On the origin and early evolution of terrestrial planet atmospheres and meteoritic volatiles
Pepin (1991) Icarus, 92, 2-72





目次 
1. Introduction20141020
2.Assumptions and Overview  
  2-A.Assumption20141020
  2-B.Overview of the models20141023
3.Processes20141104
4.Data 20141106
  4-A.Solar20141106
  4-B.Meteorites20141108
  4-C.Planetary Atmospheres 20141109
5.Apprications
  5-A.Construction of the Model 20141110
  5-B.Planetary Model 1 Noble gases on Earth, Venus, and Mars20141201
  5-C.Planetary Model 2 Combined Noble Gas-Carbon-Nitrogen Models20150217
  5-D.Noble Gases in Meteoritic Carrier Phases2014****
6.Planetary Energy Demands, Evolutionary Timescales, and Hydrogen and Noble Gas Requirements2014****
  6-A.Estimates of Initial EUV Energy Deposition2014****
  6-B.The Timing of Evolutionary Stages2014****
  6-C.Hydrogen Inventories2014****
  6-D.Hydrogen and Noble Gases Sources2014****
  6-E.Geochemical Consequences of Water Accretion, and Constraints on EUV Flux Histories2014****
7.Further Considerations  
  7-A.Retention of Xenon in Planetary Interiors2014****
  7-B.Effects of escape at Higher Temperature2014****
  7-C.Limits on Carbonaceous Chondrite Accretion by Earth2014****
  7-D.Models for Origin of Outgassed Planetary Components by Adsorption2014****
8.Summary2014****
 



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