Understanding how gasses escape from particle-rich suspensions has important applications in nature and industry. Motivated by applications such as outgassing of crystal-rich magmas, we map gas migration patterns in experiments where we vary (1) particle fractions and liquid viscosity (10–500 Pa s), (2) container shape (horizontal parallel plates and upright cylinders), and (3) methods of bubble generation (single bubble injections, and multiple bubble generation with chemical reactions). We identify two successive changes in gas migration behavior that are determined by the normalized particle fraction (relative to random close packing), and are insensitive to liquid viscosity, bubble growth rate or container shape within the explored rang...
Wettability is an important factor which controls the displacement of immiscible fluids in permeable...
Effective models for the evolution of magma permeability are key to understanding shallow magma asce...
Soft sediments exhibit complex and varied deformation behavior during in situ bubble growth, however...
Crystals can occupy ∼0 to 100% of the total magma volume, but their role in outgassing remains poorl...
Strombolian volcanic explosions are commonly attributed to the rise and burst of conduit-filling gas...
During magma ascent, bubbles nucleate, grow, coalesce, and form a variably permeable porous network....
International audienceBubble nucleation, growth, and coalescence control the ascent, degassing, and ...
As magma ascends, the bubbles that develop within it affect eruption style and, thus, understanding ...
AbstractVolcanic eruptions are driven by the growth of gas bubbles in magma. Bubbles grow when disso...
International audienceVolcanic eruptions are driven by the growth of gas bubbles in magma. Bubbles g...
Volcanic eruptions are driven by the growth of gas bubbles in magma. Bubbles grow when dissolved vol...
During magma ascent, bubbles nucleate, grow, coalesce, and form a variably permeable porous network....
International audienceThe mechanisms governing permeability development in rising magmas influence t...
Multiphase flows in deformable porous materials are important in numerous geological and geotechnica...
Gas migration through a soft granular material involves a strong coupling between the motion of the ...
Wettability is an important factor which controls the displacement of immiscible fluids in permeable...
Effective models for the evolution of magma permeability are key to understanding shallow magma asce...
Soft sediments exhibit complex and varied deformation behavior during in situ bubble growth, however...
Crystals can occupy ∼0 to 100% of the total magma volume, but their role in outgassing remains poorl...
Strombolian volcanic explosions are commonly attributed to the rise and burst of conduit-filling gas...
During magma ascent, bubbles nucleate, grow, coalesce, and form a variably permeable porous network....
International audienceBubble nucleation, growth, and coalescence control the ascent, degassing, and ...
As magma ascends, the bubbles that develop within it affect eruption style and, thus, understanding ...
AbstractVolcanic eruptions are driven by the growth of gas bubbles in magma. Bubbles grow when disso...
International audienceVolcanic eruptions are driven by the growth of gas bubbles in magma. Bubbles g...
Volcanic eruptions are driven by the growth of gas bubbles in magma. Bubbles grow when dissolved vol...
During magma ascent, bubbles nucleate, grow, coalesce, and form a variably permeable porous network....
International audienceThe mechanisms governing permeability development in rising magmas influence t...
Multiphase flows in deformable porous materials are important in numerous geological and geotechnica...
Gas migration through a soft granular material involves a strong coupling between the motion of the ...
Wettability is an important factor which controls the displacement of immiscible fluids in permeable...
Effective models for the evolution of magma permeability are key to understanding shallow magma asce...
Soft sediments exhibit complex and varied deformation behavior during in situ bubble growth, however...