Ik. Thomsen et al., TURNOVER OF N-15 IN UNDISTURBED ROOT SYSTEMS AND PLANT MATERIALS ADDED TO 3 SOILS, Soil biology & biochemistry, 28(10-11), 1996, pp. 1333-1339
Turnover of N-15 in undisturbed wheat (Triticum aestivum) root systems
was compared with turnover of N-15 in applied wheat tops, large roots
of wheat and N left in soil after removal of larger roots (root-deriv
ed N) in three soils of different texture (14, 22 and 27% clay). The N
-15 turnover was determined by measuring inorganic N-15 and biomass N-
15 after 11 and 22 weeks of incubation, respectively, and uptake of N-
15 in ryegrass (Lolium rigidus). The residues had decomposed to differ
ent extents at the first sampling with more N-15 mineralized from N de
rived from roots. However, differences among residues were insignifica
nt after 22 weeks incubation. The soil type had a significant influenc
e on N turnover throughout the incubation. Mineralization of both N-15
and soil N was negatively correlated with clay content. The amount of
N and N-15 in the microbial biomass was positively correlated with cl
ay content. More N-15 was retained in the microbial biomass at the fir
st sampling when large wheat roots and tops had been applied compared
to soil with undisturbed roots and root derived N. Within each soil, t
he type of residue had no effect on N-15 in the biomass after 22 weeks
. Uptake of N-15 and soil N in ryegrass also showed a negative correla
tion with clay content. Contrary to N-15 mineralization in the pots wi
thout plant growth, N-15 uptake in the ryegrass was significantly affe
cted by type of residue. This may be explained partly by the distribut
ion of N-15 between the ryegrass tops and the roots. Copyright (C) 199
6 Elsevier Science Ltd