T. Appel et K. Mengel, PREDICTION OF MINERALIZABLE NITROGEN IN SOILS ON THE BASIS OF AN ANALYSIS OF EXTRACTABLE ORGANIC N, Zeitschrift fur Pflanzenernahrung und Bodenkunde, 161(4), 1998, pp. 433-452
Most of the nitrogen (N) in agricultural soils is organically bound, w
hile the N uptake by plants and also the N losses from the soil-plant
system into the environment are as inorganic N. The electro-ultrafiltr
ation (EUF) method and the extraction by a CaCl2 solution extract an o
rganic N fraction (Norg) that is thought to provide information about
the amount of rapidly mineralizable N in soils. This paper aims to ill
ustrate various aspects regarding the biological meaning of the Norg-f
ractions extracted by these two extraction methods and also the opport
unities and limitations for predicting the mineralizable N based on an
Norg analysis. From an evaluation of numerous data on EUF and CaCl2 e
xtractable Norg fractions we concluded that these methods extract N co
mpounds which can be used as indices for easily mineralizable soil N.
However, both methods extract only some of the rapidly mineralizable N
in soils, and some of the Norg ecxtracted appears to be from the more
recalcitrant soil organic N. This was particularly true for the EUF-m
ethod. It may therefore be desirable to improve both the extractabilit
y and the selectivity of the extraction methods. This may be achieved
by measuring extractable amino-N-compounds instead of the total extrac
table Norg. Evaluating the numerous field experiments done during the
last decade shows that the calibration factors obtained for extractabl
e Norg were not the same for different growing seasons, geographical r
egions and management practices. Theoretically, for each combination o
f these factors separate calibrations would be necessary. It is this i
nflexibility which appears to be the most serious drawback for the use
of extractable Norg fractions in practice. A possible solution may be
to combine the flexibility of a simulation model with additional info
rmation obtained by the analysis of extractable soil organic N. Furthe
r work in this direction may be desirable.