Urease activity and its relation to soil organic matter, microbial biomassnitrogen and urea-nitrogen assimilation by maize in a Brazilian Oxisol under no-tillage and tillage systems
R. Roscoe et al., Urease activity and its relation to soil organic matter, microbial biomassnitrogen and urea-nitrogen assimilation by maize in a Brazilian Oxisol under no-tillage and tillage systems, BIOL FERT S, 32(1), 2000, pp. 52-59
We studied the relationship between urease activity (UA) and soil organic m
atter (SOM), microbial biomass N (N-biom) content, and urea-N fertilizer as
similation by maize in a Dark Red Latosol (Typic Haplustox) cultivated for
9 years under no-tillage (NT), tillage with a disc plough (DP), and tillage
with a moldboard plough (MP). Two soil depths were sampled (0-7.5 cm and 7
.5-15 cm) at 4 different times during the crop cycle. Urea was applied at f
our different rates, ranging from 0 to 240 kg N ha(-1). The levels of ferti
lizer N did not affect the UA, SOM content, and N-biom content. No signific
ant difference between the treatments (NT, DP, and MP) was observed for SOM
during the experiment, probably because the major part of the SOM was in r
ecalcitrant pools, since the area was previously cultivated (conventional t
illage) for 20 years. The N-biom content explained 97% and 69% of the varia
tion in UA in the upper and deeper soil layer, respectively. UA and biomass
N were significantly higher in the NT system compared to the DP and MP sys
tems. The highest maize productivity and urea-N recovery was also observed
for the NT system. We observed that the increase in urea-N losses under NT,
possibly as a consequence of a higher UA, was compensated for by the incre
ase in N immobilized in the biomass.