and distance from the sand source. The sandy areas are spreading. Rich and vegetated ecosystems arereplaced by sandy deserts with low fertility and water-holding capacity. Threshold values for Icelandic sand were determined with automatic sensors and dust traps. The threshold values are in¯uenced by...
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| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.578.8643 http://eusoils.jrc.ec.europa.eu/projects/scape/uploads/35/Arnalds_Gisladottir_Sigurjonsson.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.578.8643 2023-05-15T16:47:47+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.578.8643 http://eusoils.jrc.ec.europa.eu/projects/scape/uploads/35/Arnalds_Gisladottir_Sigurjonsson.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.578.8643 http://eusoils.jrc.ec.europa.eu/projects/scape/uploads/35/Arnalds_Gisladottir_Sigurjonsson.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://eusoils.jrc.ec.europa.eu/projects/scape/uploads/35/Arnalds_Gisladottir_Sigurjonsson.pdf Iceland wind erosion sand-®elds threshold aeolian processes text ftciteseerx 2016-01-08T12:53:17Z and distance from the sand source. The sandy areas are spreading. Rich and vegetated ecosystems arereplaced by sandy deserts with low fertility and water-holding capacity. Threshold values for Icelandic sand were determined with automatic sensors and dust traps. The threshold values are in¯uenced by the surface roughness and the texture of the sand. Wet sand is observed to move during storm events, and coarse, light density tephra ’1 mm is easily moved by the wind. Text Iceland Unknown |
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ftciteseerx |
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English |
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Iceland wind erosion sand-®elds threshold aeolian processes |
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Iceland wind erosion sand-®elds threshold aeolian processes |
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Iceland wind erosion sand-®elds threshold aeolian processes |
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and distance from the sand source. The sandy areas are spreading. Rich and vegetated ecosystems arereplaced by sandy deserts with low fertility and water-holding capacity. Threshold values for Icelandic sand were determined with automatic sensors and dust traps. The threshold values are in¯uenced by the surface roughness and the texture of the sand. Wet sand is observed to move during storm events, and coarse, light density tephra ’1 mm is easily moved by the wind. |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.578.8643 http://eusoils.jrc.ec.europa.eu/projects/scape/uploads/35/Arnalds_Gisladottir_Sigurjonsson.pdf |
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Iceland |
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http://eusoils.jrc.ec.europa.eu/projects/scape/uploads/35/Arnalds_Gisladottir_Sigurjonsson.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.578.8643 http://eusoils.jrc.ec.europa.eu/projects/scape/uploads/35/Arnalds_Gisladottir_Sigurjonsson.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766037886262575104 |