异波折板水解酸化-A~2O一体化反应器实验研究

设计了异波折板水解酸化-A2O一体化反应器,进行生活污水处理的实验研究。10个月的实验结果表明,系统的最佳水力停留时间(HRT)为8 h时,最适COD进水浓度为240~600 mg/L,最佳混合液回流比(r)-污泥回流比(R)为250%~100%。控制反应器于以上运行参数下,25±2℃所对应的COD、TN和TP去除率分别为96.84%、67.55%和81.92%。当温度降至7℃时,其COD、TP和TN分别降至86.35%、50.25%和65.68%。基于实验分析结果,阐明了一体化反应器高效性的机理在于异波折板水解酸化段具有高效传质特性和A2O段具有复合式活性污泥-接触氧化好氧池的特点。     

Effect of MoO3 on vanadium based catalysts for the selective catalytic reduction of NOx with NH3 at low temperature

The selective catalytic reduction(SCR) activities of the MoO_3 doped V/WTi catalysts prepared by the incipient wetness impregnation method at low temperature were investigated.The results showed that the addition of MoO_3 could enhance the NO_ xconversion at low temperature and the best SCR activity was obtained when the dosage of MoO_3 reached5 wt.%. The NH3-TPD and DRIFTS experiments indicated that the addition of MoO_3 changed the type and number of acid sites on the surface of catalysts and reaction activities of acid sites were altered at the same time. The redox capacity and amount of active oxygen species got improved for V3Mo5/WTi catalyst, which could be confirmed by the H_2-TPR and transient response experiments. Water vapor inhibited the NO_xconversion at low temperature. Deposition of ammonium sulfate or bisulfate might be main reason for the loss of catalytic activity in the presence of SO_2 at low temperature. Choosing the suitable NH_3/NO ratio and elevation of reaction temperature both could weaken the influence of SO_2 on the SCR activity of the V3Mo5/WTi catalyst. Thermal treatment of the deactivated catalyst at350°C could get the low temperature activity recovered. The decrease of GHSV improved the de NO_x efficiency at low temperature and we speculated that the rational technological process and operation parameters could contribute to the application of this kind of catalysts in real industrial environment.     

A2O工艺好氧末段溶解氧变化对脱氮除磷影响

采用连续流A2O工艺处理实际的生活污水,研究好氧末段在不同溶解氧(DO)浓度条件下对污泥沉降性能、系统脱氮除磷的影响,同时考察了DO对污泥硝化活性、厌氧释磷速率和反硝化脱氮速率的影响.结果表明,随着末段溶解氧的提高,污泥容积指数SVI从140降至100左右,后又升高到120～170;系统的硝化效果提高,氨氮的去除率从6...     

Isotope tracing of submarine groundwater discharge offshore Ubatuba, Brazil: results of the IAEA–UNESCO SGD project

Results of groundwater and seawater analyses for radioactive (³H, ²²²Rn, ²²³Ra, ²²⁴Ra, ²²⁶Ra, and ²²⁸Ra) and stable (D and ¹⁸O) isotopes are presented together with in situ spatial mapping and time series ²²²Rn measurements in seawater, direct seepage measurements using manual and automated seepage meters, pore water investigations using different tracers and piezometric techniques, and geoelectric surveys probing the coast. This study represents first time that such a new complex arsenal of radioactive and non-radioactive tracer techniques and geophysical methods have been used for simultaneous submarine groundwater discharge (SGD) investigations. Large fluctuations of SGD fluxes were observed at sites situated only a few meters apart (from 0 cm d⁻¹ to 360 cm d⁻¹; the unit represents cm³/cm²/day), as well as during a few hours (from 0 cm d⁻¹ to 110 cm d⁻¹), strongly depending on the tidal fluctuations. The average SGD flux estimated from continuous ²²²Rn measurements is 17 ± 10 cm d⁻¹. Integrated coastal SGD flux estimated for the Ubatuba coast using radium isotopes is about 7 × 10³ m³ d⁻¹ per km of the coast. The isotopic composition (δD and δ¹⁸O) of submarine waters was characterised by significant variability and heavy isotope enrichment, indicating that the contribution of groundwater in submarine waters varied from a small percentage to 20%. However, this contribution with increasing offshore distance became negligible. Automated seepage meters and time series measurements of ²²²Rn activity concentration showed a negative correlation between the SGD rates and tidal stage. This is likely caused by sea level changes as tidal effects induce variations of hydraulic gradients. The geoelectric probing and piezometric measurements contributed to better understanding of the spatial distribution of different water masses present along the coast. The radium isotope data showed scattered distributions with offshore distance, which imply that seawater in a complex coast with many small bays and islands was influenced by local currents and groundwater/seawater mixing. This has also been confirmed by a relatively short residence time of 1–2 weeks for water within 25 km offshore, as obtained by short-lived radium isotopes. The irregular distribution of SGD seen at Ubatuba is a characteristic of fractured rock aquifers, fed by coastal groundwater and recirculated seawater with small admixtures of groundwater, which is of potential environmental concern and has implications on the management of freshwater resources in the region.     

凤眼莲根系分泌物对栅藻结构及代谢的影响

研究了凤眼莲（Ｅｉｃｈｈｏｒｎｉａ ｃｒａｓｓｉｐｅｓ）根系分泌物对栅藻（Ｓｃｅｎｅｄｅｓｍｕｓ ａｒｃｕａｔｕｓ Ｌｅｍｍ）超微结构及生长代谢的影响，结果显示，凤眼莲对栅藻有明显的克生作用，藻的数量逐步减少，栅藻生长受影响后，细胞中绿体片层肿用甚至解体，线粒体嵴消失，质膜、核膜受破坏，光合放氧化速度明显下降，可溶性蛋白折含量四天后４线下降，超氧阴离子（Ｏ２－）、丙二醛（ＭＤＡ）的含量上升，知值都     

厌氧水解酸化-好氧氧化A1/A2/O工艺剩余污泥减量

在碱减量印染废水A₁/A₂/O生物处理系统,通过污泥回流、把剩余污泥回流到A₁段,利用A段污泥的水解、酸化和O段微生物的好氧氧化作用可有效实现对回流剩余污泥的减量,同时O段好氧污泥的表观产率系数下降,系统产生的剩余污泥量减少.厌氧水解酸化-好氧氧化A₁/A₂/O工艺实现污泥减量由3段共同完成:A₁段实现回流剩余污泥的“液化”和惰性化;A₂段对系统污泥减量起到了强化作用;而O段微生物的合成作用在逐渐减弱.6个月连续运行的动态试验表明,在A₁段的容积负荷(COD_Cr)为2.54 kg·(m³·d)^-1、水力停留时间为7.56h条件下,A₁段利用水解酸化作用对回流剩余污泥的减量达到67.87%,系统O段好氧污泥的表观产率系数也下降到试验初始时的45.5%.在A₁/A₂/O污泥减量系统中,各段污泥性状发生了变化,A₁段污泥[MLVSS/MLSS]值从试验开始时的0.718 2下降到0.592 2,A₂段污泥[MLVSS/MLSS]值从0.667 3下降到0.526 7,剩余污泥的减量是活性污泥逐渐惰性化过程,污泥的粒度分析也证明了这一点.     

菜地氨氧化微生物驱动的N2O和NO对有机无机肥配施的响应

氨氧化细菌（AOB）和氨氧化古菌（AOA）是驱动土壤氨氧化过程的"引擎".氨氧化过程在土壤氧化亚氮（N₂O）和一氧化氮（NO）排放过程中扮演着重要角色.有机无机肥配施是实现化肥零增长和作物稳产增产的重要途径，但在有机无机肥配施下，菜地土壤AOB和AOA对氨氧化过程的相对贡献仍不清楚.本研究采用选择性抑制的方法（辛炔和乙炔）区分有机肥添加近3年后（2016年10月—2019年5月）AOB和AOA在氨氧化过程中对碱性菜地土壤N₂O和NO产生的相对贡献.试验共设5种施肥处理：不施氮肥（CK）、单施尿素（N）、单施有机肥（M）、50%尿素+50%有机肥（M1N1）和80%尿素+20%有机肥（M1N4）.结果表明，有机无机肥配施（M1N1和M1N4）可显著增加土壤电导率、有机碳和全氮含量.培养试验发现，与N处理相比，M和M1N1处理分别使N₂O排放量增加100.7%和38.8%，NO排放量增加77.9%和42.8%，AOB基因丰度增加16.6%和10.2%，同时，AOB对N₂O排放的相对贡献增加6.5%.相反，M1N4处理分别使N₂O和NO排放量降低19.3%和4.8%，AOB基因丰度降低37.5%，同时，AOB对N₂O及NO排放的相对贡献分别降低7.8%和7.4%.相关分析表明，土壤N₂O和NO累积排放量与土壤AOB基因丰度呈显著正相关（p<0.05），与土壤AOA基因丰度无显著相关性.有机无机肥配施下AOB是氨氧化过程的主要驱动者，适当比例的有机无机肥配施（即M1N4）措施可在一定程度上减弱AOB对碱性菜地土壤N₂O及NO排放的相对贡献.     

植被收割对滨海湿地沉积物中CO_2和N_2O释放的影响

为了揭示冬季滨海湿地植被收割对其沉积物中温室气体释放的影响,以长江入海口典型滨海湿地——崇明东滩为研究对象,观测季节性(冬季)植被收割(分别于收割后第0天、第10天、第30天、第60天采样)与不收割条件下芦苇(Phragmites australis)、米草(Spartina alterniflora)、芦苇-米草交互带和光滩沉积物中CO2与N2O的释放特征.结果表明:1米草和芦苇-米草交互带植被收割并未增加沉积物中CO2的释放(P0.05),但芦苇收割可能会增加N2O的释放(P0.05),说明植被收割对湿地沉积物中CO2和N2O释放的影响与植被类型密切相关.2与芦苇带相比,米草和芦苇-米草交互带沉积物中CO2累积释放量分别高出12%~57%和17%~43%,但芦苇植被覆盖下沉积物中N2O累积释放量分别比二者高出11%~81%和8%~95%.可见,米草和芦苇-米草交互带沉积物碳的呼吸损失明显高于芦苇带,但芦苇植被覆盖下沉积物中N2O逸失量相对较高.34种植被类型下,沉积物中N2O累积释放量为0.1~0.4 mg/kg,CO2累积释放量则高达1 024~2 645 mg/kg.因此,冬季滨海湿地植被收割不会显著增加N2O的温室效应,但选择性收割米草有望减少沉积物碳的呼吸损失.     

A2O工艺处理生活污水短程硝化反硝化的研究

在常温条件下,采用A2O工艺处理低C/N比实际生活污水,通过控制好氧区DO为0.3~0.5mg/L以及增大系统内回流比以降低好氧实际水力停留时间(AHRT),成功启动并维持了短程硝化反硝化;系统亚硝态氮积累率稳定维持在90%左右.在C/N比仅为2.34的情况下,短程硝化系统对总氮(TN)的去除率高达75.4%.通过对不同碳源类型、不同硝化类型以及不同DO水平下A2O系统脱氮效率的比较研究发现,低氧短程硝化反硝化阶段与外加碳源的全程硝化反硝化阶段的TN去除率相当.同时研究表明,低DO运行并不会导致A2O工艺发生污泥膨胀.当接种污泥为膨胀污泥时,控制DO在0.3~0.5mg/L反而有助于改善污泥沉降性能和出水水质.     

V2O5/CeO2催化剂用于低温NH3-SCR的性能研究

采用浸渍法制备了系列V2O5/CeO2催化剂,用于低温NH3选择性催化还原(NH3-SCR)NO.同时,考察了催化剂中V2O5负载量和煅烧温度对催化活性的影响,并运用SEM,BET和XRD物理化学技术对催化剂进行了表征.结果表明,V2O5/CeO2催化剂对模拟烟气中的NO转化呈现出较高的活性,但是V2O5负载量和催化剂的催化活性并不呈线性递增的关系.当V2O5负载量超过10%时,催化剂的催化活性开始下降.随着煅烧温度的升高,由于钒酸铈的生成,催化剂的催化活性下降.400℃为最佳煅烧温度.