Results 11 to 20 of about 36,303 (299)

Challenges in planet formation [PDF]

open access: yesJournal of Geophysical Research E: Planets, 2016
AbstractOver the past two decades, large strides have been made in the field of planet formation. Yet fundamental questions remain. Here we review our state of understanding of five fundamental bottlenecks in planet formation. These are the following: (1) the structure and evolution of protoplanetary disks; (2) the growth of the first planetesimals; (3)
Alessandro Morbidelli, Sean N Raymond
exaly   +5 more sources

Terrestrial planet formation. [PDF]

open access: yesProc Natl Acad Sci U S A, 2011
Advances in our understanding of terrestrial planet formation have come from a multidisciplinary approach. Studies of the ages and compositions of primitive meteorites with compositions similar to the Sun have helped to constrain the nature of the building blocks of planets.
Righter K, O'Brien DP.
europepmc   +5 more sources

The planet formation imager [PDF]

open access: yesExperimental Astronomy, 2018
Published in Experimental Astronomy as part of topical collection "Future of Optical-infrared Interferometry in Europe"
Monnier, John D.   +38 more
core   +14 more sources

Continuous adaptive chemotherapy dosing by using planet-formation-inspired dynamics: analytical and in silico insights [PDF]

open access: yesFrontiers in Oncology
BackgroundCurrent therapeutic planning of chemotherapy is based on empirical dosimetry and intermittent dose administration, which can cause poorly defined therapeutic timepoints due to tumor heterogeneities and related highly uncertain tumor dynamics ...
Marco P. Soares dos Santos   +7 more
doaj   +2 more sources

Planet formation mechanisms

open access: yes
Planet formation encompasses processes that span a remarkable 40 magnitudes in mass, ranging from collisions between micron-sized grains inherited from the ISM to the accretion of gas by giant planets. The planet formation process takes place in the interior of dusty disks, which offer us only limited observational constraints.
Ormel, Chris
openaire   +3 more sources

Impact Induced Oxidation and Its Implications for Early Mars Climate

open access: yesGeophysical Research Letters, 2023
H2 in a CO2 atmosphere may serve as a potential solution to the early Mars climate paradox, but its unknown sources cast doubts on the proposed mechanism. Impact cratering is an energetic process that may modify the surface redox budget.
Lu Pan, Zhengbin Deng, Martin Bizzarro
doaj   +1 more source

A tale of planet formation: from dust to planets [PDF]

open access: yesResearch in Astronomy and Astrophysics, 2020
Abstract The characterization of exoplanets and their birth protoplanetary disks has enormously advanced in the last decade. Benefitting from that, our global understanding of the planet formation processes has been substantially improved.
Liu, Beibei, Ji, Jianghui
openaire   +2 more sources

Evidence for Very Early Planetesimal Formation and 26Al/27Al Heterogeneity in the Protoplanetary Disk

open access: yesThe Astrophysical Journal Letters, 2023
We present a U-corrected Pb–Pb age of 4566.19 ± 0.20 Ma (1.11 ± 0.26 Myr after t _0 ) for the moderately volatile element rich, andesitic meteorite Erg Chech 002 (EC002). Our Al–Mg isochron defines a ^26 Al/ ^27 Al initial ratio of (8.65 ± 0.09) × 10 ^−6
J. N. Connelly   +5 more
doaj   +1 more source

The Perseus ALMA Chemistry Survey (PEACHES). II. Sulfur-bearing Species and Dust Polarization Revealing Shocked Regions in Protostars in the Perseus Molecular Cloud

open access: yesThe Astrophysical Journal, 2023
In protostellar cores, sulfur species are effective probes for the energetic environments, such as shocked regions. With the majority of sulfur depleted on dust grains, sulfur-bearing molecules could be liberated back to gas phase by shocks associated ...
Ziwei E. Zhang   +7 more
doaj   +1 more source

Effect of pebble flux-regulated planetesimal formation on giant planet formation [PDF]

open access: yes, 2020
Context. The formation of gas giant planets by the accretion of 100 km diameter planetesimals is often thought to be inefficient. A diameter of this size is typical for planetesimals and results from self-gravity.
Klahr, Hubert   +9 more
core   +1 more source

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