POTENTIAL FOR BIOLOGICAL DENITRIFICATION OF FERTILIZER NITROGEN IN SUGARCANE SOILS

Citation
Kl. Weier et al., POTENTIAL FOR BIOLOGICAL DENITRIFICATION OF FERTILIZER NITROGEN IN SUGARCANE SOILS, Australian Journal of Agricultural Research, 47(1), 1996, pp. 67-79
Citations number
28
Categorie Soggetti
Agriculture
ISSN journal
00049409
Volume
47
Issue
1
Year of publication
1996
Pages
67 - 79
Database
ISI
SICI code
0004-9409(1996)47:1<67:PFBDOF>2.0.ZU;2-K
Abstract
Nitrogen (N) fertilizer is being lost from sugarcane soils following a pplication to the crop. This study was conducted to estimate the quant ity of N being lost from the soil through biological denitrification a nd to determine the proportion of gaseous N being emitted either as N2 O or as N-2. Field studies were conducted on four different soils (hum ic gley, alluvial massive earth, red earth and gleyed podzolic), and o n different crop management systems, by installing plastic (PVC) cylin ders (23.5 cm diam., 25 cm long) in the soil to a depth of 20 cm besid e the plant row in a ratoon sugarcane crop. N-15-labelled KNO3 was app lied as a band across each cylinder to a depth of 2.5 cm at a rate of 160 kg N/ha. After rainfall or irrigation, the cylinders were capped f or 3 h intervals and gas in the headspace sampled in the morning and a fternoon, for up to 4 days. Denitrification losses from the humic gley ranged from 247 g N/ha . day for cultivated plots to 1673 g N/ha . da y for no-till plots. Over the sampling period, this was equivalent to 3.2% and 19.7% of the N applied, respectively. Nitrous oxide accounted for 46% to 78% of the total N lost. For the alluvial, massive earth a nd the red earth and gleyed podzolic, losses over the sampling period ranged from 25 to 117 g N/h . day and represented less than or equal t o 1% of the N applied. Recovery of N-15 in the soil ranged from 67% at the first sampling on the red earth soil to 4.9% at the third samplin g on the alluvial, massive earth soil. In a glasshouse study, intact s oil cores (23.5 cm diam., 20 cm long), taken from the humic gley and t he alluvial, massive earth, were waterlogged after band application of N-15-labelled KNO3 at a rate of 160 kg N/ha. Gas samples from the hea dspace were taken after 3 h, and then morning and afternoon for the ne xt 14 days. Denitrification losses ranged from 13.2 to 38.6% of N appl ied with the majority of gaseous N loss occurring as N-2. Total N-15 r ecoveries after 14 days, including the evolved gases, ranged from 68.7 to 88.2%. We conclude that denitrification is a major cause of fertil izer N loss from fine-textured soils, with nitrous oxide the major gas eous N product when soil nitrate concentrations are high.