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生态学杂志 ›› 2022, Vol. 41 ›› Issue (11): 2278-2288.doi: 10.13292/j.1000-4890.202210.007

• 技术与方法 • 上一篇    

基于广义可加模型的广东省森林土壤有机质影响因子

刘晓彤,黄金金,张逸如,李海奎*   

  1. (中国林业科学研究院资源信息研究所, 国家林业和草原局森林经营与生长模拟重点实验室, 北京 100091)
  • 出版日期:2022-11-10 发布日期:2022-12-07

Analysis of influencing factors on forest soil organic matter in Guangdong Province based on GAM model.

LIU Xiao-tong, HUANG Jin-jin, ZHANG Yi-ru, LI Hai-kui*   

  1. (Research Institute of Forest Resource Information Techniques, Chinese Academy of Forestry, Key Laboratory of Forest Management and Growth Modelling, National Forestry and Grassland Administration, Beijing 100091, China).

  • Online:2022-11-10 Published:2022-12-07

摘要: 摸清森林土壤有机质的影响因子,可以为森林经营和森林质量提升提供依据。本研究基于1182个样地,采用克里金插值法分析了广东省森林土壤有机质的空间分布。以地理、地形、林分、气候、土壤物理和森林经营因子共52项因子为解释变量,以森林土壤有机质为响应变量,利用广义可加模型(generalized additive model, GAM)拟合,筛选出对土壤有机质影响显著的单因子。在此基础上,将影响显著的定性因子和定量因子分别交互,提取对于土壤有机质具有显著影响的交互项。结果表明:(1)森林土壤有机质的空间分布表现出明显的异质性,西北部高,中部偏西较高,南部沿海地区低。(2)采用GAM可以较好地拟合响应变量与解释变量的非线性关系。对森林土壤有机质具有极显著影响的因子包括坡度级、优势树种、土壤含水量、非毛管蓄水量和非毛管孔隙度;具有显著影响的因子包括经度、坡向、海拔、物种数量、腐殖质层厚、等温条件、年最低气温和土壤厚度。单因素GAM的修正确定系数为0.502,方差解释率为59.7%。优势树种、坡向和坡度级定性因子与经度、腐殖质层厚、等温条件、年最低气温、土壤含水量、非毛管蓄水量、非毛管孔隙度和土壤厚度定量因子的交互项对森林土壤有机质具有显著影响。交互GAM修正确定系数为0.515,方差解释率为59.8%。广东省森林土壤有机质受到地理、地形、林分、气候和土壤物理因子的共同作用,其中地形因子和土壤物理因子影响较大。研究结果能够为广东省森林质量提升和森林合理经营提供依据。


关键词: 广义可加模型, 土壤有机质, 定性因子, 定量因子, 交互作用

Abstract: Understanding the influencing factors of forest soil organic matter can provide reference for forest management and quality improvement. In this study, we used Kriging interpolation method to analyze the spatial distribution of soil organic matter in forests of Guangdong Province based on 1182 sampling plots. With 52 factors of geography, topography, stand, climate, soil physics, and forest management as explanatory variables, and soil organic matter as the response variable, the factors that significantly influenced soil organic matter were selected by using the generalized additive model (GAM). The qualitative and quantitative factors with significant effects were interacted respectively to obtain the interaction terms. The results showed that: (1) The distribution of forest soil organic matter showed spatial heterogeneity, characterized by high content in the northwest areas, moderate in the west-central areas, and low in the southern coastal areas. (2) GAM could better fit the nonlinear relationship between the response variable and explanatory variables. The factors with extremely significant effects on soil organic matter included slope level, dominant tree species, soil water content, non-capillary water storage capacity, and non-capillary porosity capacity, while the factors with significant effects were longitude, slope direction, altitude, number of species, humus layer thickness, isothermality, annual minimum temperature and soil thickness. The modified determination coefficient and the explanation rate of variance of the single-factor GAM were 0.502 and 59.7%, respectively. The interactions between three qualitative factors (dominant tree species, slope level, and slope direction) and eight quantitative factors (longitude, humus layer thickness, isothermality, annual minimum temperature, soil water content, non-capillary water storage capacity, non-capillary porosity capacity, and soil thickness) had significant effects on soil organic matter. The modified determination coefficient and the explanation rate of variance were improved to 0.515 and 59.8% by adding the interactive items. Our results indicated that forest soil organic matter in Guangdong Province was mainly affected by geography, topography, stand, climate and soil physical factors, among which topography and soil physical factors had great effects. Our results can provide reference for forest quality improvement and rational forest management in Guangdong Province.


Key words: generalized additive model, soil organic matter, qualitative factor, quantitative factor, interaction.