中文摘要：

通过室内静态实验培养装置模拟了蓝藻细胞大量聚集、沉降死亡后对水-沉积物界面处Fe、Mn、S循环的驱动作用.结果表明,藻细胞沉降到沉积物表面50min内,溶解氧就消耗殆尽,形成厌氧、强还原环境,使得界面处大量的铁锰氧化物和硫化物发生厌氧还原.实验进行到第4d沉积物-水界面处Fe2＋、Mn2＋含量达到峰值,含量分别为4.40mg/L、2.35mg/L;实验结束时Fe2＋含量表现下降,浓度仅为3.37mg/L;Mn2＋急剧降低,浓度为0.97mg/L.而S2-含量变化则表现为第2d达到最高,含量为0.63mg/L;此后浓度一直降低,实验结束后浓度为0.12mg/L.在实验结束后测定的0～1cm处沉积物的ORP值为-150mV,表明沉积物处于强还原状态.藻体死亡引起的黑水团现象,在驱动沉积物中Fe、Mn、S发生强烈的生物地球化学过程的同时,也将对水体生态环境产生极大的影响.

英文摘要：

The driving effects of algal cells settlement in the water-sediment interface on Fe,Mn,S biogeochemistry in laboratory through static cultivation device.Results showed that dissolved oxygen would be exhausted by algae cells in 50 min after the cyanobacteria cells settled to the sediment surface.Soon the water-sediment interface formed the severe anoxia and Fe-Mn oxides and sulfides were deoxidized quickly in the strong reducing environment.The Fe2 ＋,Mn2 ＋ content in interface increased to the summit at the 4th day and their concentrations were 4.40 mg /L and 2.35 mg /L,respectively.When it comes to the end of the experiment,the Fe2 ＋ content had a little reduction and Mn2 ＋ reduced quickly,their concentrations were 3.37 mg /L and 0.97 mg /L at the end of experiment.However,S2-concentration in interface reached the highest at the 2nd day and its content was 0.63 mg /L,and its concentration was only 0.12 mg /L at the end since it has been reduced.The ORP was-150 mV in the sediment surface and indicated that the sediment environment was a strong reducing environment.Phenomenon of algal cells induced black spots in water bodies was the main driving factors on Fe /Mn oxides and sulfides biogeochemistry cycle,and also the extreme anoxia environment would have great harm on the water body＇s ecology.