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沂蒙山林区不同植物群落下土壤颗粒分形与孔隙结构特征

刘霞 姚孝友 张光灿 胡续礼 Heathman G C

林业科学2011,Vol.47Issue(8):31-37,7.
林业科学2011,Vol.47Issue(8):31-37,7.

沂蒙山林区不同植物群落下土壤颗粒分形与孔隙结构特征

Fractal Features of Soil Particle Size Distribution and Characteristics of Soil Pore Space under Different Plant Communities in Forests of the Yimeng Mountain

刘霞 1姚孝友 2张光灿 1胡续礼 2Heathman G C3

作者信息

  • 1. 山东农业大学林学院,山东省土壤侵蚀与生态修复重点实验室,泰安271018
  • 2. 水利部淮河水利委员会水土保持处,蚌埠233001
  • 3. 美国农业部农业研究局国家土壤侵蚀研究实验室,美国西拉法叶47907
  • 折叠

摘要

Abstract

In order to explore the effect of changes in plant communities and land use, brought out by anthropogenic disturbance, on soil properties, we applied the theory of fractals and hydrology as a means to quantify changes in particle-size distribution (PSD) and soil porosity. Fractal dimension analysis of PSD and soil porosity was determined for the 0 -20 cm soil layer in different plant communities and land management styles in the Yimeng Mountain of the mid-eastern China. The results showed that, compared with that of the protected forest in preserve areas, soil physical properties in economic forestland (BL) , cropland (TY) and mixed shrub-grass lands (CC) were more susceptible to soil degradation under their long-term management strategies. In general, amounts of silt and clay decreased under BL, TY, and GC land practices, while fine sand content increased, resulting in lower values of the fractal dimensions, soil total porosity and capillary porosity. For protected forests, soil physical properties were improved due to litter decomposition and plant root development under long-term preservation measures. The soil types in the studied area are typical of skeletal soils found in many mountainous areas. The relationship between fractal dimension and PSD and selected soil properties were also examined. There were significant correlations between fractal dimension and the amount of silt and clay, and fine sand (R2 = 0. 83 and 0. 64, respectively) , with increasing fractal dimension values corresponding to higher silt and clay contents and lower sand content. There also existed strong linear relationships between fractal dimension and soil porositywith R2 values ranging from 0. 74 to 0. 91. This study demonstrates that fractal dimension analysis may be used to better quantify differences in PSD and soil porosity associated with soil degradation caused by anthropogenic disturbance of plant community environments.

关键词

土壤物理结构/土壤颗粒组成/分形维数/土壤孔隙/沂蒙山

Key words

soil physical properties/ soil particle size distribution/ fractal dimension/ soil pore/ Yimeng Mountain

分类

农业科技

引用本文复制引用

刘霞,姚孝友,张光灿,胡续礼,Heathman G C..沂蒙山林区不同植物群落下土壤颗粒分形与孔隙结构特征[J].林业科学,2011,47(8):31-37,7.

基金项目

国家自然科学基金项目“沂蒙山区退耕坡地土壤结构与人渗动态及其分形学机理(31070627)”,国家林业行业专项课题“干旱瘠薄山地植被恢复与重建技术研究”(201104002-6)和淮河水利委员会水土保持专项基金“淮河流域水土保持分区及其治理模式研究”(SBJ2008002). (31070627)

林业科学

OA北大核心CSCDCSTPCD

1001-7488

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