昆明市机动车尾气排放控制水平分析

选择CO做研究对象，采用累积百分比法对4类机动车尾气排放水平进行分析，得出结论；昆明市机动车总体排放控制水平较低，须改进和完善现行的检测／维护制度，应考虑加快车辆的更新换代和微车电喷化。     

人工湿地处理皂素废水生产性试验研究

黄姜是生产“药用黄金”——皂素的主要原材料，生产过程中会产生大量的工业废水。皂素废水是一种难降解、污染物浓度高的酸性废水，目前还没有成功应用于工程实际的废水处理工艺。本文主要采用人工湿地处理经两相厌氧工艺一好氧工艺组合工艺处理之后的废水，以满足达标排放的要求。经过4个月试验研究得出如下结论：人工湿地COD平均去除率为47．79％，氨氮平均去除率为75．64％，总磷平均去除率为88．82％。水平潜流型人工湿地作为皂素废水深度处理工艺是可行的。     

丹东市区段鸭绿江水体中铅、镉的含量

利用生物指示物（鳙鱼）对丹东地区鸭绿江水体中的铅、镉污染进行监测，采具鳙鱼-碳化酸溶-电热原子光谱法对丹东鸭绿江流域鳙鱼体内的铅、镉的含量进行了相关检测，在相同的实验条件下对该地区的水体中的铅、镉的含量进行对比，并对该地区的铅、镉污染进行了相关的评价，通过一年的监测未见超标。铅、镉含量分别为6．53±0．07（ng/g）、4．60±0．03（ng/g）；回收率分别为98.9％、103.5％；RSD分别为5．3％、4．1％。     

PASS混凝去除给水腐植酸的研究

用所研制的聚硅硫酸铝对含腐植酸原水进行了混凝处理 ,研究了投加量、pH值等对腐植酸去除效果的影响 ,探讨了PASS对腐植酸的混凝去除机理 ,并作了经济分析     

抚顺市空气可吸入颗粒物特征的研究

于2002年1～7月份在抚顺市区四个点位采集了环境空气中的可吸入颗粒物样品，经分析后获得了可吸入颗粒物组分的时间分布和空间分布特征，即采暖期PM10样品中有机碳（OC）、元素碳（EC）的绝对含量和相对含量均高于非采暖期，工业区PM10样品中的Fe、Zn、Pb的绝对含量和相对含量均明显高于其它点位，反映了其工业区的特点。     

螳螂川水质评价及污染防治对策

通过对螳螂川水质状况的分析，总结了水污染特征及主要污染原因，提出了污染治理对策。     

森林火险的序贯分析初探

本文利用森林着火危险度指标属于正态分布的特点,根据正态型序贯分析的原理,提出了确定林火危险性的序贯分析方法;建立了长白山林区5个站点森林火险的“安全域”与“危险域”的模型;并以东岗(长白山西坡)为例,作了正态型序贯分析全过程的应用示例。结果证明,利用正态型序贯分析来确定林火的等级是可行的、可靠的,具有实用价值。     

Numerical Simulation of Synoptic Condition on a Severe Sand Dust Storm

By using observational data and MM5, an observational analysisand numerical study was conducted on the synoptic condition of a severe dust storm that was caused by a Mongolian cyclone whichoccurred from 6 to 8 April 2001. Results illustrated thatthe cyclogenesis was due to the isentropic potential vorticity (IPV) advection in the upper troposphere and the terrain modifiedbaroclinicity in the mid-lower troposphere. The Altai-Sayan complex of mountains blocked the lower level cold air and made the isentropic surface sharply steep. When the air slid down along the isentropic surface the increasing of baroclinicity anddecreasing of stability blew up the vertical vorticity development.The formation of the dust storm was a result of a cyclonic cold front passing across the area. The occurrence of this dust stormwas closely related to the strong surface wind, which was accompanied by a cold front passing, rather than the cyclogenesis, itself. Hence, the reason for the pre-front dust storm formulation was the formation of heating convection. Reasons behind the formation of a black storm (visibilitylower than 50 m), which occurred in the mid-north part ofInner Mongolia, lay in several aspects. Firstly, in thisarea the surface wind was strong, a direct result of thedownward transport in mid-lower troposphere. Secondly,the cold front passed over the effected area near sunsetso the air obtained much more surface heating to form adeeper mixed layer (ML). Thirdly, cooperation between thelower level wind and the terrain made the atmosphere inthis area and acquired the maximum advective contributionnecessary to form a deep post-front ML. The sensitivityexperiment revealed that surface heat flux was important to the frontal lifting. In addition, the forcing of surface heating wasalso seen as the primary forcing mechanism of frontogenesis. Meanwhile, removal of the surface heat flux made the atmosphericstratification became stable and the pre-storm ML very shallow,which weakened the strength of the dust storm.     

The Relation Between Sandstorms and Strong Winds in Xinjiang,China

With observational data spanning 1961–1999 from 90 meteorological stations in Xinjiang, China, the spatial and temporal characteristics of sandstorms and strong winds, and the contribution of strong winds to the occurrence of sandstormsare analyzed. Moreover, the dominant wind direction and minimumwind speeds during sandstorm periods are discussed. The research shows that although possessing similar climatic trends, sandstorms and strong winds in Xinjiang have opposite geographical distributions, i.e. places with more sandstorms show fewer strong winds. The contribution of strongwinds to sandstorms in northern Xinjiang is larger than that insouthern Xinjiang. The dominant wind directions clearly indicatethe paths of the weather systems that introduced the sandstorms.The minimum wind speeds in the sandstorms were over 10 ms^-1in northern and eastern Xinjiang and in the Turpan and Yanqi Basins of southern Xinjiang. In Tarim Basin of southern Xinjiang,however, the minimum wind speed was about 6–8 ms^-1, and even 6 ms^-1 at its southern edge.     

油田废污泥治理研究

冀东油田废水池地处环境敏感区域，对其废污泥采用固化法进行处理。在大量实验的基础上优选出了三种固化剂体系并通过多次浸泡实验、淋洗实验和静态浸出实验对固化效果进行了分析。