Spring canola (Brassica napus L. and B. rapa L.) is sometimes planted
when soil temperatures are below the optimum, causing farmers to have
stand losses because of seed rotting in cold soil. Knowledge of the gr
owing-degree hours (GDH) required for emergence of canola from differe
nt planting depths could help producers decide when and how deep to pl
ant this crop. Our objectives were to quantify the base temperature (t
he minimum temperature required) for emergence, the number of GDH requ
ired for initial emergence of five cultivars of spring and winter cano
la, and to evaluate temperature x planting depth interactions of sprin
g canola. 'Alto', 'Global', 'Tobin', 'Crystal', and 'Glacier' cultivar
s were planted 1 cm deep into pots of Weld silt loam (fine, montmorill
onitic, mesic aridrc Paleustolls). Pots were incubated at 0, 2, 4, and
16 degrees C. Seedlings emerged were counted daily for all temperatur
es and twice daily during rapid emergence at 16 degrees C. Simple-line
ar and segmented-nonlinear-regression were used to determine base temp
eratures and GDH requirements for initial emergence. Calculated base t
emperatures were between 0.4 and 1.2 degrees C. Regardless of the cons
tant temperature regime, emergence began between 1560 and 1940 GDH for
the spring canola. Winter canola emerged at 1600 to 2800 GDH. Two cul
tivars (Tobin and Global) were also planted at 1-, 2-, 2.5-, 3-, and 4
-cm depths and incubated at 4, 8, 12, and 16 degrees C to investigate
planting depth x temperature interactions. A reduction in emergence, a
s a function of an interaction between temperature and planting depth,
was found for Global but not Tobin at the temperatures and planting d
epths used in this study. A match between the accumulated heat units i
n early spring for a location and the GDH required for initial emergen
ce of the spring cultivars tested can be used to determine early sprin
g canola planting dates. This analysis indicates that severe reduction
s in stand are possible when canola is planted at soil temperatures th
at are sustained much below 8 degrees C. The heat unit approach used a
llows for the transfer of the relationships developed in this study to
other locations.