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Abstract The message is divided into two major theoretical and practical theoretical part includes theoretical studies about the basics of aerosol Applied part was calculated coefficient of solar radiation scattering aerosol (air Turbidity) device was used Alfotomtr solar Walter multi-channel at wavelengths 380, 500 850 nm. was concluded: - turbidity increase as small wavelength measurement turbidity largest value occurring in summer and spring, and smaller values occur in winter, but the month of occurrence varies from one location to another according to style, .and the channel used by |