Fig. 11
Vapor curve for the different fits compared to the results from ANEOS. Top: case for forsterite. Bottom: case for quartz. We can see that our vapor curves fit the experimental entropy data very well and resemble the results from ANEOS with molecular gas. The critical pressure is generally lower for our models compared to the ANEOS model. For the forsterite vapor curve our model fits the experimental data better then the one from ANEOS (Collins & Melosh 2014). Experimental data for quartz is from Melosh (2007) and for forsterite is from Ahrens & O’Keefe (1972).
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