Modelling soil erosion requires an equation for predicting the sediment transport capacity by interrill overland flow on rough surfaces. The conventional practice of partitioning total shear stress into grain and form shear stress and predicting transport capacity using grain shear stress lacks rigo
Hydraulics of interrill overland flow on rough, bare soil surfaces
โ Scribed by Ingrid Takken; Gerard Govers'
- Publisher
- John Wiley and Sons
- Year
- 2000
- Tongue
- English
- Weight
- 299 KB
- Volume
- 25
- Category
- Article
- ISSN
- 0360-1269
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