K. Blankenau et al., Effect of increasing rates of N-15-labelled fertilizer on recovery of fertilizer N in plant and soil N pools in a pot experiment with winter wheat, J PLANT NU, 163(5), 2000, pp. 475-480
Citations number
26
Categorie Soggetti
Environment/Ecology
Journal title
JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE-ZEITSCHRIFT FUR PFLANZENERNAHRUNG UND BODENKUNDE
The effect of increasing rates of N-15-labelled Ca(NO3)(2) (N-0 = no N appl
ication, N-300 = 300 mg N/pot; N-600 = 600 mg N/pot; N-900 = 900 mg N/pot)
on recovery of fertilizer N in winter wheat plants and soil (total soil N,
soil microbial biomass N [N-mic], extractable organic N [N-org]) and on N m
ineralization (NMsoil) was investigated at milk-ripe growth stage in a pot
experiment. The N rates were equally split at tillering, stem elongation an
d ear emergence.
Fertilizer N recovered in crops increased with increasing N rates (N-300: 2
23.5 mg N/pot [74.5% of applied fertilizer N], N600: 445.6 mg N/pot [74.3%]
, N-900: 722.1 mg N/pot [80.2%]). NMsoil slightly increased from N-0 (43.8
mg N/pot) to N-900 (75.6 mg N/pot) indicating that N application enhanced a
vailability of soil-derived N for the plants. However, in fertilized treatm
ents NMsoil is balanced by immobilization and losses (non-recovered fertili
zer N). Therefore the effective soil N mineralization is indicated by appar
ent net N mineralization (ANNM = NMsoil - fertilizer N immobilization - los
t fertilizer N). Fertilizer N immobilization in soil increased from N-300 (
38.7 mg N/pot) to N-600 (60.7 mg N/pot) and N-900 (65.5 mg N/pot). Lost fer
tilizer N increased from N-300 (14.8 mg N/pot) to N-600 (56.7 mg N/pot) and
N-900 (61.1 mg N/pot). As a consequence negative ANNM values were calculat
ed at N-600 and N-900. Due to the small differences between N-600 and N-900
fertilizer N immobilization and lost fertilizer N did not increase linearl
y with increasing N rates, i.e. both processes were limited by factors othe
r than N rate. Only 5.6-7.4% of the immobilized fertilizer N was recovered
in N-org and 5.4-9.3% in N-mic soil pools. It is assumed that most of the i
mmobilized fertilizer N was in non-extractable organic N forms. N-mic and N
-org were weak indicators for the extent of fertilizer N immobilization.