用环形扩散管和滤纸联用采样技术采集空气中氨和铵盐

建立了环形扩散管和滤纸采样夹联用，分形态同时采集空气中所态氨和颗粒态铵盐的方法。在同一气流中，采用涂渍１．５％草酸乙醇水溶液的环形扩散管采集气态氨，用浸渍上述试剂的玻璃纤维纸和慢速定量滤纸分别采集颗粒安和第一层滤纸上的铵盐挥发产生的氨气。用靛酚蓝比色法分别测定氨和铵盐。当采气流速为１．０Ｌ／ｍｉｎ时，采样效率高于９８．２％。将本法测得的氨气和铵盐的总量与标准采样方法的测定结果比较。无显著性差异（Ｐ     

中国大气中氧化亚氮浓度及土壤排放通量的测定

收集和分析了中国不同地区的大气样品并且得出了痕量气体N_2O的浓度。用箱式法对种植不同作物农田释放N_2O的通量进行了测定。测得我国本底站N_2O大气浓度为308±5ppb(1989年),这和世界其它本底站N_2O浓度相同。在其它城、乡地区测定的N_2O浓度则较高。不同农田释放N_2O的通量虽有差异,但数值大致相当。农业活动和天气条件影响土壤释放N_2O的大小。计算得出,1990年我国来自农业源(土壤和含氮化肥释放)的N_2O平均排放量为122GgN_2O-N。     

大气中阻塞形成的一个理论

本文提出了偶极子阻塞形成的一个新理论。文中首先使用多重尺度方法研究了基本气流具有弱切变的非线性正压Rossby波,得到了它的波包满足非线性Schr-dinger方程。指出:当Rossby波的波数满足k~2/3相似文献   

大尺度大气运动方程组解的一些性质——定常外源强迫下的非线性适应

本文从大尺度大气运动方程组出发,讨论了定常外源强迫下大气系统的长期行为。建立了基本的泛函空间和算子方程,证明了解的存在唯一性定理,在此基础上讨论了整体吸收集以及其中的不变点集的存在性。揭示了系统向外源的非线性适应过程。     

中国内陆大气颗粒物的搬运、沉积及反映的气候变化——Ⅰ.现代大气气溶胶

分析了中国内陆3个地点尘暴和非尘暴期间大气颗粒物中17种微量元素的浓度-粒度分布。表明这些地点的大气颗粒物主要由矿物气溶胶(即粉尘)组成。对黄土高原上空非尘暴大气微量元素的统计分析,导出粗粒子主要有两种来源——土壤粉尘和被污染的粉尘,细粒子的两种来源是土壤粉尘和人为污染物。在年尺度上,粉尘对黄土高原的大气干输入主要取决于非尘暴过程。利用清除系数估算的粉尘湿沉积通量只占总沉积的4％—11％。     

臭氧催化分解异相反应新机理

极地云表面上的异相反应在春季南极臭氧空洞形成中起关键作用。本文主要介绍了极地云表面上异相反应两个机理 ,其中的新机理同样适用于另外一些凝聚相和表面体系中的异相反应。     

大气痕量气体NO_2的研究

为了测量大气中NO_2的含量,我们研制了自动太阳光谱光度仪。在地面遥感测量太阳直射光谱的4470—4490波段,从辐射传输方程及极大相似法,导出了大气中NO_2的含量。而大气中NO_2的浓度,在北京郊区测量了数月。本文对测量结果进行了讨论。     

通过脱碳控制全球平均温度

Establishing a reliable method to predict the global mean temperature (T_e) is of great importance because CO₂ reduction activities require political and global cooperation and significant financial resources. The current climate models all seem to predict that the earth's temperature will continue to increase, mainly based on the assumption that CO₂ emissions cannot be lowered significantly in the foreseeable future. Given the earth's multifactor climate system, attributing atmospheric CO₂ as the only cause for the observed temperature anomaly is most likely an oversimplification; the presence of water (H₂O) in the atmosphere should at least be considered. As such, T_e is determined by atmospheric water content controlled by solar activity, along with anthropogenic CO₂ activities. It is possible that the anthropogenic CO₂ activities can be reduced in the future. Based on temperature measurements and thermodynamic data, a new model for predicting T_e has been developed. Using this model, past, current, and future CO₂ and H₂O data can be analyzed and the associated T_e calculated. This new, esoteric approach is more accurate than various other models, but has not been reported in the open literature. According to this model, by 2050, T_e may increase to 15.5 ℃ under "business-as-usual" emissions. By applying a reasonable green technology activity scenario, T_e may be reduced to approximately 14.2 ℃. To achieve CO₂ reductions, the scenario described herein predicts a CO₂ reduction potential of 513 gigatons in 30 years. This proposed scenario includes various CO₂ reduction activities, carbon capturing technology, mineralization, and bio-char production; the most important CO₂ reductions by 2050 are expected to be achieved mainly in the electricity, agriculture, and transportation sectors. Other more aggressive and plausible drawdown scenarios have been analyzed as well, yielding CO₂ reduction potentials of 1051 and 1747 gigatons, respectively, in 30 years, but they may reduce global food production. It is emphasized that the causes and predictions of the global warming trend should be regarded as open scientific questions because several details concerning the physical processes associated with global warming remain uncertain. For example, the role of solar activities coupled with Milankovitch cycles are not yet fully understood. In addition, other factors, such as ocean CO₂ uptake and volcanic activity, may not be negligible.     

空间展布体系中由化学反应-扩散-热传导耦合导致的温度场对称破缺

分析了由于化学反应-扩散-热传导耦合而导致的非等温非均匀体系中温度场对称破缺.研究结果表明,在一定的边界条件下,甚至是单组分化学反应-扩散-热传导体系,温度场的这种自组织进程也不可避免.作为温度场结构的一个范例,进一步从解析解及计算机模拟两个方面研究了小展布非等温的Lindeman模型;结果表明,温度场出现时空自组织的阈值不仅与本征参数有关,而且与体系的边界条件及外控约束相关,揭示出了诱发或避免这种温度场时空自组织之途径.     

北京地区大气颗粒物中不同功能区多环芳烃的分布特征

用撞击式分级采样器同步采集了北京市城乡结合部、郊区的2003年四个季节的不同粒径大气颗粒物样品,用气相色谱-质谱分析了其中的多环芳烃。两个功能区的PAHs总质量浓度分布趋势均为：冬季>秋季>春季>夏季；不同环数PAHs在不同粒径颗粒物中的分配比例比较显示，粗颗粒物中2 环或3环PAHs的分配比例比其在高环PAHs的比例要大。