Study of the spread of PM2.5 in the atmosphere of Rustavi and its environs

A. Surmava, N. Gigauri, L. Intskirveli, Leila V. Gverdtsiteli
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Abstract

The distribution of PM2.5 in the atmosphere of the city of Rustavi and its environs was studied under eastern background light air, gentle and fresh breeze. It has been established that the maximum concentrations of PM2.5 in the atmosphere of Rustavi are almost always higher than the corresponding maximum allowable concentrations. The trend of hourly changes in concentrations showed that during the day the concentration of microparticles reaches its maximum in the various period of the day. Numerical modeling of the local distribution of microparticles carried out in the city of Rustavi during background easterly light air, gentle and fresh breeze showed us that the change in the daily regime of relief and temperature with eastern light air in Rustavi for 12 hours leads to a complex and significant change in the wind speed directed to land. It forms on the territory of Kvemo Kartli the opposite current of the background wind, which corresponds to the horizontal circular wind circulation. The value of circulation gradually decreases with increasing height and in the boundary layer of the atmosphere (600 m above the earth's surface) has the form of a wave disturbance. the picture obtained with an average background east wind is qualitatively similar to the field obtained with a background light air, and with a fresh breeze, in contrast to the case of a light air and gentle breeze, the pollution zone covers most of the simulation zone.
鲁斯塔维市及其周边地区大气中PM2.5扩散研究
在东方背景下,研究了鲁斯塔维市及其周边地区大气中PM2.5的分布。已经确定,鲁斯塔维大气中PM2.5的最大浓度几乎总是高于相应的最大允许浓度。浓度的逐时变化趋势表明,在白天,微粒浓度在一天的各个时段达到最大值。对鲁斯塔维市在背景偏东风轻空气、温和清新微风条件下的局部颗粒物分布进行数值模拟,结果表明,鲁斯塔维市东部轻空气在12小时内的日起伏和温度变化导致了指向陆地的风速的复杂而显著的变化。它在Kvemo Kartli的领土上形成了与背景风相反的气流,这与水平圆形风环流相对应。环流值随高度的增加而逐渐减小,在大气边界层(距地表600 m)以波扰动的形式存在。在平均背景东风条件下获得的图像与背景轻风条件下获得的图像在质量上相似,在微风条件下,与空气轻风条件下相比,污染区覆盖了模拟区的大部分区域。
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