Microbial community structure in recovering forests of Mount St. Helens. [PDF]
Maltz MR +8 more
europepmc +1 more source
Bananas in the aftermath of La Palma volcanic eruption (Canary Islands, Spain): A study on the nutritional and toxic element composition of post-disaster production. [PDF]
Rodríguez-Hernández Á +8 more
europepmc +1 more source
Airfall volume of the 15 January 2022 eruption of Hunga volcano estimated from ocean color changes. [PDF]
Kelly LJ +7 more
europepmc +1 more source
Iron is an important influence of volcanic ash input on the evolution of deep-sea ecosystems. [PDF]
Bai S +5 more
europepmc +1 more source
A more reduced mantle beneath the lunar South Pole-Aitken basin. [PDF]
Zhang H +16 more
europepmc +1 more source
Characterising pyroclastic density current grainsize data
Engwell, Samantha +2 more
openaire +1 more source
Pyroclastic density currents: state of the art and perspectives
Pyroclastic density currents (PDCs) are mixtures of two components, namely solid particles and fluid (gas) phase. They macroscopically behave as dense, multiphase gravity currents (flowing pyroclastic mixtures of particles and gas) immersed in a less dense, almost isotropic fluid (the atmosphere).
Sulpizio R
exaly +5 more sources
Erosional characteristics and behavior of large pyroclastic density currents
Factors influencing the erosive behavior of large pyroclastic density currents (PDCs), both mainly massive and thinly stratified, are not well understood. To investigate the parameters influencing the erosive behavior of PDCs produced during the flowing phase of large, caldera-forming Plinian (Campanian Ignimbrite) and phreatoplinian (Neapolitan Yellow
SCARPATI, CLAUDIO, Perrotta A.
core +6 more sources
Related searches:
A fast, calibrated model for pyroclastic density currents kinematics and hazard
Journal of Volcanology and Geothermal Research, 2016Abstract Multiphase flow models represent valuable tools for the study of the complex, non-equilibrium dynamics of pyroclastic density currents. Particle sedimentation, flow stratification and rheological changes, depending on the flow regime, interaction with topographic obstacles, turbulent air entrainment, buoyancy reversal, and other complex ...
Tomaso Esposti Ongaro, Fulvio Cornolti
exaly +3 more sources
Deposits of Pyroclastic Density Currents
2015Richard J Brown, Graham D M Andrews
exaly +2 more sources

