硫磺/石灰石自养反硝化系统脱氮除磷性能研究

为了考察硫磺/石灰石系统对于低C/N的城市污水进行同步脱氮除磷的性能,设计了体积比为1∶1的硫磺/石灰石柱式反应器,以人工配水为处理对象,采用厌氧生物滤池运行方式,研究了HRT、初始磷浓度、pH、温度等因素对其脱氮除磷性能的影响.结果表明,在进水NO 3^--N为30 mg/L左右,PO4^3--P为15 mg/L条件...     

厌氧时间对间歇进水-间歇曝气的好氧颗粒污泥系统影响

为启动生活污水AGS工艺,实验以间歇进水-间歇曝气方式运行,降低硝氮浓度,减轻对PAO的抑制,利用除磷中产生的磷酸盐沉淀和正电微粒促进颗粒化实现.接种污水厂污泥于SBR反应器R1、R2、R3和R4中,在总厌氧时间为30、60、90和120 min时,研究厌氧时间对生活污水AGS系统的影响.实验表明,R1、R2、R3和R4历时56、48、39和35 d启动成功;运行105 d,平均粒径达750、764、791和650μm.运行期间,R1和R2在43 d和47 d除磷恶化,延长厌氧时间至90 min后恢复;R3处理效果良好; R4在63～77 d颗粒解体,处理效果下降,DPAO富集程度降低.运行后期,R1、R2、R3和R4出水水质均满足《城镇污水处理厂污染物排放标准》一级A标准.结果表明,长厌氧时间运行能实现快速颗粒化,但长期运行时颗粒易解体.较长的厌氧时间能减轻硝氮对PAO释磷的抑制,有助于富集DPAO,能获得良好的脱氮除磷效果.     

固定化微生物法去除模拟渗滤液中氨氮的研究

采用固定化微生物曝气生物滤池（I-BAF）技术成功处理了模拟垃圾渗滤液,探讨了pH和溶解氧（DO）对系统脱氮性能的影响。结果表明,固定化微生物曝气生物滤池反应系统启动迅速,运行稳定,可以有效去除模拟垃圾渗滤液中的有机物和氨氮,其去除率分别达到97.1%和99.9%。在pH为7.5～8.5之间,DO 4.0 mg/L左右的条件下对模拟垃圾渗滤液中氮的去除最为有利,同步硝化反硝化效率以及总氮去除率均达到最高,分别为96.2%和94.3%。这主要是由于I-BAF系统中大孔载体提供了厌氧-兼氧-好氧的微环境,使硝化和反硝化反应在同一个反应器内发生,共同作用实现模拟垃圾渗滤液中总氮的去除。     

SBR工艺处理晚期垃圾渗滤液的脱氮特性研究

采用有效容积为1 200 m3的SBR反应器处理晚期垃圾渗滤液,进行生物脱氮特性研究.结果表明,通过投加粪水调节进水C/N,能显著提高SBR反应器对晚期垃圾渗滤液中氮素污染物的去除效果,其中第112~136 d的TN平均去除率高达82.62%,出水TN≤190 mg.L-1,COD≤400 mg.L-1;能在反应器内达到各种生物脱氮反应的平衡状态,BOD5与TN去除量的比值稳定在1.43左右.在稳定平衡阶段,通过对反应器内氮素污染物和SO24-的含量变化进行周期跟踪监测,发现在搅拌回流阶段存在NH4+-N和SO24-的同时等比例去除现象,去除率分别为27.06%和76.17%,反应器内存在同步硝化反硝化和同步脱氮除硫(SO24-)过程;量化分析了反应器内各种生物脱氮反应,得到异养反硝化、同步硝化反硝化、同化作用、同步脱氮除硫(SO24-)和内源呼吸反硝化对TN去除量的贡献率分别为62.6%、33.8%、7.0%、26.1%和2.7%.     

铁基质强化新型功能性化粪池高效处理黑水的试验

以铁基质生物载体为核心,将物理、生物和化学方法结合,对化粪池进行功能强化,实现黑水的原位深度处理.探究了溶解氧（DO）和碳氮比（C/N）等因素对黑水中污染物降解的影响,并在最佳运行参数下考察了氮素在系统中的转化机制.结果表明,当C/N为7.3~8.4时,好氧生物铁基质载体池DO为2.3~2.7mg/L时,系统氨氮（NH₄⁺-N）、总氮（TN） 、COD和总磷（TP）的平均去除率分别可达90.74%、85.81%、92.65%和95.78%;当进水C/N降至3.3~4.2时,系统NH₄⁺-N、TN、COD和TP的平均去除率仍可维持在81.16%、76.62%、93.87%和94.75%.铁基质生物载体内电解作用显著强化了化粪池内TN的脱除、COD的氧化和TP的固定.氮素转化机制分析表明,内电解与反硝化菌的耦合强化了反硝化作用,降低了反硝化过程对有机碳源的需求,强化了低C/N条件下TN、TP的脱除.     

唐岛湾网箱养殖区沉积物-水界面溶解无机氮的扩散通量

2004-08～2005-05分4个航次对唐岛湾网箱养殖区的10个站的沉积物间隙水和上覆水中的溶解无机氮营养盐（NH⁺₄-Ｎ、NO^-₃-Ｎ、NO^-₂-Ｎ）进行了现场调查, 并使用Fick第一定理对该海区沉积物-水界面溶解无机氮的扩散通量进行了估算.结果表明,网箱养殖区的上覆水和沉积物间隙水中溶解无机氮均以NO^-₃-Ｎ为主,分别占溶解无机氮总量的73.34%和61.45%;上覆水中溶解无机氮（DIN）和NO^-₃-Ｎ含量的季节变化趋势一致,在2004-10达到峰值,NH⁺₄-Ｎ的季节变化稍有不同;间隙水中溶解无机氮（DIN）和NO^-₃-Ｎ、NH⁺₄-Ｎ的变化趋势一致,表现为从5月份到8月份含量逐渐增加,到10月份达到最大,然后到次年2月份又减少;上覆水和间隙水中NO^-₂-Ｎ的含量随养殖进程表现为一个逐步积累的过程.NH⁺₄-Ｎ、NO^-₃-Ｎ和NO^-₂-Ｎ在沉积物-海水界面上的扩散通量分别为5.46、-5.04、8.71 μmol/（m²·d）,NO^-₂-Ｎ的扩散释放对唐岛湾网箱养殖区的水环境质量影响较大.     

Impact of atrazine and nitrogen fertilizers on the sorption of chlorotoluron in soil and model sorbents

Sorption of chlorotoluron in ammonium sulfate, urea and atrazine multi-solutes system was investigated by batch experiments. The results showed application of nitrogen fertilizers to the soil could affect the behavior of chlorotoluron. At the same concentration of N, sorption of chlorotoluron decreased as the concentration of atrazine increased on the day 0 and 6 in soil, respectively. The sorption of chlorotoluron increased from 0 to 6 d when soils were preincubated with deionized water, ammonium sulfate and urea solution for 6 d. That indicated incubation time was one of the most important factors for the sorption of chlorotoluron in nitrogen fertilizers treatments. The individual sorption isotherms of chlorotoluron in rubbery polymer and silica were strictly linear in single solute system, but there were competition sorption between pesticides or between pesticides and nitrogen fertilizers. That indicated the sorption taken place by concurrent solid-phase dissolution mechanism and sorption on the interface of water-organic matter or water-mineral matter.     

氮沉降对陆地生态系统土壤有机碳含量影响的Meta分析

研究已证实大气氮沉降的增加显著影响了土壤有机碳的含量,然而其变化幅度在不同的实验样地具有较大的差异.基于在我国开展的49个模拟氮沉降野外实验的408组数据,利用Meta分析、Meta回归和线性回归等方法系统研究了样地气候、土壤属性以及氮素施用参数对施氮后土壤有机碳含量的影响.结果表明,样地的年均温（MAT）和年均降水量（MAP）与施氮后土壤有机碳含量变化幅度显著正相关（P<0.05）.在MAT或MAP较低（MAT<3℃,MAP<500 mm）的样地中,施氮后土壤有机碳含量显著下降;而在MAT或MAP较高（MAT>3℃,MAP>500 mm）的样地中,施氮后土壤有机碳含量则显著升高.土壤属性方面,在C：N较高（>15）或酸性（pH<6.5）土壤中,施氮后土壤有机碳积累明显（P<0.05）;而在C：N较低（≤15）以及中性或碱性（pH≥6.5）土壤中,施氮后土壤有机碳变化不明显（P >0.05）.此外,施氮后草原生态系统土壤有机碳含量明显下降（-5.34%）;而湿地生态系统土壤有机碳含量变化不明显;森林生态系统土壤有机碳表现出明显积累（10.52%）,特别是阔叶林生态系统（13.10%）.所有的因子中,土壤C：N是影响施氮后土壤有机碳变化幅度的主导因子.在施氮类型方面,施加硝酸铵或尿素后土壤有机碳含量显著升高,而施加硝态氮对其影响不显著.综上所述,在精确评估、预测和分析氮沉降对土壤有机碳含量的影响时,应综合考虑样地的气候、土壤属性以及氮素施用参数等因素对实验结果的影响.     

Nitrogen deposition alters soil chemical properties and bacterial communities in the Inner Mongolia grassland

Nitrogen deposition has dramatically altered biodiversity and ecosystem functioning on the earth; however, its effects on soil bacterial community and the underlying mechanisms of these effects have not been thoroughly examined. Changes in ecosystems caused by nitrogen deposition have traditionally been attributed to increased nitrogen content. In fact, nitrogen deposition not only leads to increased soil total N content, but also changes in the NH₄⁺-N content, NO₃^--N content and pH, as well as changes in the heterogeneity of the four indexes. The soil indexes for these four factors, their heterogeneity and even the plant community might be routes through which nitrogen deposition alters the bacterial community. Here, we describe a 6-year nitrogen addition experiment conducted in a typical steppe ecosystem to investigate the ecological mechanism by which nitrogen deposition alters bacterial abundance, diversity and composition. We found that various characteristics of the bacterial community were explained by different environmental factors. Nitrogen deposition decreased bacterial abundance that is positively related to soil pH value. In addition, nitrogen addition decreased bacterial diversity, which is negatively related to soil total N content and positively related to soil NO₃^--N heterogeneity. Finally, nitrogen addition altered bacterial composition that is significantly related to soil NH₄⁺-N content. Although nitrogen deposition significantly altered plant biomass, diversity and composition, these characteristics of plant community did not have a significant impact on processes of nitrogen deposition that led to alterations in bacterial abundance, diversity and composition. Therefore, more sensitive molecular technologies should be adopted to detect the subtle shifts of microbial community structure induced by the changes of plant community upon nitrogen deposition.     

氮对酵母菌-SBR系统效能及酵母形态的影响研究

在酵母菌-SBR系统处理高含油废水中研究了氮添加对酵母细胞形态、沉降性、废水处理效果的影响及恢复能力.结果表明,氮添加量直接影响到系统中酵母菌的生物量,沉降性、pH和处理效果;氮缺乏诱发某些酵母菌菌株细胞由酵母形态向真菌丝形态转化,进而影响到酵母菌的沉降性;从系统运行效果和稳定性方面综合考虑,运行时最佳的进水BOD/N为20/1;恢复最佳氮添加能提高不同程度缺氮系统的处理效果,并可使轻度菌丝化系统快速恢复酵母形态为主,但在短期内对高度菌丝化系统的恢复效果不明显.