F. Sundermann et al., N-15 PARTITIONING BETWEEN INORGANIC AND ORGANIC N FRACTIONS IN SOIL AMENDED WITH (NH4NO3)-N-15 OR (NH4NO3)-N-15 IN POT EXPERIMENTS, Zeitschrift fur Pflanzenernahrung und Bodenkunde, 158(6), 1995, pp. 529-533
A pot experiment with soil (Cambisol) was carried out to investigate t
he fate of N-15 (supplied as (NH4NO3)-N-15 or (NH4NO3)-N-15) during an
experimental period of 56 days. The soil was either left unsown and i
ncubated at 25 degrees C or sown with grass (Lolium perenne) and culti
vated in a greenhouse. Soil samples were taken at intervals of 7 or 14
days and immediatedly frozen at -18 degrees C. After thawing at 4 deg
rees C the samples were dried at 40 degrees C for 24 hours, extracted
with 0.01 M CaCl2 for inorganic N (N-inorg) and organic N (N-org) and
analyzed for the N-15 labelling of these fractions. A method for the p
reparation of extractable N fractions for mass spectrometry by steam d
istillation was developed and used to separate the inorganic and extra
ctable organic N fraction. Additionally, N-15 in total soil N (N-t) wa
s determined at day 42 and 56 to analyze whether N-15 had been incorpo
rated into nonextractable N fractions. The results showed that, within
the experimental period, the incorporation of N-15 into N-org is negl
igible. Furthermore, there were no indications that this extractable N
-org fraction had mediated N flux from inorganic N to nonextractable o
rganic N pools. N-15 losses in the range of 20-30% of the amount suppl
ied were noted.