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低浊水源铁锰与磷耦合转化研究
Coupling Transformations of Iron-Manganese-Phosphorous in Low Turbidity Drinking Water Resources
【摘要】 采用现场检测和相关性分析相结合的方法 ,研究了水库水源铁锰和磷元素的耦合转化关系。结果表明 ,当水库出现温跃层时 ,底部形成厌氧区 ,铁和锰浓度大幅度上升 ,同时磷的浓度也相应大幅度升高 ,底部水体中铁、锰和总磷的平均含量分别是表层水体的 12 7倍、16 3倍和 3 4倍 ;铁、锰和磷转化过程的相关性非常显著 ,具有内在耦合关系 ,提出了饮用水水源中铁锰与磷耦合转化的概念模型。
【Abstract】 The coupling transformation relationships among Fe, Mn and P in a low turbidity reservoir were studied by means of site -monitoring and data correlation analysis. The results indicate that the concentrations of Fe and Mn and P as well will increase in a large scale when thermocline layer and anaerobic layer formed in the reservoir in summer. Concentrations of Fe, Mn and TP in the hypolimnion were 12.7, 16.3 and 3.4 times greater than those in the epilimnion respectively. Correlation analysis clearly demonstrated that there are evident coupling relationships amount Fe, Mn and P transformation. A concept model of iron, manganese and phosphorous transformation in this reservoir has been established.
- 【文献出处】 给水排水 ,Water & Wastewater Engineering , 编辑部邮箱 ,2003年11期
- 【分类号】TU991.2
- 【被引频次】13
- 【下载频次】119