ABSTRACT
This research aimed to identify and characterize individual spherical fly ash particles extracted from surface snow at Laohugou Glacier No. 12, western Qilian Mountains, China. Characterization of the spherical particles (i. e. morphology, chemical composition and genesis) was obtained by scanning electron microscopy coupled with energy dispersive X-ray spectrometer (SEM-EDX). Spherical particles and agglomerates were identified according to their morphology in nine snow samples. Prevalent particle types in all samples were granular spherical particles, hollow spherical particles, and agglomerates. The vast majority of spherical particles in our samples had mostly smooth and glossy surfaces. Individual particle analyses of elemental composition showed that particles formed in combustion were mainly composed of silicon, aluminum and trace elements. On the basis of chemical information obtained from EDX, the fly ash particles deposited in the snow could be classified into three types, which were Si-dominant particles, Fe-dominant particles, and Ti-dominant spherical particles. Backward air mass trajectory and dispersion analysis suggested that the developed urban regions of central Asia and surrounding Yumen city contributed the primary fly ash particles from industrial combustion to the study site through the high-level atmospheric circulation.
