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林业科学 ›› 2026, Vol. 62 ›› Issue (9): 28-41.doi: 10.11707/j.1001-7488.LYKX20260079

• 前沿热点 • 上一篇    

晋西黄土区典型人工林树种和林分密度对土壤呼吸及其温度敏感性的影响

罗鸿1,2,许行1,2,*(),张晓花1,2,张志强1,2   

  1. 1. 山西吉县森林生态系统国家野外科学观测研究站 北京林业大学 北京 100083
    2. 北京林业大学水土保持学院 北京 100083
  • 收稿日期:2026-02-04 修回日期:2026-07-28 出版日期:2026-09-10 发布日期:2026-09-16
  • 通讯作者: 许行 E-mail:hangxu@bjfu.edu.cn
  • 基金资助:
    国家自然科学基金项目(32271967, 32301664);中国科协青年人才托举工程(YESS20230091);北京林业大学科技创新计划项目(JCYJ202507)。

Effects of Tree Species and Stand Density on Soil Respiration and Its Temperature Sensitivity in Typical Plantations on the Loess Plateau of Western Shanxi Province

Hong Luo1,2,Hang Xu1,2,*(),Xiaohua Zhang1,2,Zhiqiang Zhang1,2   

  1. 1. National Field Scientific Observation and Research Station of Forest Ecosystem in Jixian County of Shanxi Province  Beijing Forestry University Beijing 100083
    2. School of Soil and Water Conservation, Beijing Forestry University Beijing 100083
  • Received:2026-02-04 Revised:2026-07-28 Online:2026-09-10 Published:2026-09-16
  • Contact: Hang Xu E-mail:hangxu@bjfu.edu.cn

摘要:

目的: 探究晋西黄土区人工林不同树种、不同密度条件下的土壤呼吸速率(RS)和土壤呼吸温度敏感性指数(Q10)特征,识别其关键驱动因子,为该区域人工林密度调控、树种配置优化和碳循环模型参数化提供依据。方法: 在晋西黄土区刺槐和油松人工纯林分别选择5个林分密度梯度,其中刺槐林密度为900、1 200、1 500、1 800和2 400株·hm–2,油松林密度为900、1 200、1 800、2 400和2 800株·hm–2,于2024年生长季(5—10月)采用LI-8100土壤碳通量监测系统测定土壤呼吸速率(RS);同时测定土壤的理化性质、土壤微生物特征、凋落物现存量、凋落物碳含量、细根生物量密度以及细根碳氮磷含量,并通过指数模型估算Q10值,进一步解析RSQ10值变异的主要驱动机制。结果: 1) 在控制土壤温度、土壤含水量和月份后,树种对RS的影响达显著水平,油松林RS[(3.47±0.17) μmol·m–2s–1]显著高于刺槐林[(3.02±0.09) μmol·m–2s–1],其Q10值(3.23±0.26)也高于刺槐林(2.50±0.13)。2) 随林分密度升高,两树种RS均呈上升趋势,但同一树种不同密度间差异不显著。Q10值响应呈树种分异:刺槐林各密度间Q10值差异不显著,油松林2 800 株·hm–2密度的Q10值显著高于1 200 株·hm–2P<0.05)。3) 相关分析表明,土壤黏粒含量和凋落物现存量是RS变异的关键驱动因子,凋落物特征、细根特征和土壤微生物特性在Q10值变化中发挥核心作用。结论: 人工林土壤呼吸和土壤呼吸温度敏感性指数受树种和林分密度的共同调控。植物凋落物特征、细根特征和土壤微生物特性是驱动土壤碳释放温度响应的关键因素。树种主要通过凋落物输入数量和质量的差异来影响土壤呼吸,油松林凋落物现存量大、碳含量高,为微生物呼吸提供了更充足的底物,使其RSQ10值整体高于刺槐林。林分密度对土壤呼吸的影响则因树种而异:刺槐林各密度间Q10值变化不显著;油松林的高密度林分下底物充足,微生物代谢对温度的敏感性更强,驱动Q10值显著升高。本研究深化了对人工林土壤碳通量变化及其温度响应机制的认识,为人工林密度调控和结构优化提供了理论依据。

关键词: 土壤呼吸, 温度敏感性, 人工林树种, 林分密度

Abstract:

Objective: The objective of this study is to reveal the characteristics of soil respiration rate (RS) and soil respiration temperature sensitivity index (Q10) under different tree species and stand density conditions in plantations in the Loess Plateau of western Shanxi Province, and identify the key driving factors, so as to provide a scientific basis for plantation management and parameter optimization of carbon cycle models in this region. Method: Five stand density gradients were selected in pure Robinia pseudoacacia and Pinus tabuliformis plantations. The densities were 900, 1 200, 1 500, 1 800, and 2 400 trees·hm–2 for R. pseudoacacia, and 900, 1 200, 1 800, 2 400, and 2 800 trees·hm–2 for P. tabuliformis. A LI-8100 soil carbon flux monitoring system was used to continuously measure RS during the growing season (from May to October, 2024). Soil physicochemical properties, soil microbial characteristics, as well as litter standing crop, litter carbon content, fine root biomass density, and carbon, nitrogen and phosphorus contents of fine roots simultaneously determined. Q10 was estimated using an exponential model, and the main driving mechanisms underlying the variation in RS and Q10 were further elucidated. Result: 1) After controlling for soil temperature, soil water content, and month, tree species significantly affected RS. The RS in the P. tabuliformis plantations [(3.47±0.17) μmol·m–2s–1 ] was significantly higher than that in the R. pseudoacacia plantations [(3.02±0.09) μmol·m–2s–1]. The Q10 of P. tabuliformis plantations (3.23±0.26) was also numerically higher than that of R. pseudoacacia plantations (2.50±0.13). 2) As the forest density increased, RS in the two plantations increased, but there were no significant differences in RS among different density treatments within each species. The response of Q10 to stand density differed between the two species. There was no significant difference in Q10 among different density treatments in R. pseudoacacia plantations, while in P. tabuliformis plantations, Q10 values at the density of 2 800 trees·hm?2 was significantly higher than that at 1 200 trees·hm?2 (P<0.05). 3) Correlation analysis indicated that soil clay content and litter standing crop were key drivers for variation in RS, and plant litter traits, fine root traits, and soil microbial properties played central roles in fluctuations in Q10 values. Conclusion: Soil respiration and soil respiration temperature sensitivity index in plantations are jointly regulated by tree species and stand density. Specifically, the characteristics of plant litter, fine root, and soil microorganisms are the key factors driving the temperature response of soil carbon release. Tree species influence soil respiration primarily through differences in the quantity and quality of litter input. P. tabuliformis plantation has larger litter standing crop and higher carbon content, providing more abundant substrates for microbial respiration, resulting in overall higher RS and Q10 values than R. pseudoacacia plantations. The effect of stand density on soil respiration ias species-dependent: Q10 values remains stable across density classes in R. pseudoacacia plantation, while the high-density P. tabuliformis stands have sufficient substrates, and the microbial metabolism is more sensitive to temperature, jointly driving a significant increase in Q10 values. This study deepens understanding of changes in soil carbon flux and the mechanisms underlying its temperature response in plantations, and provides a theoretical basis for density regulation and structural optimization of plantations.

Key words: soil respiration, temperature sensitivity, plantation tree species, stand density

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