河北平原潮土中微生物对氮降解特征

了解土壤中微生物对氮素降解规律,对于土壤氮污染修复具有重要现实意义.从河北平原潮土中筛选出8种高效氨化细菌、硝化细菌、异养硝化好氧反硝化细菌,对所筛菌种进行16S r DNA分析,选出最适菌株通过固定化载体将菌种制成菌剂.探讨了用加入所筛菌种及拮抗菌的菌液和地表水分别滴灌小白菜对土壤中的氮降解产生的影响,并测定土样磷脂脂肪酸(PLFA)的值.结果表明:以硅藻土为载体硝化细菌的氨氮降解率达到38%,硝态氮合成率为205%;以硅藻土为载体的氨化细菌氨氮合成率为1 711%,异养硝化好氧反硝化细菌的硝态氮降解率达到367%.加所筛菌液滴灌对土壤总氮和氨氮的降解效果较好,硝化作用也较强,加菌后土壤中微生物量明显增加,且更快到达峰值.对不同土样不同时间磷脂脂肪酸数据分析发现,在白菜生长过程中,土壤中的微生物含量均产生了1次峰值,且加入所筛菌的先到达峰值.对于任丘和阜城土样来说,加入所筛菌后,土壤中微生物种类相应增多,对土壤微生物环境有所改善,微生物也比较活跃.     

两段式曝气对好氧颗粒污泥脱氮性能的影响

基于4个不同进水条件的小试实验探究,得出所接种好氧颗粒污泥表面异养菌在曝气初期阶段大量消耗碳源,对于NO-2-N和NO_3~--N的反硝化效率较低.为此,实验在常温(20~23℃)条件下,在同一周期内先采用低曝气量曝气之后再用高曝气量曝气的两段式曝气方式运行好氧颗粒污泥SBR反应器,低曝气量时长分别取1、2、3 h这3个阶段分别运行,并运用扫描电镜(SEM)和荧光原位杂交技术(FISH)对颗粒污泥进行分析,结果表明AGS粒径增大,反硝化能力提升,NO-2-N的反硝化速率(以LVSS计)在低曝气时长为2 h时升至最高,达9.66 mg·(g·h)~(-1).亚硝态氮积累率不断升高至77.84%,总氮去除率最高达70%.颗粒污泥内部孔隙增多,且细菌多以球菌、椭球状及杆菌为主,氨氧化菌(AOB)占总菌的比例由13.70%升至15.40%.因此,通过两段式曝气过程实现了短程同步硝化反硝化过程并具有较好的脱氮性能.     

多层填料生物转鼓去除NO废气的效能比较研究

生物转鼓过滤器能有效去除一氧化氮(NO)废气,为进一步提高生物转鼓过滤器的去除效能,实验改变了生物转鼓的填料结构,并与单层填料的生物转鼓进行了比较研究.结果表明,多层填料生物转鼓比单层填料生物转鼓更能有效去除NO,运行也更加稳定.8个月的连续运行实验表明,多层填料生物转鼓对NO去除率稳定在53.9％ ～93.4％之间,平均去除效率79.8％,而单层填料生物转鼓的平均去除率仅有68.7％;在相同实验条件下,空床停留时间(EBRT)可从单层填料生物转鼓的86.4 s降至多层填料生物转鼓的57.6 s.多层填料生物转鼓的最优工艺条件为,营养液量为1.3～3L,转速为0.75 r·min-1,在以葡萄糖为碳源时,TOC＞ 1250 mg·L-1后,去除效率增长幅度趋于平缓.     

生物陶粒反应器的氢自养反硝化研究

利用氢自养反硝化生物陶粒反应器处理硝酸盐废水,探讨了生物陶粒反应器中氢自养反硝化生物脱氮的实现过程.考察了水力停留时间、进水硝氮负荷、进水pH值、温度、供氢量等因素对反应器脱氮效果的影响.结果表明,当水力停留时间为24 h和48 h时,反应器对硝酸氮的平均去除率分别达到94.54%和97.47%.在水力停留时间为5~16 h时,NO-3-N去除率随水力停留时间的缩短而降低;进水NO-3-N浓度较低时,NO-3-N的降解速率随其浓度的升高而增大,当NO-3-N浓度大于110mg·L-1时,氢自养反硝化反应受到抑制;中偏碱性环境较酸性或碱性环境更利于反应器对硝酸盐的去除;反应器有较宽的温度适应范围,最适温度为25~30℃;当反应器供氢不足时,脱氮效果明显降低,表明了氢自养反硝化菌对氢气利用的专一性.在整个运行阶段,出水中亚硝酸氮浓度一直保持在较低水平.     

Effect of ammonium on nitrous oxide emission during denitrification with different electron donors

Nitrous oxide(N2O) emission during denitrification is receiving intensive attention due to its high potential to cause greenhouse effects.In this study,denitrifiers were acclimated in sequencing batch reactors with methanol or acetate as the electron donor and nitrate as the electron acceptor.The effects of ammonium on N2O emission were examined in batch experiments with various electron donors.With the addition of ammonium,N2O emission increased under all the examined conditions compared to experiments without ammonium addition.With different electron donors,the highest ratio of N2O emission to the removed oxidized nitrogen was 0.70% for methanol,5.34% for acetate,and 34.79% for polyhydroxybutyrate.     

Identification of key factors governing chemistry in groundwater near the water course recharged by reclaimed water at Miyun County, Northern China

Reclaimed water was successfully used to recover the dry Chaobai River in Northern China, but groundwater may be polluted. To ensure groundwater protection, it is therefore critical to identify the governing factors of groundwater chemistry. Samples of reclaimed water, river and groundwater were collected monthly at Chaobai River from January to September in 2010. Fifteen water parameters were analyzed. Two kinds of reclaimed water were different in type (Na-Ca-Mg-Cl-HCO3 or Na-Ca-Cl-HCO3 ) and concentration of nitrogen. The ionic concentration and type in river were similar to reclaimed water. Some shallow wells near the river bed had the same type (Na-Ca-Mg-Cl-HCO3 ) and high concentration as reclaimed water, but others were consistent with the deep wells (Ca-Mg-HCO3 ). Using cluster analysis, the 9 months were divided into two periods (dry and wet seasons), and all samples were grouped into several spatial clusters, indicating different controlling mechanisms. Principal component analysis and conventional ionic plots showed that calcium, magnesium and bicarbonate were controlled by water-rock interaction in all deep and some shallow wells. This included the dissolution of calcite and carbonate weathering. Sodium, potassium, chloride and sulfate in river and some shallow wells recharged by river were governed by evaporation crystallization and mixing of reclaimed water. But groundwater chemistry was not controlled by precipitation. During the infiltration of reclaimed water, cation exchange took place between (sodium, potassium) and (calcium, magnesium). Nitrification and denitrification both happened in most shallow groundwater, but only denitrification in deep groundwater.     

反硝化菌株DA-1的脱氮研究

菌株DA-1被发现能在好氧和厌氧环境中将硝酸盐转化为气态氮。在以NO3-为唯一氮源的条件下研究了碳源、C/N和pH值对菌株DA-1好氧和厌氧反硝化脱氮的影响。结果表明:同等条件下,48 h内菌株DA-1的厌氧脱氮效率高于好氧脱氮率;菌株DA-1能在好氧和厌氧条件下利用乙酸、柠檬酸以及葡萄糖进行细胞增殖和反硝化。在厌氧条件下,三者作为碳源时的反硝化效率分别为(34.04±0.15)%、(22.72±0.32)%和(11.32±0.06)%,均低于好氧条件下的(25.38±0.14)%、(17.52±0.11)%和(8.06±0.01)%。2种条件下均是乙酸为碳源时反硝化效率最高。而丁二酸仅能在厌氧环境中作为电子供体参与反硝化反应。C/N越高越有利于菌株DA-1的厌氧反硝化,当C/N为10时,反硝化效率最高为(35.06±0.19)%。而在好氧条件下,菌株反硝化效率随着C/N的升高,先升高再降低,当C/N为8时,反硝化效率最高;好氧和厌氧脱氮的最适pH值为7.0。体系偏酸或者偏碱都会造成菌株DA-1脱氮效率的降低并出现亚硝酸盐累积。厌氧环境中pH=5.0时累积的亚硝酸盐浓度高达(8.95±2.05)mg/mL。     

2种生物反硝化法去除地下水中硝酸盐的研究

采用砂柱装置,在实验室研究了自养微生物和异养微生物2种生物反硝化方法对地下水中硝酸盐的去除效果。自养反硝化反应在以硫作为电子供体的硫/石灰石/细沙反应柱中进行,异养反硝化反应在石灰石/细沙反应柱中进行,进水增加乙醇作为外加碳源。实验结果用以比较2种反硝化方法在硝酸盐去除率、微生物反应动力学和反应产物三者的异同。结果表明,自养反硝化反应中NO3--N去除率达95.4%,异养反硝化反应去除率可达99.3%;分别与Monod微生物0级、1/2级和1级反应动力学方程进行拟合,2种反硝化反应均符合1/2级微生物反应动力学,适合用1/2级微生物反应方程描述;在反应结束阶段,自养反硝化主要反应产物SO42-出水浓度低于250mg/L,异养反硝化副产物CH3OO-易成为二次污染源,异养反硝化的反硝化速率明显高于自养反硝化反应。     

九龙江河口区夏季反硝化作用初探

河口反硝化是削减入海河流氮污染的重要途径,为探明地处亚热带的九龙江河口混合区的反硝化作用,于2010年7月开展13个站位的面上调查,利用N2：Ar法和膜进样质谱分析仪（MIMS）直接测定反硝化产物溶解N2浓度,用吹扫捕集-气相色谱法测定溶解N2O浓度,并估算二者净增量和水气交换通量.结果表明,溶解N2和N2O净增量有明显的区域变化,从淡水端向海域减少,N2净增量为-9.9～66.8μmol.L-1,N2O净增量为4.3～31.5 nmol.L-1;N2O饱和度为170%～562%,平均352%;N2水气通量为-2.9～53.2 mmol.（m2.d）-1,N2 O水气通量为5.2～23.9μmol.（m2.d）-1,N2 O通量占总通量的0.03%～1.2%（平均0.25%）.温度和营养盐（氮、磷）是影响九龙江河口区反硝化作用的重要因子;淡水端（盐度〈0.5）反硝化作用及其空间分布主要受硝酸盐含量控制,海水端溶解N2与N2O的增加主要来自淡水端的输送,并受盐度梯度（混合作用）影响.     

T型氧化沟工艺处理低碳源生活污水的效果研究

详细介绍了T型氧化沟工艺的特征,并考察研究了该工艺处理低碳源生活污水的长期运行效果。研究结果表明,工艺出水COD、BOD5、NH3-N、TN和TP年平均浓度分别为13.9、3.8、0.91、18.80和1.67 mg/L,去除率分别为88.99%、94.37%、96.74%、37.57%和41.58%,均能达到相应的排放标准。由于T型氧化沟中以好氧环境为主,缺乏厌氧和缺氧环境以及进水的BOD5/TN值低,工艺对有机物及NH3-N的去除效果较好,但TN和TP去除效果较低。提出了加强工艺脱氮除磷的措施,为同类型污水处理厂改造提供参考。