Winter wheat, rye and triticale were sown at a depth of 12 cm to promo
te internode elongation. The root-shoot junction was separated by an i
nternode about 4.5 cm long. The rate of ice propagation was measured s
eparately across the root-internode and crown-internode at -4 degrees
C. Ice nucleation in seminal roots was experimentally induced by ice n
ucleating bacteria. The rate of movement of the ice front was measured
by differential thermal analysis. The highest rate of ice propagation
occurred in the internode. The rate of ice propagation across the roo
t-internode section was slower than in the internode alone, but differ
ences exist in the various genotypes. The rate of ice propagation betw
een the seminal roots and the internode did not correlate with the num
ber of roots with unsafe vessels, as detected by the pressurized air m
ethod. The rate of ice propagation between the internode and the crown
was approximately one third of the rate in the internode. The discont
inuity in internode-crown section reached nearly 100% as was observed
by the pressurized air method. Anatomical studies supported the discon
tinuity of vessels evaluated by the pressurized air method. Experiment
al data support the view that the barriers in root-internode and in in
ternode-crown section reduced the rate of ice propagation but these ba
rriers are not correlated with either cold hardiness or number of safe
roots.