NUMERICAL SIMULATION OF INDUSTRIAL DUST DISTRIBUTION IN THE TERRITORY OF ZESTAFONI, GEORGIA

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

Dust distribution of the industrial town of Zestafoni located in the complex territory of Georgia in case of basic meteorological situations and stationary pollution sources is studied with the use of regional model of atmospheric process development in the Caucasus and non-stationary threedimensional equation of transfer-diffusion of passive admixtures. Distribution patterns of dust dissipated in the atmosphere are obtained at different levels from the surface. It is shown that dust dissipated from cities in the atmosphere is basically concentrated in the boundary layer. Maximum values of dust concentration are obtained in the lower 100 m of surface air layer. Spatial dust distribution region increases and concentration decreases along with height increase. An influence of local orography on the pollution cloud is investigated. During a background western light air Likhi and Racha ridges impede dust transfer to the east and cause dust cloud deformation. Dust spreads along the valleys of Kvirila and Chkherimela rivers located between the ridges. In the case of gentle and fresh breezes the impact of local orography on the dust dispersion process is insignificant. Dust is basically transferred in the direction of background flows. The zone of influence of industrial town dust on the environmental pollution is determined. A width of this area varies from 5 to 20 km in dependence of the background wind velocity. Kinematics of dust propagation is studied. It is determined that in 2–100 m layer of atmosphere the process of turbulent diffusion takes precedence in the process of dust spreading. From 100 m to 1 km the processes of diffusive and advective transfers are identical, while above 1 km the preference is given to advective transfer.
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乔治亚州zestafoni境内工业粉尘分布的数值模拟
利用高加索地区大气过程发展的区域模式和被动外加剂的非平稳传递-扩散三维方程,研究了在基本气象条件和固定污染源的情况下,位于格鲁吉亚复杂领土上的工业城镇Zestafoni的粉尘分布。在大气中消散的尘埃分布模式从地表得到不同的水平。结果表明,城市在大气中消散的尘埃基本集中在边界层。尘浓度最大值出现在地面空气层下100 m处。随着高度的增加,空间粉尘分布区域增大,粉尘浓度减小。研究了当地地形对污染云的影响。在背景西部的轻空气中,Likhi和Racha脊阻碍沙尘向东部转移并造成沙尘云变形。尘埃沿着山脊之间的Kvirila河和Chkherimela河的山谷扩散。在微风和风爽的情况下,当地地形对粉尘扩散过程的影响微不足道。尘埃基本上是沿着背景气流的方向转移的。确定了工业城镇扬尘对环境污染的影响范围。该区域的宽度随背景风速的变化从5公里到20公里不等。研究了粉尘传播的运动学。结果表明,在2 ~ 100 m大气层内,粉尘扩散过程以湍流扩散为主。在100 ~ 1 km范围内,扩散传递和对流传递的过程基本一致,而在1 km以上以对流传递为主。
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