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Chinese Journal of Applied Ecology ›› 2024, Vol. 35 ›› Issue (3): 615-621.doi: 10.13287/j.1001-9332.202403.005

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Soil C:N:P stoichiometry in rhizosphere and non-rhizosphere of Pinus sylvestris var. mongolica forests

LIU Yilin1, REN Yue1, GAO Guanglei1,2,3,4,5*, DING Guodong1,3,4,5, ZHANG Ying1,3,4,5, LIU Ye1   

  1. 1School of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China;
    2State Key Laboratory of Efficient Production of Forest Resources, Beijing 100083, China;
    3Yanchi Ecology Research Station of the Mu Us Desert, Yanchi 751500, Ningxia, China;
    4Engineering Research Center of Forestry Ecological Engineering, Beijing 100083, China;
    5Key Laboratory of State Forestry and Grassland Administration on Soil and Water Conservation, Beijing 100083, China
  • Received:2023-12-13 Revised:2024-01-24 Online:2024-03-18 Published:2024-06-18

Abstract: The aim of this study was to reveal the stoichiometric characteristics of carbon, nitrogen and phosphorus in rhizosphere and non-rhizosphere soils of Pinus sylvestris var. mongolica in the Hulunbuir desert. We investigated the contents and stoichiometry of organic carbon, total nitrogen, and total phosphorus contents of rhizosphere and non-rhizosphere soils across different stand ages (28, 37 and 46 a) of P. sylvestris var. mongolica plantations, with P. sylvestris var. mongolica natural forest as the control. We analyzed the correlation between soils properties and soil stoichiometry. The results showed that rhizosphere effect significantly affected soil N:P, and stand age significantly affected soil organic carbon content in P. sylvestris var. mongolica plantation. Soil organic carbon content in plantation was significantly lower than that in natural forest. Soil organic carbon and total nitrogen contents of plantations in both rhizosphere and non-rhizosphere soils firstly decreased and then increased with increasing stand age, while total phosphorus firstly increased and then decreased in rhizosphere soils, and firstly decreased and then increased in non-rhizosphere soils. There was significant positive correlations between C:N and C:P in rhizosphere soils but not in non-rhizosphere soils, suggesting that higher synergistic rhizosphere soil N and P limitation. The mean N:P values of rhizosphere and non-rhizosphere soils were 4.98 and 8.40, respectively, indicating that the growth of P. sylvestris var. mongolica was restricted by soil N and the rhizosphere soils were more N-restricted. The C:N:P stoichiometry of rhizosphere and non-rhizosphere soils were significantly influenced by soil properties, with available phosphorus being the most important driver. The growth of P. sylvestris var. mongolica was limited by N in the Hulunbuir desert, and root system played an obvious role in enriching and maintaining soil nutrients. It was recommended that soil nitrogen should be supplemented appropriately during the growth stage of P. sylvestris var. mongolica plantation, and phosphorus should be supplemented appropriately according to the synergistic nature of nitrogen and phosphorus limitation.

Key words: Pinus sylvestris var. mongolica, ecological stoichiometry, soil, rhizosphere effect, stand age