草甸草原模拟氮沉降抑制甲烷吸收、促进氧化亚氮排放

Few studies are conducted to quantify the effects of enhanced N deposition on soil nitrous oxide (N2O) emission and methane (CH4) uptake in the meadow steppe of Inner Mongolia,China.A two-year field experiment was conducted to assess the effects of nitrogen (N) deposition rates (0,10,and 20 kg N ha-1 year-1 as (NH4)2SO4) on soil N2O and CH4 fluxes.The seasonal and diurnal variations of soil N2O and CH4 fluxes were determined using the static chamber-gas chromatography method during the two growing seasons of 2008 and 2009.Soil temperature,moisture and mineral N (NH4+-N and NO3--N) concentration were simultaneously measured.Results showed that low level of (NH4)2SO4 (10 kg N ha-1 year-1) did not significantly affect soil CH4 and N2O fluxes and other variables.High level of (NH4)2SO4 (20 kg N ha-1 year-1) significantly increased soil NO3--N concentration by 24.1％ to 35.6％,decreased soil CH4 uptake by an average of 20.1％,and significantly promoted soil N2O emission by an average of 98.2％.Soil N2O emission responded more strongly to the added N compared to CH4 uptake.However,soil CH4 fluxes were mainly driven by soil moisture,followed by soil NO3--N concentration.Soil N2O fluxes were mainly driven by soil temperature,followed by soil moisture.Soil inorganic N availability was a key integrator of soil CH4 uptake and N2O emission.These results suggest that the changes of availability of inorganic N induced by the increased N deposition in soil may affect the CH4 and N2O fluxes in the cold semi-arid meadow steppe over the short term.     

一株干酪乳杆菌对养殖水体亚硝酸盐去除机理的研究

为了解乳酸菌去除养殖水体亚硝酸盐的作用机理,实验研究了一株干酪乳杆菌L821a(Lactobacillus casei)对淡水鱼养殖水体亚硝酸盐的去除状况,通过对菌体、酶及代谢产物的实验,证明其去除亚硝酸盐的机理包括胞内酶作用、代谢产物乳酸的直接化学反应2H++3NO2-=NO3-+2NO↑+H2O作用和间接促进微生物反硝化作用3种作用机理。在养殖水体中主要以间接作用方式发挥作用。分析认为乳酸促进反硝化作用的原因在于为反硝化微生物提供了易于利用的有机碳源(能量物质)。     

好氧反硝化菌筛选方法的研究进展

好氧反硝化菌是一类可利用好氧反硝化酶,在有氧条件下进行反硝化作用的细菌。与传统的细菌缺氧反硝化脱氮相比,利用好氧反硝化菌发展好氧脱氮技术具有独特优势。笔者就好氧反硝化菌间歇曝气法、酸碱指示剂法、呼吸抑制剂法、选择性培养基法、滴加试剂法、极限稀释法和综合筛选法等筛选方法及其机理,进行了系统综述,并对其未来的研究趋势进行了展望。     

负载型纳米零价铁(nZVI)强化垂直流人工湿地反硝化作用研究

通过在垂直流人工湿地缺氧反硝化区添加负载型纳米零价铁(n ZVI),分析不同负载型n ZVI投加量对反硝化的影响,研究不同进水C/N条件下负载型nZVI参与反硝化的效果。结果表明:投加负载型nZVI 4 g的人工湿地装置对硝氮去除效果最佳,当C/N为6、HRT=1 d、进水NO_3~--N为50 mg·L~(-1)时,其NO_3~--N去除率比未添加负载型n ZVI的人工湿地装置提高15%;随负载型n ZVI投加量的增加,人工湿地装置出水pH值和NH_4~+-N、NO_2~--N的浓度增加;在进水C/N为0、2、4、6的人工湿地装置中,其对NO_3~--N的去除率随C/N升高而升高;统计分析表明,进水C/N与负载型n ZVI投加量对人工湿地反硝化都具有显著影响,且两者具有协同作用,碳源的存在可以促进负载型nZVI参与人工湿地反硝化。     

有机肥与无机肥配施对菜地土壤N2O排放及其来源的影响

该研究采用同位素自然丰度法,通过室内培养试验研究北京地区菜地有机肥和无机肥配施对土壤释放N2O及同位素位嗜值SP（site preference）的影响,以期获得不同肥料及其配比下土壤N2O的来源及变化规律。结果表明：施用无机肥释放的N2O显著高于有机肥,其累积排放量是有机肥的6.63倍,且无机肥施用比例越高,排放量越大;各肥料组合在施用后7天内均以反硝化作用生成N2O为主,贡献最高达到78.89%,SP为6.97‰,之后硝化作用逐渐增强并成为主要途径,最高占比达76.48%,SP为25.24‰;培养期内施用无机肥可以促进反硝化作用,平均占比52.98%,SP为15.52‰,而有机肥会使硝化作用增强,平均占比71.35%,SP为23.55‰。因此,在北京潮褐土地区菜地土壤施用有机肥对N2O有良好的减排效果,可为蔬菜生产中肥料的合理应用提供科学依据。     

水稻土和菜田添加碳氮后的气态产物排放动态

【目的】动态连续监测添加碳氮底物后各气体产物—O2、 NO、 N2O、 CH4和N2的排放,对土壤碳氮转化过程和气体产生过程做更深入的理解,揭示不同土地利用方式典型红壤的温室气体产生机制。【方法】采集长江中游金井小流域不同土地利用方式稻田和菜地土壤为研究对象,利用全自动连续在线培养检测体系(Robot系统),通过两组试验分别研究土壤碳氮转化过程中各气体产物的动态变化。试验1采用菜地和稻田土壤进行好气培养,设置不施氮对照、 添加40 mg/kg铵态氮、 添加40 mg/kg铵态氮+1%硝化抑制剂、 添加40 mg/kg硝态氮、 添加40 mg/kg硝态氮+1%葡萄糖、 缺氧条件下添加40 mg/kg硝态氮+1%葡萄糖6个处理。试验2采用稻田土壤进行淹水培养,设不施氮对照、 添加40 mg/kg铵态氮、 添加40 mg/kg铵态氮+1%硝化抑制剂、 添加40 mg/kg铵态氮+1%秸秆、 缺氧条件下添加40 mg/kg铵态氮+1%的葡萄糖、 添加40 mg/kg硝态氮、 添加40 mg/kg硝态氮+1%葡萄糖、 缺氧条件下添加40 mg/kg硝态氮+1%葡萄糖8个处理。培养温度均为20℃,土壤水分含量为70% WFPS (土壤孔隙含水量),培养周期为15天。【结果】从菜地和稻田土壤不同碳氮添加处理气态产物及无机氮的动态变化可看出: 1)菜地土壤好气培养初期硝化作用产生了大量N2O; 受低碳和低含水量的限制,反硝化作用较弱。当提供充足碳源和厌氧条件,出现N2O和NO的大量排放。2)在好气稻田和淹水稻田培养过程中,反硝化作用是N2O产生的主要途径。3)稻田土壤中,提供充足碳源和厌氧条件,各气态产物出现的顺序依次是NO、 N2O和N2,与三种气体在反硝化链式反应过程中的生成顺序一致。淹水稻田加铵态氮和碳源处理N2为主要产物,添加硝态氮处理后,N2O成为主要气态产物。当土壤碳源充足时,反硝化过程进行彻底,反硝化产物以终产物(N2)为主。4)在稻田土壤出现厌氧或添加碳源条件下,均检测到大量CH4产生; 且在甲烷产生的同时,NO-3几乎消耗殆尽。【结论】金井小流域典型红壤菜地N2O主要来自于硝化作用,好气和淹水稻田N2O主要来源于反硝化作用; 当碳源充足和厌氧时,菜地及稻田反硝化作用增强; 反硝化产物组成、 产物累积量及出峰顺序与碳源和氧气浓度有关。     

反硝化细菌的分离筛选及其反硝化特性的初步研究

从不同的水样、土样中用反硝化选择性培养基分离出202株反硝化细菌.以硝酸盐的降解、亚硝酸盐的积累和脱氮率为筛选指标,从这些菌株中得到1株反硝化能力强的菌株A13,经牛理生化试验和16s rDNA序列分析,鉴定该菌株为地衣芽胞杆菌(Bacillus licheni formis).然后将该菌株与保存的反硝化菌DNF409联合应用,脱氮率比应用单株菌提高近30%.在此基础上采用响应面分析法(中心组合一致精度设计,SAS9.1.3),建立了初始硝态氮浓度为25 mg/L水样脱氮率的回归方程,同时得出最佳反硝化条件是CODMn为35.1mg/L,温度为32.5℃,投菌量为6.2×106cfu/mL,反硝化时间为114.2 h,此时脱氮率达99%以上.     

Nitrous oxide fluxes and denitrification sensitivity to temperature in Irish pasture soils

Nitrous oxide (N₂O) emissions from grazed pastures constitute approximately 28% of total global anthropogenic N₂O emissions. The aims of this study were to investigate the effect of inorganic N fertilizer application on fluxes of N₂O, quantify the emission factors (EFs) for a sandy loam soil which is typical of large areas in Ireland and to investigate denitrification sensitivity to temperature. Nitrous oxide flux measurements from a cut and grazed pasture field for 1 year and denitrification laboratory incubation were carried out. The soil pH was 7.3 and had a mean organic C and N content at 0–20 cm of 44.1 and 4.4 g/kg dry weight, respectively. The highest observed peaks of N₂O fluxes of 67 and 38.7 g N₂O‐N per hectare per day were associated with times of application of inorganic N fertilizer. Annual fluxes of N₂O from control and fertilized treatments were 1 and 2.4 kg N₂O‐N per hectare, respectively. Approximately 63% of the annual flux was associated with N fertilizer application. Multiple regression analysis revealed that soil nitrate and the interaction between soil nitrate and soil water content were the main factors controlling N₂O flux from the soil. The derived EF of 0.83% was approximately 66% of the IPCC default EF value of 1.25% as used by the Irish EPA to estimate greenhouse gases (GHGs) in Ireland. The IPCC‐revised EF value is 0.9%. A highly significant exponential regression (r² = 0.98) was found between denitrification and incubation temperature. The calculated Q₁₀ ranged from 4.4 to 6.2 for a temperature range of 10–25 °C and the activation energy was 47 kJ/mol. Our results show that denitrification is very sensitive to increasing temperature, suggesting that future global warming could lead to a significant increase in soil denitrification and consequently N₂O fluxes from soils.