B. Linden et al., EVALUATION OF THE ABILITY OF 3 LABORATORY METHODS TO ESTIMATE NET NITROGEN MINERALIZATION DURING THE GROWING-SEASON, Swedish Journal of Agricultural Research, 23(4), 1993, pp. 161-170
Three laboratory methods for estimating net N mineralization in arable
soils were evaluated on the basis of two 3-year field experiments wit
h spring barley in each of the countries Denmark, Finland, Norway and
Sweden. In these, net N mineralization and crop uptake of soil N durin
g the growing season were recorded. Soil samples were taken at the har
vest of the preceding crop and in the forgoing late autumn and early s
pring. The laboratory methods were: (1) aerobic incubation at 30 degre
es C for 14 days, (2) UV light absorption at 205 and 260 nm in water e
xtracts and (3) electro-ultrafiltration (EUF). Net N mineralization un
der field conditions and crop uptake of soil N generally were not rela
ted to nitrogen release during incubation but were significantly assoc
iated with mineral nitrogen in soil prior to incubation of air-dried s
oil samples (''initial'' mineral N), and generally also with light abs
orption at 205 nm and EUF-NO3-N. Mostly, the best relationships were d
etected for samples taken in late autumn. Light absorbance at 205 nm a
nd EUF-NO3-N were closely related to nitrate N in the samples, extract
ed with 2 M KCl. This indicates that light absorption at 205 nm and EU
F-NO3-N reflected ''initial'' mineral N. During sample handling and pr
eparation, nitrogen was mineralized, thus affecting the amounts of ''i
nitial'' mineral N. It was supposed that this released N could have co
rresponded to part of the nitrogen mineralized in the held trials duri
ng the subsequent growing season. Tests of the best relationships for
light absorption at 205 nm and EUF-NO3-N yielded rather encouraging re
sults as regards their ability to predict N mineralization under held
conditions. It was judged, however, that predictions of N mineralizati
on for advisory purposes must be more reliable if they are based on di
rect field measurements of plant-available soil N.