Fundamental changes of granular flow dynamics, deposition, and erosion processes at high slope angles: Insights from laboratory experiments. Issue 3 (13th March 2014)
- Record Type:
- Journal Article
- Title:
- Fundamental changes of granular flow dynamics, deposition, and erosion processes at high slope angles: Insights from laboratory experiments. Issue 3 (13th March 2014)
- Main Title:
- Fundamental changes of granular flow dynamics, deposition, and erosion processes at high slope angles: Insights from laboratory experiments
- Authors:
- Farin, Maxime
Mangeney, Anne
Roche, Olivier - Abstract:
- <abstract abstract-type="main" id="jgrf20183-abs-0001"> <title> <x xml:space="preserve">Abstract</x> </title> <p id="jgrf20183-para-0001">Entrainment of underlying debris by geophysical flows can significantly increase the flow deposit extent. To study this phenomenon, analog laboratory experiments have been conducted on granular column collapse over an inclined channel with and without an erodible bed made of similar granular material. Results show that for slope angles below a critical value <italic>θ</italic><sub><italic>c</italic></sub>, between 10° and 16°, the run out distance <italic>r</italic><sub><italic>f</italic></sub> depends only on the initial column height <italic>h</italic><sub>0</sub> and is unaffected by the presence of an erodible bed. On steeper slopes, the flow dynamics change fundamentally, with a slow propagation phase developing after flow front deceleration, significantly extending the flow duration. This phase has characteristics similar to those of steady uniform flows. Its duration increases with increasing slope angle, column volume, column inclination with respect to the slope and channel width, decreasing column aspect ratio (height over length), and in the presence of an erodible bed. It is independent, however, of the maximum front velocity. The increase in the duration of the slow propagation phase has a crucial effect on flow dynamics and deposition. Over a rigid bed, the development of this phase leads to run out distances<abstract abstract-type="main" id="jgrf20183-abs-0001"> <title> <x xml:space="preserve">Abstract</x> </title> <p id="jgrf20183-para-0001">Entrainment of underlying debris by geophysical flows can significantly increase the flow deposit extent. To study this phenomenon, analog laboratory experiments have been conducted on granular column collapse over an inclined channel with and without an erodible bed made of similar granular material. Results show that for slope angles below a critical value <italic>θ</italic><sub><italic>c</italic></sub>, between 10° and 16°, the run out distance <italic>r</italic><sub><italic>f</italic></sub> depends only on the initial column height <italic>h</italic><sub>0</sub> and is unaffected by the presence of an erodible bed. On steeper slopes, the flow dynamics change fundamentally, with a slow propagation phase developing after flow front deceleration, significantly extending the flow duration. This phase has characteristics similar to those of steady uniform flows. Its duration increases with increasing slope angle, column volume, column inclination with respect to the slope and channel width, decreasing column aspect ratio (height over length), and in the presence of an erodible bed. It is independent, however, of the maximum front velocity. The increase in the duration of the slow propagation phase has a crucial effect on flow dynamics and deposition. Over a rigid bed, the development of this phase leads to run out distances <italic>r</italic><sub><italic>f</italic></sub> that depend on both the initial column height <italic>h</italic><sub>0</sub> and length <italic>r</italic><sub>0</sub>. Over an erodible bed, as the duration of the slow propagation phase increases, the duration of bed excavation increases, leading to a greater increase in the run out distance compared with that over a rigid bed (up to 50%). This effect is even more pronounced as bed compaction decreases.</p> </abstract> … (more)
- Is Part Of:
- Journal of geophysical research. Volume 119:Issue 3(2014:Sep.)
- Journal:
- Journal of geophysical research
- Issue:
- Volume 119:Issue 3(2014:Sep.)
- Issue Display:
- Volume 119, Issue 3 (2014)
- Year:
- 2014
- Volume:
- 119
- Issue:
- 3
- Issue Sort Value:
- 2014-0119-0003-0000
- Page Start:
- 504
- Page End:
- 532
- Publication Date:
- 2014-03-13
- Subjects:
- Geomorphology -- Periodicals
551.3 - Journal URLs:
- http://onlinelibrary.wiley.com/journal/10.1002/(ISSN)2169-9011 ↗
http://onlinelibrary.wiley.com/ ↗ - DOI:
- 10.1002/2013JF002750 ↗
- Languages:
- English
- ISSNs:
- 2169-9003
- Deposit Type:
- Legaldeposit
- View Content:
- Available online (eLD content is only available in our Reading Rooms) ↗
- Physical Locations:
- British Library DSC - 4995.004000
British Library DSC - BLDSS-3PM
British Library HMNTS - ELD Digital store - Ingest File:
- 3279.xml