双波长标准加入法同时测定水中硝酸盐和亚硝酸盐

本文应用双波长标准加入法同时测定了硝酸盐和亚硝酸盐，在研究硝酸盐和亚硝酸盐紫外光谱的基础上，精确选择亚硝酸盐等吸收点波长２０２．５ｎｍ，２１６．５ｎｍ为测定波长。亚硝酸盐含量回归方程经推导得Ｃ＝－３．８４１＋１５６．６Ａ，相关系Ｒ＝１．０００。将该法用于合成样品及实际水样分析，所得结果较满意。     

水分和氮素供应对菠菜硝酸盐累积和钾素吸收的影响

研究了水分和氮素供应对露地秋菠菜的硝酸盐累积和钾、氮吸收的影响。结果表明：与传统的水氮管理措施相比，采用水分平衡法和氮素专家系统进行的水氮供应并没有造成作物减产，但对钾、氮元素的吸收却有明显的影响，同氮素吸收相比，作物对钾素的吸收数量更高；并且作物对钾、氮的吸收比例随氮素供应水平的增加而降低，试验还动态监测了菠菜最新展开叶的叶柄汁液中的硝酸盐和K^ 浓度在一天内的变化情况。结果表明，不同水氮处理的菠菜叶柄汁液的硝酸盐浓度在白天均没有发生显著变化；叶柄汁液中的K^ 浓度和NO3^-／K^ 的浓度比在白天受氮素供应水平的影响很大，供氮量高，K^ 浓度和NO3^-／K^ 浓度比的变化也大，但受灌水量影响不大。图3表2参17。     

一种新的好氧反硝化菌筛选方法的建立及新菌株的发现

利用间歇曝气富集,氰化钾(KCN)选择培养基筛选好氧反硝化的细菌,通过形态学特征、生理生化反应及16SrDNA同源性比较对筛得菌株进行鉴定,并对其好氧反硝化相关基因napA进行扩增并测序比较.筛选到一株可以柠檬酸钠为碳源,硝酸钾为氮源,进行好氧反硝化的细菌.在溶解氧(DO)为(9.0±0.5)mg/L的培养基中,该菌株5 d内将硝态氮由282.0 mg L-1降解至149.2 mg L-1,其硝态氮去除率为46.47 ng mg-1min-1,同时亚硝态氮仅有少量的积累.经鉴定,初步判定它为假单胞菌属,命名为Pseudomonas sp.Y2-1-1.从其基因组中扩增出与好氧反硝化相关的周质硝酸盐还原酶(NAR)的亚基napA基因,并与已报道的napA基因进行Blast比较,发现具有较大差别.利用间歇曝气富集,氰化钾(KCN)选择培养基筛选好氧反硝化的细菌是非常有效的.初步认为Pseudomonas sp.Y2-1-1是一株新的好氧反硝化菌.图6表3参12     

川中丘陵区典型小流域地下水硝酸盐污染分析

对川中丘陵区典型小流域地下水N素含量及形态分配的监测结果表明,硝酸盐(NO3--N)是该地区地下水N素存在的主要形态。川中丘陵区54.5%的地下水NO3--N含量超过世界卫生组织(WHO)饮用水准则规定的10mg.L-1标准,另有27.3%的地下水NO3--N含量接近这一标准,表明该区地下水已经大范围地受到NO3--N污染的威胁。土地利用状况可能是影响川中丘陵区地下水NO3--N含量的主要因素。降雨量和水井深度也影响该区地下水NO3--N含量。紫色土坡耕地NO3--N随壤中流向浅层地下水迁移,可能是造成该区地下水NO3--N含量较高的最重要原因。     

王哥庄湾陆源硝酸盐氮输送通量研究

以汇水区域相对独立的崂山王哥庄地区为例 ,通过研究该区的水文地质条件、分析地表水和地下水中的硝酸盐氮 (NO3 N) ,采用流量法和断面法分别对河流和地下水向王哥庄湾的NO3 N输送量进行了计算。结果表明 ,1999年 5月下旬地下水向海洋输送的NO3 N占整个陆源输入量的 30 .0 6 % ,说明地下水向海洋的营养盐输送量是海洋环境评估的重要边界条件。     

填闲作物防治菜田土壤硝酸盐污染的研究进展

探讨了通过调整蔬菜生产的轮作结构 ,运用生物修复的原理 ,引入适宜的深根系填闲作物对深层土壤硝酸盐吸收利用 ,以避免硝酸盐进一步淋失 ,提高氮素的利用率的可行性。填闲作物应选择生长迅速、生物量大、氮素累积能力强的作物 ,在考虑填闲作物防治硝酸盐淋溶的同时 ,要兼顾其经济利用价值 ,并指出结合深根系的填闲作物进行合理轮作是蔬菜安全生产及可持续发展的途径之一     

Aerosol light-scattering in The Netherlands

The relation between the (midday) aerosol light-scattering and the concentrations of nitrate and sulfate has been assessed at a site near the coast of the North Sea in The Netherlands. Midday was selected for the measurements because this is the time at which the aerosol is most effective in the scattering of solar radiation. Automated thermodenuders were used for the hourly measurement of the concentration of nitrate and sulfate with a lower detection limit of 0.1 μ m⁻³. The site is operational since October 1993. The first-year average dry aerosol light-scattering (measured with an integrating nephelometer at a wavelength of 525 nm) was 0.71 × 10⁻⁴ m^1̄. In arctic marine air the aerosol light-scattering was a factor of 10 lower than the average value, in polluted continental air it was up to a factor of 10 higher. The ratio of the total aerosol light-scattering to the concentration of sulfate was 20 m² g⁻¹. The contribution of nitrate to the aerosol light-scattering was higher than that of sulfate in the winter and of about equal magnitude in the summer period. In November and December of 1993, the humidity dependence of the aerosol light-scattering was investigated. Two types of (continental) aerosol were found with respect to the humidity behavior. One type showed a significant increase in light-scattering at the deliquescence points of ammonium nitrate and ammonium sulfate, with that of ammonium nitrate the most pronounced. The second type of continental aerosol did not show deliquescence, but followed the typical humidity dependence of aerosol in a supersaturated droplet state. In this latter aerosol type, nitrate dominated over sulfate. It was concluded from the study that the aerosol light-scattering in The Netherlands, in particular its humidity dependence, is governed by (ammonium) nitrate.     

The transformation of outdoor ammonium nitrate aerosols in the indoor environment

Recent studies associate particulate air pollution with adverse health effects; however, the exposure to indoor particles of outdoor origin is not well characterized, particularly for individual chemical species. We conducted a field study in an unoccupied, single-story residence in Clovis, California to provide data and analyses to address issues important for assessing exposure. We used real-time particle monitors both outdoors and indoors to quantify nitrate, sulfate, and carbon particulate matter of particle size 2.5 μm or less in diameter (PM-2.5). The results show that measured indoor ammonium nitrate concentrations were significantly lower than would be expected based solely on penetration and deposition losses. The additional reduction can be attributed to the transformation indoors of ammonium nitrate into ammonia and nitric acid gases, which are subsequently lost by deposition and sorption to indoor surfaces. A mass balance model that accounts for the kinetics of ammonium nitrate evaporation was able to reproduce measured indoor ammonium nitrate and nitric acid concentrations, resulting in a fitted value of the deposition velocity for nitric acid of 0.56 cm s⁻¹. The results indicate that indoor exposure to outdoor ammonium nitrate in Central Valley of California are small, and suggest that exposure assessments based on total particle mass measured outdoors may obscure the actual causal relationships for indoor exposure to particles of outdoor origin.     

反硝化除磷的影响特性试验

采用SBR反应器（厌氧/缺氧/好氧工艺）,分别研究了乙酸盐及硝酸盐浓度变化对反硝化除磷的影响特性.试验结果表明,当进水COD浓度＞230 mg/L时,乙酸盐浓度的变化对释磷、除磷速率等影响并不显著.在硝酸盐浓度＜30 mg/L时,硝酸盐浓度越高,缺氧段除磷速率也就越高.在C/P＞23,C/N＞5条件下,SBR系统对磷、氮去除率在90%以上.     

地下水环境中反硝化作用

地下水氮污染已是全球性的环境问题 ,反硝化作用是地下水脱氮的主要机制。本文综述了地下水环境中反硝化作用的判据、速率、影响因素以及人工强化措施 ,指出了存在的问题和今后的发展方向