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- W2360260057 abstract "The long axis direction of saucer blowouts is WNW-ESE in Hulun Buir sandy grassland.According to the angle between wind direction and the blowout's long axis direction,airflows could be classified as perpendicular flow,left oblique flow,right oblique flow and axis-parallel flow.Field observations show that right oblique flow and perpendicular flow result in blowout's lateral expansion and deepening;left oblique flow and axis-parallel flow lead to sand outward transportation and blowout extending longitudinally.Right oblique flow and perpendicular flow can form clockwise perpendicular whirl in south margin of the saucer blowout;axis-parallel flow and left oblique flow can form anticlockwise perpendicular whirl in its northwest margin.Along the long axis direction of the saucer blowout,air flow separates and decelerates when it approaches the blowout's margin,then re-attaches at the bottom of the blowout,and then accelerates and climbs along the outlet slope till the top of the dune,lastly diffuses and decelerates in the leeward of the dune behind the saucer blowout.In cross section or arc section of the saucer blowout,airflow monotonicly increases or reduces.Deposition process principally dominated the blowout during observation period.The intensity of erosion and deposition is determined by resultant sand-transporting potential,while the angle between resultant sand-transporting potential direction and the long axis direction determines the spatial distribution pattern of erosion and deposition." @default.
- W2360260057 created "2016-06-24" @default.
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- W2360260057 date "2012-01-01" @default.
- W2360260057 modified "2023-09-25" @default.
- W2360260057 title "Interaction between Airflow and Shape of Saucer Blowout in Sandy Grassland" @default.
- W2360260057 hasPublicationYear "2012" @default.
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