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Recovery of 15 N‐Labelled Urea Applied to Wheat ( Triticum aestivum L.) in the Ethiopian Highlands as Affected by P Fertilization
Author(s) -
Gorfu A.,
Kühne R. F.,
Tanner D. G.,
Vlek P. L. G.
Publication year - 2003
Publication title -
journal of agronomy and crop science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.095
H-Index - 74
eISSN - 1439-037X
pISSN - 0931-2250
DOI - 10.1046/j.1439-037x.2003.00006.x
Subject(s) - fertilizer , nutrient , agronomy , phosphorus , nitrogen , human fertilization , urea , crop , zoology , grain yield , biology , chemistry , ecology , organic chemistry , biochemistry
Soil degradation and depletion of soil nutrients are among the major factors threatening sustainable cereal production in the Ethiopian highlands. Fertilizer use as a means of mitigating nutrient depletion has become widely accepted. The fate of fertilizer nitrogen (N) applied to a semidwarf bread wheat system was determined in microplots receiving 41 kg N ha −1 in the form of urea labelled with 5.617 % atom excess 15 N, without and with the application of phosphorus (P) at 20 kg P ha −1 . The study was conducted in three different agro‐ecological zones at 2200, 2400 and 2800 m above sea level (masl) (Kulumsa, Asasa and Bekoji, respectively) in the south‐eastern Ethiopian highlands. Yield and yield response to N diminished with elevation, while the response to P increased with elevation, with a significant increase in wheat grain yield observed at Bekoji (2800 masl). N harvest index and N use efficiency improved in response to P application at Asasa (2400 masl). Crop removal accounted for 25–64 and 36–64 % of the applied N without and with P, respectively. The corresponding fractions of 15 N recovered in the soil ranged from 2.9 to 3.5 % and from 3.2 to 3.7 %, respectively. Recoveries of applied 15 N were 67 and 52 % at Kulumsa and Asasa, but only 25 % at the highest elevation site, Bekoji. Fertilizer P significantly enhanced N recovery at Asasa (60 %) and Bekoji (36 %), but not at Kulumsa, where the soil had a high level of residual P from previous applications. The fraction of 15 N recovered in the soil–plant system was rather low at Bekoji. However, the rate of 15 N recovery was significantly improved (by 37 %) when fertilizer P was added to the soil. Across all locations, the unaccounted 15 N may have been lost primarily through denitrification and volatilization.