沿海湿地松防护林土壤pH 值空间变异分析

    Spatial variation analysis on soil pH values of coastalprotection forest of Pinus elliottii E.

    • 摘要: 以福建省福州市22 年生沿海湿地松林地土壤为研究对象,运用野外样地法和地统计学方法,结合实验测定并分析了0~20(Ⅰ)、20~40(Ⅱ)、40~60 cm(Ⅲ)土层pH 值的统计学分布和空间变异特征。结果表明:该湿地松林土壤pH 值整体呈强酸性,Ⅰ、Ⅱ、Ⅲ土层pH 值分别为4.59、4.86 和4.90,相应的变异系数分别为5.75%、5.01% 和7.63%;Ⅰ、Ⅱ、Ⅲ土层pH 值块金效应值分别为0.859、0.136 和1.000;空间变异最优拟合模型分别为线性有基台值模型、指数模型和线性有基台值模型。克里格最优内插值分析表明,Ⅰ层和Ⅲ层土壤pH 值主要由结构因素决定,Ⅱ层土壤pH 值则受林分部分影响;该林土壤酸化主要受土壤母质、酸雨和林分等因素共同作用。

       

      Abstract: The descriptive statistics and spatial variation of pH values in the soil of a 22 years old coastal forest ofPinus elliottii E. in Fuzhou were analyzed by the method of geo-statistics after field work. The results showed that the soilwas strongly acidic,with 4.59,4.86 and 4.90 of pH values as well as 5.75%,5.01% and 7.63% of variable coefficients inthe depth of 0-20 cm(Layer Ⅰ),20-40 cm(Layer Ⅱ)and 40-60 cm(Layer Ⅲ)in the soil,respectively. The nuggetvalues were 0.859,0.136 and 1.000,respectively. And the optimal spatial autocorrelation models of pH values in LayerⅠ,Ⅱ and Ⅲ were liner model with sill,exponential model and liner model with sill,respectively. The results of Krigingoptimal interpolation values indicated that soil pH values in Layer Ⅰ and Ⅲ were mainly influenced by structural factorswhile the ones in Layer Ⅱ were partly affected by forest factors. The soil acidity may be due to several reasons such assoil parent material,air acid deposition,soil water content and forests.