Abstract
The soil nitrogen (N) cycle is an essential role of the biogeochemical cycle. Bacteria play an irreplaceable part in the soil N cycle, but the impact of different N gradients on bacterial communities remains unclear. The purpose of this research was to explore the bacterial abundance, community composition, and diversity under different N application rates in a water-limited area. We investigated the bacterial abundance, diversity, community composition, and structure under five different N gradients (0, 90, 150, 210, and 270 kg ha−1) using real-time quantitative PCR and high-throughput sequencing, and then explored bacterial functional groups with FAPROTAX. N application significantly affected bacterial abundance and community composition. Bacterial diversity was enhanced at low N application rates and reduced at higher N application rates. Principal coordinate analysis showed that bacterial community structure was separated into two groups between low N application rates and high N application rates; these differences in bacterial community structure may be driven by available nitrogen (AN). The results of FAPROTAX revealed that N application promoted the functions of Aerobic_nitrite_oxidation, Nitrate_reduction, and Aerobic_ammonia_oxidation, but inhibited the Nitrogen_fixation function of the bacterial community. The high N network caused the reduction of network structure stability. Our results revealed that N fertilizer driven bacterial community structure and soil nutrients were the main influential factors in the variation of bacterial community structure. We suggest that the optimal N application rate in this study may be approximately 150 kg ha−1, based on the variations of soil properties and bacterial community structure in semi-arid areas.
Highlights
Nitrogen (N) is an essential nutrient element for plant growth
The bacterial abundance of different N gradients ranged from 2.78 × to 3.10 × copies g−1 soil (Figure 1)
Our results showed that the impacts of diverse N application rates on soil properties varied significantly, and contributed to increases in soil nutrient levels
Summary
Nitrogen (N) is an essential nutrient element for plant growth. The annual N input into agricultural systems accounts for about 25% of global N use, of which about 100 Tg of N fertilizer per year enters the N cycle in agricultural ecosystems [1,2]. Several studies have reported that increasing N absorption can increase maize yield, which has led to excessive N application in agricultural ecosystems [3]. The N rates applied by farmers in. North China are much higher than the N absorption rates of crops. The N application rates for farmers exceed 100% of N required by crops [4]. Vitousek et al [5]
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