石英砂负载氧化铁的表征及其除锑吸附性能研究

通过SEM/EDAX以及Nova-1000表面分析仪对石英砂负载的氧化铁颗粒进行了表征,发现负载氧化铁的粒径为200 nm左右,其表面孔径及孔隙率分别为2×10-9～9×10-9m及0.11%,负载氧化铁的石英砂的比表面积为原砂的5倍.考察了石英砂负载氧化铁(IOCS)在不同的实验条件下(吸附时间,pH值,温度等)对水溶液中锑的去除效果,在pH为3～9范围内,其去除率均超过了98%.吸附动力学及吸附等温线实验数据分别符合二级反应动力学模型及Langmuir等温吸附模型.热动力学实验结果进一步表明:IOCS吸附锑的过程是自发的、吸热的化学吸附反应.     

钛基金属氧化物电极的制备及性能

采用聚合物前驱体法制备了Ti/SnO₂-Sb₂O₃电极,再通过恒电流电沉积法制备了 Ti/SnO₂-Sb₂O₃/PbO₂和Ti/SnO₂-Sb₂O₃/MnO₂电极。采用SEM技术对3种金属氧化物电极表面的形貌进行了表征,并分别以3种电极为阳极进行了苯酚的电催化氧化实验。实验结果表明：电解时间为2.5 h时,Ti/SnO₂-Sb₂O₃电极、Ti/SnO₂-Sb₂O₃/PbO₂电极和Ti/SnO₂-Sb₂O₃/MnO₂电极对苯酚的降解率分别为85.9%,83.2%,44.6%;苯酚在3种电极上的电催化氧化反应均遵循一级反应动力学方程;苯酚在Ti/SnO₂-Sb₂O₃ 电极和Ti/SnO₂-Sb₂O₃/PbO₂电极上的反应速率较快,并具有较高的析氧电位;Ti/SnO₂-Sb₂O₃/PbO₂电极具有更好的耐腐蚀性和更长的使用寿命。     

好氧条件下生物转鼓同步脱硫脱硝性能及相应动力学模型的优化

为探究高效同步脱硫脱硝的生物工艺,以生物转鼓反应器为实验对象,研究了好氧条件下SO₂质量浓度、NO_x质量浓度、营养液体积和气体停留时间(EBRT)的变化对生物转鼓同步脱硫脱硝效果的影响,并用动力学模型拟合值与实验数据进行了对比。实验结果表明：生物转鼓同步脱硫脱硝最适条件为SO₂质量浓度1 200 mg·m⁻³,NO_x质量浓度800 mg·m⁻³,营养液体积20.6 L,气体停留时间(EBRT) 75.36 s;SO₂过程净化主要受液相传质控制,NO_x传质过程由生物相和液相协同完成;修正求得了能较好描述好氧条件下生物转鼓脱硫脱硝效果的动力学模型,因存在生物相、液膜、污染物流动等变量与假设的差异,SO₂和NO_x模拟数据与实验数据分别有2.68%和3.18%的平均绝对误差;在最佳条件下,SO₂和NO_x的平均去除率分别为96.81%和92.98%,平均去除负荷分别为55.50 mg·(L·h)⁻¹和35.53 mg·(L·h)⁻¹,且出气质量浓度均低于100 mg·m⁻³。可见,生物转鼓是一种可行的高效同步脱硫脱硝生物工艺。     

Mitigation of methane and nitrous oxide emissions from drained irrigated rice fields

One of the important cultural practices that affect methane and nitrous oxide emissions from tropical rice plantations is the water drainage system. While drainage can reduce methane emissions, it can also increase nitrous oxide emissions, as well as reduce yields. In this experiment, four different water drainage systems were compared in a rice field in central Thailand including: (1) continuous flooding, (2) mid-season drainage, (3) multiple drainage and (4) a local method (drainage was done according to local cultural practice) in order to find a system of drainage that would optimize yields while simultaneously limiting methane and nitrous oxide emissions. Methane and nitrous oxide emission were observed and compared with rice yield and physical changes of rice plants. It was found that drainage during the flowering period could reduce methane emission. Interestingly, nitrous oxide emission was related to number of drain days rather than the frequency of draining. Fewer drain days can help reduce nitrous oxide emission. The mid-season drainage and the multiple drainage, with 6.9% and 11.4% reduction in rice yield, respectively, had an average methane emission per crop 27% and 35% lower when compared to the local method. Draining with fewer drain days during the flowering period was recommended as a compromise between emissions and yield. The field drainage can be used as an option to reduce methane and nitrous oxide emissions from rice fields with acceptable yield reduction. Mid-season drainage during the rice flowering period, with a shortened drainage period (3 days), is suggested as a compromise between the need to reduce global warming and current socio-economic realities.     

C/N和pH值对高温好氧反硝化菌产N2O的影响研究

以50℃高温、好氧条件下能进行高效好氧反硝化的菌株TAD1为研究对象,在不同C/N和pH值培养条件下,对其24 h的反硝化效率和反硝化过程中N2O的逸出量进行了研究。结果显示,C/N和pH值对菌株TAD1的反硝化效率和N2O产生量有明显影响.菌株TAD1最适宜的C/N为9,pH值为7,此时反硝化效率达到99.12%,N2O产生量仅为3.35×10-2 mg/L,N2 O转化率为0.045%,反硝化产物以氮气为主。另外,菌株TAD1不适宜在酸性条件下生长,pH值为6时反硝化效率为83.18%,N2O产生量为13.88×10-2 mg/L,是pH值为7时的4.14倍,是pH值为8时的5.07倍。     

湖北省油菜测土配方施肥下N2O减排潜力估算

以油菜种植大省-湖北省为案例地,在分析农田氮肥施用与油菜籽产量的基础上,依据氮肥利用率变化,估算测土配方施肥技术在湖北省全面推广的情况下,带来的N2O减排潜力.结果表明,在湖北省油菜种植中,测土配方施肥技术的推广将带来646.32ktCO2-eq的理论减排.以2012年湖北省油菜测土配方推广情况为基础,进一步全面实施该项技术,将产生173.91ktCO2-eq的减排量,占油菜种植因氮肥使用而产生的N2O排放总量的13.98%.测土配方施肥通过优化营养元素配比,提高油菜氮肥利用效率,是一项控制与减少农业N2O排放、减少氮素在环境中盈余量的有效措施.     

Nano-sized Fe2O3/Fe3O4 facilitate anaerobic transformation of hexavalent chromium in soil–water systems

The purpose of this study is to investigate the effects of nano-sized or submicro Fe_2O_3/Fe_3O_4 on the bioreduction of hexavalent chromium(Cr(VI)) and to evaluate the effects of nano-sized Fe_2O_3/Fe_3O_4 on the microbial communities from the anaerobic flooding soil.The results indicated that the net decreases upon Cr(VI) concentration from biotic soil samples amended with nano-sized Fe_2O_3(317.1 ± 2.1 mg/L) and Fe_3O_4(324.0 ± 22.2 mg/L) within21 days,which were approximately 2-fold of Cr(VI) concentration released from blank control assays(117.1 ± 5.6 mg/L).Furthermore,the results of denaturing gradient gel electrophoresis(DGGE) and high-throughput sequencing indicated a greater variety of microbes within the microbial community in amendments with nano-sized Fe_2O_3/Fe_3O_4 than the control assays.Especially,Proteobacteria occupied a predominant status on the phylum level within the indigenous microbial communities from chromium-contaminated soils.Besides,some partial decrease of soluble Cr(VI) in abiotic nano-sized Fe_2O_3/Fe_3O_4 amendments was responsible for the adsorption of nano-sized Fe_2O_3/Fe_3O_4 to soluble Cr(VI).Hence,the presence of nano-sized Fe_2O_3/Fe_3O_4 could largely facilitate the mobilization and biotransformation of Cr(VI) from flooding soils by adsorption and bio-mediated processes.     

Methane and nitrous oxide emissions from a subtropical coastal embayment (Moreton Bay, Australia)

Surface water methane (CH₄) and nitrous oxide (N₂O) concentrations and fluxes were investigated in two subtropical coastal embayments (Bramble Bay and Deception Bay, which are part of the greater Moreton Bay, Australia). Measurements were done at 23 stations in seven campaigns covering different seasons during 2010-2012. Water-air fluxes were estimated using the Thin Boundary Layer approach with a combination of wind and currents-based models for the estimation of the gas transfer velocities. The two bays were strong sources of both CH₄ and N₂O with no significant differences in the degree of saturation of both gases between them during all measurement campaigns. Both CH₄ and N₂O concentrations had strong temporal but minimal spatial variability in both bays. During the seven seasons, CH₄ varied between 500% and 4000% saturation while N₂O varied between 128 and 255% in the two bays. Average seasonal CH₄ fluxes for the two bays varied between 0.5 ± 0.2 and 6.0 ± 1.5 mg CH₄/(m²·day) while N₂O varied between 0.4 ± 0.1 and 1.6 ± 0.6 mg N₂O/(m²·day). Weighted emissions (t CO₂-e) were 63%-90% N₂O dominated implying that a reduction in N₂O inputs and/or nitrogen availability in the bays may significantly reduce the bays' greenhouse gas (GHG) budget. Emissions data for tropical and subtropical systems is still scarce. This work found subtropical bays to be significant aquatic sources of both CH₄ and N₂O and puts the estimated fluxes into the global context with measurements done from other climatic regions.     

Al_2O_3光催化降解染料性能研究

液相加热法制备了Al2O3作为光催化剂,研究了不同光源、光照时间、催化剂用量和溶液酸度等条件对常见有机染料光催化降解性能影响。结果表明,用太阳光作为光源照射3h,50mL染料溶液中加入Al2O3 30mg,溶液pH8～10,孔雀石绿,酚藏花红,甲基紫等染料脱色率达93%以上。将使用过的Al2O3经过简单处理,孔雀石绿溶液脱色率仍达到94.1%,催化性能稳定,可以重复利用。通过紫外可见光谱分析,表明染料分子在催化剂和光照条件下发生了降解。     

Effects of long-term amendment of organic manure and nitrogen fertilizer on nitrous oxide emission in a sandy loam soil

To understand the effects of long-term amendment of organic manure and N fertilizer on N2O emission in the North China Plain, a laboratory incubation at different temperatures and soil moistures were carried out using soils treated with organic manure （OM）, half organic manure plus half fertilizer N （HOM）, fertilizer NPK （NPK）, fertilizer NP （NP）, fertilizer NK （NK）, fertilizer PK （NK） and control （CK） since 1989. Cumulative N2O emission in OM soil during the 17 d incubation period was slightly higher than in NPK soil under optimum nitrification conditions （25℃ and 60% water-filled pore space, WFPS）, but more than twice under the optimum denitrification conditions （35℃ and 90% WFPS）. N2O produced by denitrification was 2.1-2.3 times greater than that by nitrification in OM and HOM soils, but only 1.5 times greater in NPK and NP soils. These results implied that the long-term amendment of organic manure could significantly increase the N2O emission via denitrification in OM soil as compared to NPK soil. This is quite different from field measurement between OM soil and NPK soil. Substantial inhibition of the formation of anaerobic environment for denitrification in field might result in no marked difference in N2O emission between OM and NPK soils. This is due in part to more rapid oxygen diffusion in coarse textured soils than consumption by aerobic microbes until WFPS was 75% and to low easily decomposed organic C of organic manure. This finding suggested that addition of organic manure in the tested sandy loam might be a good management option since it seldom caused a burst of N2O emission but sequestered atmospheric C and maintained efficiently applied N in soil.