千岛湖溶解氧的动态分布特征及其影响因素分析

基于2011~2012年1~12月千岛湖6个站点的溶解氧浓度实时监测数据,分析了千岛湖溶解氧的垂直分布以及时空分布特征,并探讨了影响水体溶解氧动态分布特征的影响因子.结果表明,溶解氧分布特征有明显的垂向差异以及季节差异.冬季,平均溶解氧值较高,除大坝前站点,其余各站点溶解氧无显著垂向差异;夏季,溶解氧垂向差异显著大于春秋两季.水深较深的小金山、三潭岛和大坝前站点其夏季溶解氧最大值出现在真光层,分别达到11.59、12.52和10.96 mg·L-1.千岛湖表层溶解氧最大值出现在春季,而最小值出现在秋季.相关性分析结果表明,溶解氧与水温、pH、叶绿素a浓度的相关性存在季节性差异.夏季,水温与溶解氧存在极其显著的线性相关,温度热力分层是影响溶解氧在夏季垂直分布的关键因素.春夏季,pH、叶绿素a浓度与溶解氧的相关系数较高,主要与浮游植物光合作用有关.

Dynamic Distributions of Dissolved Oxygen in Lake Qiandaohu and Its Environmental Influence Factors

Based on monthly in situ data collected at six sampling sites in Qiandaohu Lake between 2011 and 2012, the dynamic distributions of dissolved oxygen (DO) were analyzed and the relationships between DO and the environmental factors were investigated. The results showed that there were obviously vertical and temporal variations in the distributions of DO. In winter, the average values of DO were generally higher than those in other seasons, but no significant vertical distribution variation was found except Dabaqian. However, the vertical differences of DO in summer were larger than those in spring and autumn. Moreover, the maximum values of DO found in euphotic zone at the sites of Xiaojinshan, Santandao, Dabaqian in summer were 11.59, 12.52, 10.96 mg·L^-1, respectively. The maximum DO at surface layer was found in spring while the minimum value appeared in autumn. Seasonal differences in relationships between dissolved oxygen and water temperature, pH, and Chla concentration were discussed. In summer, highly significant linear correlation between DO and water temperature was found indicating that the temperature thermal stratification was the key factor to influence the vertical distribution of DO. The relative higher correlation coefficients between DO and pH, Chla concentration in spring and summer were due to the phytoplankton photosynthesis.