The Basal Friction Coefficient of Granular Flows With and Without Excess Pore Pressure: Implications for Pyroclastic Density Currents, Water‐Rich Debris Flows, and Rock and Submarine Avalanches-Reference-Cited by-同舟云学术

The Basal Friction Coefficient of Granular Flows With and Without Excess Pore Pressure: Implications for Pyroclastic Density Currents, Water‐Rich Debris Flows, and Rock and Submarine Avalanches

Published:2020-12 Issue:12 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Breard Eric C. P.¹^ORCID,Dufek Josef¹^ORCID,Fullard Luke²^ORCID,Carrara Alexandre³^ORCID

Affiliation:

1. Department of Earth Sciences University of Oregon Eugene OR USA

2. School of Food and Advanced Technology Massey University Palmerston North New Zealand

3. Institut des Sciences de la Terre University Grenoble Alpes, Université Savoie Mont Blanc, CNRS, IRD, IFSTTAR Grenoble France

Funder

Royal Society Te Apārangi

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JB020203

Reference97 articles.

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2. Viscoinertial regime of immersed granular flows

3. Granular Media

4. Effective Wall Friction in Wall-Bounded 3D Dense Granular Flows

5. Well-posed and ill-posed behaviour of the -rheology for granular flow

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