조 소멸시기의 H. akashiwo 성장제한은 미생물요인에 의한 것으로 평가되었다.

An algal assay procedure using an indigenous phytoplankton assemblage was tested to estimate the propagation of red tide phytoplankton species and determine the optimal time interval at which to measure growth yield in eutrophic marine waters where red tides frequently occur. Various red tide phytoplankton species were propagated on a large scale by adding nitrogen or phosphorous. This procedure was useful for estimating the limiting nutrient, elucidating the mechanisms underlying red tides, and determining the levels of increases in organic matter in eutrophic coastal waters. The algal assay using indigenous C. polykrikoides showed that this species did not always propagate, apparently because of very low concentrations of trigger elements that are necessary for its growth, rather than as a result of other environmental characteristics, e.g., water temperature or stress from sampling. In the winter, when water temperatures are lower than in spring, summer, or autumn, maximum propagation and the limiting nutrient could be estimated by measuring phytoplankton biomass at 2–3-day intervals. However, in the other seasons, when water temperatures are higher, phytoplankton biomass should be measured at 2-day intervals. In particular, daily monitoring will be required to determine precise growth yields in warm seasons.

In order to understand the impact for decomposition of blue-green algae Microcystis on water quality, the algae were cultivated with collection of natural population during approximately one month, when water-bloom of Microcystis dominated at August 31, 1999 in the lower part of the Okchon Stream. The enrichment of inorganic N·P nutrients didn't in algal assay and the effect of Microcystis on water quality was assessed from the variation of nutrients by algal senescence. Microcystis population seemed to play a temporary role of sink for nutrients in the water body. Initial algal density of Microcystis was 2.3×106 cells/ml. When Microcystis population died out under light condition, algal N·P nutrients between 9∼12 days affected to increase of biomass after reuse by other algal growth as soon as release to the ambient water. However, cellular nutrients under dark condition were almost moved into the water during algal cultivation. NH4, NO3 and SRP concentration were highly increased with 160, 17 and 79 folds, respectively relatve to the early. As a result, the senescence of Microcystis population seemed to be an important biological factor in which cause more eutrophy and increase of explosive algal development by a lot of nutrients transfer to water body. There are significantly observed an effort of reduce for production of inner organic matters such a phytoplankton as well as load pollutants from watershed in side of the water quality management of reservoir.