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浙西南针阔混交林碳通量动态特征及环境响应

Dynamic Characteristics and Environmental Response of Carbon Flux in the Coniferous and Broad-leaved Mixed Forest in Southwest of Zhejiang Province

  • 摘要: 浙西南针阔混交林受中亚热带季风气候和复杂地形共同影响,生态系统碳交换过程具有明显季节波动。明确其碳通量动态特征及环境响应,有助于理解亚热带山地森林碳汇形成过程,并为区域森林碳汇评估和经营管理提供依据。本研究基于2024年48 m通量塔涡度相关观测数据,对浙西南典型针阔混交林净生态系统碳交换量(NEE)、总初级生产力(GPP)和生态系统呼吸(Reco)的季节动态及其与环境因子的关系进行分析。结果表明:(1)2024年研究区生态系统整体表现为碳汇,NEE全年以负值为主,日尺度变化范围为−8.39~6.83 g·m−2·d−1,年平均值为−1.38 g·m−2·d−1;5—8月为净碳吸收较强阶段,7月月均NEE最低,为−3.75 g·m−2·d−1。(2)GPP和Reco均表现出明显季节变化,整体呈冬季较低、春季升高、夏季较高、秋冬回落的变化趋势,NEE的年内波动与GPP和Reco的相对变化密切相关。(3)相关分析表明,GPP与空气温度(Ta)、土壤温度(Ts)、总辐射(Rg)和饱和水汽压亏缺(VPD)呈极显著正相关(P<0.01);Reco主要与Ta和Ts呈显著正相关(P<0.05);NEE与GPP、Rg呈极显著负相关(P<0.01),与VPD呈显著负相关(P<0.05),与Reco呈极显著正相关(P<0.01)。Ta、Ts、Rg和VPD是与研究区碳通量年内变化密切相关的环境因子。研究结果可为浙西南亚热带山地针阔混交林碳汇功能评估及区域森林经营管理提供连续观测依据。

     

    Abstract: Coniferous and broad-leaved mixed forests in Southwest of Zhejiang Province are jointly affected by the mid-subtropical monsoon climate and complex mountainous topography, resulting in pronounced seasonal fluctuation in ecosystem carbon exchange. Clarifying the dynamic characteristics of carbon flux and its environmental responses is helpful for understanding the formation process of carbon sinks in subtropical mountain forests and provides a basis for regional forest carbon sink assessment and management. Based on the eddy covariance observational data from a 48-m flux tower in 2024, this study analyzed the seasonal dynamics of net ecosystem exchange (NEE), gross primary productivity (GPP) and ecosystem respiration (Reco), as well as their relationships with environmental factors in this typical coniferous and broad-leaved mixed forest. The results showed that: (1) in 2024, the ecosystem of the study area wholly functioned as carbon sink, with NEE being predominantly negative throughout the year. NEE ranged from −8.39 to 6.83 g·m−2·d−1 at the daily scale, with an annual mean value of −1.38 g·m−2·d−1. May to August was a period of relatively strong net carbon uptake, and the monthly mean NEE was lowest in July, at −3.75 g·m−2·d−1. (2) Both GPP and Reco showed obvious seasonal variation, generally exhibiting a trend of being lower in winter, increasing in spring, higher in summer, and declining in autumn and winter. The intra-annual fluctuation of NEE was closely related to the relative changes in GPP and Reco. (3) Correlation analysis showed that GPP was highly significantly positively correlated with air temperature (Ta), soil temperature (Ts), total radiation (Rg) and vapor pressure deficit (VPD) (P<0.01); Reco was mainly significantly positively correlated with Ta and Ts (P<0.05); NEE was highly significantly negatively correlated with GPP and Rg (P<0.01), significantly negatively correlated with VPD (P<0.05), and highly significantly positively correlated with Reco (P<0.01). Ta, Ts, Rg and VPD were environmental factors closely related to the intra-annual variation of carbon flux in the study area. The results can provide continuous observational evidence for assessing the carbon sink function of subtropical coniferous and broad-leaved mixed forests in southwestern Zhejiang and for regional forest management.

     

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