Effect of Cu loading content on the catalytic performance of Cu-USY catalysts for selective catalytic reduction of NO with NH3

Series of Cu-USY zeolite catalyst with different Cu loading content were synthesized through simple impregnation method. The obtained catalysts were subjected to selective catalytic reduction of NO_x with NH₃ (NH₃-SCR) performance evaluation, structural/chemical characterizations such as X-ray diffraction (XRD), N₂ adsorption/desorption, H₂ temperature-programmed reduction (H₂-TPR), NH₃ temperature-programmed desorption (NH₃-TPD) as well as detailed in situ diffuse reflectance infrared Fourier transform spectroscopy (DRIFTS) experiments including CO adsorption, NH₃ adsorption and NO+O₂ in situ reactions. Results show that Cu-USY with proper Cu loading (in this work 5Cu-USY with 5 wt.% Cu) could be promising candidates with highly efficient NH₃-SCR catalytic performance, relatively low byproduct formation and excellent hydrothermal stability, although its SO₂ poisoning tolerability needs alleviation. Further characterizations reveal that such catalytic advantages can be attributed to both active cu species and surface acid centers evolution modulated by Cu loading. On one hand, Cu species in the super cages of zeolites increases with higher Cu content and being more conducive for NH₃-SCR reactivity. On the other hand, higher Cu loading leads to depletion of Brønsted acid centers and simultaneous formation of abundant Lewis acid centers, which facilitates NH₄NO₃ reduction via NH₃ adsorbed on Lewis acid centers, thus improving SCR reactivity. However, Cu over-introduction leads to formation of surface highly dispersed CuO_x, causing unfavorable NH₃ oxidation and inferior N₂ selectivity.     

Effects of WOx modification on the activity, adsorption and redox properties of CeO2 catalyst for NOx reduction with ammonia

A series of WO₃/CeO₂ (WOx/CeO₂) catalysts were synthesized by wet impregnation of ammonium metatungstate on a CeO₂ support. The resulting solid acid catalysts were characterized by X-ray diffraction (XRD), UV-Vis spectroscopy (UV-Vis), Raman spectroscopy (Raman), in-situ Fourier transform infrared spectroscopy (in-situ FT-IR) of ammonia adsorption, NH₃-TPD, H₂ temperature-programmed reduction (H₂-TPR), NH₃/NO oxidation and activity measurements for NOx reduction by NH₃ (NH₃-SCR). The results show that polytungstate (WOx) species are the main species of tungsten oxide on the surface of ceria. The addition of tungsten oxide enhances the Brönsted acidity of ceria catalysts remarkably and decreases the amount of surface oxygen on ceria, with strong interaction between CeO₂ and WOx. As a result, the N₂ selectivity of NH₃ oxidation and NH₃-SCR at high temperatures (> 300℃) is enhanced. Therefore, a wide working temperature window in which NOx conversion exceeds 80% (NOx conversion > 80%) from 200 to 450℃, is achieved over 10 wt.% WOx/CeO₂ catalyst. A tentative model of the NH₃-SCR reaction route on WOx/CeO₂ catalysts is presented.     

凤眼莲对富营养化水体硝化、反硝化脱氮释放N2O的影响

以往有关大型水生漂浮植物消减富营养化水体氮(N)的研究主要侧重于植物对N的吸收效果,而忽略了硝化、反硝化反应途径对水体脱氮的贡献.基于此,本研究中借助具创新性的收集凤眼莲种植水体释放N₂O的装置和方法,通过模拟实验研究了凤眼莲对富营养化水体硝化、反硝化脱氮中间产物N₂O的影响.结果表明,凤眼莲可以促进富营养化水体的硝化、反硝化、成对硝化-反硝化反应过程,在本实验条件下凤眼莲种植水体在整个培养期内释放的N₂O气体浓度累积升高幅度较大,为453~4055 nL·L^-1(未加硝化抑制剂处理),通过释放N₂O而脱除氮素的量占整个水体N消减量的1.36%,为相应未种植凤眼莲水体的4.31倍.种植凤眼莲水体试验期间释放N₂O-N的量与水体氨态氮或硝态氮浓度的变化量均存在显著相关关系(p<0.05),说明N₂O释放量受到水体中NH₄⁺、NO₃^-浓度变化的影响.种植凤眼莲在实验中后期可以增加水体中硝化、反硝化细菌的数量,但其数量远低于凤眼莲根系附着的硝化反硝化细菌.水体中反硝化细菌数量与水体释放N₂O浓度之间并无显著相关性,说明种植凤眼莲水体反硝化脱氮释放N₂O过程可能主要是由根系共生微生物驱动的.     

Fluxes of nitric and nitrous oxides from agricultural soils in a cool temperate climate

Fluxes of NO and N₂O from sandy loam soils cropped with winter wheat and a clay loam soil under ryegrass, with and without the addition of NH₄NO₃ fertilizer, were measured using static and dynamic chamber methods. Nitric oxide fluxes ranged from −0.3 (deposition) to 6.9 (emission) ng NO-N m⁻² s⁻¹. The corresponding N₂O flux ranged from 0 to 91 (emission) ng N₂O-N m⁻² s⁻¹. The NO flux was temperature dependent. Activation energies ranged from 40 to 81 kJ mol⁻¹. Nitric oxide and N₂O fluxes increased linearly with soil available nitrogen (NH₄ + NO₃). Emissions of NO and N₂O were not detectable from unfertilized ryegrass plots. Instead, nitric oxide was absorbed by the soil and vegetation at a maximum rate of 0.31 ng NO-N m⁻² s⁻¹. The aeration state of the soil controlled the relative rates of NO and N₂O emission. Nitric oxide was the major gas emitted from well aerated soils, conditions that favour nitrification. The NO/N₂O emission ratio was >100 for the coarse-textured sandy loam soil and the clay loam soil only during low rainfall periods. Nitrous oxide was the major gas emitted from less aerated soils, conditions that allowed denitrification to occur. The NO/N₂O emission ratio was <0.001 for the clay loam soil when rainfall was high and soils were wet. Extrapolation to the U.K. situation showed that agricultural land may account for 2–6% of the total annual NO_x emission and for 16–64% of the total annual N₂O emission in the U.K.     

Effects of synthesis methods on catalytic activities of CoOx–TiO2 for low-temperature NH3-SCR of NO

A series of cobalt doped TiO_2(Co-TiO_2) and Co Oxloaded TiO_2(Co/TiO_2) catalysts prepared by sol–gel and impregnation methods respectively were investigated on selective catalytic reduction with NH_3(NH_3-SCR) of NO. It was found that Co-TiO_2 catalyst showed more preferable catalytic activity at low temperature range. From characterization results of XRD,TEM, Raman and FT-IR, Co species were proved to be doped into TiO_2 lattice by replaced Ti atoms. After being characterized and analyzed by NH_3-TPD, PL, XPS, EPR and DRIFTS, it was found that the better NH_3-SCR activities of Co-TiO_2 catalysts, compared with Co/TiO_2 catalyst, were ascribed to the formation of more oxygen vacancies which further promoted the production of more superoxide ions(O-2). The superoxide ions were crucial for the formation of low temperature SCR reaction intermediates(NO-3) by reacting with adsorbed NO molecule. Therefore, these aspects were responsible for the higher low temperature NH_3-SCR activity of Co-TiO_2 catalysts.     

卫河新乡市区段春季溶解CH4与N2O浓度特征

对卫河新乡市区段春季CH_4与N_2O浓度进行调查分析,初步探讨了城市河流中典型温室气体的溶存量空间变化及其影响因素.结果表明,受到水中污染物质浓度及人类活动影响,春季卫河表层水中CH_4与N_2O浓度处于超饱和状态,饱和度分别为147.59~2 667.85和4.06~188.25.影响市区内N_2O浓度的主要环境因素为NH~+_4-N(P0.01),而新区污水处理厂排水输入显著提高了N_2O的溶存量,说明污染物类型影响温室气体的产生和积累,NH~+_4-N的硝化过程是城市河流N_2O产生的主要来源.逐步回归分析表明CH_4浓度是NH~+_4-N浓度与水温的相关函数,其中CH_4浓度与NH~+_4-N极显著相关(R2=0.70,P0.01),说明春季卫河中NH~+_4-N浓度是影响卫河春季CH_4溶存的关键因素.此外研究结果显示在NO~-_3-N浓度较低并且NH~+_4-N浓度高时水中CH_4与N_2O浓度具有显著正相关关系,表明有效态氮浓度差异影响CH_4与N_2O产生过程的耦合机制.     

稻田气溶胶NH3和气体NOx排放在线测定研究

气溶胶NH3和气体NOx是大气颗粒物和降水的主要成分,是形成气溶胶的关键物种.田间集约化氮肥施用是气溶胶NH3和气体NOx的一个重要来源,目前该领域的研究鲜有报道.2010年5月～2010年10月,在线监测了稻田施用尿素后气溶胶NH3和气体NOx的排放情况.监测系统的时间分辨率设置为1 h.在4次稻田施肥试验中,施肥后对气溶胶NH3排放和相应的气象因子连续采样20 d.在第4次施肥试验中,施肥后连续采样47 d,进而研究气体NOx的排放规律及其与气象因子的关系.结果表明,气溶胶NH3的排放因子分别为2.6%、5.5%、4.0%和1.6%,相应的排放通量分别为3.97、2.08、1.52和1.22 kg·hm-2.温度(空气温度和土壤温度)是影响稻田施肥气溶胶NH3排放的主要因子,而空气湿度和土壤水分对其排放的影响却不明确.通过分析监测数据可知,稻田施肥后NO2-N排放量与NO-N排放量的比值为9/4,气体NOx的排放因子和排放通量分别为0.14%和0.30 kg·hm-2.气象因子与气体NOx排放通量的关系也进行了初步探讨.     

Nitrous oxide emissions from black soils with different pH

N₂O fluxes as a function of incubation time from soil with different available N contents and pH were determined. Cumulative carbon dioxide (CO₂) emissions were measured to indicate soil respiration. A 144-hr incubation experiment was conducted in a slightly acidic agricultural soil (pH_H2O 5.33) after the pH was adjusted to four different values (3.65, 5.00, 6.90 and 8.55). The experiments consisted of a control without added N, and with NH₄⁺-N and NO₃^--N fertilization. The results showed that soil pH contributed significantly to N₂O flux from the soils. There were higher N₂O emissions in the period 0-12 hr in the four pH treatments, especially those enhanced with N-fertilization. The cumulative N₂O-N emission reached a maximum at pH 8.55 and was stimulated by NO₃^--N fertilization (70.4 μg/kg). The minimum emissions appeared at pH 3.65 and were not stimulated by NO₃^--N or NH₄⁺-N fertilization. Soil respiration increased significantly due to N-fertilization. Soil respiration increased positively with soil pH (R² = 0.98, P < 0.01). The lowest CO₂-C emission (30.2 mg/kg) was presented in pH 3.65 soils without N-fertilization. The highest CO₂-C emissions appeared in the pH 8.55 soils for NH₄⁺-N fertilization (199 mg/kg). These findings suggested that N₂O emissions and soil respiration were significantly influenced by low pH, which strongly inhibits soil microbial nitrification and denitrification activities. The content of NO₃^--N in soil significantly and positively affected the N₂O emissions through denitrification.     

Structures and catalytic performances of Me/SAPO-34 (Me = Mn, Ni, Co) catalysts for low-tem perature SCR of NOx by ammonia

Me/SAPO-34 (Me = Mn, Ni, Co) series of catalysts were prepared by a wetness impregnation method and investigated for the selective catalytic reduction of nitrogen oxides with ammonia (NH₃-SCR). Among them, Mn/SAPO-34 catalyst was found as the most promising candidate based on its superior low-temperature activity. The catalysts were characterized by X-ray diffraction (XRD), transmission electron microscopy images (TEM), nuclear magnetic resonance (NMR), X-ray photoelectron spectroscopy (XPS), temperature programmed reduction and desorption (TPR and TPD), and diffuse reflectance infrared Fourier transformed spectroscopy (DRIFTS) of NH₃/NO_x adsorption. Mn/SAPO-34 is obviously different from Ni/SAPO-34 and Co/SAPO-34 in the active species state and distribution. Surface MnO_x species which play an essential role in NO oxidation and NO₂ adsorption, act as better active sites than nickel and cobalt mostly in the form of the aluminates and silicates.     

Observations of N2O5 and NO3 at a suburban environment in Yangtze river delta in China: Estimating heterogeneous N2O5 uptake coefficients

The nitrate radical (NO₃) and dinitrogen pentoxide (N₂O₅) play an important role in the nocturnal atmosphere chemistry. Observations of NO₃ radicals and N₂O₅ were performed in a semirural ground site at Tai'Zhou in polluted southern China using cavity ring down spectroscopy (CRDS) from 23 May to 15 June 2018. The observed NO₃ and N₂O₅ concentrations were relatively low, with 1 min average value of 4.4 ± 2.2 and 26.0 ± 35.7 pptV, respectively. The N₂O₅ uptake coefficient was determined to be from 0.027 to 0.107 based on steady state lifetime method. Fast N₂O₅ hydrolysis was the largest contributor to the loss of NO₃ and contributed to substantial nitrate formation, with an average value of 14.83 ± 6.01 µg/m³. Further analysis shows that the N₂O₅ heterogeneous reactions dominated the nocturnal NO_x loss and the nocturnal NO_x loss rate is 0.14 ± 0.02 over this region.     

海峡西岸经济区大气污染物排放清单的初步估算

以2009年为基准年,结合污染源普查数据、统计年鉴及工业活动、居民生活等多个方面对海峡西岸经济区包括SO2、NOx、PM2.5、VOCs和NH3在内的大气污染物的排放量进行了估算,建立了海西区大气污染物排放清单.结果发现,上述5类污染物基准年的排放量分别为40.67×104、55.84×104、50.57×104、152.26×104和26.18×104t.其中,SO2、NOx及PM2.5的排放主要来自电厂,占排放总量的比例分别为25.58%、34.89%和38.75%;VOCs和NH3的主要排放源分别来自植被排放和养殖业,其贡献量分别为49.12%和47.07%.采用GIS对排放清单进行网格化处理,得出SO2、NOx及PM2.5的高排放强度区域与固定源的空间分布较为一致.此外,结合国家和地方"十二五"发展规划,采用情景分析方法估算了2015年海西区大气污染物的排放清单.与基准年相比,SO2、NOx和NH3的排放量呈下降趋势,PM2.5和VOCs的排放量呈大幅度增加.基准年排放清单的不确定性分析显示,VOCs排放估算的不确定度最大,为225%.     

Investigation of the common intermediates over Fe-ZSM-5 in NH3-SCR reaction at low temperature by in situ DRIFTS

The surface species formed in the reaction of NO and NO₂ with pre-adsorbed NH₃ over a Fe-ZSM-5 catalyst (1.27 wt.% Fe, SiO₂/Al₂O₃ = 25) at low temperature (140°C) were studied by in situ diffuse reflectance infrared Fourier transform spectroscopy (DRIFTS). Through using a background spectrum of NH₃-saturated Fe-ZSM-5, we clearly observed the formation of common intermediates resulting from the reaction of NO₂ or NO + O₂ with pre-adsorbed NH₃. This presents strong evidence that the oxidation of NO to form surface nitrates and nitrites is the key step for standard SCR at low temperature. In addition, the results suggest that in the SCR reaction at low temperature, the NH₄⁺ ions absorbed on Brønsted acid sites are less active than NH₃ adsorbed on Lewis acid sites related to Fe species.     

内蒙古温带草原氮沉降的观测研究

在内蒙古太仆寺旗对温带草原地区的氮沉降进行了为期1 a(2011年11月～2012年10月)的观测.在线分析大气NH3和NO2浓度,用CMAQ模型计算的干沉降速率计算了气体干沉降量;采集降水、降尘和穿透雨样品并测定NH4+和NO3-浓度,分别得到湿沉降、颗粒物干沉降和穿透雨沉降量.观测结果表明该地区的氮沉降量已经高达3.43 g.(m2.a)-1,有可能对草原生态系统产生危害.其中,湿沉降占44%,气体干沉降占38%,颗粒物干沉降占18%.干沉降对氮沉降的贡献大于湿沉降,必需重视干沉降的测定,而穿透雨沉降明显小于总沉降,说明穿透雨法不适合于草原地区.从组分上看,还原态氮(包括NH4+和NH3)对氮沉降的贡献为71%,而氧化态氮(NO3-和NO2)的贡献仅29%,因此在控制氮沉降时,不应只针对NOx排放进行削减,NH3减排同样重要.     

Numerical evaluation of the effectiveness of NO2 and N2O5 generation during the NO ozonation process

Wet scrubbing combined with ozone oxidation has become a promising technology for simultaneous removal of SO₂ and NO_x in exhaust gas. In this paper, a new 20-species, 76-step detailed kinetic mechanism was proposed between O₃ and NO_x. The concentration of N₂O₅ was measured using an in-situ IR spectrometer. The numerical evaluation results kept good pace with both the public experiment results and our experiment results. Key reaction parameters for the generation of NO₂ and N₂O₅ during the NO ozonation process were investigated by a numerical simulation method. The effect of temperature on producing NO₂ was found to be negligible. To produce NO₂, the optimal residence time was 1.25 sec and the molar ratio of O₃/NO about 1. For the generation of N₂O₅, the residence time should be about 8 sec while the temperature of the exhaust gas should be strictly controlled and the molar ratio of O₃/NO about 1.75. This study provided detailed investigations on the reaction parameters of ozonation of NO_x by a numerical simulation method, and the results obtained should be helpful for the design and optimization of ozone oxidation combined with the wet flue gas desulfurization methods (WFGD) method for the removal of NO_x.     

Chemical and optical properties of aerosols and their interrelationship in winter in the megacity Shanghai of China

A field campaign on air quality was carried out in Shanghai in winter of 2012. The concentrations of NO, NO₂, NO_x, SO₂, CO, and PM_2.5 increased during haze formation. The average masses of SO₄^2-, NO₃^- and NH₄⁺ were 10.3, 11.7 and 6.7 μg/m³ during the haze episodes, which exceeded the average (9.2, 7.9, and 3.4 μg/m³) of these components in the non-haze days. The mean values for the aerosol scattering coefficient (b_sp), aerosol absorption coefficient (b_ap) and single scattering albedo (SSA) were 288.7, 27.7 and 0.91 Mm^-1, respectively. A bi-peak distribution was observed for the mass concentrations of CO, NO, NO₂, and NO_x. More sulfate was produced during daytime than that in the evening due to photochemical reactions. The mass concentration of NH₄⁺ achieved a small peak at noontime. NO₃^- showed lower concentrations in the afternoon and higher concentrations in the early morning. There were obvious bi-peak diurnal patterns for bsp and bap as well as SSA. bsp and bap showed a positive correlation with PM_2.5 mass concentration. (NH₄)₂SO₄, NH₄NO₃, organic mass, elemental carbon and coarse mass accounted for 21.7%, 19.3%, 31.0%, 9.3% and 12.3% of the total extinction coefficient during non-haze days, and 25.6%, 24.3%, 30.1%, 8.1% and 8.2% during hazy days. Organic matter was the largest contributor to light extinction. The contribution proportions of ammonium sulfate and ammonium nitrate to light extinction were significantly higher during the hazy time than during the non-haze days.     

不同SAPO分子筛负载MnOx催化剂的低温NH3-SCR性能研究

以磷酸硅铝分子筛SAPO-5、SAPO~(-1)1和SAPO-34为载体,采用乙醇分散法制备了用于低温氨选择性还原(NH_3-SCR)NO_x的分子筛负载MnO_x催化剂.活性测试结果显示,3种分子筛催化剂均展现出优良的NH_3-SCR活性,但三者在低温区间的SCR活性存在较明显差异,其SCR活性顺序如下:MnO_x/SAPO-34MnO_x/SAPO-5MnO_x/SAPO~(-1)1.借助XRD、N2吸附-脱附、XPS、H2-TPR、NH_3-TPD、NH_3FT-IR等技术对催化剂的表面活性物种及表面酸性等进行表征分析,结果表明,MnO_x主要以无定型状态分散于载体上,负载后载体的比表面积和孔体积均有所下降.XPS和H2-TPR分析证实,不同分子筛载体上MnO_x的表面浓度与氧化态明显不同.NH_3-TPD和NH_3FT-IR分析揭示了催化剂表面均存在Bronsted酸位和Lewis酸位,其中,Lewis酸性位对低温SCR反应起着关键作用.研究表明,催化剂的催化性能会因载体不同而存在差异,高Mn4+表面浓度和丰富的Lewis酸性位对催化剂在低温区间实现优良的催化活性尤为重要.     

Emissions of N2O and NH3, and nitrogen leaching from direct seeded rice under different tillage practices in central China

Tillage practices affect the fate of fertilizer nitrogen (N) through influencing transformations of N, but few studies have examined N₂O and NH₃ emissions, and N leaching from different rice tillage systems. Thus the objective of this study was to assess N₂O emission, NH₃ volatilization and N leaching from direct seeded rice in conventional tillage (CT) and no-tillage (NT) production systems in the subtropical region of China during the 2008 and 2009 rice growing seasons. Treatments were established following a split-plot design of a randomized complete block with tillage practices as the main plot and N fertilizer level as the sub-plot treatment, and there were four treatments: NT + no fertilizer (NT0), CT + no fertilizer (CT0), NT + compound fertilizer (NTC) and CT + compound fertilizer (CTC), respectively. Results showed that N fertilization significantly increased (p < 0.01) N₂O emissions, NH₃ volatilization and N leaching from rice fields in both years. In general, there was no significant difference in N₂O emissions and NH₃ volatilization between NT0 and CT0 in both years, while NTC had significantly higher (p < 0.05) N₂O emissions and NH₃ volatilization compared to CTC. Over the two rice growing seasons, NTC showed 32% and 47% higher N₂O emissions, and 29% and 52% higher NH₃ losses than CTC. Higher (p < 0.05) N₂O emissions from NTC than CTC were presumably due to higher soil organic C and greater denitrification. Total N and NO₃^? concentrations were higher (p < 0.05) in CTC than NTC, but larger volumes of percolation water in NTC than CTC resulted in no significant difference in leakage of total N and NO₃^?. Hence, application of N fertilizer in combination with NT appeared to be ineffective in reducing N losses from N fertilizer in paddy fields.     

Selective catalytic reduction of nitrogen oxides over a modified silicoaluminophosphate commercial zeolite

Nitrogen oxides(NO_x:NO,NO_2)are a concern due to their adverse health effects.Diesel engine transport sector is the major emitter of NO_x.The regulations have been strengthened and to comply with them,one of the two methods commonly used is the selective catalytic reduction of NO_xby NH_3(NH_3-SCR),NH_3being supplied by the in-situ hydrolysis of urea.Efficiency and durability of the catalyst for this process are highly required.Durability is evaluated by hydrothermal treatment of the catalysts at temperature above 800°C.In this study,very active catalysts for the NH_3-SCR of NO_xwere prepared by using a silicoaluminophosphate commercial zeolite as copper host structure.Characterizations by X-ray diffraction(XRD),scanning electron microscopy(SEM)and temperature programmed desorption of ammonia(NH_3-TPD)showed that this commercial zeolite was hydrothermally stable up to 850°C and,was able to retain some structural properties up to950°C.After hydrothermal treatment at 850°C,the NO_xreduction efficiency into NH_3-SCR depends on the copper content.The catalyst with a copper content of 1.25 wt.%was the most active.The difference in activity was much more important when using NO than the fast NO/NO_2reaction mixture.     

不同施肥方式下紫色土N2O与NOx的排放特征

利用紫色土长期施肥试验平台,采用静态箱-气相色谱法开展紫色土"冬小麦-夏玉米"轮作系统N_2O和NO_x排放的连续两周年(2014年11月~2016年9月)定位观测.研究了氮肥总量相同条件下的常规氮磷钾化肥(NPK)、猪厩肥(OM)、秸秆还田配施氮磷钾化肥(RSDNPK)、猪厩肥配施氮磷钾化肥(OMNPK)和氮磷钾化肥配合硝化抑制剂(DCDNPK)等施肥方式对N_2O和NO_x排放的影响,短期不施肥处理(CK)作为排放系数计算的对照.结果表明,所有施肥方式下紫色土N_2O排放峰均出现在施肥初期和大降雨过程期;NO_x排放过程与N_2O类似,排放峰出现在施肥初期,但强降雨期未出现明显排放峰.NPK、OM、RSDNPK、OMNPK和DCDNPK处理的N_2O年均累积排放量分别为:1.35、4.38、1.43、2.46、0.92 kg·hm~(-2),排放系数分别为:0.33%、1.41%、0.36%、0.73%、0.18%;相应处理的NO_x年均累积排放量分别为:0.11、0.38、0.10、0.27、0.04kg·hm~(-2),排放系数分别为:0.03%、0.13%、0.03%、0.09%、0.01%.较常规化肥,增加有机物料如施用猪厩肥和猪厩肥配施氮磷钾肥分别显著增加226%和83%的N_2O排放(P0.01),同时NO_x排放分别显著增加262%和157%(P0.01);常规化肥配合硝化抑制剂(DCDNPK)使用减少32%的N_2O排放和62%的NO_x排放(P0.01),秸秆还田配施氮磷钾肥对N_2O排放略有增加(P0.05),NO_x排放略有减少(P0.05).统计分析进一步表明,土壤无机氮含量是N_2O和NO_x二者排放的主控因子,而土壤孔隙充水率与温度分别作为N_2O与NO_x各自排放的主控因子之一.     

SBR双颗粒污泥系统脱氮除磷性能研究

以模拟废水为研究对象,对SBR双颗粒污泥系统的脱氮除磷性能进行了考察.试验结果表明,A₂N双颗粒污泥系统能使硝化菌和聚磷菌分别在各自最佳的环境中生长,有利于系统脱氮除磷的稳定和高效运行,可控制性也得到了提高.在COD为300 mg·L^-1条件下,系统对COD的平均去除率达到78.8%,大部分COD被聚磷菌用来合成PHA;当溶解氧控制在3.55~4.90 mg·L^-1和5.60~6.60 mg·L^-1之间时,硝化SBR对氨氮的去除率分别为87.0%和94.5%.除磷SBR仅设置缺氧段时,磷去除率为72%;增设后曝气段后,磷去除率增至85%.NO_x^--N(NO₂^--N+ NO₃^--N)的去除主要发生在缺氧段,在反硝化除磷时作为电子受体被去除,平均去除率为90.6%.