Optimized fertigation maintains high yield and mitigates N2O and NO emissions in an intensified wheat–maize cropping system
Graphical abstract
Introduction
Globally, agricultural soils contribute approximately 67% and 18% of total anthropogenic N2O and NO emissions, respectively (Reay et al., 2012; Gaihre et al., 2015). Total fertilized cropland annually emits 1.7–4.8 Tg of N2O-N and 1.6–8.9 Tg of NO-N (IPCC, 2007; Cui et al., 2012; Yao et al., 2017). Accordingly, it is important to mitigate N2O and NO emissions through optimized farming practices in agricultural sectors.
Drip irrigation combined with dissolved N fertilizer (fertigation), which provides an appropriate amount of N and water to crop roots in a more precise and timely manner than does broadcast fertilization, has been confirmed to be an efficient method of irrigation and fertilization (Abalos et al., 2014; Farneselli et al., 2015). Many studies have shown that drip fertigation can decrease N losses (Badr et al., 2012; Koocheki et al., 2014) and reduce transformable N to N2O and/or NO (Maris et al., 2015). Wang et al. (2016a) reported a significant reduction (14.6%) of N2O in the winter wheat season under drip irrigation, compared with flood irrigation. However, Tian et al. (2016) found that drip fertigation reduced N2O emissions by 7.7%, but increased NO emissions by 21.7% during the summer maize season. These findings indicated that edaphic properties, climate conditions, and farming practices may exert different effects on soil N2O and NO emissions (Barnard et al., 2005; Deppe et al., 2016; Zhou et al., 2017).
Northern China, one of the most intensified agricultural regions in China, produced 67% and 28% of the nation’s wheat (Triticum aestivum L.) and maize (Zea mays L.), respectively, in 2014 (NBSC, 2015). Various sound farming practices have been implemented to reduce fertilizer N and water inputs and maintain the high crop yield in this region since the 1990s (Zhang et al., 2011). The fertilizer N efficiency in the region has been reported to be <30% for maize and wheat (Miao et al., 2011). The reported proportions of N losses from applied fertilizers via nitrification and denitrification range from 0.9% to 10.9% (Zhang et al., 2008; Ju et al., 2009). Such gaseous N losses (including NH3) exert potential pressure on the aquatic environment (Chien et al., 2009) and air quality (Xu et al., 2016), and contribute to regional and global greenhouse gas emissions (Zhang et al., 2017). In northern China, agriculture is dependent on pumping deep groundwater for irrigation, and irrigation water accounts for 80% of total water use in the region (Deng et al., 2006). As a result, the groundwater level is declining rapidly at a rate of 0.8 m yr−1 in this region (Fang et al., 2010). Heavy irrigation has also increased NO3− leaching from cropland (Deng et al., 2006), resulting in the entry of NO3− to deeper profiles, after which it infiltrates groundwater or is permanently lost from the system (Currell et al., 2012). Optimizing fertilization and irrigation by methods such as sprinkling and drip irrigation has been suggested as a priority farming measure and is being expanded in the region. Currently, these processes are applied to >1 million ha of maize and >0.3 million ha of wheat agricultural areas, with a target of total 2.7 million ha in China by 2020 (the “Promotion of Implementation of Fertigation” policy; MOA, 2016).
In this study, we hypothesized that drip fertigation would substantially decrease N2O emissions but increase NO production because of higher oxidation of N2O to NO during drip fertigation than during flood irrigation. To test this hypothesis, we monitored the N2O and NO losses, crop production, and soil conditions in northern China under flood and drip irrigation with different N rates in the typical winter wheat–summer maize cropping system of the region. We aimed to analyze the effects of optimized fertilization and irrigation on crop production and N2O and NO emissions. The overall aim of this research is to develop appropriate practices to mitigate the production of greenhouse gases and improve resource use while maintaining high land productivity.
Section snippets
Study area
We initiated the field experiment in 2015 at the Huantai Experimental Station of China Agricultural University, Shandong province (36°51′50″–37°06′00″N, 117°50′00″–118°10′40″E). The region has a typical continental monsoon climate, with an annual average temperature of 12.5 °C (Chen et al., 2010). Rainfall occurs mainly in June, July, and August. The annual precipitation is 542.8 mm and the annual frost-free season is about 198 days (Liao et al., 2015). The soil parent materials are mainly
Climate and soil conditions
During the study period, the higher frequencies of fertilization/irrigation events in drip irrigation (11 times) than in flood irrigation (four times) treatments caused the mean soil temperature to be 13.9 °C (wheat season) and 25.2 °C (maize season) in the flood irrigation treatments (FN600 and FN0). These values were significantly higher than those in the drip irrigation (N600, N400, and N0) treatments (by 9.4% and 5% in wheat and maize season, respectively; Table 1, Fig. 1, Fig. 2). Soil
N2O and NO generation and diffusion in alkaline agricultural soils
Both N2O and NO are produced through the microbial processes of nitrate dissimilation (denitrification and nitrate ammonification) and nitrification (ammonia oxidation and nitrifier denitrification) and through abiotic chemo-denitrification reactions (Baggs, 2008; Kool et al., 2011; Zhu et al., 2013). In previous studies, the NO emissions from agricultural fields were mainly ascribed to nitrification, whereas the N2O emissions were ascribed to both nitrification and denitrification (Maljanen et
Conclusions
Drip fertigation and flood irrigation with synthetic N fertilizer in a winter wheat–summer maize cropping system in northern China resulted in different N2O and NO emissions. Drip fertigation (at the same N level as FN600) significantly reduced N2O emissions by 19.9% during the maize season but did not significantly affect significant N2O emissions during the wheat season, and increased the NO emissions in the wheat and maize seasons by 20.9% and 11.0%, respectively, when compared with flood
Acknowledgements
This study was supported by the State's Key Project of Research and Development Plan (2016YFD0800104 and 2017YFD0800605). We thank the anonymous reviewers for their valuable comments, which greatly improved the manuscript. We thank Jeremy Kamen, MSc, and Jennifer Smith, PhD, from Liwen Bianji, Edanz Group China (www.liwenbianji.cn/ac), for editing the English text of drafts of this manuscript.
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