高氨氮废水半短程硝化控制及曝气经济性运行优化

本研究进水模拟了污泥消化液、晚期垃圾渗滤液等高氨氮低碱度低碳氮比的废水,在碱度缺乏（不足以实现完全短程硝化）条件下获得了稳定的半短程硝化,并通过曝气量和污泥浓度（MLSS）双因素调控,实现了半短程硝化的高效经济运行.研究表明,进水碱度缺乏条件下短程硝化体系出水亚硝氮/氨氮浓度比值y与进水HCO₃^-∶NH₄⁺物质的量的比x之间存在化学计量关系 y=x/（2-x）,当进水HCO₃^-∶NH₄⁺物质的量的比为1,即进水碱度/氨氮浓度（mg·L^-1）比值为3.6时可实现半短程硝化,并通过游离氨（FA）和游离亚硝酸（FNA）联合抑制能够实现稳态运行,亚硝酸盐积累率平均可达95%以上.实验探究了MLSS和曝气量对短程硝化反应器曝气经济性和氨氧化率的影响,通过平衡两因素作用,在保证处理效果的同时最大程度提升了反应系统的曝气经济性：当曝气量为36 L·h^-1和MLSS为2243 mg·L^-1时,反应器的曝气经济性较好,可节省约40%曝气量,且能维持较高的容积氨氮负荷（0.93 kg·m^-3·d^-1）.     

改进型Orbal氧化沟在污水处理厂的应用

介绍了江山市鹿溪污水处理厂的设计概况和特色。工程一期处理规模为4.0万m3/d。采用"微孔曝气+推流器"的方式,充氧调节幅度为45%～100%,同时设计水深增加到5.5m,有效减少氧化沟的占地面积,节约运行费用。污水厂进水的主要污染指标为COD和NH3-N,主要处理工艺为改进型Orbal氧化沟。此外为了适应雨季的水量冲击,系统采用灵活的进水方式,雨季污水直接进入中沟,在保证出水达标的同时,减少了污泥流失。两年多的运行结果表明,该工艺具有良好的环境和经济效益。     

控制氧化对湿法烟气脱硫过程的影响研究

在喷射鼓泡反应器上进行了控制氧化对湿法烟气脱硫过程的影响研究,测定了脱硫率η和pH随时间t的变化规律,得出了η与t的回归式及η与pH值的关系规律,讨论了不同曝气强度及抑制剂浓度对CaCO3利用率α、pH值及脱硫率η的影响。实验表明强制氧化及抑制氧化均能提高脱硫效率η及CaCO3利用率α,但对浆液pH值的影响正好相反,强制氧化使浆液pH值下降的更快,而抑制氧化则使浆液pH值有所提高。     

昆船污水处理站微孔曝气池的启动研究

昆明船舶公司生活区污水处理站采用改进型的A2/O工艺,直接利用其生活污水培养污泥,并随时观察和分析工艺中的微孔曝气池运行状况。结果表明:采用自然培菌的方法,通过近3个半月的污泥培养,顺利实现微孔曝气池的启动。其中,COD、NH3-N的去除变化反映了曝气池启动的进程,至曝气池启动结束,COD和NH3-N的去除率分别达到了78.4%、75.7%。     

Performance of completely autotrophic nitrogen removal over nitrite process under different aeration modes and dissolved oxygen

In this study, three sequential batch biofilm reactors (SBBRs) were operated for 155 days to evaluate the performance of completely autotrophic nitrogen removal over nitrite (CANON) process under different aeration modes and dissolved oxygen (DO). Synthetic wastewater with 160-mg NH4 ⁺-N/L was fed into the reactors. In the continuously-aerated reactor, the efficiency of the ammonium nitrogen conversion and total nitrogen (TN) removal reached 80% and 70%, respectively, with DO between 0.8–1.0 mg/L. Whereas in the intermittently-aerated reactor, at the aeration/non-aeration ratio of 1.0, ammonium was always under the detection limit and 86% of TN was removed with DO between 2.0–2.5 mg/L during the aeration time. Results show that CANON could be achieved in both continuous and intermittent aeration pattern. However, to achieve the same nitrogen removal efficiency, the DO needed in the intermittently-aerated sequential batch biofilm reactor (SBBR) during the aeration period was higher than that in the continuously-aerated SBBR. In addition, the DO in the CANON system should be adjusted to the aeration mode, and low DO was not a prerequisite to CANON process.     

Household organic waste composting using bins with different types of passive aeration

The objective of this study was to study the performances of six 200-L polyethylene bins, each with different design for passive aeration to organic wastes composting. Food scraps and dry leaves (1.6 kg) were added to each bin once a day until the bin was full. Temperatures at the middle portion were measured daily. The compost from each bin was taken once a week for 120 days for analysis of C, N, volatile solids, and a germination index once a week for 120 days. After 120 days, the compost sample from each bin was taken to determine the mass reduction, size distribution, CEC, N, P and K values. The results showed that the temperatures inside the bins were in the ranges of 24 °C-57 °C. The composts in all bins were found to be stable at around 56-91 days. The wastes decayed fastest in bins with lateral and vertical systems of natural ventilation. It took about two months to stabilize the organic wastes, with a 59-62% decrease of mass. The C/N ratio, CEC, N, P, and K values of the final composts were 14.8-16.0, 66-68 cmol/kg, and 1.26-1.50% N, 0.52-0.56% P₂O₅ and 1.66-1.92% K₂O, respectively.     

提高水中BOD5测定质量的探讨

介绍了环境空气质量、分析用水、接种液加入量、曝气方法的选择等因素对BOD5测定的影响。提出测定过程中实验室空气质量、分析用水的选择、接种液的选择和加入量以及曝气方法应注意事项,以期得到较为准确的测定结果,提高废水中BOD5测定质量。     

Integrating soil carbon cycling with that of nitrogen and phosphorus in the watershed model SWAT: Theory and model testing

In this paper we describe and test a sub-model that integrates the cycling of carbon (C), nitrogen (N) and phosphorus (P) in the Soil Water Assessment Tool (SWAT) watershed model. The core of the sub-model is a multi-layer, one-pool soil organic carbon (S_C) algorithm, in which the decomposition rate of S_C and input rate to S_C (through decomposition and humification of residues) depend on the current size of S_C. The organic N and P fluxes are coupled to that of C and depend on the available mineral N and P, and the C:N and N:P ratios of the decomposing pools. Tillage explicitly affects the soil organic matter turnover rate through tool-specific coefficients. Unlike most models, the turnover of soil organic matter does not follow first order kinetics. Each soil layer has a specific maximum capacity to accumulate C or C saturation (S_x) that depends on texture and controls the turnover rate. It is shown in an analytical solution that S_x is a parameter with major influence in the model C dynamics. Testing with a 65-yr data set from the dryland wheat growing region in Oregon shows that the model adequately simulates the S_C dynamics in the topsoil (top 0.3 m) for three different treatments. Three key model parameters, the optimal decomposition and humification rates and a factor controlling the effect of soil moisture and temperature on the decomposition rate, showed low uncertainty as determined by generalized likelihood uncertainty estimation. Nonetheless, the parameter set that provided accurate simulations in the topsoil tended to overestimate S_C in the subsoil, suggesting that a mechanism that expresses at depth might not be represented in the current sub-model structure. The explicit integration of C, N, and P fluxes allows for a more cohesive simulation of nutrient cycling in the SWAT model. The sub-model has to be tested in forestland and rangeland in addition to agricultural land, and in diverse soils with extreme properties such high or low pH, an organic horizon, or volcanic soils.     

曝气复氧对底泥氮素生物地球化学循环影响的作用机制研究

通过分析底泥氮污染物释放规律和转化过程,以及底泥生境、氮形态变化和氮循环功能微生物群落结构变化的规律,探讨了不同曝气复氧条件影响底泥氮生物地球化学循环的生物代谢、物理化学联合作用的机制。结果表明：曝气复氧对底泥中氮的生物地球化学循环影响是一个包括微生物代谢作用和物理化学作用的复杂联合作用过程。水体好氧环境的改变主要引起参与底泥氮循环的硝化、亚硝化和反硝化功能菌群群落结构的演变,对异养菌和氨化菌的影响不大,证明环境好氧条件的改变对底泥有机质生物分解产生氨氮的微生物代谢过程影响不大,主要对底泥释放的氨氮硝化、反硝化等生物转化过程产生大的影响。不同溶解氧条件下,底泥释放的氮素在微生物作用下主要以NH4＋-N和NO3--N的形式进入试验体系,并在特定的氧化还原电位（临界值-200 mV）和pH（临界值6.70）条件下通过物理化学作用在底泥中以离子交换态氮（IEF-N）、碳酸盐结合态氮（CF-N）、铁锰氧化态氮（IMOF-N）及有机态和硫化物结合态氮（OSF-N）等不同形态氮相互转化,同时,在氮的转化和循环过程中部分输入上覆水体。在低溶解氧组实验条件下[ρ（DO）〈0.5 mg.L-1],底泥向水体输出氮总量为底泥可转化态氮的19.7%,主要为氨氮,最大释放速率达到289.13 mg.m-2.d-1,释放的质量浓度可达到18.8 mg.L-1;好氧条件下（DO饱和）,底泥向水体输出氮总量为底泥可转化态氮的1.8%;好氧-缺氧条件下为11.7%,主要以N2的形式释出系统。     

射流曝气MBR处理啤酒废水的试验

射流曝气提高了系统的氧利用效率及传质效率.通过逐渐提高进水的容积负荷来考察系统的处理效果, 试验表明, 利用射流曝气MBR处理模拟啤酒废水是可行的, 系统对COD、氨氮、浊度平均去除率为95.74%,97.84%,99.5%.由于系统运行期间不排泥, 因此系统对P O43-的去除效果不佳, 平均去除率为42.9%.膜对...