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  • Aeolian deflation ; Aeolian features ; Agricultural practice ; Agropedology ; Cultivated land ; Experimentation ; Hungary ; Irrigation ; Soil ; Soil erosion ; Soil properties ; Wind
  • This study gives account of the most important results of 3 series of wind tunnel experiments : deflational losses of 10 different types of dry soil at various wind speeds; resistance to deflation of soils cultivated (rolled) in different ways
  • ; deflation-moderating impact of irrigation varied in extent with 27 different soil samples. The experiments are capable of providing useful data for the initial stage of form development in wind-blown sand areas, as well.
  • Aeolian features ; Aeolian transport ; Barchan ; Canary Islands ; Carbonate ; Dune ; Land use ; Model ; Plant cover ; Sand ; Wind
  • On the eastern Canary Islands a wide variety of carbonate sand dune types exists, controlled by sediment supply, topographic position, landforms, and wind regime. Detailed field studies were carried out over a period of about 15 years. This paper
  • Aeolian features ; Arid area ; Asia ; China ; Frost action ; Loess ; Microstructure ; Mongolia ; Mountain ; Plant cover ; Plateau ; Quartz ; Spatial distribution ; Tibet ; Wind
  • is restricted to areas with steppe vegetation, low surface-wind speeds and a low percentage of surface sand. SEM-analyses of quartz-grain surfaces show aeolian transport and frost weathering in these cold-arid mountain environments. In several samples
  • Aeolian features ; Arid area ; Aridity ; Dune ; Egypt ; Holocene ; Palaeoclimate ; Palaeogeomorphology ; Pleistocene ; Salinity ; Sand ; Wind
  • Aeolian features ; China ; High mountain ; Holocene ; Loess ; Mountain ; Pedogenesis ; Pollen diagram ; Quaternary ; Shaanxi ; Soil erosion ; Spatial distribution ; Stratigraphy ; Weathering ; Wind
  • are moving in the direction of the prevailing winds build up natural dams, which block the surface flow of rainfall. There exist sedimentary traps for fine-grained sediments for a short moment. The distribution and the geomorphological position of these fine