We have used high-temperature ab initio molecular dynamic simulations to st
udy the equation of state of orthorhombic MgSiO3 perovskite under lower man
tle pressure-temperature conditions. We have determined the Gruneisen param
eter, gamma, as a function of volume. Our state-of-the-art simulations, acc
urate to within 10%, resolve the long-standing controversy on thermal expan
sion (a) and Gruneisen parameter of MgSiO3 perovskite. Under ambient condit
ions we find the values for alpha and gamma of 1.86 x 10(-5) K-1 and 1.51,
respectively, in excellent agreement with the latest experimental studies.
Calculated elastic constants and the static equation of state at 0 K agree
well with previous simulations. We have found no evidence for the high-temp
erature phase transitions of orthorhombic MgSiO3 perovskite to cubic or tet
ragonal phases at mantle temperatures. (C) 2001 Elsevier Science B.V. All r
ights reserved.