The centrifuge method for measuring the resistance of xylem to cavitation b
y water stress was modified to also account for any additional cavitation t
hat might occur from a freeze-thaw cycle. A strong correlation was found be
tween cavitation by freezing and mean conduit diameter. On the one extreme,
a tracheid-bearing conifer and diffuse-porous angiosperms with small-diame
ter vessels (mean diameter <30 mu m) showed no freezing-induced cavitation
under modest water stress (xylem pressure = -0.5 MPa), whereas species with
larger diameter vessels (mean >40 mu m) were nearly completely cavitated u
nder the same conditions. Species with intermediate mean diameters (30-40 m
u m) showed partial cavitation by freezing. These results are consistent wi
th a critical diameter of 44 mu m at or above which cavitation would occur
by a freeze-thaw cycle at -0.5 MPa. As expected, vulnerability to cavitatio
n by freezing was correlated with the hydraulic conductivity per stem trans
verse area. The results confirm and extend previous reports that small-diam
eter conduits are relatively resistant to cavitation by freezing. It appear
s that the centrifuge method, modified to include freeze-thaw cycles, may b
e useful in separating the interactive effects of xylem pressure and freezi
ng on cavitation.