Wind erosion starts when the threshold wind velocity (m t ) is exceeded. We evaluated the sensitivity of m t to determine the wind erosion susceptibility of soils under variable climatic conditions. Three years field data were used to calculate m t by means of the equation m t ΒΌ u Β―-s F Γ1 (g), wher
Assessment of soil susceptibility to compaction using soil and climatic data bases
β Scribed by W.B. Voorhees
- Publisher
- Elsevier Science
- Year
- 1987
- Tongue
- English
- Weight
- 578 KB
- Volume
- 10
- Category
- Article
- ISSN
- 0167-1987
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