Fig. 5
Predicted porosities of pure H2O and H2O:CO2 ice samples as a function of the growth temperature, following the Maxwell-Garnett (MG) and the Bruggeman (BR) EMAs. Due to overlap the dark symbols cannot be distinguished well. The error in the predicted porosities (bottom right corner) depends on the error in the refractive indices (0.4%) and on the error in the H2O:CO2 ratios (30%).
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.