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Journal of Arid Land  2014, Vol. 6 Issue (5): 550-560    DOI: 10.1007/s40333-014-0023-7
Research Articles     
Fractal features of soil profiles under different land use patterns on the Loess Plateau, China
Lie XIAO, Sha XUE, GuoBin LIU, Chao ZHANG
1 State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, China;
2 Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, China
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Abstract  Fractal theory is becoming an increasingly useful tool to describe soil structure dynamics for a better understanding of the performance of soil systems. Changes in land use patterns significantly affect soil physical, chemical and biological properties. However, limited information is available on the fractal characteristics of deep soil layers under different land use patterns. In this study, the fractal dimensions of particle size distribution (PSD) and micro-aggregates in the 0–500 cm soil profile and soil anti-erodibility in the 0–10 cm soil profile for 10 typical land use patterns were investigated in the Zhifanggou Watershed on the Loess Plateau, China. The 10 typical land use patterns were: slope cropland, two terraced croplands, check-dam cropland, woodland, two shrublands, orchard, artificial and natural grasslands. The results showed that the fractal dimensions of PSD and micro-aggregates were all significantly influenced by soil depths, land use patterns and their interaction. The planta-tions of shrubland, woodland and natural grassland increased the amount of larger micro-aggregates, and decreased the fractal dimensions of micro-aggregates in the 0–40 cm soil profile. And they also improved the aggregate state and aggregate degree and decreased dispersion rate in the 0–10 cm soil profile. The results indicated that fractal theory can be used to characterize soil structure under different land use patterns and fractal dimensions of micro-aggregates were more effective in this regard. The natural grassland may be the best choice for improving soil structure in the study area.

Key wordsalien      invasive plants      geographical distribution      the Caspian Sea coast     
Received: 10 October 2013      Published: 12 October 2014

The research was supported by the Strategic Technology Pro-ject of Chinese Academy of Sciences (XDA05060300) and the Science and Technology R&D Program of Shaanxi Province (2011KJXX63).

Corresponding Authors: GuoBin LIU     E-mail:
Cite this article:

Lie XIAO, Sha XUE, GuoBin LIU, Chao ZHANG. Fractal features of soil profiles under different land use patterns on the Loess Plateau, China. Journal of Arid Land, 2014, 6(5): 550-560.

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Ahmadi A, Neyshabouri M, Rouhipour H, et al. 2011. Fractal dimension of soil aggregates as an index of soil erodibility. Journal of Hydrol-ogy, 400: 305−311.

Anderson A N, McBratney A B, Crawford J W. 1997. Application of fractals to soil studies. Advances in Agronomy, 63: 1−76.

Ayres Q C. 1936. Soil Erosion and its Control. New York: McGram-Hill: 20−30.

Basic F, Kisic I, Mesic M, et al. 2004. Tillage and crop management effects on soil erosion in central Croatia. Soil and Tillage Research, 78(2): 197−206.

Baver L D, Rhoades H F. 1932. Aggregate analysis as an aid in the study of soil structure relationships. Journal of the American Society of Agronomy, 24: 920−930.

Bremner J M, Mulvaney C S. 1982. Nitrogen-total. Agronomy monography 9. In: Page A L, Miller R H, Keeney D R. Methods of Soil Analysis, Part 2, Chemical and Microbial Properties, Madison: Agronomy Society of America, 595−624.

Caravaca F, Masciandaro G, Ceccanti B. 2002. Land use in relation to soil chemical and biochemical properties in a semiarid Mediterra-nean environment. Soil and Tillage Research, 68(1): 23−30.

Clifton J, Mcdonald P, Plater A, et al. 1999. An investigation into the efficiency of particle size separation using stokes’ law. Earth Surface Processes and Landforms, 24(8): 725−730.

Dang Y A, Li S Q, Wang G D, et al. 2009. Fractal characteristics of soil particle composition for typical types of soil profile on Loess Plateau. Transactions of the Chinese Society of Agriculture Engineering, 25(9): 74−78.

Erskine W D, Mahmoudzadeh A, Myers C. 2002. Land use effects on sediment yields and soil loss rates in small basins of Triassic sand-stone near Sydney, NSW, Australia. Catena. 49(4): 271−287.

Filgueira R R, Fournier L L, Cerisola C I, et al. 2006. Particle-size distribution in soils: a critical study of the fractal model validation. Geoderma, 134(3−4):327−334.

Gao L, Shao M A. 2012. Temporal stability of soil water storage in diverse soil layers. Catena, 95: 24−32.

Grout H, Tarquis A M, Wiesner M R. 1998. Multifractal analysis of particle size distributions in soil. Environmental Science and Tech-nology, 32(9): 1176−1182.

Gui D W, Lei J Q, Zeng F J, et al. 2010. Characterizing variations in soil particle size distribution in oasis farmlands−A case study of the Cele Oasis. Mathematical and Computer Modelling, 51: 1306−1311.

Kravchenko A, Zhang R D. 1998. Estimating the soil water retention from particle-size distribution: a fractal approach. Soil Science, 163(3): 171−179.

Li D C, Zhang T L. 2000. Fractal features of particle-size distribution of soils in China. Soil and Environmental Sciences, 9(4): 263−265.

Liu X, Zhang G C, Heathman G C, et al. 2009. Fractal features of soil particle-size distribution as affected by plant communities in the forested region of Mountain Yimeng, China. Geoderma, 154(1−2): 123−130.

Lobe I, Amenlung W, Du Preez C C. 2001. Loesses of carbon and nitrogen with prolonged arable cropping from sandy soils of the South African Highveld. European Journal of Soil Science, 52(1): 93−101.

Mariotte C A, Hudson G, Hamilton D. 1997. Spatial variability of soil total C and N and their stable isotopes in an upland Scottish grassland. Plant and Soil, 196(1): 151−162.

Martinez-Mena M, Deeks L K, Williams A G. 1999. An evaluation of fragmentation fractal dimension technique to determine soil erodi-bility. Geoderma, 90: 87−98.

Millan H, Gonzalez-Posada M, Aguilar M, et al. 2003. On the fractal scaling of soil data. Particle-size distributions. Geoderma, 117(1−2): 117−128.

Millan H, Orellana R. 2001. Mass fractal dimensions of soil aggregates from different depths of a compacted Vertisol. Geoderma, 101(3−4): 65−76.

Montero E. 2005. Rényi dimensions analysis of soil particle-size dis-tributions. Ecological Modelling, 182(3−4): 305−315.

Nelson D W, Sommers L E. 1982. Total carbon, organic carbon, and organic matter. Agronomy nonograph 9. In: Page A L, Miller R H, Keeney D R. Methods of Soil Analysis, Part 2, Chemical and Mi-crobial Properties. Madison: Agronomy Society of America, 539−552.

Paz-Ferreiro J, Vidal Vazquez E, Miranda J G V. 2010. Assessing soil particle-size distribution on experimental plots with similar texture under different management systems using multifractal parameters. Geoderma, 160(1): 47−56.

Posadas A N D, Gimenez D, Bittelli M, et al. 2001. Multifractal char-acterization of soil particle-size distributions. Soil Science Society of American Journal, 65:1361−1367.

Pulleman M M, Six J, Uyl A, et al. 2005. Earthworms and management affect organic matter incorporation and microaggregate formation in agricultural soils. Applied Soil Ecology, 29(1): 1−15.

Su Y Z, Zhao H L, Zhao W Z, et al. 2004. Fractal features of soil particle size distribution and the implication for indicating desertification. Geoderma, 122(1): 43−49.

Turcotte D L. 1986. Fractal and fragmentation. Journal of Geophysical Research, 91:1921−1926.

Tyler S W, Wheatcraft S W. 1989. Application of fractal mathematics to soil water retention estimation. Soil Science Society of America Journal, 53(4): 987−996.

Tyler S W, Wheatcraft S W. 1992. Fractal scaling of soil particle-size distributions: analysis and limitations. Soil Science Society of America Journal, 56(2): 362−369.

Wang B, Liu G B, Xue S, et al. 2011. Changes in soil physicochemical and microbiological properties during natural succession on aban-doned farmland in the Loess Plateau. Environmental Earth Sciences, 62(5): 915−925.

Wang B, Xue S, Liu G B, et al. 2012. Changes in soil nutrient and enzyme activities under different vegetations in the Loess Plateau area, Northwest China. Catena, 92: 186−195.

Wang D, Fu B J, Zhao W W, et al. 2008. Multifractal characteristics of soil particle size distribution under different land-use types on the Loess Plateau, China. Catena, 72(1): 29−36.

Wang X D, Li M H, Liu S Z, et al. 2006. Fractal characteristics of soils under different land-use patterns in the arid and semiarid regions of the Tibetan Plateau, China. Geoderma, 134(1−2): 56−61.

Wang Y Q, Zhang X C. Huang C Q. 2009a. Spatial variability of soil total nitrogen and soil total phosphorus under different land uses in a small watershed on the Loess Plateau, China. Geoderma, 150(1−2): 141−149.

Wang Z Q, Liu B Y, Zhang Y. 2009b. Soil moisture of different vegeta-tion types on the Loess Plateau. Journal of Geographical Sciences, 19(6): 707−718.

Wang G L, Liu G B, Xu M X. 2009c. Above and below ground dynamics of plant community succession following abandonment of farmland on the Loess Plateau, China. Plant and Soil, 316(1−2): 227−239.

Wei J, Zhou J, Tian J L, et al. 2006. Decoupling soil erosion and human activities on the Chinese Loess Plateau in the 20th century. Catena, 68(1): 10−15.

Xu Y F, Sun D A. 2002. A fractal model for soil pores and its application to determination of water permeability. Physica A, 316: 56−64.

Yang P L, Luo Y P, Shi Y C. 1993. Fractal features of soil defined by grain weight distribution. Chinese Science Bulletin, 38(20): 1896−1899.

Zalibekov Z G. 2002. Changes in the soil cover as a result of desertifi-cation. Eurasian Soil Science, 35(12): 1276−1281.

Zhang C, Xue S, Liu G B, et al. 2011. A comparison of soil qualities of different revegation types in the Loess Plateau, China. Plant and Soil, 347(1−2): 163−178.

Zhang C, Liu G B, Xue S, et al. 2013. Soil organic carbon and total nitrogen storage as affected by land use in a small watershed of the Loess Plateau, China. European Journal of Soil Biology, 54: 16−24.

Zhang Z, Wei C F, Xie D T, et al. 2008. Effects of land use patterns on soil aggregate stability in Sichuan Basin, China. Particuology, 6(3): 157−166.

Zhao P, Shao M A, Wang T J. 2011. Multifractal analysais of particle-size distributions of alluvial soils in the dam farmland on the Loess Plateau of China. African Journal of Agricultural Research, 6(18): 4177−4184.

Zhao S W, Su J, Yang Y H, et al. 2006. A fractal method of estimating soil structure changes under different vegetations on Ziwuling Mountains of the Loess Plateau, China. Agriculture Sciences in China, 5(7): 530−538.

Zheng Z C, He S Q, Li T X. 2011. Fractal dimensions of soil structure and soil anti-erodibility under different land use patterns. African Journal of Agriculture Research, 24(6): 5496−5504.

Zheng Z C, Li T X, Zhang X Z, et al. 2009. Study on the composition and stability of soil aggregates under different land use. Journal of Soil and Water Conservation, 23(5): 228−231.

Zou X Y, Li S, Zhang C L, et al. 2002. Desertification and control plan in the Tibet Autonomous Region of China. Journal of Arid Environments, 51(2): 183−198.
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