Plant and Soil ( IF 4.9 ) Pub Date : 2024-04-18 , DOI: 10.1007/s11104-024-06656-0 Muyu Tian , Nan Jiang , Chunjia Yu , Yulan Zhang , Weiwen Qiu , Zhenhua Chen , Jingkuan Wang , Lijun Chen
Aims
The degradation and transformation of soil organic nitrogen (SON) in semi-arid steppe are regulated by a series of enzymes involved in nitrogen(N) hydrolysis, the influence of N and carbon (C) additions on the soil N reserves, activities of N-hydrolyzing enzymes, and their relationships remain unclear.
Methods
In the Inner Mongolia prairie of China, a field experiment was conducted to study the effects of N (0, 25, 50, 100, 200 kg N ha−1 yr−1) and C (0, 250, 500 kg C ha−1 yr−1) additions on SON fractions and their relationships with N-hydrolyzing enzymes.
Results
Our results indicated that N addition significantly increased active-SON and N-acetyl-β-D-glucosaminidase (NAG) activities and decreased urease activities. C addition significantly increased microbial biomass carbon (MBC), NAG, and urease activities, and decreased protease activity and hydrolyzable unknown-N. N and C additions interacted affected the microbial biomass nitrogen (MBN), MBC: MBN, protease, and amidase activities. Structural equation modeling suggested that N addition had a direct positive effect on hydrolyzable NH4+-N and amino acid-N. Furthermore, N addition indirectly affected amino sugar-N through MBN and the activities of NAG and protease. C addition directly affected urease activity.
Conclusion
Our findings suggest that active-SON responded significantly to N addition, whereas stable-SON did not. Moreover, N-hydrolysis enzymes, especially NAG and proteases, play a fundamental role in the N turnover under N and C additions in semi-arid steppe soils. As such, our work provides useful information for the development of sustainable steppe farming practices.