Molecular Dynamics Simulation of a Dust-Core Formation Stage in Space: H2O Formation on Surface Mg Sites at Around 3500 K

Astronomy and Astrophysics – Astronomy

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

Ism: Dust, Extinction, Ism: Molecules, Molecular Processes

Scientific paper

The dust formation process was simulated by a molecular dynamics method for the system consisting of Si, Mg, Al, O, H, and He in roughly cosmic abundance. As the temperature was lowered from 6000 K, the coagulation due to random collisions made the clusters grow, and solidification proceeded to make amorphous Mg-Al-silicate clusters of various sizes having an average coordination number of 2.2 for Si at 1000 K. Water formation was observed at around 3500 K on the surface Mg atoms that have been squeezed out from the inside due to thermal vibrations. These water molecules in the gas phase at 500 K might turn out to be the ice mantle at very cold temperatures that covers the thus formed dust.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Molecular Dynamics Simulation of a Dust-Core Formation Stage in Space: H2O Formation on Surface Mg Sites at Around 3500 K does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Molecular Dynamics Simulation of a Dust-Core Formation Stage in Space: H2O Formation on Surface Mg Sites at Around 3500 K, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Molecular Dynamics Simulation of a Dust-Core Formation Stage in Space: H2O Formation on Surface Mg Sites at Around 3500 K will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1701335

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.