- Astro and Planetary Science
- Astrophysics and Star Formation Studies
- Stellar, planetary, and galactic studies
- Molecular Spectroscopy and Structure
- Planetary Science and Exploration
- Astronomy and Astrophysical Research
- Atmospheric Ozone and Climate
- Atmospheric chemistry and aerosols
- High-pressure geophysics and materials
- Advanced Combustion Engine Technologies
- Space Exploration and Technology
- Geological and Geochemical Analysis
- Atomic and Molecular Physics
- Spectroscopy and Laser Applications
- Cryospheric studies and observations
- Scientific Research and Discoveries
- Spacecraft and Cryogenic Technologies
- Modular Robots and Swarm Intelligence
- Thermodynamic properties of mixtures
- Meteorological Phenomena and Simulations
- Gas Dynamics and Kinetic Theory
- Science and Climate Studies
- Methane Hydrates and Related Phenomena
- Laser-induced spectroscopy and plasma
- Particle Dynamics in Fluid Flows
Tsinghua University
2019-2025
University of Amsterdam
2014-2019
University of California, Berkeley
2012-2015
Max Planck Institute for Astronomy
2009-2011
Max Planck Society
2010
University of Groningen
2006-2010
Heidelberg University
2010
SRON Netherlands Institute for Space Research
2010
Astronomical Institute of the Slovak Academy of Sciences
2005
Planetary bodies form by accretion of smaller bodies. It has been suggested that a very efficient way to grow protoplanets is accreting particles size <<km (e.g., chondrules, boulders, or fragments larger bodies) as they can be kept dynamically cold. We investigate the effects gas drag on impact radii and rates these particles. As simplifying assumptions we restrict our analysis 2D settings, law linear in velocity, laminar disk characterized smooth (global) pressure gradient causes drift...
The sticking of micron sized dust particles due to surface forces in circumstellar disks is the first stage production asteroids and planets. key ingredients that drive this process are relative velocity between environment complex physics aggregate collisions. Here we present results a collision model, which based on laboratory experiments these aggregates. We investigate maximum size mass can be reached by coagulation protoplanetary disks. model growth aggregates at 1 AU midplane three...
The growth processes from protoplanetary dust to planetesimals are not fully understood. Laboratory experiments and theoretical models have shown that collisions among the aggregates can lead sticking, bouncing, fragmentation. However, no systematic study on collisional outcome of has been performed so far a physical model evolution in disks is still missing. We intend map parameter space for interaction arbitrarily porous aggregates. This encompasses dust-aggregate masses, their porosities...
Context. Grains in circumstellar disks are believed to grow by mutual collisions and subsequent sticking due surface forces. Results of many fields research involving disks, such as radiative transfer calculations, disk chemistry, magneto-hydrodynamic simulations largely depend on the unknown grain size distribution. Aims. As detailed calculations growth fragmentation both numerically challenging computationally expensive, we aim find simple recipes analytical solutions for distribution a...
Close-in super-Earths having radii 1–4 R⊕ may possess hydrogen atmospheres comprising a few percent by mass of their rocky cores. We determine the conditions under which such can be accreted cores from parent circumstellar disks. Accretion nebula is problematic because it too efficient: we find that 10 M⊕ embedded in solar metallicity disks tend to undergo runaway gas accretion and explode into Jupiters, irrespective orbital location. The threat especially dire at ∼0.1 AU, where solids...
The formation of planetesimals in protoplanetary disks is not well-understood. Streaming instability a promising mechanism to directly form from pebble-sized particles, provided high enough solids-to-gas ratio. However, local enhancements the ratio are difficult realize smooth disk, which motivates consideration special disk locations such as snowline. In this article we investigate viability planetesimal by streaming near snowline due water diffusion and condensation. We adopt viscous...
In this note we present complete, closed-form expressions for random relative velocities between colliding particles of arbitrary size in nebula turbulence. These results are exact very small (those with stopping times much shorter than the large eddy overturn time) and also surprisingly accurate complete generality (that is, apply comparable to, or longer than, time). We that some previous studies may have adopted simple expressions, which find to be error regarding dependence particle regime.
Context.Sticking of colliding dust particles through van der Waals forces is the first stage in grain growth process protoplanetary disks, eventually leading to formation comets, asteroids and planets. A key aspect collisional evolution coupling between gas motions, which depends on internal structure (porosity) aggregates.
The cores in molecular clouds are the densest and coldest regions of interstellar medium (ISM). In these ISM-dust grains have potential to coagulate. This study investigates collisional evolution dust population by combining two models: a binary model that simulates collision between aggregates coagulation computes size distribution with time. first, results from parameter quantify outcome – sticking, fragmentation (shattering, breakage, erosion) effects on internal structure particles...
Following Paper I we investigate the properties of atmospheres that form around small protoplanets embedded in a protoplanetary disc by conducting hydrodynamical simulations. These are now extended to three dimensions, employing spherical grid centred on planet. Compression gas is shown reduce rotational motions. Contrasting 2D case, no clear boundary demarcates bound atmospheric from material; instead, find an open system where enters Bondi sphere at high latitudes and leaves through...
It is unknown how far dust growth can proceed by coagulation. Obstacles to collisional are the fragmentation and bouncing barriers. However, in all previous simulations of dust-size evolution protoplanetary disks, only mean collision velocity has been considered, neglecting that a small but possibly important fraction collisions will occur at both much lower higher velocities. We study effect probability distribution impact velocities on Assuming Maxwellian for colliding particles determine...
The dust size distribution in molecular clouds can be strongly affected by ice-mantle formation and (subsequent) grain coagulation. Following previous work where the has been calculated from a state-of-the art collision model for aggregates that involves both coagulation fragmentation (Paper I), corresponding opacities are presented this study. applying effective medium theory assuming mix of 0.1{\mu}m silicate graphite grains vacuum. In particular, we explore how affects near-IR opacity...
Context. Observations at sub-millimeter and mm wavelengths will in the near future be able to resolve radial dependence of spectral slope circumstellar disks with a resolution around few AU distance closest star-forming regions. Aims. We aim constrain physical models grain growth fragmentation by large sample (sub-)mm observations pre-main sequence stars Taurus-Auriga Ophiuchus Methods. State-of-the-art coagulation/fragmentation disk-structure codes are coupled produce steady-state size...
TRAPPIST-1 is a nearby 0.08 M M-star, which was recently found to harbor planetary system of at least seven Earth-mass planets, all within 0.1 au. The configuration confounds theorists as the planets are not easily explained by either in situ or migration models. In this Paper we present scenario for formation and orbital architecture system. our model, planet starts H2O iceline, where pebble-size particles -- whose origin outer disk concentrate trigger streaming instabilities. After their...
The population of close-in super-Earths, with gas mass fractions up to 10% represents a challenge for planet formation theory: how did they avoid runaway accretion and collapsing hot Jupiters despite their core masses being in the critical range $M_\mathrm{c} \simeq 10 M_\mathrm{\oplus}$? Previous three-dimensional (3D) hydrodynamical simulations indicate that atmospheres low-mass planets cannot be considered isolated from protoplanetary disc, contrary what is assumed 1D-evolutionary...
Context: Planet formation by pebble accretion is an alternative to planetesimal-driven core accretion. In this scenario, planets grow accreting cm-to-m-sized pebbles instead of km-sized planetesimals. One the main differences with increased thermal ablation experienced pebbles. This provides early enrichment planet's envelope, which changes process growth. Aims: We aim predict masses and envelope compositions that form compare mass deposition Methods: model growth a proto-planet calculating...
Turbulence plays a key role in the transport of pebble-sized particles. It also affects ability pebbles to be accreted by protoplanets, because it stirs out disk midplane. In addition, turbulence can suppress pebble accretion once relative velocities become too large for settling mechanism viable. Following Paper I, we aim quantify these effects calculating efficiency $\varepsilon$ using three-body simulations. To model effect on pebbles, derive stochastic equation motion (SEOM) applicable...
Recently, seven Earth-sized planets were discovered around the M-dwarf star TRAPPIST-1. Thanks to transit-timing variations, masses and therefore bulk densities of have been constrained, suggesting that all TRAPPIST-1 are consistent with water mass fractions on order 10%. These fractions, as well similar planet within system, constitute strong constraints origins system. In a previous work, we outlined pebble-driven formation scenario. this paper investigate scenario in more detail. We used...
Aims: ARCiS, a novel code for the analysis of exoplanet transmission and emission spectra is presented. The aim modelling framework to provide tool able link observations physical models atmospheres. Methods: philosophy chosen in this paper use chemical constrain certain parameters while keeping free parts where our understanding still more limited. This approach, between full parameterisation, allows us processes we understand well parameterise those less understood. A Bayesian retrieval...
Our understanding of planet formation has been rapidly evolving in recent years. The classical theory, developed when the only known planetary system was our own Solar System, revised to account for observed diversity exoplanetary systems. At same time, increasing observational capabilities young stars and their surrounding disks bring new constraints on process. In this chapter, we summarize information derived from exoplanets population circumstellar observations. We present developments...
In the past decade, ALMA observations have revealed that a large fraction of protoplanetary discs contains rings in dust continuum. These are locations where pebbles accumulate, which is beneficial for planetesimal formation and subsequent planet assembly. We investigate viability inside trapped by either Gaussian-shape pressure bump or strong backreaction. Planetesimals form at midplane ring via streaming instability. By conducting N-body simulations, we study growth these planetesimals...