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Optimizing nitrogen input by balancing winter wheat yield and residual nitrate-N in soil in a long-term dryland field experiment in the Loess Plateau of China
•Nitrate-N residue in dryland soil was mainly affected by N rate, grain yield, time, precipitation and its distribution.•Nitrate-N was able to be residual even at no N application as high as 59kgNha−1.•Residual nitrate-N was found to be leached down to deep soil by 13.3–33.3cmy−1.•To reduce the nitr...
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Published in: | Field crops research 2015-09, Vol.181, p.32-41 |
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Main Authors: | , , , , , , , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
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Online Access: | Get full text |
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Summary: | •Nitrate-N residue in dryland soil was mainly affected by N rate, grain yield, time, precipitation and its distribution.•Nitrate-N was able to be residual even at no N application as high as 59kgNha−1.•Residual nitrate-N was found to be leached down to deep soil by 13.3–33.3cmy−1.•To reduce the nitrate-N residue, N application rates of 66–92kgNha−1 were recommended.
Nitrate-N residue (NR) in soil is attracting increasing attention because of its environmental risks. However, research information to regulate NR in soil by optimizing chemical nitrogen (N) fertilizer input and at the same time ensuring a satisfactory high grain yield is still lacking, particularly in the drylands of northwestern China. A 9-yr field experiment was initiated in 2004 in the Loess Plateau of China to investigate the dominant factors affecting NR in soil at harvest and optimize the N input for winter wheat by balancing the grain yield and NR in soil. Obtained results showed that varied grain yields and N application rates resulted in different NR in soil in dryland. The NR increased quadratically with the N rates, and the average NR was 59.0, 98.7, 175.1, 326.0, and 475.5kgNha−1 in 0–300cm soil, respectively, at N rates of 0, 80, 160, 240, and 320kgNha−1, of which 35.1, 54.5, 94.5, 186.5, and 222.0kgNha−1 was in the 0–100cm soil. Seasonal N residue (SNR) in soil also increased quadratically with N rate, with the yearly increases correspondingly being 0, 4.4, 8.8, 13.2, and 17.7kgNha−1. The fertilizer N residue (FNR) increased linearly with N rate, with the yearly FNR increases, respectively, to be 0.02, 7.1, 14.1, and 21.1kgNha−1 at N rates of 80, 160, 240, and 320kgNha−1. The seasonal nitrate-N residual depth (NRD) was mainly within the 0–100cm soil layer. The NR, SNR, FNR and NRD were all affected by but not correlated with precipitation. In the experimental site, the NR was able to be slowly leached downward to deeper soil by 13.3–33.3cm each year driven by precipitation. The findings suggest that if the NR is to be decreased to 55–67kgNha−1 in the 0–100cm soil while maintaining a relatively high grain yield (4487–5000kgha−1), an N application rate of 66–92kgNha−1 should be recommended. |
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ISSN: | 0378-4290 1872-6852 |
DOI: | 10.1016/j.fcr.2015.06.014 |