Article
Geochemistry & Geophysics
L. Battershill, C. N. Whittaker, E. M. Lane, S. Popinet, J. D. L. White, W. L. Power, P. Nomikou
Summary: This study explores the impact of pyroclastic density currents (PDCs) on tsunami generation and uses experimental assumptions to approximate the fluid dynamics of PDC. The results show that the boundary condition of the slope and the viscosity of the dense granular-fluid have significant influence on the characteristics of generated waves.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2021)
Article
Geosciences, Multidisciplinary
Jorge Macias, Cipriano Escalante, Manuel J. Castro
Summary: The study aims to propose a numerical tool benchmarked by NTHMP for assessing landslide-generated tsunami hazards. The Multilayer-HySEA model is validated using laboratory data and applied to granular slides. The results demonstrate the effectiveness of using the multilayer model to deal with tsunamis generated by granular slides.
NATURAL HAZARDS AND EARTH SYSTEM SCIENCES
(2021)
Article
Geosciences, Multidisciplinary
Yaxiong Shen, Colin N. Whittaker, Emily M. Lane, James D. L. White, William Power, Bruce W. Melville
Summary: In laboratory experiments, it was found that submarine volcanic eruptions can generate localized tsunamis through injections of non-condensable expanding air into fresh water. The maximum wave height reaches a saturation duration above which it will not increase as the eruption continues, with the saturation duration positively correlated with source intensity and negatively with water depth. Additionally, there is a critical water depth where an eruption with a given source intensity can generate the largest waves, influencing tsunami size and hazard.
GEOPHYSICAL RESEARCH LETTERS
(2021)
Article
Oceanography
Natalia Lipiejko, Colin N. Whittaker, Emily M. Lane, William L. Power
Summary: This study investigates tsunami generation by fluidized granular flows and analyzes published relationships predicting maximum wave amplitudes. The results show that flows of greater mass generate high-amplitude waves, while flows of lower mass generate low-amplitude waves that decrease with distance from the shore. The predictive equations provide relatively accurate predictions of the maximum wave amplitudes.
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
(2023)
Article
Engineering, Geological
B. Cagnoli
Summary: The study on simulating granular flows of angular rock fragments using the discrete element method found that while large-scale flows generate stresses that affect flow mobility, those that slide en mass are not influenced by stress levels. However, stress level governs flow mobility in cases where granular flow dynamics is affected by clast agitation and collisions.
Article
Engineering, Civil
Valentin Heller, Tommaso Attili, Fan Chen, Roman Gabl, Guido Wolters
Summary: Mass balance analysis of ice sheets is crucial to understanding the impacts of global warming, particularly in the context of iceberg calving which can lead to significant iceberg-tsunamis. Experimental studies on different calving mechanisms revealed that gravity-dominated mechanisms produce much larger tsunamis. Empirical equations were developed to predict maximum wave height, amplitude, and period for different calving mechanisms, with key dimensionless parameters identified for hazard assessment and mitigation.
COASTAL ENGINEERING
(2021)
Article
Multidisciplinary Sciences
Manon Robbe-Saule, Cyprien Morize, Yann Bertho, Alban Sauret, Anthony Hildenbrand, Philippe Gondret
Summary: Modeling tsunami waves generated by subaerial landslides is crucial for accurate hazard and risk assessments in coastal areas. Small-scale laboratory experiments show a strong correlation between the amplitude of generated waves and the volume of grains, offering a reliable way to estimate the amplitudes of paleo-tsunamis. Despite differences in scale and geometry, there is a good agreement between experimental laws and field data.
SCIENTIFIC REPORTS
(2021)
Article
Materials Science, Multidisciplinary
Breard C. P. Eric, Fullard Luke, Dufek Josef, Tennenbaum Michael, Fernandez-Nieves Alberto, Dietiker Jean-Francois
Summary: Natural geophysical mass flows are complex granular systems affected by the presence of interstitial fluid. This study uses discrete element modelling and post-processing techniques to investigate the rheology of these flows. The results highlight the need to understand velocity fluctuations for predicting the effective viscosity of sheared fluidized mixtures, with implications for various geophysical flows.
Article
Geosciences, Multidisciplinary
M. Arran, A. Mangeney, J. De Rosny, M. Farin, R. Toussaint, O. Roche
Summary: Geophysical granular flows produce seismic signals via basal forces, with various models attempting to predict these signals' high-frequency components. Experimental results show that Farin et al.'s thin-flow model is the most accurate, and normalization of force fluctuations is determined by the flow's bulk inertial number.
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE
(2021)
Article
Mechanics
Manon Robbe-Saule, Cyprien Morize, Robin Henaff, Yann Bertho, Alban Sauret, Philippe Gondret
Summary: The study investigates the generation of a tsunami wave by an aerial landslide through model laboratory experiments. It is found that the collective entry of granular material into water governs the wave generation process, with the amplitude of the wave linearly scaling with the water height. The density of the falling grains has a negligible influence on the wave amplitude, suggesting that the volume of grains entering the water is the relevant parameter in wave generation.
JOURNAL OF FLUID MECHANICS
(2021)
Article
Geosciences, Multidisciplinary
Junhan Du, Gordon G. D. Zhou, Kahlil F. E. Cui
Summary: In this study, DEM simulations are conducted to investigate particle-bed interactions in granular flows. Basal normal and shear stresses are recorded and analyzed, showing a transition from dense to dilute flow regime at a critical Savage number of 0.1. Maximum basal stresses scale with particle-bed impact velocities in a power law relation, while stress fluctuations scale with granular temperature. A unified scaling law is proposed to relate the standard deviation of basal stresses to free particle volume. This study provides important physical insights into granular flow behavior for hazard risk management.
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE
(2023)
Article
Geosciences, Multidisciplinary
Alvaro Aravena, Laurent Chupin, Thierry Dubois, Olivier Roche
Summary: Numerical simulations were conducted to investigate the influence of gas pore pressure on granular flows, revealing that a constant effective pore pressure diffusion coefficient can accurately reproduce dam-break experiment dynamics. Increasing the surface slope angle significantly increases the run-out distance of the flow, with implications for pyroclastic density currents at gentle slope angles.
BULLETIN OF VOLCANOLOGY
(2021)
Article
Geochemistry & Geophysics
Indujaa Ganesh, Luke A. McGuire, Lynn M. Carter
Summary: The study investigates the potential formation of young deposits with unique radar characteristics near volcanic and coronal summits on Venus. It suggests that pyroclastic density currents (PDCs) could be responsible for these extensive, long-runout deposits showing moderate to high radar backscatter. Modeling the dynamics of dense PDCs reveals the importance of pyroclastic flow fluidization via high pore pressure in emplacing long-runout deposits along gently sloping volcanic flanks.
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
(2021)
Article
Geochemistry & Geophysics
B. Cagnoli
Summary: Numerical simulations indicate that the positive correlation between grain size increase, particle agitation increase, and granular flow mobility increase observed in laboratory experiments is not a causal relationship. Instead, the flow interruption is caused by a collision with the horizontal flume at the bottom of a steep incline. Laboratory experiments and simulations demonstrate that unhindered dense granular flows exhibit increased mobility when grain size and clast agitation decrease. Consequently, there is no evidence to support the idea that high mobility in large natural rock avalanches is due to increased particle agitation.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2023)
Article
Mechanics
Lu Jing, Julio M. Ottino, Paul B. Umbanhowar, Richard M. Lueptow
Summary: The drag force on a spherical intruder in dense granular shear flows is studied using discrete element method simulations. Three regimes of the intruder dynamics are observed depending on the magnitude of the drag force and the flow inertial number. A quantitative similarity is found between the intruder drag in granular shear flows and the Stokesian drag on a sphere in a viscous fluid. A modified Stokes drag model is developed that accounts for the secondary dependence of the drag coefficient on the inertial number and the intruder size and density ratios.
JOURNAL OF FLUID MECHANICS
(2022)
Article
Multidisciplinary Sciences
S. van den Wildenberg, X. Jia, O. Roche
SCIENTIFIC REPORTS
(2020)
Article
Geosciences, Multidisciplinary
Allan Fries, Olivier Roche, Guillaume Carazzo
Summary: The study conducted analogue laboratory experiments on pyroclastic fountain collapse, revealing that the concentration of particles is inversely proportional to the drop height, and the separation between particles and ambient air causes the material to deflate and propagate laterally. Measurements at the impingement surface showed that high air-particle relative velocity during deflation can generate pore fluid pressure up to 50% of the weight of the granular flow.
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH
(2021)
Article
Oceanography
Alexis Bougouin, Olivier Roche, Raphael Paris, Herbert E. Huppert
Summary: Granular flows moving down mountainsides and entering water bodies create granular jets and particle-driven gravity currents, with hydrodynamic forces mainly slowing down and reducing the spread of granular masses. The experimental study demonstrates that the temporal evolution of these flows can be described by ballistic motion theory and scaling laws, highlighting the complexity of dynamics and deposits when granular masses encounter water bodies.
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
(2021)
Article
Geosciences, Multidisciplinary
Alessandro Tadini, Olivier Roche, Pablo Samaniego, Nourddine Azzaoui, Andrea Bevilacqua, Arnaud Guillin, Mathieu Gouhier, Benjamin Bernard, Willy Aspinall, Silvana Hidalgo, Julia Eychenne, Mattia De' Michieli Vitturi, Augusto Neri, Raffaello Cioni, Marco Pistolesi, Elizabeth Gaunt, Silvia Vallejo, Marjorie Encalada, Hugo Yepes, Antonio Proano, Mia Pique
Summary: This study probabilistically assesses the future occurrence of explosive eruptive activity at Cotopaxi and Guagua Pichincha volcanoes in Ecuador utilizing expert elicitation. The findings suggest that the most probable next eruption type for Cotopaxi is an andesitic hydrovolcanic/ash-emission, while for Guagua Pichincha it is a vulcanian event. There is also a significant chance of a violent explosive event, particularly for Cotopaxi.
BULLETIN OF VOLCANOLOGY
(2021)
Article
Geosciences, Multidisciplinary
M. Arran, A. Mangeney, J. De Rosny, M. Farin, R. Toussaint, O. Roche
Summary: Geophysical granular flows produce seismic signals via basal forces, with various models attempting to predict these signals' high-frequency components. Experimental results show that Farin et al.'s thin-flow model is the most accurate, and normalization of force fluctuations is determined by the flow's bulk inertial number.
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE
(2021)
Article
Geochemistry & Geophysics
Olivier Roche, Nourddine Azzaoui, Arnaud Guillin
Summary: Through quantitative analysis of 47 data sets, this study demonstrates the significant impact of discharge rate of explosive volcanic eruptions on the runout distance of pyroclastic density currents. It also reveals a linear correlation between runout distance and discharge rate for dilute turbulent flows and two-layer flows with concentrated bases.
EARTH AND PLANETARY SCIENCE LETTERS
(2021)
Article
Geosciences, Multidisciplinary
Alvaro Aravena, Laurent Chupin, Thierry Dubois, Olivier Roche
Summary: Numerical simulations were conducted to investigate the influence of gas pore pressure on granular flows, revealing that a constant effective pore pressure diffusion coefficient can accurately reproduce dam-break experiment dynamics. Increasing the surface slope angle significantly increases the run-out distance of the flow, with implications for pyroclastic density currents at gentle slope angles.
BULLETIN OF VOLCANOLOGY
(2021)
Article
Geochemistry & Geophysics
A. Tadini, N. Azzaoui, O. Roche, P. Samaniego, B. Bernard, A. Bevilacqua, S. Hidalgo, A. Guillin, M. Gouhier
Summary: This study conducts a hazard assessment for tephra fallout on two active volcanoes in Ecuador, using probabilistic maps and numerical models. The uncertainty of the input parameters, physical approximations, and eruption type occurrence probabilities are quantified through expert elicitation, correlations between parameters, and correction coefficients. The results include maps of exceedance probability and thickness, as well as hazard curves for sensitive sites in Quito.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2022)
Article
Geosciences, Multidisciplinary
Jean-Guillaume Feignon, Nicolas Cluzel, Federica Schiavi, Severine Moune, Olivier Roche, Jorge Clavero, Pierre Schiano, Marion Auxerre
Summary: Mocho-Choshuenco volcano is one of the most hazardous volcanoes in the southern volcanic zone of Chile, but it is still relatively little studied. A study of the 1600-year-old Enco eruption revealed that it was triggered by the mixing of a CO2-rich basaltic magma with a shallower andesitic magma.
BULLETIN OF VOLCANOLOGY
(2022)
Article
Geochemistry & Geophysics
Baptiste Penlou, Olivier Roche, Michael Manga, Siet van den Wildenberg
Summary: The dynamics of geophysical dilute turbulent gas-particles mixtures are influenced by particle concentration, which depends mainly on particle settling velocity. This study investigates air-particle mixtures in a vertical pipe where the ascending air flux matches the settling velocity of glass particles. The results show an interplay between hindered settling and cluster-induced enhanced settling, which have implications for volcanic plumes and pyroclastic currents.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2023)
Article
Physics, Fluids & Plasmas
Olivier Roche, Siet van den Wildenberg, Alexandre Valance, Renaud Delannay, Anne Mangeney, Lucas Corna, Thierry Latchimy
Summary: The study investigated the basal force components of granular material flowing down a smooth incline, finding that the basal friction coefficient increases with slope angle and weakens with increasing particle holdup. At low angles, the basal friction is slightly less than or equal to tan theta, with deviation interpreted as a contribution from the sidewall friction. At larger angles, basal friction saturates at an asymptotic value dependent on the chute's gate opening. The study's data confirmed recent discrete numerical simulations, showing that the variation of basal friction can be captured through a unique Froude number and that mean velocity scales with particle holdup.