PREDICTION OF MINERALIZABLE NITROGEN IN SOILS ON THE BASIS OF AN ANALYSIS OF EXTRACTABLE ORGANIC N

Authors
Citation
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
Citations number
105
Categorie Soggetti
Agriculture Soil Science","Plant Sciences",Agriculture
ISSN journal
00443263
Volume
161
Issue
4
Year of publication
1998
Pages
433 - 452
Database
ISI
SICI code
0044-3263(1998)161:4<433:POMNIS>2.0.ZU;2-K
Abstract
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.