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Porosity and size gradation of saturated gravel with percolated fines

Autor
Núñez, F.; Martín-Vide, J.P.; Kleinhans, G.
Tipus d'activitat
Article en revista
Revista
Sedimentology
Data de publicació
2016-08
Volum
63
Número
5
Pàgina inicial
1209
Pàgina final
1232
DOI
https://doi.org/10.1111/sed.12257 Obrir en finestra nova
Repositori
http://hdl.handle.net/2117/88894 Obrir en finestra nova
URL
http://onlinelibrary.wiley.com/doi/10.1111/sed.12257/abstract Obrir en finestra nova
Resum
Fine particles may infiltrate through coarse alluvial beds and eventually saturate the subsurface pore space. It is essential to understand the conditions that lead to bed saturation, and to forecast the packing characteristics of saturated beds to assess the effect of excess fine sediment supply on a number of processes that occur in the stream-sediment boundary. To address this problem, in this study, a new method is introduced to predict the grain-size distribution for the saturated condition...
Citació
Núñez, F., Martín-Vide, J.P., Kleinhans, G. Porosity and size gradation of saturated gravel with percolated fines. "Sedimentology", Agost 2016, vol. 63, núm. 5, p. 1209-1232.
Paraules clau
BED RIVERS, Clogging, DEPOSITION, FRAMEWORK DILATION, HYPORHEIC INTERSTICES, MODEL, PARTICLE MIXTURES, RANDOM PACKING, SAND, SEDIMENT INFILTRATION, TRANSPORT RATES, colmation, infiltration, porosity, sediment mixtures, siltation

Participants

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