Using energy-dispersive x-ray diffraction techniques together with the theo
ry describing lattice strains under nonhydrostatic compression, the behavio
r of a layered sample of gold and rhenium has been studied at pressures of
14-37 GPa. For gold, the uniaxial stress component t is consistent with ear
lier studies and can be described by t = 0.06 + 0.015P where P is the press
ure in GPa. The estimated single-crystal elastic moduli are in reasonable a
greement with trends based on extrapolated low-pressure data. The degree of
elastic anisotropy increases as alpha, the parameter which characterizes s
tress-strain continuity across grain boundaries, is reduced from 1.0 to 0.5
. For rhenium, the apparent equation of state has been shown to be strongly
influenced by nonhydrostatic compression, as evidenced by its dependence o
n-the angle psi between the diffracting plane normal and the stress axis. T
he bulk modulus obtained by inversion of nonhydrostatic compression data ca
n differ by nearly a factor of 2 at angles of 0 degrees and 90 degrees. On
the other hand; by a proper choice of psi, d spacings corresponding to quas
ihydrostatic compression can be obtained from data obtained under highly no
nhydrostatic Conditions. The uniaxial stress in rhenium over the pressure r
ange from 14-37 GPa can be described by t = 2.5 + 0.09P. The large discrepa
ncy between x-ray elastic:moduli and-ultrasonic data and theoretical calcul
ations indicates that additional factors such as texturing or orientation d
ependence of t need to be incorporated to more fully describe the strain di
stribution in hexagonal-close-packed metals. [S0163-1829(99)02845-5].