𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Sediment transport in alluvial streams

✍ Scribed by V. S. Altunin


Publisher
Springer
Year
1975
Tongue
English
Weight
443 KB
Volume
9
Category
Article
ISSN
1570-1468

No coin nor oath required. For personal study only.


πŸ“œ SIMILAR VOLUMES


Relating stream-bank erosion to in-strea
✍ Timothy R. Green; Sara G. Beavis; Claude R. Dietrich; Anthony J. Jakeman πŸ“‚ Article πŸ“… 1999 πŸ› John Wiley and Sons 🌐 English βš– 219 KB

We seek an improved and quantitative understanding of the sources and transport of sediment and attached phosphorus in upland catchments and downstream reaches of the Namoi River in New South Wales, Australia. Study of the sources of phosphorus and related sediment was motivated by severe problems w

Sediment mobility and bedload transport
✍ Luca Mao; Mario Aristide Lenzi πŸ“‚ Article πŸ“… 2007 πŸ› John Wiley and Sons 🌐 English βš– 236 KB

## Abstract The mobility conditions of bedload transport in an alpine high‐gradient step–pool stream (Rio Cordon) are analysed. Since 1986, a device system at the downstream end section of the stream has been operating in order to monitor the water discharge, suspended sediment and bedload transpor

Hydrogeomorphic linkages of sediment tra
✍ Takashi Gomi; Roy C. Sidle; Douglas N. Swanston πŸ“‚ Article πŸ“… 2004 πŸ› John Wiley and Sons 🌐 English βš– 440 KB

## Abstract Hydrogemorphic linkages related to sediment transport in headwater streams following basin wide clear‐cut logging on Prince of Wales Island, southeast Alaska, were investigated. Landslides and debris flows transported sediment and woody debris in headwater tributaries in 1961, 1979, and

Modelling sediment transport in stream c
✍ K. D. Sharma; J. S. R. Murthy πŸ“‚ Article πŸ“… 1994 πŸ› John Wiley and Sons 🌐 English βš– 318 KB

## Abstract Ephemeral channels in arid regions convey larger amounts of sediment than perennial channels in humid regions. Sediment graphs at the outlet of channels have been derived by the standard sediment rating curve technique and by a lumped model based on the instantaneous unit sediment graph