Abstract
This study was evaluated about the seasonal variations of ecosystem in Nammae Reservoir based on the interrelation of physico-chemical characteristics, nutrients, chlorophyll a, b, c and standing crops of phytoplanktons. The amounts of chlorophyll a, b, c were respectively maximum (295 mg/, 9.5mg/l and 48mg/l) at station 1 in June and the standing crop of phytoplanktons was the highest ($1.7{\time}10^5$ cells/1) at stations 3 in July. The range of temperature was $7{\sim}37.4^{\circ}C$. The maxium of pH was $9.9{\sim}10.1$ at all stations in August, the minimum was 7 in September. SS was maximum (308 mg/1) at station 1 in June, while it was minimum (4 mg/l) at the same station in November. The maximal COD and DOC were 33 mg/1 and 16 mg/1 respectively at station 1 in June. As for phytoplanktons, Microcystis aeruginosa, blue-green alga in July${\sim}$August, Scenedesmus acutus, green alga in March${\sim}$May and November${\sim}$January and Cyclotella orientalis, Diatoms in October were dominant species. The amounts of P and Si were generally high in summer, they were low in autumn and winter. Nammae Reservoir assessed by trophic state index was eutrophicated and overtrophicated. These results indicated that Nammae Reservoir was faced with heavy water pollution. As preceding management for the basin of the Reservoir, it will have to be continually studied for an ecosystem reservation.
경북 경산시에서 농업용수로 이용되는 남매지의 3개 정점을 선정하여 2000년 3월부터 2001년 2월까하였다. 다양한 이화학적 환경요인과 식물플랑크톤의 엽록소 a, b, a 농도 및 현존지 매월1회 조사량의 상호관계를 통해 남매지 생태계의 계절적 변화를 파악하였다. 엽록소 a, b와 c의 농도가 6월에 정점 1에서 각각 최고치 (295nlg/1, 9.Smg/1, 48mg/1)를 나타냈고, 식물플랑크톤은 현존량이 정점 3에서 여름에 가장 높았다(7월: $1.7{\time}10^5$scells/1). 수온 분포는 $7{\sim}37.4^{\circ}C$ 범위 이었다. 수소이온 농도는 8월에 $9.9{\sim}10.1$ 범위로 최고치를 나타냈고, 최저는 7로서 9월이었다. SS저는의 최대 및 최 정점 1에서 6월과 11월에 각각 308 mg/1, 4 mg/1이었다. COD와 DOC는 동일한 정점에서 6월에 각각 33mg/1와 16mg/1로 높았다. 식물플랑크톤의 남조류 Microcystis aeruginosa는 7${\sim}$8월에, 녹조류 Scenedesmus acutus는 3${\sim}$5월과 11l${\sim}$1월에, 규조류 Cyclotella orientalis는 10월에 각각가장 우점종하였고, 인산이온과 규산이온의 농도는 여름에 비교적 높은 반면에 가을과 겨울에 전반적으로 낮았다. TSI는 16.6${\sim}$86.4범위로서 전 정점이 부영양화 혹은 과영양화 상태이었고, 유역관리가 선행된 지속적인연구의 필요성이 요구되었다.
