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林业科学 ›› 2011, Vol. 47 ›› Issue (8): 31-37.doi: 10.11707/j.1001-7488.20110806

• 论文 • 上一篇    下一篇

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1, 姚孝友2, 张光灿1, 胡续礼2   

  1. 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
  • 收稿日期:2009-05-25 修回日期:2011-05-15 出版日期:2011-08-25 发布日期:2011-08-25
  • 通讯作者: 张光灿

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

Liu Xia1, Yao Xiaoyou2, Zhang Guangcan1, Hu Xuli2   

  1. 1. Forestry College of Shandong Agricultural University Key Laboratory of Agricultural Ecology and Environment of Shandong Taian 271018;2. Branch of Soil and Water Conservation, Huaihe River Commission, Ministry of Water Resources Bengbu 233001;3. USDA-ARS National Soil Erosion Research Laboratory West Lafayette, USA 47907
  • Received:2009-05-25 Revised:2011-05-15 Online:2011-08-25 Published:2011-08-25

摘要:

为探索人为活动干扰下植物群落变化对土壤物理结构特征的影响,运用土壤分形学和水文学原理与方法研究沂蒙山林区7种植物群落下的土壤颗粒组成、分形维数、土壤孔隙度及其相关性。结果表明: 在长期农业耕作等人为干扰下,玉米作物、板栗经济林和灌草丛群落下的土壤颗粒呈粗粒化特征,分形维数显著降低,土壤总孔隙度和毛管孔隙度下降,非毛管孔隙度增加,土壤物理结构呈现退化状态; 而处于长期封禁保护下的森林群落,土壤颗粒分形维数较大,粉黏粒等细粒物质的含量较高,孔隙结构状况较好。研究区土壤颗粒组成具有石质山地典型的粗骨土结构特征,森林群落能显著增加土壤中粉黏粒等细粒物质的含量和对土壤空隙的填充能力,是其改善土壤物理结构的分形学机制。土壤颗粒分形维数与土壤粉黏粒含量、总孔隙度和毛管孔隙度之间存在明显的线性正相关,而与土壤砂粒含量和非毛管孔隙度具有线性负相关关系,它能较好表征植物群落变化对土壤颗粒组成和孔隙状况的影响,因而可作为评价土壤物理结构质量的一项综合性指标。

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

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 (GC) 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 porosity with 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.

Key words: soil physical properties, soil particle size distribution, fractal dimension, soil pore, Yimeng Mountain

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