Organic acids can enhance inorganic nitrogen transformation in rhizosphere soil, however the specific influence of long-chain organic acids on the community and functional structure of soil microorganisms that control nitrogen cycling is poorly understood. Organic acids have shown potential to increase the resilience of alpine ecosystems against desertification. To address this knowledge gap, we conducted a controlled experiment in a microcosm rhizosphere system. Using artificial roots (7.85 cm2 surface area), we amended Qinghai-Tibet Plateau soil with palmitic acid for 45 days at three secretion rates (½ × , 1 × , and 2 × the in situ rate of 3.20 μg C d-1 cm-2), corresponding to 12.56, 25.12, and 50.24 μg C d-1 root-1 respectively, with a control group receiving only osmoregulation solution. The results revealed a remarkable 81 % increase in soil NH4+-N concentration at the highest addition rate of palmitic acid. Moreover, both microbial biomass and the abundance of nitrogen-fixing genes nifK (12.25 times), nifH (7.63 times), and nifD (27.33 times) increased significantly, alongside a substantial rise in the relative abundance of Azospirillum (12.9-fold). Notably, 82 % of biomarkers in the high-rate palmitic acid treatment were linked to nitrogen fixation. The structural equation model indicated a direct impact of nitrogen fixation on NH4+-N concentration. Our findings suggest that palmitic acid primarily enhances microbial biomass and drives nitrogen fixation processes through its decline to pH, rather than serving as a direct carbon source. Consequently, within the range of our experimental setup, the preferential selection of plant species with a high root exudation rate of palmitic acid can optimize NH4+-N retention in rhizosphere soil, thereby promoting plant growth and facilitating vegetation restoration across the desertification alpine grasslands in the Qinghai-Tibet Plateau.
Keywords: Alpine grassland; Desertification restoration; Microbial functional taxa; Nitrogen cycle; Root exudate.
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