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Analysis of meteorological information shows that strong winds and a dust storm were formed at the Hami in the Xinjiang Province and the west part of Inner Mongolia. The storm first moved eastward. As it reached the Inner Mongolia and Hebei Province, it turned southeastward. The structure of the atmospheric boundary layer during the dust storm process is based on data from a 325-meter meteorological tower and radiosonde information.

The values of aerosol concentrations during the dust storm are ten times higher than the ordinary days. Instrumental activation analysis was carried on to determine the contents of 30 trace elements...

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