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长泥龄SBR亚硝化系统的污泥适应性
Acclimation in Partial Nitrification Process of Long MCRT
【摘要】 亚硝化系统稳定运行一段时间之后,硝化菌能逐渐适应亚硝化条件,恢复活性,从而使污泥产生适应性,亚硝化现象消失。污泥产生适应性是一个渐变过程,一旦污泥开始适应后,只需几天亚硝化现象就会彻底消失。研究结果表明:长泥龄SBR系统不能建立长期稳定的亚硝化系统,要建立稳定亚硝化系统必须保证污泥的更新率,寻求合适的污泥龄,而杆状絮体是良好亚硝化现象的特征污泥相。
【Abstract】 Nitrite accumulation will drop down when the nitrite oxidation bacteria have acclimated to the nitrifying conditions after stable performance for some times. Accumulation is a gradating course, nitrite disappear will take only a few days. A long MCRT can not maintain a long term stable partial nitrifying process. The refreshment of system sludge and suitable MCRT is key for nitrite accumulation, and bacillar sludge is its typical feature.
- 【文献出处】 重庆大学学报(自然科学版) ,Journal of Chongqing University(Natural Science Edition) , 编辑部邮箱 ,2004年04期
- 【分类号】X703.1
- 【被引频次】35
- 【下载频次】249