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Driving factors of variation in fertilizer nitrogen recovery efficiency in maize cropping systems across China and its microbial mechanism

文献类型： 外文期刊

作者： Xiao, Xun 1 ; Wang, Yuekai 3 ; Dai, Wentai 1 ; Liu, Kailou 4 ; Jiang, Fahui 1 ; Xie, Zubin 1 ; Shen, Ren Fang 1 ; Zhao, Xue Qiang 1 ;

作者机构： 1.Chinese Acad Sci, Inst Soil Sci, State Key Lab Soil & Sustainable Agr, Nanjing 210008, Peoples R China

2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China

3.Nanjing Agr Univ, Key Lab Crop Physiol Ecol & Prod Management, Minist Agr & Rural Affairs, Nanjing, Peoples R China

4.Jiangxi Inst Red Soil & Germplasm Resources, Natl Engn & Technol Res Ctr Red Soil Improvement, Nanchang 331717, Peoples R China

关键词： Absolute quantification sequencing; Nitrogen fate; Nitrogen recovery efficiency; Soil organic matter; Soil pH

期刊名称：GEODERMA （ 影响因子：6.6； 五年影响因子：7.3 ）

ISSN： 0016-7061

年卷期： 2024 年 451 卷

页码：

收录情况： SCI

摘要： Maize ( Zea mays L.) fertilizer nitrogen (N) recovery efficiency (FNRE) shows regional differences in China, and is more strongly affected by soil properties than by climate. However, how soil factors regulate maize FNRE is poorly understood. Herein, 15 N tracer pot experiments combined with absolute microbial quantification sequencing were conducted using eight soils covering the main maize cropping systems from northern to southern China. The aim was to elucidate which soil factors affect maize FNRE and identify their optimal range for maximizing FNRE while minimizing N loss. Our results show that soil pH, soil organic matter (SOM), and clay and sand contents were the key factors affecting maize biomass and FNRE across the eight tested soils. Maize biomass and FNRE had parabolic relationships with soil pH, SOM, clay, and sand contents, whereas N loss displayed the opposite trend. The highest maize biomass and FNRE and lowest fertilizer N loss were in the soils with pH of 6.50-6.62, SOM level of 35.25-46.90 g kg- 1 , clay content of 41.12 %-44.42 %, and sand content of 17.71 %-23.41 %. Under these soil conditions, maize growth and soil N retention capabilities exhibited a high degree of coordination. Bacterial communities differed significantly among the soils, sharing the same soil drivers as maize biomass and FNRE. The abundance of N cycling genes ( nasA , narI, narJ, nrfA, and nrfB) involved in dissimilatory nitrate reduction to ammonium (DNRA) was positively correlated with FNRE and negatively correlated with fertilizer N loss, suggesting that DNRA may contribute to soil N retention and enhance FNRE by affecting substrates for nitrification and denitrification. Our study demonstrates that soil pH, SOM, and texture are three key factors driving FNRE variation in maize cropping systems across China, and high microbial-driven DNRA may account for maximum maize FNRE. These findings highlight the importance of tailored FNRE enhancement strategies based on soil characteristics.

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