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弃管年限对毛竹林土壤有机碳含量及其组分的影响

Effect of the Duration of Abandonment Management on Soil Organic Carbon and Its Fractions of Phyllostachys edulis Forests

  • 摘要: 为探究不同弃管年限对毛竹(Phyllostachys edulis)林土壤有机碳(SOC)含量及其组分的影响,本研究以浙江省典型毛竹林为对象,选取弃管0 a(CK)、2~5 a(U-I)、7~10 a(U-II)和11~14 a(U-III)的样地,测定0~15 cm土层SOC、矿质结合态碳(MOC)、非易氧化有机碳(NEOC)、惰性碳(ROC)、易氧化有机碳(EOC)、溶解性有机碳(DOC)和微生物生物量碳(MBC)的含量变化,并结合土壤理化性质分析其驱动因子。结果表明:随着弃管年限的延长,SOC含量呈上升趋势;在6种碳组分中,NEOC是增幅最大的组分,而MOC、ROC等其他组分变化不显著或波动较小;从组分占比来看,弃管后MOC和EOC占比下降,NEOC占比上升,表明弃管促进了土壤有机碳向稳定态转化。逐步回归分析显示,土壤总氮是影响SOC变化的首要环境因子。上述结果为科学的管理和提升毛竹林碳汇功能提供科学依据。

     

    Abstract: To investigate the effect of the duration of abandonment on soil organic carbon (SOC) content and its fractions in Phyllostachys edulis forests, this study selected typical P. edulis forests in Zhejiang Province, using plots with abandonment durations of 0 years (CK), 2~5 years (U-I), 7~10 years (U-II), and 11~14 years (U-III). The total SOC, mineral-associated organic carbon (MOC), non-easily oxidizable organic carbon (NEOC), recalcitrant organic carbon (ROC), easily oxidizable organic carbon (EOC), dissolved organic carbon (DOC), and microbial biomass carbon (MBC) contents in the 0~15 cm soil layer were determined, and the driving factors were analyzed in combination with soil physicochemical properties. The results showed that with the increasing years of abandonment, SOC content exhibited an upward trend. Among the six carbon fractions, NEOC showed the greatest increase, while changes in MOC, ROC, and other fractions were not significant or fluctuated only slightly. In terms of the proportions of fractions, the proportions of MOC and EOC decreased while the proportion of NEOC increased after abandonment, indicating that abandonment promoted the transformation of soil organic carbon toward more stable forms. Stepwise regression analysis revealed that soil total nitrogen was the primary environmental factor affecting SOC changes. The results provide a scientific basis for the effective management and enhancement of carbon sink function of P. edulis forests.

     

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