Roche Olivier, Montserrat S., Nino Y., Tamburrino A. (2010). Pore fluid pressure and internal kinematics of gravitational laboratory air-particle flows : insights into the emplacement dynamics of pyroclastic flows. Journal of Geophysical Research.Solid Earth, 115, p. B09206. ISSN 0148-0227.
Titre du document
Pore fluid pressure and internal kinematics of gravitational laboratory air-particle flows : insights into the emplacement dynamics of pyroclastic flows
Roche Olivier, Montserrat S., Nino Y., Tamburrino A.
Source
Journal of Geophysical Research.Solid Earth, 2010,
115, p. B09206 ISSN 0148-0227
The emplacement dynamics of pyroclastic flows were investigated through noninvasive measurements of the pore fluid pressure in laboratory air-particle flows generated from the release of fluidized and nonfluidized granular columns. Analyses of high-speed videos allowed for correlation of the pressure signal with the flow structure. The flows consisted of a sliding head that caused underpressure relative to the ambient, followed by a body that generated overpressure and at the base of which a deposit aggraded. For initially fluidized flows, overpressure in the body derived from advection of the pore pressure generated in the initial column and decreased by diffusion during propagation. Relatively slow diffusion caused the pore pressure in the thinner flow to be larger than lithostatic at early stages. Furthermore, partial auto-fluidization, revealed in initially nonfluidized flows, also occurred and contributed to maintain high pore pressure, whereas dilation or contraction of the air-particle mixture with associated drag and/or pore volume variation transiently led the pressure to decrease or increase, respectively. The combination of all these processes resulted in long-lived high pore fluid pressure in the body of the flows during most of their emplacement. In the case of the initially fluidized and slightly expanded (similar to 3-4%) flows, (at least) similar to 70%-100% of the weight of the particles was supported by pore pressure, which is consistent with their inertial fluid-like behavior. Dense pyroclastic flows on subhorizontal slopes are expected to propagate as inertial fluidized gas-particle mixtures consisting of a sliding head, possibly entraining basement-derived clasts, and of a gradually depositing body.
