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Sediment transport rate-based model for rainfall-induced soil erosion

✍ Scribed by Zhi-Qiang Deng; João L.M.P. de Lima; Hoon-Shin Jung

Book ID
116344290
Publisher
Elsevier Science
Year
2008
Tongue
English
Weight
759 KB
Volume
76
Category
Article
ISSN
0341-8162

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The European Soil Erosion Model (EUROSEM
The European Soil Erosion Model (EUROSEM): a dynamic approach for predicting sediment transport from fields and small catchments
✍ Morgan, R. P. C.; Quinton, J. N.; Smith, R. E.; Govers, G.; Poesen, J. W. A.; Au 📂 Article 📅 1998 🏛 John Wiley and Sons 🌐 English ⚖ 167 KB 👁 2 views

The European Soil Erosion Model (EUROSEM) is a dynamic distributed model, able to simulate sediment transport, erosion and deposition over the land surface by rill and interill processes in single storms for both individual fields and small catchments. Model output includes total runoff, total soil

Discussion on ‘The European Soil Erosion
Discussion on ‘The European Soil Erosion Model (EUROSEM): a dynamic approach for predicting sediment transport from fields and small catchments’
✍ Kinnell, P.I.A. 📂 Article 📅 1999 🏛 John Wiley and Sons 🌐 English ⚖ 56 KB 👁 2 views

All combinations of detachment by flow or raindrops, and transport by flow, raindrop-induced flow or splash have not been fully incorporated into EUROSEM. In particular, neglecting raindrop detachment combined with raindrop-induced flow transport (RIFT) leads to underestimation of erosion under cert

Reply to discussion on ‘The European Soi
Reply to discussion on ‘The European Soil Erosion Model (EUROSEM): a dynamic approach for predicting sediment transport from fields and small catchments’
✍ Morgan, R. P. C.; Quinton, J. N.; Smith, R. E.; Govers, G.; Poesen, J. W. A.; Au 📂 Article 📅 1999 🏛 John Wiley and Sons 🌐 English ⚖ 51 KB 👁 2 views

It is considered that EUROSEM is already able, in principle, to replicate all the combinations of detachment and transport considered by Kinnell's discussion, with suitable parameter values. Some effects will only be reproducible when EUROSEM contains a more explicit representation of particle sizes