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.     

矿山呼吸性粉尘危害程度评价法研究

矿山呼吸性粉尘危害程度评价法研究侯祺棕（武汉工业大学资源与环境工程系）［摘要］通过对矿山呼吸性粉尘实际危害程度评价法的研究，并经实例检验，推荐两种具有可操作性和足够准确的评价法，这对矿山呼吸性粉尘监测新技术的推广具有重要意义。［关键词］呼吸性粉尘，危...     

岷江都江堰段水环境容量计算及水质综合评价

岷江水域兼有灌溉，供水，发电等多重功能。本文对岷江都江堰段水环境现状进行了模糊综合评价，并计算了水环境容量。     

生态足迹分析方法及其在国内的应用

生态足迹分析方法是90年代提出的可以定量的反映一个国家、地区、城市的可持续发展程度分析的计算模型。本文介绍了生态足迹模型的理论依据和计算方法，分析了生态足迹分析方法在我国的应用，并且指出了生态足迹分析方法的优缺点及其改进。     

布袋式除尘在大型煤炭筛分系统中的成功应用

煤炭筛分系统在工作时产生的大量煤尘对环境造成污染，为解决这一问题，我们设计安装了两套煤炭筛分除尘系统，通过布袋式除尘器，把煤尘用布袋收集起来，解决了煤炭粉尘污染问题，通过三年的使用观察，效果非常明显。     

芜湖市生态占用测度方法的分析与应用

应用Wackemagel等提出的生态占用测度方法对芜湖市2004年的生态占用和生态容量进行了分析和计算。利用生态占用分析方法从宏观上度量了芜湖市社会经济发展的可持续性以及生态状况。结果表明，计算年的人均生态赤字为3．757429226hm^2．并提出了相应的对策和措施，为芜湖市建设“生态城市”提供量化依据。     

安徽省土地资源人口承载力的动态研究

基于《安徽省统计年鉴》，对全省近10年的土地资源、粮食生产及人口增长状况进行了分析。在此基础上，运用相关数学模型对2005-2020年全省人口数量、耕地面积和粮食单产分别进行了预测。为了提高预测精确度，取各种预测方法的平均值。根据安徽省情将其划分为温饱型、小康型和富裕型三档生活标准，分别探讨了预测期内安徽省土地承载力状况，提出了相应的发展对策和建议，为全省发展粮食生产提供科学依据。     

半敞开烟气排放的测试方法的研究

综合分析了除尘系统进入的烟尘量、排放方式、排放浓度等5个参数及其相互关系,根据在一定时间内进入除尘系统烟气烟尘的量;对除尘器进口和出口即百叶窗内各方向烟尘浓度的测试,利用物料平衡方程,确定百叶窗内各测点各方向测定的烟气烟尘浓度,确定半敞开排放烟气烟尘的排放浓度,笔者发现,外排烟尘浓度与百叶窗内侧向烟尘浓度具有良好的线性关系,百叶窗内侧向测定烟尘浓度能够反映半敞开烟气排放浓度。据此,提出以半敞开方式排放烟气烟尘的除尘系统烟气烟尘浓度测试方法,即侧向间接测试法。     

抽出式通风煤巷掘进过程中粉尘浓度分布规律的数值模拟

根据气固两相流理论，针对矿井掘进工作面的特点，采用计算流体力学的离散相模型（DPM）对掘进工作面通风过程中粉尘浓度进行数值模拟，总结抽出式通风掘进巷道中粉尘浓度的沿程分布及变化规律。     

管帏冲击式除尘器的应用

介绍了管帏冲击式除尘器的结构及其捕尘机理。介绍了对该除尘器进行除尘和防淋雨性能测试的实验方法和装置。分析了实验数据，得出了相应的结论。