Stokes' viscometry combined with in situ X-ray radiographic observation, us
ing the 6-8 type multi-anvil press and synchrotron radiation, has been appl
ied to the viscosity measurement of the Fe-FeS melt up to pressures of 7 GP
a. The viscosity is found to be about 2 x 10(-2) Pa-s at 5 to 7 GPa and tem
peratures about 1350 K, in marked contrast to previous viscosity measuremen
ts, which showed high viscosity, 0.5 to 14 Pa-s, at 2 to 5 GPa (LeBlanc and
Secco 1996). Our viscosity data, however, is consistent with all other evi
dence, which include 1 atm viscosity data, X-ray structure analysis, and ab
initio simulations. Recent viscosity measurements (Dobson et al. 2000) als
o showed the viscosity of Fe-FeS melt to be about 10(-2) Pa-s at 2.5 GPa. T
hus, we are confident that the viscosity of the Fe-FeS melt is close to a t
ypical value (10(-2) Pa-s) of viscosity for liquid metal even at high press
ures.