“…Most prominent are shock wave experiments (McQueen et al, 1983;Neal, 1976;Collins et al, 2001;Knudson et al, 2003;Fortov et al, 2007) but other techniques can explore different regions in phase space (see, e.g., Weir et al, 1959;Jayarama, 1986;Bakshi et al, 2009). Quasi-isentropic compression using ramp wave loading (RWL) (Reisman et al, 2000;Hayes, 2001;Cauble et al, 2002;Hayes et al, 2004;Rothman et al, 2005;Davis, 2006;Chhabildas & Barker, 1986;Barnes et al, 1974;Lorenz et al, 2004Lorenz et al, , 2005Smith et al, 2007;Swift & Johnson, 2005) allows sampling EOS data along an isentrope up to several Mbar pressures, located on the phase diagram between the parameter regions accessible with diamond anvil cells (Weir et al, 1959;Jarayama, 1986) and shock wave experiments (McQueen et al, 1983;Neal, 1976).…”