Ih. Salcedo et al., NUTRIENT AVAILABILITY IN SOIL SAMPLES FROM SHIFTING CULTIVATION SITESIN THE SEMIARID CAATINGA OF NE BRAZIL, Agriculture, ecosystems & environment, 65(2), 1997, pp. 177-186
Soil fertility differed substantially among three neighboring sites re
presenting different stages of a shifting cultivation cycle on a deepl
y weathered Oxisol on the Chapada de Araripe in the semiarid region of
NE Brazil. Samples taken from a native thorn forest area (Caatinga),
from a recently slashed and burnt area (Burnt) and from a site abandon
ed after five years of manual cultivation to cassava (Abandoned), were
compared using subtractive and additive fertilization greenhouse tria
ls and incubations for C and N mineralization. The effect of burning w
as to increase soil nutrient content relative to the Caatinga area sam
ples, followed by decreases of N and organic P by 20%: available P by
70%, and exchangeable bases by 55%, on average, after abandonment. The
unfertilized control of the missing-element trial gave the lowest dry
matter (DM) yields, but still those of the Burnt were twice as large
as those of the Abandoned area samples. The relative yield ratios were
not changed by nutrient addition, although total yields were increase
d by a factor of 5. In all three areas, the most severe nutrient limit
ation was of P, followed by N. The N deficiency somewhat increased rel
ative to P in the Abandoned samples. Addition of 25 mg P kg(-1) soil p
roduced 4 to 5-fold dry matter increases in the Caatinga and 7 to 8-fo
ld increases in the Burnt area samples. Further increasing P levels im
proved yields only marginally and only at high additions of N and K. I
n samples from the abandoned area, 25 mg P kg(-1) not even doubled the
dry matter yield, and no additional effects were observed for higher
N and K rates. Carbon mineralization during the 12 week incubation fol
lowed the order Caatinga > Abandoned > Burnt, whereas the order for N
removed in 13 leachings was Caatinga > Burnt > Abandoned. Accordingly,
organic matter mineralized from the abandoned soil had a higher C:N r
atio. In addition to the nutrient limitations of this Oxisol, samples
from the Abandoned area exhibited further limitations resulting in yie
ld reductions, which were not explained by any of the factors examined
. This indicates that alternatives to long-fallow shifting cultivation
will require further refinement of methodologies to measure and predi
ct soil quality. (C) 1997 Elsevier Science B.V.