以松花江滤后水为研究对象,利用不同质量浓度臭氧氧化降解水中有机污染物.结果表明臭氧氧化对CODMn的去除能力随臭氧投量增加而增加,但去除率并不是随着臭氧投量的增加而相应的呈线性增加,说明臭氧氧化存在最佳臭氧投量.臭氧对UV254的...以松花江滤后水为研究对象,利用不同质量浓度臭氧氧化降解水中有机污染物.结果表明臭氧氧化对CODMn的去除能力随臭氧投量增加而增加,但去除率并不是随着臭氧投量的增加而相应的呈线性增加,说明臭氧氧化存在最佳臭氧投量.臭氧对UV254的去除效果很明显,较短时间内,就可以达到较好的去除效果.臭氧氧化在1 m in内对DOC去除效果明显,之后随着臭氧质量浓度降低,反应速率下降,并且臭氧氧化使得一些POC转化为DOC,从而去除率呈现为负值.臭氧氧化难以去除氨氮,较易将有机氮氧化生成氨,从而使得氧化后水中的氨氮有所升高,氨氮去除率呈现负值.臭氧对松花江水中有机物的氧化不完全,对氨氮去除效果不佳,而且生成的中间产物会阻止臭氧进一步氧化,因此臭氧氧化后再接生物处理效果会更好.展开更多
This work aims at characterizing organic matter produced by an alga Euglena gracil~ and a cyanobacteria Microcystis aeruginosa and assessing the evolution of its characteristics during growth. A culture medium was opt...This work aims at characterizing organic matter produced by an alga Euglena gracil~ and a cyanobacteria Microcystis aeruginosa and assessing the evolution of its characteristics during growth. A culture medium was optimized. The species growth phases were monitored using both visible spectrophotometry and flow cytometry cell counting. Organic matter fractionation according to hydrophobicity and specific UV absorbance （SUVA） index were used to specifically characterize the produced algal organic matter （AOM）. The AOM characteristics were both growth phase and species dependent. However, a similar evolution was observed. The hydrophilic fraction （HPI） was the major fraction whatever the growth phases and was almost the only one produced during lag and exponential phases. It represented around 75% of AOM during exponential phase and then decreased when the stationary phase appeared. It represented 46% and 60% of the AOM during late decline phase for the cyanobacteria and the alga respectively. The hydrophobic （HPO） and transphilic （TPH） fractions started to appear from the beginning of the stationary phase with more hydrophobic compounds coming from intracellular organic material of dying cells. HPO and TPH percentages still increased during the decline phase probably because of two additional processes： photo-dissolution and leaching of particulate organic matter from cells fragments. A comparison of AOM during late decline phase and natural organic matter （NOM） from Glane River （France） underlined that AOM was more fiydrophilic and presented a lower SUVA for each fractions than NOM. However, the difference between NOM and AOM hydrophobicity narrowed during decline phase.展开更多
文摘以松花江滤后水为研究对象,利用不同质量浓度臭氧氧化降解水中有机污染物.结果表明臭氧氧化对CODMn的去除能力随臭氧投量增加而增加,但去除率并不是随着臭氧投量的增加而相应的呈线性增加,说明臭氧氧化存在最佳臭氧投量.臭氧对UV254的去除效果很明显,较短时间内,就可以达到较好的去除效果.臭氧氧化在1 m in内对DOC去除效果明显,之后随着臭氧质量浓度降低,反应速率下降,并且臭氧氧化使得一些POC转化为DOC,从而去除率呈现为负值.臭氧氧化难以去除氨氮,较易将有机氮氧化生成氨,从而使得氧化后水中的氨氮有所升高,氨氮去除率呈现负值.臭氧对松花江水中有机物的氧化不完全,对氨氮去除效果不佳,而且生成的中间产物会阻止臭氧进一步氧化,因此臭氧氧化后再接生物处理效果会更好.
基金the FEDER (European Found forRegional Development)the Regional Council of Limousin for their financial supportnt
文摘This work aims at characterizing organic matter produced by an alga Euglena gracil~ and a cyanobacteria Microcystis aeruginosa and assessing the evolution of its characteristics during growth. A culture medium was optimized. The species growth phases were monitored using both visible spectrophotometry and flow cytometry cell counting. Organic matter fractionation according to hydrophobicity and specific UV absorbance （SUVA） index were used to specifically characterize the produced algal organic matter （AOM）. The AOM characteristics were both growth phase and species dependent. However, a similar evolution was observed. The hydrophilic fraction （HPI） was the major fraction whatever the growth phases and was almost the only one produced during lag and exponential phases. It represented around 75% of AOM during exponential phase and then decreased when the stationary phase appeared. It represented 46% and 60% of the AOM during late decline phase for the cyanobacteria and the alga respectively. The hydrophobic （HPO） and transphilic （TPH） fractions started to appear from the beginning of the stationary phase with more hydrophobic compounds coming from intracellular organic material of dying cells. HPO and TPH percentages still increased during the decline phase probably because of two additional processes： photo-dissolution and leaching of particulate organic matter from cells fragments. A comparison of AOM during late decline phase and natural organic matter （NOM） from Glane River （France） underlined that AOM was more fiydrophilic and presented a lower SUVA for each fractions than NOM. However, the difference between NOM and AOM hydrophobicity narrowed during decline phase.
