长江流域资源与环境 >> 2024, Vol. 33 >> Issue (11): 2440-2450.doi: 10.11870/cjlyzyyhj202411010

• 自然资源 • 上一篇    下一篇

三峡库区柑橘园土壤有机碳关键影响因子分析

陈吉臻1,沈琛琛1,樊子豪1,张馨1,黄志霖1,2*   

  1. (1.中国林业科学研究院森林生态环境与自然保护研究所,国家林业和草原局森林生态环境重点实验室,北京100091;2.南京林业大学南方现代林业协同创新中心,江苏 南京210037)
  • 出版日期:2024-11-20 发布日期:2024-11-27

Influencing Factors of Soil Organic Carbon in Citrus Orchard in the Three Gorges Reservoir Area

CHEN Ji-Zhen1 ,SHEN Chen-Chen1 ,FAN Zi-Hao1 ,ZHANG Xin1 ,HUANG Zhi-Lin1,2   

  1. (1.Key Laboratory of Forest Ecology and Environment of National Forestry and Grassland Administration, Ecology and Nature Conservation Institute, Chinese Academy of Forestry,   Beijing 100091 , China;2.Co-Innovation Center for Sustainable Forestry in Southern China , Nanjing Forestry University , Nanjing 210037 , China)
  • Online:2024-11-20 Published:2024-11-27

摘要: 揭示三峡库区柑橘园地土壤有机碳(Soil Organic Carbon, SOC)含量及其关键影响因子,阐明关键影响因子对园地土壤有机碳含量的影响机制。基于三峡库区156个柑橘园样地的实测数据,结合地形、气候、土壤属性和植被等影响土壤有机碳含量的潜在变量,采用随机森林模型(Random Forest, RF)分别筛选影响3个土层(0~10、10~20和20~40 cm)土壤有机碳含量的关键因子,并运用结构方程模型(Structural Equation Modeling, SEM)进一步研究关键因子对土壤有机碳含量的影响机制。结果表明:(1)土壤全氮和年平均气温是影响土壤有机碳的关键因子,其相对重要性分数均随着土层深度的增加而逐渐减少。土壤全氮对各土层的相对重要性分数为35.96、34.35和32,年平均温度的相对重要性分数为7.68、7.45和5.58。(2)关键影响因子与土壤有机碳间存在显著的非线性关系,并在各土层中呈现出相似的偏依赖模式。土壤有机碳与土壤全氮存在正相关关系,与年平均气温的关系则呈现出复杂的非线性波动。(3)土壤全氮对SOC在3个土层中均表现出显著的正效应(0~10 cm, β = 0.881; 10~20 cm, β = 0.829; 20~40 cm, β = 0.820);年平均气温对SOC在较浅的土层中表现出负效应(0~10 cm, β = -0.012; 10~20 cm, β = -0.069),在较深的土层中表现出正效应(20~40 cm, β = 0.027)。土壤全氮是柑橘园土壤有机碳的相对重要性得分最高的影响因子并表现出最显著的正效应,合理调控柑橘园土壤氮素将有利于提高园地土壤有机碳储量。

Abstract: The aim of this study is to investigate the soil organic carbon (SOC) content and its influencing factors in citrus orchards in the Three Gorges Reservoir region, and to elucidate the mechanisms affecting SOC levels in the orchards. Leveraging actual measured data from 156 sample sites in the study area, this study considered potential variables affecting soil organic carbon content, such as topography, climate, and vegetation. The Random Forest (RF) model was employed to separately identify key factors that may influence the organic carbon content in three soil layers (0~10 cm, 10~20 cm, and 20~40 cm). Further, the Structural Equation Modeling (SEM) was utilized to explore the impact of key factors on soil organic carbon (SOC) content. The findings indicated: (1) Soil total nitrogen and annual average temperature were key factors affecting soil organic carbon, with their relative importance score gradually decreasing with an increase in soil layer depth. Specifically, the relative importance score of soil total nitrogen in the three soil layers were 35.96, 34.35, and 32.08, respectively, while those of annual average temperature were 7.68, 7.45, and 5.58, respectively.(2) A significant non-linear relationship existed between the key influencing factors and soil organic carbon, demonstrating a similar partial dependence pattern across all soil layers. (3) Soil total nitrogen had a significant positive effect on SOC across all observed soil layers (β=0.881 for 0~10 cm; β=0.829 for 10~20 cm; β=0.820 for 20~40 cm). The total effect of the annual average temperature on SOC was not significant, demonstrating a negative effect in shallower soil layers (β=-0.012 for 0~10 cm; β=-0.069 for 10~20 cm) and a positive effect in deeper layers (β=0.027 for 20~40 cm). Soil total nitrogen demonstrated the highest relative importance score and played a critical, and positive role in influencing soil organic carbon in citrus orchards, which highlighted the potential benefits of strategic nitrogen management to increase soil organic carbon storage.

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