Javascript must be enabled to continue!
Morphology and spectral properties of the DART impact ejecta with VLT/MUSE
View through CrossRef
Context.On September 26, 2022, the NASA DART mission impacted the asteroid Dimorphos, the smaller component of the Didymos binary asteroid system. This provided a unique opportunity to observe, in real time, the evolution of the ejecta cloud produced by the impact and the formation of a tail.Aims.We present observations performed with the MUSE instrument at the Very Large Telescope to characterise the morphology, spectral properties, and evolution of the ejecta. The Didymos system was observed with MUSE on 11 nights from just before impact to almost one month post-impact, using both wide-field observations without adaptive optics and narrow-field observations with adaptive optics.Methods.We produced white light images that were used to study the morphology of the ejecta at different spatial scales. The spectral information was used to search for gas emission from either exposed ice or propellant, and to study the spatial and temporal variation of the ejecta dust reflectance through reflectance maps.Results.We searched for, but did not detect, emission from [OI], Xe, NH2, and H2O+in a 1′×1′ field of view in our observations starting almost 4h after impact. We detected a number of morphological features, including a short-lived ejecta cloud visible on September 27 towards the east, spirals, clumps, and a tail that started forming only a few hours after impact. The analysis of the reflectance maps showed that the initial ejecta was bluer than the system before impact, while the tail and spirals were redder than the initial ejecta, consistent with them being made of larger particles. Over the few weeks following impact, the tail became redder. No significant colour differences could be seen between the clumps and the initial ejecta.
Title: Morphology and spectral properties of the DART impact ejecta with VLT/MUSE
Description:
Context.
On September 26, 2022, the NASA DART mission impacted the asteroid Dimorphos, the smaller component of the Didymos binary asteroid system.
This provided a unique opportunity to observe, in real time, the evolution of the ejecta cloud produced by the impact and the formation of a tail.
Aims.
We present observations performed with the MUSE instrument at the Very Large Telescope to characterise the morphology, spectral properties, and evolution of the ejecta.
The Didymos system was observed with MUSE on 11 nights from just before impact to almost one month post-impact, using both wide-field observations without adaptive optics and narrow-field observations with adaptive optics.
Methods.
We produced white light images that were used to study the morphology of the ejecta at different spatial scales.
The spectral information was used to search for gas emission from either exposed ice or propellant, and to study the spatial and temporal variation of the ejecta dust reflectance through reflectance maps.
Results.
We searched for, but did not detect, emission from [OI], Xe, NH2, and H2O+in a 1′×1′ field of view in our observations starting almost 4h after impact.
We detected a number of morphological features, including a short-lived ejecta cloud visible on September 27 towards the east, spirals, clumps, and a tail that started forming only a few hours after impact.
The analysis of the reflectance maps showed that the initial ejecta was bluer than the system before impact, while the tail and spirals were redder than the initial ejecta, consistent with them being made of larger particles.
Over the few weeks following impact, the tail became redder.
No significant colour differences could be seen between the clumps and the initial ejecta.
Related Results
The Exotic Materials at the Chang’e-5 Landing Site
The Exotic Materials at the Chang’e-5 Landing Site
IntroductionThe Chang’e-5 (CE-5) mission is China’s first lunar sample return mission. CE-5 landed at Northern Oceanus Procellarum (43.06°N, 51.92&...
DART and LICIACUBE: Documenting Kinetic Impact
DART and LICIACUBE: Documenting Kinetic Impact
The NASA Double Asteroid Redirection Test (DART) mission will demonstrate asteroid deflection by a kinetic impactor. DART will impact Dimorphos, the secondary member of the (65803)...
Refinement of the Lunar Production Function - The CSFD-Slope of Small Crater Diameters on Ejecta Blankets
Refinement of the Lunar Production Function - The CSFD-Slope of Small Crater Diameters on Ejecta Blankets
<p><strong>Introduction:</strong> The dating of geological surfaces on the Moon is crucial for understanding its geological history and ev...
Ballistic landslides on comet 67P/Churyumov–Gerasimenko
Ballistic landslides on comet 67P/Churyumov–Gerasimenko
<p><strong>Introduction:</strong></p><p>The slow ejecta (i.e., with velocity lower than escape velocity) and l...
VLT/MUSE Characterization of Dimorphos Ejecta from the DART Impact
VLT/MUSE Characterization of Dimorphos Ejecta from the DART Impact
Abstract
We have observed the Didymos-Dimorphos binary system with the MUSE integral field unit spectrograph mounted at the Very Large Telescope before and after DAR...
Kinematics, structure and abundances of supernova remnant 0540-69.3
Kinematics, structure and abundances of supernova remnant 0540-69.3
Aims. Our goal is to investigate the structure, elemental abundances, physical conditions, and the immediate surroundings of supernova remnant 0540-69.3 in the Large Magellanic Clo...
Ries and Chicxulub: Impact craters on Earth provide insights for Martian ejecta blankets
Ries and Chicxulub: Impact craters on Earth provide insights for Martian ejecta blankets
Abstract— Terrestrial impact structures provide field evidence for cratering processes on planetary bodies that have an atmosphere and volatiles in the target rocks. Here we discus...
Popigai impact ejecta layer and extraterrestrial spinels recovered in a new Italian location—The Monte Vaccaro section (Marche Apennines, Italy)
Popigai impact ejecta layer and extraterrestrial spinels recovered in a new Italian location—The Monte Vaccaro section (Marche Apennines, Italy)
ABSTRACT
The Popigai (100 km in diameter) and the Chesapeake Bay (40–85 km diameter) impact structures formed within ~10–20 k.y. in the late Eocene during a 2 m.y. p...

