Idea about Mars atmospheric loss

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SUMMARY

Mars currently has an atmosphere of 0.006 bar, significantly thinner than Earth's 1 bar atmosphere. The loss of Mars' atmosphere is attributed to three primary factors: the absence of a magnetic field, lack of geological activity, and the escape velocity of lighter molecules during its warmer early period. Impacts from planetoids and asteroids further contributed to atmospheric loss by increasing temperatures, facilitating gas escape. Current understanding indicates that Mars was once hospitable to life billions of years ago.

PREREQUISITES
  • Understanding of planetary atmospheres and their composition
  • Knowledge of geological activity and its effects on planetary bodies
  • Familiarity with the concepts of escape velocity and gas retention
  • Awareness of the role of magnetic fields in atmospheric protection
NEXT STEPS
  • Research the effects of solar wind on Martian atmospheric loss
  • Study the geological history of Mars to understand past conditions
  • Explore the implications of low gravity on atmospheric retention
  • Investigate the potential for past life on Mars based on atmospheric conditions
USEFUL FOR

Astronomers, planetary scientists, and researchers interested in Mars' atmospheric evolution and its implications for past habitability.

willstaruss22
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Mars current atmosphere is 0.006 bar. It is theorized that the atmosphere was thicker in the past possibly thicker than Earths 1 bar atmosphere. There are many processes that could have done this such as having no magnetic field, lack of geological activity, a planetoid crashing into it and escape velocity of lighter molecules. According to the link below Mars can hold CO2, oxygen and nitrogen now but water vapor will escape and this is at 210 K.
http://astro.unl.edu/naap/atmosphere/animations/gasRetentionPlot.html
Mars early in its life was likely much warmer which would have caused gases to escape much easier, this coupled with the lack of geological activity would have made things even worse for Mars. There is also the heat from planetoid and asteroid impacts that would cause the temperatures to soar hundred of degrees not just from the initial impact but from the reentry of materials. As you see on the link if you increase the temperature the gases will escape including CO2.

Therefore its my believe that the triple effect from lack of a magnetic field, lack of geological activity and the escape velocity from both its warmer period and the heat from its many asteroid collisions caused the gases to escape.

Would this make any sense?
 
Space news on Phys.org
The low gravity of Mars and its lack of a dynamo effect generating a magnetic shield are the main culprits. Sputtering of the atmosphere by the sun is the primary consequence. It is now widely believed that Mars was hospitable to life a few billion years ago.
 

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