计划火烧对滇中云南松根系碳氮磷生态化学计量特征的影响
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1.西南林业大学 水土保持学院;2.西南林业大学 生态与环境学院(湿地学院)

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S7, S76

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云南省科技厅面上项目“15N稳定同位素示踪云南松土壤氧化亚氮排放对计划火烧响应的过程及机制”(202401AT070262);云南省农业基础研究联合专项“计划火烧影响滇中亚热带云南松凋落物呼吸的微生物学机制”(202301BD070001-059)


Effects of planned fire on ecological and chemical characteristics of carbon, nitrogen and phosphorus in pine root system in central Yunnan province
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Fund Project:

General project of Yunnan Provincial Science and Technology Department, "15N Stable Isotope Tracing of the Process and Mechanism of Nitrous Oxide Emissions from Yunnan Pine Soil in Response to Planned Burning" (202401AT070262); Joint Special Project of Basic Agricultural Research in Yunnan Province, "Microbiological Mechanism of Planned Burning Affecting Litter Respiration of Yunnan Pine in Central Yunnan Subtropical Zone" (202301BD070001-059)

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    摘要:

    摘 要:[目的] 为深入研究计划火烧对云南松根系和碳氮磷生态化学计量特征的影响。[方法] 本研究以云南省玉溪市新平县照壁山计划火烧后一年的火烧迹地为研究对象,采集对照样地(UB)和火烧样地(PB)内的云南松乔木根系,分析了活根系生物量(B)、形态分布和根系有机碳(ROC)、根系全氮(RTN)、根系全磷(RTP)及生态化学计量特征的变化。[结果] ① 火烧后一年云南松不同径级B为7.553-288.368 g/m2,在0-20 cm土层低于UB(6.9%-21.5%);火烧后一年细根根系生物量密度(RBD)、根长密度(RLD)、根表面积密度(SAD)在0-20 cm土层降低(0.5%-21.5%),细根和中根的比根长(SRL)、比表面积(SSA)在0-20 cm土层增加(4.1%-21.5%);② 火烧后一年细根和中根ROC为335.87-492.8 g/kg、RTN为1.934-5.724 g/kg、RTP为0.793-1.154 g/kg,在0-10 cm土层升高(2.19%-38.35%);火烧后一年吸收根和运输根根系C:N(RC:N)为58.646-140.45 g/kg、根系C:P(RC:P)为299.336-422.846 g/kg,在10-20 cm土层显著降低(29.57%-39.35%)(p<0.05);不同径级根系N:P(RN:P)均小于14,可能受N限制;③ 相关性分析表明,PB下,SRL、SSA、RLD、RTN、RTP及RN:P呈极显著正相关(p<0.001),B、RBD、ROC、RC:P、RC:N呈极显著正相关(p<0.001)。[结论] 计划火烧后云南松通过协同细根高效吸收养分的形态可塑性与增加粗壮根系结构支撑性来响应火烧干扰,并通过调整形态特征与化学计量性状适应火后恢复环境。

    Abstract:

    Abstract: [Objective] In order to further study the effects of planned fire on the ecological stoichiometry of carbon, nitrogen and phosphorus in the roots of Pinus yunnanensis. [method] In this study, a year after the planned fire in Zhaobi mountain, Xinping County, Yuxi City, Yunnan Province, was taken as the research object. The root systems of Pinus yunnanensis in the control plot (UB) and the fire plot (PB) were collected, and the changes of living root biomass (B), morphological distribution, root organic carbon (ROC), root total nitrogen (RTN), root total phosphorus (RTP) and eco stoichiometry characteristics were analyzed. [results] ① one year after the fire, the diameter class B of Pinus yunnanensis was 7.553-288.368 g / m2, which was lower than that of UB (6.9% - 21.5%) in 0-20 cm soil layer; One year after fire, the biomass density (RBD), root length density (RLD), and root surface area density (SAD) of fine roots decreased (0.5% - 21.5%) in 0-20 cm soil layer, while the specific root length (SRL) and specific surface area (SSA) of fine roots and middle roots increased (4.1% - 21.5%) in 0-20 cm soil layer; ② One year after fire, the ROC of fine and middle roots was 335.87-492.8 g / kg, RTN was 1.934-5.724 g / kg, RTP was 0.793-1.154 g / kg, and increased in 0-10 cm soil layer (2.19% - 38.35%); The root C:N (RC:N) and root C:P (RC:P) of absorbing and transporting roots were 58.646-140.45 g / kg and 299.336-422.846 g / kg, respectively, which significantly decreased (29.57% - 39.35%) in 10-20 cm soil layer (P < 0.05); The root N:P (RN:P) of different diameter classes were less than 14, which may be limited by N; ③ Correlation analysis showed that under PB, SRL, SSA, RLD, RTN, RTP and RN:P showed extremely significant positive correlation (P < 0.001), and B, RBD, ROC, RC:P, RC:N showed extremely significant positive correlation (P < 0.001). [Conclusion] It is planned that Pinus yunnanensis will respond to the fire disturbance by cooperating with the morphological plasticity of fine roots to efficiently absorb nutrients and increasing the structural support of robust roots, and adapt to the post fire recovery environment by adjusting morphological characteristics and stoichiometry.

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  • 收稿日期:2025-08-01
  • 最后修改日期:2025-10-19
  • 录用日期:2025-10-20
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