粒径对粉体类暖云雾消除剂消雾效果的影响研究
详细信息    查看官网全文
摘要
将经吸湿性能实验筛选出的某吸湿性盐与2%纳米疏水白炭黑机械混合后,采用多种粉碎设备将混合物粉碎成不同粒径范围的粉体,真空干燥后密封备用;利用马尔文激光粒度仪干法分散模式测试了各个样品的粒径范围;在50m~3暖云雾实验室内造雾,采用高压旋流分散装置分别将不同粒径范围的样品喷入暖云雾中,对比研究了其对暖云雾的消除效果。结果表明,若消雾剂样品粒度太小(如D_(90)小于10μm),刚开始喷入暖云雾中时,反而会使得雾气变浓,可见光透过率变小,起到了造雾的作用,消雾效果不好;若消雾剂样品粒度太大,则粒子沉降很快,不能充分吸收雾气,消雾效果也不好;只有消雾剂粒径大小合适(如D_(50)在20μm左右最合适),才能起到良好的消雾效果。最后,简要描述了消雾原理,主要是吸湿凝结和重力碰并两种机制。
The specifically selected hygroscopic salts and hydrophobic nano-silica are mixedmechanically, pulverized into varies of powders with different particle sizes by grinders and dried in vacuum for further use. The particle sizes of powders are measured by Malvern laser particle size analyzer. Fog is formed in a 50 m~3 cloud chamber and then these eliminators, powders in different sizes, are sprayed into the chamber by high pressure swirl dispersal device to eliminate the fog. The results show that when the particle sizes of eliminators are too small(D_(90) <10μm), the spray of particles strengthens the fog and reduces the light transmission; when the particle sizes of eliminators are too large, the sprayed particles are easy to aggregate and subside; only when the particles are at the appropriate size(D_(50) ≈20μm), the eliminators can have best eliminating effects for the warm fog. In the end, the elimination theory of warm fog, which consists of hygroscopic condensation and gravitational coalescence is discussed.
引文
[1]何金梅,王冬梅,李晓霞.干旱气象,2006,24(1):48.
    [2]高建秋,冯永基,肖伟生.广东气象,2010,32(1):31.
    [3]W.N.赫斯主编.王昂生,徐华英译.人工影响天气和气候[M].北京:科学出版社,1985,252.
    [4]康凤琴.人工影响天气展望[J].干旱气象,2001,19(1):25.
    [5]刘香翠,代梦艳,史卫东等.中国兵工学会火工烟火专业委员会第十七届学术年会论文集,2013,7:316.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700