Abstract
A comparison of the data dealing with suspended sediment transport with the characteristics of the channel geometry parameters suggests the possibility of constructing a model in which the rate of change in the suspended sediment concentration downstream increases in small and very large drainage basins and decreases in basins of intermediate size.-Author
| Original language | English |
|---|---|
| Pages (from-to) | 491-494 |
| Number of pages | 4 |
| Journal | Zeitschrift fur Geomorphologie |
| Volume | 26 |
| Issue number | 4 |
| State | Published - 1982 |
ASJC Scopus subject areas
- Geography, Planning and Development
- Earth and Planetary Sciences (miscellaneous)