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Ammonia emissions from urea, stabilized urea and calcium ammonium nitrate: insights into loss abatement in temperate grassland
Author(s) -
Forrestal P. J.,
Harty M.,
Carolan R.,
Lanigan G. J.,
Watson C. J.,
Laughlin R. J.,
McNeill G.,
Chambers B. J.,
Richards K. G.
Publication year - 2016
Publication title -
soil use and management
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.709
H-Index - 81
eISSN - 1475-2743
pISSN - 0266-0032
DOI - 10.1111/sum.12232
Subject(s) - urea , ammonia volatilization from urea , ammonia , chemistry , fertilizer , temperate climate , ammonium , zoology , grassland , ammonium nitrate , nitrogen , nitrate , agronomy , environmental chemistry , botany , biology , biochemistry , organic chemistry
Fertilizer nitrogen (N) contributes to ammonia ( NH 3 ) emissions, which European Union member states have committed to reduce. This study focused on evaluating NH 3 ‐N loss from a suite of N fertilizers over multiple applications, and gained insights into the temporal and seasonal patterns of NH 3 ‐N loss from urea in Irish temperate grassland using wind tunnels. The fertilizers evaluated were calcium ammonium nitrate ( CAN ), urea and urea with the N stabilizers N‐( n ‐ butyl ) thiophosphoric triamide ( NBPT ), dicyandiamide ( DCD ), DCD + NBPT and a maleic and itaconic acid polymer ( MIP ). 200 (and 400 for urea only) kg N/ha/yr was applied in five equal applications over the growing season at two grassland sites (one for MIP ). Mean NH 3 ‐N losses from CAN were 85% lower than urea and had highly variable loss (range 45% points). The effect of DCD on NH 3 emissions was variable. MIP did not decrease NH 3 ‐N loss, but NBPT caused a 78.5% reduction and, when combined with DCD , a 74% reduction compared with urea alone. Mean spring and summer losses from urea were similar, although spring losses were more variable with both the lowest and highest losses. Maximum NH 3 ‐N loss usually occurred on the second day after application. These data highlight the potential of stabilized urea to alter urea NH 3 ‐N loss outcomes in temperate grassland, the need for caution when using season as a loss risk guide and that urea hydrolysis in temperate grassland initiates quickly. Micrometeorological measurements focused specifically on urea are needed to determine absolute NH 3 ‐N loss levels in Irish temperate grassland.

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