International audienceWe revisit, via a very simplified set of equations, a linear streaming instability (technically an overstability), which is present in, and potentially important for, dusty protoplanetary discs. The goal is a better understanding of the physical origin of such instabilities, which are notoriously subtle. Rotational dynamics seem to be essential to this type of instability, which cannot be captured by one-dimensional Cartesian models. Dust 'pile-ups' in moving pressure maxima are an important triggering mechanism of the instability, and drag feedback of dust upon the gas allows these maxima to be strengthened. Coriolis forces and the background drift counteract the effects of the pressure force
We identify and study a number of new, rapidly growing instabilities of dust grains in protoplanetar...
According to the core accretion theory, rocky planets form by growing the initial micron-sized dust ...
We investigate streaming instability using two-fluid approximation (neutral gas and dust) in a quasi...
International audienceWe revisit, via a very simplified set of equations, a linear streaming instabi...
We revisit, via a very simplified set of equations, a linear streaming instability (tech-nically an ...
We develop simple, physically motivated models for drag-induced dust–gas streaming instabilities, wh...
We develop simple, physically motivated models for drag-induced dust–gas streaming instabilities, wh...
International audienceStreaming instability is a powerful mechanism which concentrates dust grains i...
International audienceStreaming instability is a powerful mechanism which concentrates dust grains i...
The radial pressure gradient (RPG), along the midplane of gaseous protoplanetary disks (PPD) – plane...
The streaming instability is a promising mechanism to induce the formation of planetesimals. Nonethe...
International audienceStreaming instability is a powerful mechanism which concentrates dust grains i...
The radial pressure gradient (RPG) along the midplane of gaseous protoplanetary disks – planetary nu...
The streaming instability is a leading candidate mechanism to explain the formation of planetesimals...
The streaming instability is a promising mechanism to induce the formation of planetesimals. Nonethe...
We identify and study a number of new, rapidly growing instabilities of dust grains in protoplanetar...
According to the core accretion theory, rocky planets form by growing the initial micron-sized dust ...
We investigate streaming instability using two-fluid approximation (neutral gas and dust) in a quasi...
International audienceWe revisit, via a very simplified set of equations, a linear streaming instabi...
We revisit, via a very simplified set of equations, a linear streaming instability (tech-nically an ...
We develop simple, physically motivated models for drag-induced dust–gas streaming instabilities, wh...
We develop simple, physically motivated models for drag-induced dust–gas streaming instabilities, wh...
International audienceStreaming instability is a powerful mechanism which concentrates dust grains i...
International audienceStreaming instability is a powerful mechanism which concentrates dust grains i...
The radial pressure gradient (RPG), along the midplane of gaseous protoplanetary disks (PPD) – plane...
The streaming instability is a promising mechanism to induce the formation of planetesimals. Nonethe...
International audienceStreaming instability is a powerful mechanism which concentrates dust grains i...
The radial pressure gradient (RPG) along the midplane of gaseous protoplanetary disks – planetary nu...
The streaming instability is a leading candidate mechanism to explain the formation of planetesimals...
The streaming instability is a promising mechanism to induce the formation of planetesimals. Nonethe...
We identify and study a number of new, rapidly growing instabilities of dust grains in protoplanetar...
According to the core accretion theory, rocky planets form by growing the initial micron-sized dust ...
We investigate streaming instability using two-fluid approximation (neutral gas and dust) in a quasi...