On-farm estimation of indigenous nitrogen supply for site-specific nitrogen management in the North China plain |
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Authors: | Zhenling Cui Fusuo Zhang Xinping Chen Yuxin Miao Junliang Li Liwei Shi Jiufei Xu Youliang Ye Chunsheng Liu Zhiping Yang Qiang Zhang Shaomin Huang Dejun Bao |
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Affiliation: | (1) Department of Plant Nutrition, College of Resources and Environmental Sciences, China Agricultural University, Beijing, 100094, China;(2) Department of Agronomy, Qingdao Agricultural University, Qingdao, Shandong, 266023, China;(3) College of Resource and Environmental Sciences, Henan Agricultural University, Zhengzhou, Henan, 450000, China;(4) College of Resource and Environmental Sciences, Shandong Agricultural University, Taian, Shandong, 271018, China;(5) Institute of Soil Science and Fertilizer, Shanxi Academy of Agricultural Sciences, Taiyuan, Shanxi, 030031, China;(6) Institute of Soil Science and Fertilizer, Henan Academy of Agricultural Sciences, Zhengzhou, Henan, 450000, China |
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Abstract: | Estimating indigenous nitrogen supply (INS) by measurement of crop N uptake in N omission plots for site-specific N management is not feasible on a routine basis because it involves destructive plant sampling and plant tissue analysis, which is time-consuming and expensive. The objective of this study was to determine the amount of INS and develop a method to estimate it using soil testing in the North China plain (NCP). On-farm experiments at 229 sites were conducted from 2003 to 2005 in seven key winter wheat (Triticum aestivum L.)/summer maize (Zea mays L.) production regions of the NCP. The mean INS during the wheat-growing season was129 kg N ha−1 with a range from 62 to 212 kg N ha−1, and it varied from 69 to 202 kg N ha−1 with a mean of 142 kg N ha−1 during the maize-growing season. Considering all sites, the variability of INS was not simulated by initial soil N min or apparent N mineralization (N organic) alone, while together they could explain about 38% and 60% of INS during the wheat and maize-growing seasons, respectively. During the wheat-growing season, mean N organic was 63 kg N ha−1, and 59% and 33% of its variation could be explained by SOM in high-yielding regions (mean yield, 7.6 t ha−1) and low-yielding regions (mean yield, 5.3 t ha−1), respectively. Mean N organic during the maize-growing season was 109 kg N ha−1, 22% of which could be explained by SOM across all sites. An average of 40% and 42% of INS variation could be explained by both SOM and initial soil N min content during the wheat and maize-growing seasons, respectively. We conclude that the accuracy of estimating crop N requirement for site-specific N management will be increased by using initial soil N min and SOM. |
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Keywords: | Indigenous nitrogen supply Soil N supply Apparent N mineralization Soil organic matter |
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