Ji Nai-yun, Zhao Wei-hong, Wang Jiang-tao, Cui Xin, Miao Hui
Key Laboratory of Marine Ecology & Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China.
Huan Jing Ke Xue. 2006 Feb;27(2):257-62.
Fluorescence excitation-emission matrix spectroscopy (EEMS) was employed to characterize the dissolved organic matter (DOM) in algal bloom seawater of Jiaozhou Bay in February, 2004. The relationships of DOM fluorescence characteristics with phytoplankton multiplication, dissolved organic carbon (DOC), salinity, dissolved oxygen and pH were discussed. In addition, the protein-like and humic-like fluorescence changes fore and aft cross-flow ultrafiltration (CFF) were primarily evaluated. The results show that the intensities of high and low-excitation protein-like fluorescence, which have the same sources, are stronger than that of humic-like during algal bloom. Both correlations between protein-like fluorescence intensities and chlorophyll-a and between humic-like fluorescence intensities and chlorophyll-a are relevant to the phytoplankton multiplication. As a whole, the fluorescence intensities of protein-like and humic-like increases with chlorophyll-a increasing. Furthermore the ratios of new to old DOM increase with phytoplankton biomass increasing. Good positive correlations between protein-like fluorescence intensities and DOC and between the ratios of protein-like to humic-like fluorescence intensities and DOC suggest that the DOC is mainly composed of newly produced matter during algal bloom. Some inorganic factors, such as salinity, dissolved oxygen and pH, have little effects on protein-like and humic-like fluorescence. Fore and aft the CFF experiments, the positions of protein-like and humic-like fluorescence peaks have little alteration, the balance of fluorescence intensity is not so good as organic carbon mass balance as a whole. Fluorescence balance should be used only as a supplementary technique for evaluating contaminations or loss by organic carbon mass balance.
采用荧光激发-发射矩阵光谱法(EEMS)对2004年2月胶州湾赤潮海水溶解有机物(DOM)进行表征。探讨了DOM荧光特性与浮游植物增殖、溶解有机碳(DOC)、盐度、溶解氧和pH值之间的关系。此外,初步评估了错流超滤(CFF)前后类蛋白和类腐殖质荧光的变化。结果表明,在赤潮期间,具有相同来源的高激发和低激发类蛋白荧光强度均强于类腐殖质荧光强度。类蛋白荧光强度与叶绿素a之间以及类腐殖质荧光强度与叶绿素a之间的相关性均与浮游植物增殖有关。总体而言,类蛋白和类腐殖质的荧光强度随叶绿素a的增加而增加。此外,新老DOM的比例随浮游植物生物量的增加而增加。类蛋白荧光强度与DOC之间以及类蛋白与类腐殖质荧光强度之比与DOC之间呈良好的正相关,表明DOC主要由赤潮期间新产生的物质组成。一些无机因素,如盐度、溶解氧和pH值,对类蛋白和类腐殖质荧光影响较小。CFF实验前后,类蛋白和类腐殖质荧光峰的位置变化不大,总体荧光强度平衡不如有机碳质量平衡好。荧光平衡仅应作为通过有机碳质量平衡评估污染或损失的补充技术。