SUSTAINING PRODUCTIVITY OF A VERTISOL AT WARRA, QUEENSLAND, WITH FERTILIZERS, NO-TILLAGE OR LEGUMES .3. EFFECTS OF NITRATE ACCUMULATED IN FERTILIZED SOIL ON CROP RESPONSE AND PROFITABILITY
Wm. Strong et al., SUSTAINING PRODUCTIVITY OF A VERTISOL AT WARRA, QUEENSLAND, WITH FERTILIZERS, NO-TILLAGE OR LEGUMES .3. EFFECTS OF NITRATE ACCUMULATED IN FERTILIZED SOIL ON CROP RESPONSE AND PROFITABILITY, Australian journal of experimental agriculture, 36(6), 1996, pp. 675-682
Unreliable rainfall during the crop growing season leads to a variable
use of applied fertiliser nitrogen (N) by the crop, which may leave s
ubstantial fertiliser N residue in the soil. Residual effects of ferti
liser N (0-150 kg/ha) applied to a succession of wheat crops over the
period 1987-94 were studied in terms of increased crop returns ($A/ha)
from fertiliser application and increased soil mineral N for the subs
equent crop. In spite of the unreliability of wheat responses to appli
ed N in this region, increases in financial returns over this sequence
of crops suggest that a strategy of routine N application to wheat wa
s highly profitable on this fertility-depleted soil. When increases in
returns from 1 fertiliser application were summed over successive cro
ps, financial returns generally increased with increasing rate of N ap
plied up to the highest N rate (100 or 150 kg/ha). When N was applied
to each successive crop, financial returns were similarly increased bu
t applications >50 kg/ha were less profitable than rates less than or
equal to 50 kg/ha. Increased financial returns for the 7 crops grown w
ith conventional tillage increased by $A306/ha, $794/ha, $867/ha and $
867/ha for fertiliser N applied at rates of 12.5, 25, 50 and 75 kg N/h
a to each crop, respectively. Total N fertiliser costs for the 7 crops
were $A63/ha, $126/ha, $253/ha and $380/ha. Increased financial retur
ns of $608/ha and $962/ha were derived from applications of 25 and 75
kg N/ha to each of the 7 crops with zero tillage. When N uptake by whe
at was reduced by water deficit, or where a longer fallow period creat
ed much higher nitrate levels, a single fertiliser N application of 75
or 150 kg/ha resulted in nitrate accumulated to 1.2 m depth in the fo
llowing May. Where N was applied to each crop in the sequence, applica
tion of 75 kg/ha increased soil nitrate to 1.2 m in the following May,
except in 1989 and 1990. The 3-crop sequence, 1988-90, placed high de
mands on soil N supplies, with high wheat yields (about 4.5 t/ha) and
grain N contents (100-115 kg/ha) in 1988 but lower yields (>2t/ha) in
1989 and 1990. Consequently, low levels (46-63 kg/ha) of soil mineral
N were apparently carried over for crops in 1989 and 1990 even where 7
5 kg N/ha was applied to the preceding crop. Subsequent recovery of fi
nancial losses, incurred in years of water deficit, made the routine a
pplication of 75 kg N/ha to fertility-depleted soils of this region pr
ofitable.