INTERACTIONS BETWEEN ROTATION BREAKS, TILLAGE AND N MANAGEMENT ON SUGARCANE GROWN AT BUNDABERG AND INGHAM
By MJ BELL; AL GARSIDE; N HALPIN; B SALTER; PW MOODY; G PARK
THE IMPACT of cropping histories (sugarcane, maize and soybean), tillage
practices (conventional tillage and direct drill) and fertiliser N in the plant
and 1st ratoon (1R) crops of sugarcane were examined in field trials at
Bundaberg and Ingham. Average yields at Ingham (Q200A) and
Bundaberg (Q151A) were quite similar in both the plant crop (83 t/ha and
80 t/ha, respectively) and the 1R (89 t/ha v 94 t/ha, respectively), with
only minor treatment effects on CCS at each site. Cane yield responses to
tillage, break history and N fertiliser varied significantly between sites.
There was a 27% yield increase in the plant crop from the soybean fallow
at Ingham, with soybeans producing a yield advantage over continuous
cane, but there were no clear break effects at Bundaberg – possibly due to
a complex of pathogenic nematodes that responded differently to
soybeans and maize breaks. There was no carryover benefit of the
soybean break into the 1R crop at Ingham, while at Bundaberg the maize
break produced a 15% yield advantage over soybeans and continuous
cane. The Ingham site recorded positive responses to N fertiliser addition
in both the plant (20% yield increase) and 1R (34% yield increase) crops,
but there was negligible carryover benefit from plant crop N in the 1R
crop, or of a reduced N response after a soybean rotation. By contrast, the
Bundaberg site showed no N response in any history in the plant crop,
and only a small (5%) yield increase with N applied in the 1R crop. There
was again no evidence of a reduced N response in the 1R crop after a
soybean fallow. There were no significant effects of tillage on cane yields
at either site, although there were some minor interactions between
tillage, breaks and N management in the 1R crop at both sites. Crop Ncontents at Bundaberg were more than 3 times those recorded at Ingham
in both the plant and 1R crops, with N concentrations in millable stalk at
Ingham suggesting N deficiencies in all treatments. There was negligible
additional N recovered in crop biomass from N fertiliser application or
soybean residues at the Ingham site. There was additional N recovered in
crop biomass in response to N fertiliser and soybean breaks at Bundaberg,
but effects were small and fertiliser use efficiencies poor. Loss pathways
could not be quantified, but denitrification or losses in runoff were the
likely causes at Ingham while leaching predominated at Bundaberg.
Results highlight the complexity involved in developing sustainable
farming systems for contrasting soil types and climatic conditions. A
better understanding of key sugarcane pathogens and their host range, as
well as improved capacity to predict in-crop N mineralisation, will be key
factors in future improvements to sugarcane farming systems.