Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Cometary ion dynamics under weakly outgassing conditions

View through CrossRef
Plasma density observations from the Rosetta Plasma Consortium reveal two distinct physical regimes for the ion dynamics in the coma of comet 67P/Churyumov-Gerasimenko. At lower rates of outgassing when the Rosetta spacecraft was close to the cometary nucleus, ions moved with the neutral gas background; at higher rates of outgassing, a diamagnetic cavity formed, and the observed plasma density attested to ion acceleration with respect to the background neutral gas. The diamagnetic cavity was detected around perihelion from April 2024 to February 2016. The end of this period corresponds to the transition between the two regimes, as the comet moved away from the Sun, outgassing decreased and Rosetta got closer to the cometary nucleus.Current global 3D plasma models of the cometary ionosphere underestimate observed ion number densities during the low outgassing regime. A simple radial model lacking acceleration better explains Rosetta plasma observations. In order to identify the cause of the underestimation by the current global plasma model, we assess the sensitivity of the cometary ion dynamics to several parameters during the transition. For that purpose, we use our in-house 3D ion test particle model driven by the fields generated by a hybrid model. First, we assess the sensitivity of the ion dynamics to collisions between the ions and the neutral background. This process is not sufficient to explain the discrepancy. Next, we evaluate the sensitivity of the ion dynamics with electron temperature through the ambipolar electric field. Current models assume adiabatic electron behavior; however, electrons trapped close to the cometary nucleus by the ambipolar field are collisional, not adiabatic, and the resultant cooling feeds back to weaken the ambipolar electric field. We show that the resulting simulated plasma density is affected by the use of a more realistic electron temperature profile derived from electron test particle modelling, bringing it closer to the Rosetta plasma density.
Title: Cometary ion dynamics under weakly outgassing conditions
Description:
Plasma density observations from the Rosetta Plasma Consortium reveal two distinct physical regimes for the ion dynamics in the coma of comet 67P/Churyumov-Gerasimenko.
At lower rates of outgassing when the Rosetta spacecraft was close to the cometary nucleus, ions moved with the neutral gas background; at higher rates of outgassing, a diamagnetic cavity formed, and the observed plasma density attested to ion acceleration with respect to the background neutral gas.
The diamagnetic cavity was detected around perihelion from April 2024 to February 2016.
The end of this period corresponds to the transition between the two regimes, as the comet moved away from the Sun, outgassing decreased and Rosetta got closer to the cometary nucleus.
Current global 3D plasma models of the cometary ionosphere underestimate observed ion number densities during the low outgassing regime.
A simple radial model lacking acceleration better explains Rosetta plasma observations.
In order to identify the cause of the underestimation by the current global plasma model, we assess the sensitivity of the cometary ion dynamics to several parameters during the transition.
For that purpose, we use our in-house 3D ion test particle model driven by the fields generated by a hybrid model.
First, we assess the sensitivity of the ion dynamics to collisions between the ions and the neutral background.
This process is not sufficient to explain the discrepancy.
Next, we evaluate the sensitivity of the ion dynamics with electron temperature through the ambipolar electric field.
Current models assume adiabatic electron behavior; however, electrons trapped close to the cometary nucleus by the ambipolar field are collisional, not adiabatic, and the resultant cooling feeds back to weaken the ambipolar electric field.
We show that the resulting simulated plasma density is affected by the use of a more realistic electron temperature profile derived from electron test particle modelling, bringing it closer to the Rosetta plasma density.

Related Results

Outgassing on Stagnant-Lid Planets: Influence of Rheology
Outgassing on Stagnant-Lid Planets: Influence of Rheology
Outgassing from the interior is a key process influencing the evolution of the atmospheres of rocky planets. For planets with a stagnant lid tectonic mode, previous models have ind...
Assessing the potential composition of Europa’s subsurface ocean from water-rock interactions.
Assessing the potential composition of Europa’s subsurface ocean from water-rock interactions.
<p><strong>Introduction:</strong> Constraining the composition of Europa’s ocean is critical to understanding whether it cou...
Development of surface materials analogues of the main-belt comet 133P/Elst-Pizarro
Development of surface materials analogues of the main-belt comet 133P/Elst-Pizarro
Introduction:The main-belt comets (MBCs) are objects that exhibit cometary activity but occupy stable orbits in the main asteroid belt. MBCs are considered as a hidden reservoir of...
Evolution of the ion dynamics at comet 67P during the escort phase
Evolution of the ion dynamics at comet 67P during the escort phase
Comet 67P/Churyumov-Gerasimenko was escorted by the Rosetta spacecraft through a 2 year section of its 6 year orbit around the Sun. This enabled the observation of a large variatio...
Out-of-equilibrium volatile outgassing in planetary magma oceans
Out-of-equilibrium volatile outgassing in planetary magma oceans
Terrestrial planets likely experienced at least one early global silicate magma ocean stage. Upon cooling, vigorous convective motions  are commonly thought to efficiently outgas d...
Photometric and spectrophotometric measurements of the CoPhyLab dust mixtures.
Photometric and spectrophotometric measurements of the CoPhyLab dust mixtures.
Abstract:Even as the late space exploration ESA/ROSETTA mission allowed to perform the most complete investigation of a cometary nucleus to date [1], and observations of interstell...
Outcome of Collisions in the Early Outer Solar System
Outcome of Collisions in the Early Outer Solar System
AbstractThe processes leading to the formation of planetary systems leave behind a significant mass of small bodies - up to 35 Earth masses depending on the model [1] - orbiting at...
Ion velocity distribution functions at a low activity comet
Ion velocity distribution functions at a low activity comet
We study the transition period of induced comet magnetospheres between the simple deflection of the solar wind due to mass loading and a fully developed bow shock. We present exper...

Back to Top