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91.
对工业废气污染状况进行分析讨论,综述了工业废气的多种脱硫除尘技术。并指出应选择脱硫除尘效率高,运转可靠,不产生二次污染的方法。 相似文献
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以石家庄市显像管玻壳厂排放的铅尘为研究对象,通过在该玻壳厂周围土壤布点采样,较系统地研究了铅尘在大气和周围土壤中的迁移和转化规律,研究表明,用高斯模式能成功地预测铅尘在大气中的迁移扩散规律,玻壳厂周围土壤表层铅含量较大值出现在当地年主导风向(SSE,N)下风向,铅在土壤中的分布主要集中在0-20cm的耕作层,在20-40cm深度范围内,铅含量呈下降趋势,最大降幅达50%。 相似文献
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James R Payne John R Clayton Jr. Bruce E Kirstein 《Spill Science & Technology Bulletin》2003,8(2):201-221
The interactions of physically dispersed oil droplets with suspended particulate material (SPM) can be important for the transport of bulk quantities of spilled crude oil and polycyclic aromatic hydrocarbons (PAH) to subtidal sediments. The literature regarding oil/SPM interactions is reviewed, and results from whole-oil droplet/SPM interaction kinetics and pure-component (Prudhoe Bay crude oil distillate cut) equilibrium partitioning experiments are presented. The effects of oil type, SPM characteristics, and salinity on the interaction rates are examined, and the importance of whole-oil droplet/SPM interactions on particle agglomeration and settling behavior are discussed. Whole-oil droplet/SPM interactions are retarded as oil droplet dispersion into the water column is inhibited by oil viscosity increases due to evaporation weathering and water-in-oil emulsification. Compared to whole oil droplet/SPM interactions, dissolved-component/SPM adsorption is not as significant for transport of individual components to sediments. The information presented in this paper can be used to augment computer-based models designed to predict oil-spill trajectories, oil-weathering behavior, and spilled oil impacts to the marine environment. 相似文献
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铁合金电炉烟尘治理技术分析 总被引:2,自引:0,他引:2
本文在分析了半封闭铁合金电炉产生的烟气、烟尘的特性和各种除尘设备性能的基础上,提出了净化铁合金电炉烟尘的三种技术:袋式除尘、强化湿式除尘和文丘里除尘器。并对袋式除尘工艺和Calvert洗涤器除尘工艺作了介绍,分析了它们的经济技术指标。半封闭铁合金电炉烟尘只能采用布袋除尘器净化,只有那些建在环境空气质量三类区的铁合金电炉,当资金非常紧缺时,才可采用Cavlert洗涤器除尘。 相似文献
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Jiang Xue-Gong Shen Jian-Guo Liu Jing-Tao Chung Yong-Seung 《Water, Air, & Soil Pollution: Focus》2003,3(2):191-212
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. 相似文献