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Fractal features of soil particle-size distribution as affected by plant communities in the forested region of Mountain Yimeng, China

Permanent URL:
http://handle.nal.usda.gov/10113/50119
Abstract:
Fractal dimension analyses of PSD and soil porosity were determined for the 0–20 cm soil layer representing different plant communities and land management in the Yimeng mountainous region of mid-eastern China. The soil types in this area are typically comprised of coarse sand and gravel. The results show that, compared with the protected forest preserve areas, soil physical properties in commercial Chinese chestnut groves (CM), cropland (ZM) and mixed shrub–grass lands (SH) were more sensitive to soil degradation under their respective long-term management strategies. In general, amounts of silt and clay decreased under CM, ZM, and SH land practices, while fine sand content increased, resulting in lower values for soil total porosity and capillary porosity. For protected forest, soil physical properties were enhanced due to litter decomposition and plant root development under long-term preservation measures. Considering the different plant communities, the overall fractal dimensions of PSD ranged from 2.141 to 2.526, with the fractal dimensions of ZM, SH and CM being far lower (2.141 to 2.166) than the mean value (2.395) of the protected forest land. The relationships between fractal dimension and PSD and soil porosity were also examined. There were significant correlations found between fractal dimension and the amount of silt and clay (R2 = 0.83), and fine sand (R2 = 0.64), 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. Correlations of Dm with capillary porosity, in association with the type of plant community, provided strong evidence that vegetation management affects small scale aggregation which influences the water-holding capacity of the soil, thus implying that Dm may be considered a good measure for quantifying aggregation and the effects of vegetation management on soil quality or soil degradation. 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.
Author(s):
Liu, Xia , Zhang, Guangcan , Heathman, Gary C. , Wang, Yaqin , Huang, Chi-hua
Subject(s):
forest soils , agricultural soils , grassland soils , land use change , fractal dimensions , particle size distribution , plant communities , soil pore system , porosity , soil types , soil physical properties , soil texture , clay fraction , silt fraction , soil-plant interactions , soil degradation , water holding capacity , China
Format:
p. 123-130.
Note:
Includes references
Source:
Geoderma 2009 Dec. 15, v. 154, no. 1-2
Language:
English
Year:
2009
Collection:
Journal Articles, USDA Authors, Peer-Reviewed
File:
Download [PDF File]
Rights:
Works produced by employees of the U.S. Government as part of their official duties are not copyrighted within the U.S. The content of this document is not copyrighted.