A hydrocode equation of state for SiO2

304 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

Validation of numerical codes for impact and explosion cratering: Impacts on strengthless and metal targets (2008, methodology): “An updated version of ANEOS is now available, which includes, among other things, the treatment of bi- and tri-atomic molecular gases (Melosh 2000, 2007).”
The Origin of the Moon Within a Terrestrial Synestia (2018, methodology): “The impacting bodies were differentiated (2/3 rocky mantle, 1/3 iron core by mass) with forsterite mantles and iron cores modeled using M-ANEOS equations of state (Canup, 2012; Melosh, 2007).”
Melting and mixing states of the Earth’s mantle after the Moon-forming impact (2015, methodology): “d solution series and is the major mineral phase in the upper mantle (P<˘14GPa). The forsterite EOS is derived from the semi-analytic equation of state known as M-ANEOS (Thompson and Lauson, 1972; Melosh, 2007). M-ANEOS has been commonly used for hydrodynamic simulations and it can treat phase ch”