中国北方土壤硝态氮的累积及其对环境的影响

运用统计资料和调查研究资料，揭示中国氮肥用量在地区之间和作物之间分配的不平衡现象，经济发达的东南部地区和城郊地区氮肥施用量远高于西北部地区，经济作物远高于粮食作物，氮肥短缺和过量施用并存。中国北方某些地区土壤剖面硝态氯的大量累积对水体环境构成了某种程度的威胁。由于大田作物获得较高产量的“平均适宜施氮量(N150—180kg／hm^2)”与氮素环境安全指标尚有一定距离，中国完全可以实现水体环境安全和农业高产优质的双重目标。氮肥对水体环境的影响主要是由不合理大量施用氮肥造成的。因此，中国应制定施肥技术标准和法规，鼓励农民降低氮肥用量。     

氧化铈在非贵金属燃烧催化剂中热稳定性的研究

本文考察了Ｃｅ含量对提高催化剂的热稳定性的作用，并采用Ｘ－射线衍射分析Ｃｅ含量对催化剂活性组成的影响。结果表明，合适的Ｃｅ含量能够提高催化剂的热稳定性，这主要是氧化铈能够阻止ＮｉＣｏ２Ｏ４相的生成，而ＮｉＣｏ２Ｏ４的生成对本系列催化剂的燃烧活性是不利的。实验还表明，在空气气氛下有利于形成ＮｉＣｏ２Ｏ４相，在Ｎ２／Ｈ２Ｏ气氛中不利于ＮｉＣｏ２Ｏ４相的生成。     

河北省藁城市蔬菜种植区化肥施用与地下水硝酸盐污染研究

通过农户问卷调查和地下水田间取样分析 ,主要对河北省藁城市蔬菜种植区的化肥施用与地下水硝酸盐污染现状进行了研究。结果表明 :2 0 0 1年藁城市蔬菜种植区化肥施用纯量为 1 4 0 8.6kg·hm-2 ,其中氮肥施用纯量为 84 0 .8kg·hm-2 ;藁城市各蔬菜种植模式下氮肥施用量由高到低的顺序依次为大棚 >温室 >中棚 >小棚 >地膜 >露地 ;温室、中棚和露地蔬菜区地下水硝酸盐含量最高值出现在 8月 ,而地膜蔬菜区则在 1 1月 ;各蔬菜种植模式对地下水影响的大小顺序为地膜 >中棚 >温室 >露地 ,影响因素主要有密集度、种植模式、种植年限、氮肥施用量和土壤质地等。     

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>230mg/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<30mg/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。     

Formation of Nitrate and Sulfate in the Plume of Berlin (8 pp)

Background, Aims and Scope Secondary inorganic aerosol (SIA), i.e. particulate sulphate (S(VI)), ammonium and nitrate (N(V)) is formed from gaseous precursors i.e., sulfur dioxide (S(IV)), ammonia and nitrogen oxides, in polluted air on the time-scale of hours to days. Besides particulate ammonium and nitrate, the respective gaseous species ammonia and nitric acid can be formed, too. SIA contributes significantly to elevated levels of respirable particulate matter in urban areas and in strongly anthropogenically influenced air in general. Methods The near-ground aerosol chemical composition was studied at two stationary sites in the vicinity of Berlin during a field campaign in summer 1998. By means of analysis of the wind field, two episodes were identified which allow to study changes within individual air masses during transport i.e., a Lagrangian type of experiment, with one station being upwind and the other downwind of the city. By reference to a passive tracer (Na+) and estimates on dry depositional losses, the influences of dispersion and mixing on concentration changes can be eliminated from the data analysis. Results and Discussion Chemical changes in N(-III), N(V) and S(VI) species were observed. SIA i.e., N(V) and S(VI), was formed from emissions in the city within a few hours. The significance of emissions in the city was furthermore confirmed by missing SIA formation in the case of transport around the city. For the two episodes, SIA formation rates could be derived, albeit not more precise than by an order of magnitude. N(V) formation rates were between 1.4 and 20 and between 1.9 and 59 % h-1 on the two days, respectively, and S(VI) formation rates were > 17 and > 10 % h-1. The area south of the city was identified as a source of ammonia. Conclusion The probability of occurrence of situations during which the downwind site (50 km downwind of Berlin) would be hit by an urban plume is > 7.4%. Furthermore, for the general case of rural areas in Germany it is estimated that for more than half of these there is a significant probability to be hit by an urban plume (> 8%). The S(VI) formation rates are higher than explainable by homogeneous gas-phase chemistry and suggest the involvement of heterogeneous reactions of aerosol particles. Recommendation and Outlook The possible contribution of heterogeneous processes to S(VI) formation should be addressed in laboratory studies. Measurements at more than two sites could improve the potential of Lagrangian field experiments for the quantification of atmospheric chemical transformations, if a second downwind site is chosen in such a way that, at least under particular stability conditions, measurements there are representative for the source area.     

Aromatic photonitration in homogeneous and heterogeneous aqueous systems

This work describes the nitration of aromatics upon near-UV photolysis of nitrate and nitrite in aqueous solution and upon photocatalytic oxidation of nitrite in TiO2 suspensions. Phenol is used in this work as a model aromatic molecule and as a probe for *NO2/N2O4. The photoinduced nitration of phenol in aqueous systems occurs upon the reaction between phenol and *NO2 or N2O4, and is enhanced by the photocatalytic oxidation of nitrite to *NO2 by TiO2. Aromatic photonitration in the liquid phase can play a relevant role in the formation of nitroaromatics in natural waters and atmospheric hydrometeors, thus being a potential pathway for the condensed-phase nitration of aromatics. Furthermore, the photoinduced oxidation of nitrite to nitrogen dioxide suggests a completely new role for nitrite in natural waters and atmospheric aerosols.     

城市污水生物除磷系统的特点工艺及其改进

本文以废水生物除磷的原理及特点为基础，介绍了城市污水生物除磷的主要工艺及其改进方法。     

玉米自交系氮效率基因型差异的比较研究

采用溶液培养的方法。选用经田间，土壤试验对N反应有典型差异的玉米自交系478，H21，Wu312,Zong31,Baici，在4个供氮水平下（0.04,0.4,2和4nmol/L)，研究了不同基因型玉米苗期氮素吸收，利用的差异及其原因，结果表明：极低N胁迫条件下（０.04mmol/L),总干重的基因型差异是由根系，地上部的共同作用的结果，高N下，总干重是由地上部的差异所决定的（表1），极低供N条件下，4578的总干重最大，且有较高的氮效率，Wu312,Zong31相对较低，478相对较高的氮效率主要来源于吸收效率的差异。该基因型在低N下总吸氮量最高，H21居中，Baici,Zong31相对较低，478相对较高的氮效率主要来源于吸收效率的差异。该基因型在低N下总吸氮量最高，H21居中，Baici,Zong31,Wu312相对较低（图1），吸收效率的差异主要是由于根系全N量的不同所致（图3），而根系全N量的差异主要是由于根系大小不同（表1），在极低氮水平下，不同基因型玉米根系全氮量的变幅比地上部高出28.1%，高N下（4mmol/L)，全N量的变幅比地上部高出15.4%(图2，图3），在0.04mmol/L下，478与Wu312,Zong31的利用效率不存在显著差异（表2）。     

应用GLEAMS模型评估我国东南地区农业小流域硝态氦的渗漏淋失

应用GLEAMS模型估算我国东南亚热带地区农业小流域硝态氮的渗漏淋失。在五川流域8种不同土地利用方式的农田中埋设渗漏监测装置，每月采集水样分析硝态氮含量。用2002年4—12月作物生长季节的实测数据进行模型校验的结果表明，模型对水稻田除外的其他土地利用方式下硝态氮渗漏淋失模拟效果较好。五川流域2002年硝态氮淋失模拟计算结果表明，不同土地利用方式下硝态氮淋失时空差异显著，全年渗漏量（以氮计）为4．64～38．39kg·hm^-2，流域面积加权平均为29．99kg·hm^-2。甘蔗地、香蕉地和蔬菜地的年硝态氮渗漏量最高。渗漏峰值一般出现在7—8月。降雨、土地利用和化肥施用等人类活动是影响硝态氮渗漏淋失的主要因素。     

电子受体及中间产物对厌氧氨氧化的影响

研究了厌氧氨氧化混合培养物对不同基质(硝酸盐、亚硝酸盐)的转化特性，确定了氨和硝酸盐、亚硝酸盐转化比例(物质的量)分别为1.085、0.897．亚硝酸盐转化成硝酸盐的比率为14.97％．在培养液中加入厌氧氨氧化的中间产物羟胺可以加速反应的进行．图3表2参9