Release, movement and recovery of 3,4-dimethylpyrazole phosphate (DMPP), ammonium, and nitrate from stabilized nitrogen fertilizer granules in a silty clay soil under laboratory conditions

Citation
F. Azam et al., Release, movement and recovery of 3,4-dimethylpyrazole phosphate (DMPP), ammonium, and nitrate from stabilized nitrogen fertilizer granules in a silty clay soil under laboratory conditions, BIOL FERT S, 34(2), 2001, pp. 118-125
Citations number
26
Categorie Soggetti
Environment/Ecology
Journal title
BIOLOGY AND FERTILITY OF SOILS
ISSN journal
01782762 → ACNP
Volume
34
Issue
2
Year of publication
2001
Pages
118 - 125
Database
ISI
SICI code
0178-2762(200108)34:2<118:RMARO3>2.0.ZU;2-L
Abstract
In model experiments under laboratory conditions the release of 3,4-dimethy lpyrazole phosphate (DMPP; ENTEC), NH4+-N, and NO3--N from the ENTEC-fertil izer granules placed on a silty clay soil was studied. The air-dried soil c ontained in Petri dishes was moistened to 18% or 24% water holding capacity , and incubated for 10 days at 4 degreesC, 15 degreesC or 25 degreesC after placing the granules in the centre of the plates. Plates without granules served as controls. At appropriate intervals, soil cores were taken at 5-20 and 25-40 mm distance from the granules and analysed for DMPP, NH4+-N and NO3--N. Amongst the three fertilizer ingredients, NO3- was found to be the most mobile showing a fairly uniform distribution in both soil zones during 10 days of incubation. Under the different temperature and moisture condit ions, more than 80% of DMPP remained within the 0- to 5-mm region around th e granule. Between 5% and 15% of DMPP was found in the 5- to 20-mm region, and <3% moved into the 25- to 40-mm region. Increasing temperature and mois ture facilitated the movement of DMPP in soil. NH4+ diffused faster than DM PP and showed a recovery of up to 13% in the 25- to 40-mm region under the given conditions. NH4+ was separated from the DMPP within 10 days, as revea led by an increase in the NH4+-N to DMP ratios. An intensive N2O flux was o bserved within the 5- to 20-mm zone of the fertilizer granules. which was a scribed to heterotrophic denitrification rather than nitrification.