Abstract
Iverson and George largely agree with our mathematical description of the dispersive pressure and dilatancy for a dry granular avalanche; however, they disagree with our views of effective stress and pore-fluid pressure in a debris flow containing solid granular material fully or partially submerged in a muddy fluid. Here we counter their concerns by deriving time-dependent relations for pore-fluid pressure in a two-component debris flow in which the solid phase is undergoing dilations and contractions. This analysis was not contained in our original paper. We explicitly show how the excess fluid pressure arises from dispersive accelerations associated with changes in configuration of the solid material. Additional contributions to the pore-fluid pressure are associated with the solid–fluid drag and buoyancy. In our analysis, we find that pore-fluid pressures can only be calculated (1) by modelling their time-dependent source, the frictional work rate, and (2) by accounting for the time-dependent inertial forces associated with the solid configuration’s center of mass. This leads to an alternative physical description of pore-fluid pressure, especially when the debris flow is far from equilibrium.
References
Bartelt P, Buser O (2016) The relation between dilatancy, effective stress and dispersive pressure in granular avalanches. Acta Geotech 549–557. doi:10.1007/s11440-016-0463-7
Bartelt P, Buser O, Vera Valero C, Bühler Y (2016) Configurational energy and the formation of mixed flowing/ powder snow and ice avalanches, Ann Glaciol 57(71) doi:10.3189/2016AoG71A464
Buser O, Bartelt P (2015) An energy-based method to calculate streamwise density variations in snow avalanches. J Glaciol 61(227): doi:10.3189/2015JoG14J054
George D, Iverson RM (2014) A depth-averaged debris-flow model that includes the effects of evolving dilatancy. II. Numerical predictions and experimental tests. In: Proceedings of Royal Society A 470: 20130820. http://dx.doi.org/10.1098/rspa.2013.0820
Iverson R, George D (2014) A depth-averaged debris-flow model that includes the effects of evolving dilatancy. I. Physical basis. In: Proceedings of Royal Society. A 470: 20130819. http://dx.doi.org/10.1098/rspa.2013.0819
McArdell BW, Bartelt P, Kowalski J (2007) Field observations of basal forces and fluid pressure in a debris flow. Geophys Res Lett 34:L07406. doi:10.1029/2006GL029183
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Bartelt, P., Buser, O. Reply to “Discussion of “The relation between dilatancy, effective stress and dispersive pressure in granular avalanches” by P. Bartelt and O. Buser (DOI: 10.1007/s11440-016-0463-7)” by Richard Iverson and David L. George (DOI: 10.1007/s11440-016-0502-4). Acta Geotech. 11, 1469–1473 (2016). https://doi.org/10.1007/s11440-016-0503-3
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DOI: https://doi.org/10.1007/s11440-016-0503-3