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Arid Land Geography ›› 2025, Vol. 48 ›› Issue (8): 1492-1501.doi: 10.12118/j.issn.1000-6060.2024.700

• Soil Resources • Previous Articles     Next Articles

Soil carbon, nitrogen and phosphorus stoichiometric characteristics of typical artificial vegetation in Qingshuihe County, Inner Mongolia

MIN Xue1(), WU Yeli1, ZHANG Ying1,2, DING Guodong1,2,3,4(), YANG Zhiheng5   

  1. 1. School of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China
    2. Key Laboratory of Soil and Water Conservation, State Forestry and Grassland Administration, Beijing Forestry University, Beijing 100083, China
    3. Engineering Research Center of Forestry Ecological Engineering, Ministry of Education, Beijing Forestry University, Beijing 100083, China
    4. National Positioning Observation and Research Station of Mu Us Sandy Land Ecosystem, Yanchi 751500, Ningxia, China
    5. Beijing Greensource Environment Planning & Design Institute Co., Ltd., Beijing 100083, China
  • Received:2024-11-14 Revised:2025-01-06 Online:2025-08-25 Published:2025-08-21
  • Contact: DING Guodong E-mail:minxue11@163.com;dch1999@263.net

Abstract:

The stoichiometric relationship of carbon (C), nitrogen (N), and phosphorus (P) in soil is crucial for understanding the ecological function of different vegetation types. This study examined four typical artificial vegetation types (Populus L., Pinus sylvestris, Pinus tabulaeformis, and Caragana korshinskii) in Qingshuihe County, Inner Mongolia, China, with natural gramineous grassland as the control. The concentrations of soil C, N, and P along with their stoichiometric ratios, within the 0-100-cm soil profile, were investigated. The key results were as follows. (1) In the surface-soil layer (0-20 cm), C, N, and P levels across the five vegetation types were 3.29-6.02 g·kg−1, 0.52-0.69 g·kg−1, and 0.37-0.62 g·kg−1, respectively. Soil C and N levels were below the national surface-soil average, indicating poor soil fertility. (2) In the 0-20 cm layer, soils under artificial vegetation had lower C content, N levels, and C/N ratios compared with those under grassland, with significantly lower C and C/N observed in P. sylvestris and C. korshinskii (P<0.05). At depths of 20-50 cm and 50-100 cm, C and N levels were highest under grassland and lower under artificial vegetation, with P. sylvestris showing the lowest C/N ratio. Soil P content was significantly higher under artificial vegetation than those under grassland at all depths, whereas C/P and N/P ratios were significantly lower than those under grassland. (3) Correlation analysis revealed strong positive relationships between soil C and N and between C/P and N/P (P<0.001). Soil C, N, and P levels were significantly affected by vegetation type and soil depth (P<0.001) and all decreased with increasing depth, indicating strong surface accumulation. Given the high soil phosphorus availability in the study area, which supports the growth of herbaceous vegetation, and the superior soil nutrient conservation capacity of herbaceous plants relative to artificial irrigated vegetation, ecological restoration efforts in this region should primarily focus on conserving and restoring native herbaceous vegetation. This study contributes to understanding the soil nutrient cycle, assessing the ecological benefits of different vegetation types, and providing a scientific basis for regional ecological restoration and resource management.

Key words: artificial vegetation, natural grassland, soil nutrients, ecological stoichiometry