Equation of state fits to experimental P,V,T data were examined by the inve
rsion of synthetic data sets using the thermoelastic parameters of MgSiO3 p
erovskite. Our results show that by extending the pressure and temperature
range to 130 GPa and 2500 K, the Volume dependence of the Gruneisen paramet
er, q (=partial derivative ln gamma/partial derivative lnV), could be resol
ved to similar to 10% under the best circumstances. However, simulations al
so showed strong correlation between the bulk modulus, K-T0, and its pressu
re derivative, K'(T0), and q within the currently accepted uncertainty of e
lastic parameters for MgSiO3 perovskite. n/e considered the effect of rando
m error based on the reported uncertainty for different measurement techniq
ues. Even though the laser heated diamond-anvil cell (LHDAC) technique has
significantly larger temperature uncertainty, the ability to extend the pre
ssure and temperature ranges allows for improved resolution of higher order
thermodynamic parameters. However, systematic error from temperature inhom
ogeneity in the LHDAC sample could result in overestimation of q. We also p
erformed Birch-Murhanghan-Debye (BMD) equation of state (EOS) fits for curr
ently available data sets. Consistent with the simulation results, combinin
g recent LHDAC (Fiquet et al. 1998) and resistance heated diamond-anvil cel
l (RHDAC) (Saxena et al. 1999) with lower P-T measurements (Ross and Hazen
1989; Wang et al. 1994; Utsumi et al. 1995; Funamori et al. 1996) we obtain
ed q = 2.0(3) and gamma(0) = 1.42(4). The difference between q = 2.0(3) and
the normally assumed value of q = 1 strongly affects calculated values for
higher order thermoelastic parameters [e.g., alpha, (partial derivative K-
T/partial derivative T)(P)] as well as first order parameters, such as dens
ity and bulk modulus at lower mantle conditions. However, possible systemat
ic error sources need to be further investigated and measurements at higher
P-T conditions promise to yield better constraints on the thermoelastic pa
rameters of MgSiO3 perovskite.