摘要
新庙泡是前郭灌区排水进入查干湖的前置湖,水体溶解氧浓度受自然气候、水文地质、水生植物及浮游生物的交织影响,年内变动幅度较大,在吉林西部湖泡中具有典型性。其演化规律与驱动机制对吉林西部河湖连通后的水生态系统构建与生态修复具有重要参照意义。
Xinmiao Lake is the front lake through which water can be transported out of Qianguo Irrigation District into Chagan lake,The intensity of dissoyled oxygen has been influenced by the weather hydrogeology,aquatic plants and plankton,the annual variation of which changes in large scale.Xinmiao Lake is very typical among jilin western lakes and its evolution law and driving mechanism has been of great importanmce to the construction of water ecosystem and the restoration after river-lake interconnection in the western part of Jilin Province.
出处
《吉林水利》
2018年第9期1-4,7,共5页
Jilin Water Resources
基金
<吉林省西部河湖连通湖泡湿地生态恢复技术研究与示范>(课题编号:20180201011SF)
关键词
新庙泡
河湖连通
溶解氧
驱动机制
Xinmiao Lake
dissolved oxgyen
river-lake interconnection
driving mechanism
