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ferrosilicon dust catcher in Tajikistan Central Asia

The vast expanse and diverse desert types acrossCentral Asiagenerateduststorms of different frequencies, intensities and durations. The spatial distribution of DS for 1936–1960, 1936–1980 and 1980–2000 are shown in Fig. 2, Fig. 3, Fig. 4.During the 1936–1960Central Asiawas affected by a greater number ofduststorms (DS) compared to the following decades – the region was ...

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