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Journal of Desert Research ›› 2025, Vol. 45 ›› Issue (4): 153-165.DOI: 10.7522/j.issn.1000-694X.2025.00106

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Spatial patterns and influencing factors of soil microbial carbon, nitrogen and phosphorus stoichiometry in Horqin Sandy Land

Bo Yao1,2,3(), Jie Lian1,2,3, Xiangwen Gong4, Xiaoming Mou1,2,3, Yulin Li1,2,3, Yuqiang Li1,2,3, Xuyang Wang2,3()   

  1. 1.State Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands /, Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China
    2.Naiman Desertification Research Station, Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China
    3.University of Chinese Academy of Sciences,Beijing 100049,China
    4.School of Geographical Sciences / Chongqing Jinfo Mountain Karst Ecosystem National Observation and Research Station,Southwest University,Chongqing 400715,China
  • Received:2025-04-25 Revised:2025-07-10 Online:2025-07-20 Published:2025-08-18
  • Contact: Xuyang Wang

Abstract:

Understanding the spatial pattern of soil and microbial carbon, nitrogen and phosphorus (C∶N∶P) stoichiometry and its drivers are important for regulating ecosystem function and responding to global climate change. In this study, we applied geostatistical methods and constructed a random forest model to quantify the drivers of the spatial distribution of soil and microbial C∶N∶P stoichiometry in the Horqin Sandy Land through a regional field survey. The results showed that low-value zones for soil microbial carbon (MBC), nitrogen (MBN) and phosphorus (MBP) were primarily located in the central part of the Horqin Sandy Land. In contrast, high-value zones were mainly found in the northern part of the Horqin Sandy Land, specifically in the foothills of the Greater Khingan Mountains. The ratios of MBC∶MBP and MBN∶MBP gradually increased from south to north. In the Horqin Sandy Land, the MBC∶MBN ratio ranged from 0.63 to 28.29 (average: 7.3), the MBC∶MBP ratio from 0.35 to 91.27 (average: 11.26), and the MBN∶MBP ratio from 0.07 to 10.16 (average: 1.56). These values were all lower than the global and Chinese stoichiometric ratios. Overall, the region exhibited limitations in C, N and P, with MBC and MBN content primarily influencing the spatial variation of soil microbial biomass C∶N∶P in the Horqin Sandy Land.

Key words: soil carbon, nitrogen and phosphorus, soil microbial biomass, ecological stoichiometry, spatial pattern, Horqin Sandy Land

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