Hyperconcentrated flow — transitional process between water flow and debris flow
Author:
- Thomas C. PiersonTPThomas C. Pierson
- 26 December 2007
- book chapter
- Published by Springer Nature
- p. 159-202
Abstract
No abstract availableThis publication has 52 references indexed in Scilit:
- Suspended sediment transport during tropical‐cyclone floods in FijiHydrological Processes, 2002
- Implication of relationships among suspended sediment size, water discharge and suspended sediment concentration: the Yellow River basin, ChinaCATENA, 2002
- Erosion caused by hyperconcentrated flow on the Loess Plateau of ChinaCATENA, 1999
- The physics of debris flowsReviews of Geophysics, 1997
- Changes in Whangaehu river lahar characteristics during the 1995 eruption sequence, Ruapehu volcano, New ZealandJournal of Volcanology and Geothermal Research, 1997
- Settling behaviour of concentrated dispersions and some volcanological applicationsJournal of Volcanology and Geothermal Research, 1995
- The non-layering of gravel streambeds under ephemeral flood regimesJournal of Hydrology, 1994
- Stream‐driven, high‐density gravelly traction carpets: possible deposits in the Trabeg Conglomerate Formation, SW Ireland and some theoretical considerations of their originSedimentology, 1989
- Volcanic influences on terrestrial sedimentationGeology, 1989
- The yield stress myth?Rheologica Acta, 1985