The mercuric chloride (HgCl2) vapor pressure was measured between 343
and 454 K by the Knudsen cell method at relatively high pressures wher
e the flow rate is not purely molecular. Four cells with different ori
fice sizes were used. Knudsen equation cannot explain accurately the e
xperimental mass loss by using molecular plus hydrodynamical equations
. Calculations from our measurements were performed taking into accoun
t of an ''effective radius'' for our orifices, and this radius depends
on the relative weight of the two contributions. We compare our resul
ts with those existing in literature.