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Grain yield and crop N offtake in response to residual fertilizer N in long‐term field experiments
Author(s) -
Petersen J.,
Thomsen I. K.,
Mattsson L.,
Hansen E. M.,
Christensen B. T.
Publication year - 2010
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/j.1475-2743.2010.00297.x
Subject(s) - fertilizer , agronomy , crop , manure , nutrient , yield (engineering) , field experiment , residual , crop yield , zoology , mathematics , environmental science , biology , ecology , materials science , algorithm , metallurgy
Organic inputs [e.g. animal manure (AM) and plant residues] contribute directly to the soil organic N pool, whereas mineral N fertilizer contributes indirectly by increasing the return of the crop residues and by microbial immobilization. To evaluate the residual effect of N treatments established in four long‐term (>35 yr) field experiments, we measured the response of barley (grain yield and N offtake at crop maturity) to six rates (0, 30, 60, 90, 120 and 150 kg N/ha) of mineral fertilizer N (N new ) applied in subplots replacing the customary long‐term plot treatments of fertilizer inputs (N prev ). Rates of N prev above 50–100 kg N/ha had no consistent effect on the soil N content, but this was up to 20% greater than that in unfertilized treatments. Long‐term unfertilized plots should not be used as control to test the residual value of N in modern agriculture with large production potentials. Although the effect of mineral N prev on grain yield and N offtake could be substituted by N new within a range of previous inputs, the value of N prev was not eliminated irrespective of N new rate. Provided a sufficient supply of plant nutrients other than N, the use‐efficiency of N new did not change significantly with previous mineral N fertilizer rate. The residual effect of mineral N fertilizer was negligible compared with the residual effect of N from AM and catch crop residues.