The behaviour of suspended sediment in rivers is often a function of energy conditions, i.e. sediment is stored at low Β―ow and transported under high discharge conditions. The timing of maximum sediment transport can, however, also be related to mixing and routing of water and sediment from dierent
β¦ LIBER β¦
Suspended sediment flux through a salt marsh drainage basin
β Scribed by J.L. Settlemyre; L.R. Gardner
- Book ID
- 113310233
- Publisher
- Elsevier Science
- Year
- 1977
- Weight
- 807 KB
- Volume
- 5
- Category
- Article
- ISSN
- 0302-3524
No coin nor oath required. For personal study only.
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