基于ZrO2/TiO2催化H2O2氧化低温脱硝的实验研究

以纳米TiO_2为载体,采用等体积浸渍法掺杂过渡金属氧化物ZrO_2进行改性,制备了一系列ZrO_2/TiO_2催化剂,以催化H_2O_2低温氧化NO脱硝,并采用X射线衍射(XRD)、H_2程序升温还原(H_2-TPR)、O_2程序升温氧化(O_2-TPO)、X射线光电子能谱(XPS)及电子顺磁共振(EPR)等表征分析探究了影响H_2O_2脱硝活性的因素.表征结果表明ZrO_2的负载量会影响催化剂中晶格氧的含量,晶格氧相对含量的增加有利于氧化还原反应中的电子传递,这是促进H_2O_2活化分解的关键.在微观表征的基础上,通过实验研究筛选获得了催化剂的最佳ZrO_2负载量,同时对比考察了非催化和纳米TiO_2催化作用下的H_2O_2氧化低温脱硝性能;针对获取的最优催化剂,进一步考察了不同烟气工况对催化剂活性的影响.实验结果表明,ZrO_2/TiO_2催化剂能有效促进H_2O_2的活化分解实现低温脱硝,且ZrO_2负载量为4%(质量分数)时,催化活性最高;在烟温为160℃、[H_2O_2]/[NO]物质的量比为2及空速为30000 h~(-1)时,NO转化率最高可达81%.     

鼎湖山臭氧、氮氧化物和太阳可见光辐射相互关系的研究

给出了１９９６年了在广东肇庆鼎湖山自然保护区对太阳可见光 段辐射，地面臭氧、ＮＯ、ＮＯ２浓度的观测结果，对影响地面臭氧、ＮＯ、ＮＯ２的主要因子进行了分析，并得到了较好的结果，晴天条件下，地面臭氧浓度、ＮＯ、ＮＯ２浓度有明显的日变化；阴天条件下，地面臭氧浓度、ＮＯ、ＮＯ２浓度的日变化要复杂一些。     

籼爪交后代的花药培养效率

对爪畦稻J15、J21、J20以及J211与不同的籼型杂交稻三系亲本杂交后代不同世代进行了花药培养.结果表明:当同一爪哇稻与三系亲本杂交时,其F1花药培养力高低顺序为:爪哇稻/保持系>爪哇稻/恢复系>爪哇稻/不育系的杂种后代.这种差异可能存在细胞质效应.4个爪哇稻品种中,以J15所配组合的出愈率和培养力为最高,绿苗分化率以J20所配组合最高.低代材料花药在适合籼粳交的SK3培养基上反应较好,高代材料的花药在适合籼稻的M8培养基上反应较好.改良M8和改良SK3培养基的花培效果分别优于M8和SK3培养基.F5、F6代材料的花药在改良M8培养基上出愈率可超过50％.琼脂糖代替琼脂可显著提高出愈率和培养力.高温预培养(30-32℃)24 h其花药培养效率达到最高值.图2表3参15     

富氧生物硝化处理微污染原水除NO2--N研究

为去除微污染原水中的NO2--N和提高水厂的饮水安全性,采用弹性填料微孔曝气富氧生物硝化法处理某微污染水源原水,探讨了原水不同水质及天然水体温度下富氧生物硝化工艺的除NO2--N效果,研究了水温与富氧生物硝化工艺NO2--N去除效果的相关性。结果表明,当富氧生物硝化工艺正常稳定运行HRT为1.2h,气水比为1∶1,pH6.5~7.4,DO为8~10mg·L–1,原水水温26~30℃、NO2--N0.05~0.4mg·L–1、NH4 -N0.4~1.8mg·L–1和CODMn7.01~9.61mg·L–1时,富氧生物硝化工艺NO2--N的去除率为77%～100%;原水水温20～22℃、NO2--N0.09~0.5mg·L–1、NH4 -N0.7~2.5mg·L–1和CODMn5.84~9.11mg·L–1时,去除率为44%～63%;原水水温10～12℃、NO2--N0.04~0.8mg·L–1、NH4 -N0.9~4.5mg·L–1·和CODMn6.53~9.27mg·L–1时,去除率为25%～40%。原水水温与富氧生物硝化工艺NO2--N去除率呈现明显的线性相关性,相关方程为:y=3.3628x-9.528,相关系数为0.8744。     

Optimum Nitrogen Use and Reduced Nitrogen Loss for Production of Rice and Wheat in the Yangtse Delta Region

A long-term field and lysimeter experiment under different amount of fertilizer-N application was conducted to explore the optimal N application rates for a high productive rice–wheat system and less N leaching loss in the Yangtse Delta region. In this region excessive applications of N fertilizer for the rice–wheat production has resulted in reduced N recovery rates and environment pollution. Initial results of the field experiments showed that the optimal N application rate increased with the yield. On the two major paddy soils (Hydromorphic paddy soil and Gleyed paddy soil) of the region, the optimal N application rate was 225–270 kg N hm^–2 for rice and 180–225 kg N hm^–2 for wheat, separately. This has resulted in the highest number of effective ears and Spikelets per unit area, and hence high yield. Nitrogen leaching in the form of NO ₃ ^– -N occurs mainly in the wheat-growing season and in the ponding and seedling periods of the paddy field. Its concentration in the leachate increased with the N application rate in the lysimeter experiment. When the application rate reached 225 kg N hm^–2, the concentration rose to 5.4–21.3 mgN l^–1 in the leachate during the wheat-growing season. About 60% of the leachate samples determined contained NO ₃ ^– -N beyond the criterion (NO ₃ ^– -N 10 mg l^–1) for N pollution. In the field experiment, when the N application rate was in the range of 270–315 kg hm^–2, the NO ₃ ^– -N concentration in the leachate during the wheat-growing season ranged from 1.9 to 11.0 mg l^–1. About 20% of the leachate samples reached close to, and 10% exceeded, the criterion for N pollution. Long-term accumulation of NO ₃ ^– -N from leaching will no doubt constitute a potential risk of N contamination of the groundwater in the Yangtse Delta Region.     

Kinetics and mechanism of nitrite oxidation by hypochlorous acid in the aqueous phase

The rate coefficient for the reaction of nitrite with hypochlorite and hypochlorous acid has been studied using spectrophotometric measurements. The reaction rate has been determined in a wide range of H(+) concentration (5< or =-log[H(+)]< or =11). The kinetics were carried out as a function of NO(2)(-), H(+) and total hypochlorite ([HOCl](total)=[HOCl]+[ClO(-)]+[ClNO(2)]) concentrations. The observed overall rate law is described by: -d[HClO](T)dt=[a[NO(2)(-)](2)+b[NO(2)(-)]][H(+)](2)c+d[H(+)]+e[NO(2)(-)][H(+)](2)[HOCl](total)At T=298 K and in Na(2)SO(4) at an ionic strength (I=1.00 M), we obtained using a nonlinear fitting procedure: a=(1.83+/-0.36)x10(7) s(-1), b=(1.14+/-0.23)x10(5) Ms(-1), c=(1.12+/-0.17)x10(-13) M, d=(1.43+/-0.29)x10(-6) M(2) and e=(1.41+/-0.28)x10(3) M where the errors represent 2sigma. According to the overall rate law, a/b=k(1)/k(3), b/e=k(3), c=K(w), d/c=K(a), d=K(a)K(w) and e=K(1)K(a). In Na(2)SO(4) at an ionic strength (I=1.00 M), the values of K(1) and K(a) are (1.1+/-0.1)x10(-4) and 1.28x10(7) M(-1), respectively. A mechanism is proposed for the NO(2)(-) oxidation which involves the reversible initial step: NO(2)(-)+HOCl left harpoon over right harpoon ClNO(2)+OH(-) (K(1)), while ClNO(2) undergoes the two parallel reactions: attack by NO(2)(-) (k(1)) and hydrolysis (k(3)). ClNO(2) and N(2)O(4) are proposed as important intermediates as they control the mechanism. The rate coefficients k(1) and k(3) have been determined at different ionic strengths in NaCl and Na(2)SO(4). The influence of the ionic strength and ionic environment has been studied in this work.     

氧化镁基催化吸附剂的制备及脱硝性能研究

采用共混合法制备氧化镁基催化吸附剂,通过正交实验设计找出其组分的最佳配比.利用该催化吸附剂对烟气进行脱硝实验,考察了焙烧温度、焙烧时间和床层温度对氧化镁基催化吸附剂去除NO的影响.结果表明,利用氧化镁基催化吸附剂可以对烟气进行直接催化分解脱硝,其最佳的焙烧温度和时间分别为350～500 ℃和3～4 h,脱硝率可达85%～95%.利用红外光谱(FT-IR)、X射线衍射(XRD)对脱硝处理前后的氧化镁基催化吸附剂进行了分析,探讨其脱硝的机制.     

Antennal responses of four species of tree-killing bark beetles (Coleoptera: Scolytidae) to volatiles collected from beetles,and their host and nonhost conifers

Summary. Host selection in tree-killing bark beetles (Coleoptera: Scolytidae) is mediated by a complex of semiochemical cues. Using gas chromatographic-electroantennographic detection (GC-EAD) and GC-mass spectrometric analyses, we conducted a comparative study of the electrophysiological responses of four species of tree-killing bark beetles, the Douglas-fir beetle, Dendroctonus pseudotsugae, Hopkins, the mountain pine beetle, D. ponderosae Hopkins, the spruce beetle, D. rufipennis Kirby, and the western balsam bark beetle, Dryocoetes confusus Swaine, to volatiles captured by aeration of 1) bole and foliage of four sympatric species of conifers, Douglas-fir, Pseudotsuga menziesii (Mirb.) Franco, lodgepole pine, Pinus contorta var. latifolia Engelm., interior spruce, Picea engelmannii x glauca, and interior fir, Abies lasiocarpa x bifolia, and 2) con- and heterospecific beetles at three stages of attack. We identified 13 monoterpenes in the conifers and nine compounds in the volatiles of beetles that elicited antennal responses. There was no qualitative difference in the terpene constitution of the four species of conifers and very little difference across beetle species in their antennal response to compounds from conifers or beetles. The lack of species-specific major or minor components in conifers suggests that beetles would need to detect differences in the ratios of different compounds in conifers to discriminate among them. Attraction to hosts and avoidance of nonhost conifers may be accentuated by perception of compounds emitted by con- and heterospecific beetles, respectively. The 22 compounds identified are candidate semiochemicals with potential behavioural roles in host location and discrimination.     

叠氮化钠对亚硝酸根分解能力的探讨

分析了采用叠氮化钠修正法测定水中溶解氧时，对水中亚硝酸根含量与叠氮化钠加入量的关系。     

Dynamics of Turbulence in Low-Speed Oscillating Bottom-Boundary Layers of Stratified Basins

This paper focuses on the impact of an oscillating low-speed current on the structure and dynamics of the bottom-boundary layer (BBL) in a small stratified basin. A set of high-resolution current profile measurements in combination with temperature-microstructure measurements were collected during a complete cycle of the internal oscillation (`seiching') in the BBL of Lake Alpnach, Switzerland. It was found that even a relatively long seiching period of 24 hours significantly changed the form of the near-bottom current profiles as well as the dynamics of the turbulent dissipation rate compared to the steady-state law-of-the-wall. A logarithmic fit to the measured current profiles starting at a distance of 0.5 m above the sediment led to inconsistent estimates of both friction velocity and roughness length. Moreover, a phase lag between the current and the turbulent dissipation of 1.5 hours and a persistent maximum in the current profile at a height of 2.5 to 3 m above the sediment were observed. The experimental findings were compared to the results of a k- turbulence model and showed good agreement in general. Specifically, the inconsistent logarithmic fitting results and the observed phase lag were reproduced well by the model.