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Characterization of Soil Particle Size Distribution with a Fractal Model in the Desertified Regions of Northern China

Wybrane pełne teksty z tego czasopisma
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
We constructed an aeolian soil database across arid, semi-arid, and dry sub-humid regions, China. Soil particle size distribution was measured with a laser diffraction technique, and fractal dimensions were calculated. The results showed that: (i) the predominant soil particle size distributed in fine and medium sand classifications, and fractal dimensions covered a wide range from 2.0810 to 2.6351; (ii) through logarithmic transformations, fractal dimensions were significantly positive correlated with clay and silt contents (R2 = 0.81 and 0.59, P < 0.01), and significantly negative correlated with sand content (R2 = 0.50, P < 0.01); (3) hierarchical cluster analysis divided the plots into three types which were similar to sand dune types indicating desertification degree. In a large spatial scale, fractal dimensions are still sensitive to wind-induced desertification. Therefore, we highly recommend that fractal dimension be used as a reliable and quantitative parameter to monitor soil environment changes in desertified regions. This improved information provides a firm basis for better understanding of desertification processes.
Czasopismo
Rocznik
Strony
1--14
Opis fizyczny
Bibliogr. 34 poz.
Twórcy
autor
  • Yanchi Research Station, School of Soil and Water Conservation, Beijing Forestry University, Beijing, P.R. China
  • Key Laboratory of Soil and Water Conservation and Desertification Combating, Ministry of Education, Beijing Forestry University, Beijing, P.R. China
autor
  • Yanchi Research Station, School of Soil and Water Conservation, Beijing Forestry University, Beijing, P.R. China
  • Key Laboratory of Soil and Water Conservation and Desertification Combating, Ministry of Education, Beijing Forestry University, Beijing, P.R. China
autor
  • Yanchi Research Station, School of Soil and Water Conservation, Beijing Forestry University, Beijing, P.R. China
  • Key Laboratory of Soil and Water Conservation and Desertification Combating, Ministry of Education, Beijing Forestry University, Beijing, P.R. China
autor
  • Yanchi Research Station, School of Soil and Water Conservation, Beijing Forestry University, Beijing, P.R. China
  • Key Laboratory of Soil and Water Conservation and Desertification Combating, Ministry of Education, Beijing Forestry University, Beijing, P.R. China
autor
  • Yanchi Research Station, School of Soil and Water Conservation, Beijing Forestry University, Beijing, P.R. China
  • Key Laboratory of Soil and Water Conservation and Desertification Combating, Ministry of Education, Beijing Forestry University, Beijing, P.R. China
autor
  • Yanchi Research Station, School of Soil and Water Conservation, Beijing Forestry University, Beijing, P.R. China
  • Key Laboratory of Soil and Water Conservation and Desertification Combating, Ministry of Education, Beijing Forestry University, Beijing, P.R. China
autor
  • Yanchi Research Station, School of Soil and Water Conservation, Beijing Forestry University, Beijing, P.R. China
  • Key Laboratory of Soil and Water Conservation and Desertification Combating, Ministry of Education, Beijing Forestry University, Beijing, P.R. China
autor
  • Yanchi Research Station, School of Soil and Water Conservation, Beijing Forestry University, Beijing, P.R. China
autor
  • Yanchi Research Station, School of Soil and Water Conservation, Beijing Forestry University, Beijing, P.R. China
autor
  • Yanchi Research Station, School of Soil and Water Conservation, Beijing Forestry University, Beijing, P.R. China
Bibliografia
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  • Chen, Y., and H. Tang (2005), Desertification in north China: Background, anthropogenic impacts and failures in combating it, Land Degrad. Develop. 16, 4, 367-376, DOI: 10.1002/ldr.667.
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  • Ding, G.D. (2010), Blown Sand Physics, China Forestry Publishing, Beijng (in Chinese). Duan, Z.H., H.L. Xiao, X.R. Li, Z.B. Dong, and G. Wang (2004), Evolution of soil properties on stabilized sands in the Tengger Desert, China, Geomorphology 59, 1-4, 237-246, DOI: 10.1016/j.geomorph.2003.07.019.
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  • Gao, G.L., G.D. Ding, B. Wu, Y.Q. Zhang, S.G. Qin, Y.Y. Zhao, Y.F., Bao, Y.D. Liu, L. Wan, and J.F. Deng (2014a), Fractal scaling of particle size distribution and relationships with topsoil properties affected by biological soil crusts, PLoS One 9, 2, e88559, DOI: 10.1371/journal.pone.0088559.
  • Gao, G.L., G.D. Ding, Y.Y. Zhao, B. Wu, Y.Q. Zhang, S.G. Qin, Y.F. Bao, M.H. Yu, and Y.D. Liu (2014b), Fractal approach to estimating changes in soil properties following the establishment of Caragana korshinskii shelterbelts in Ningxia, NW China, Ecol. Indic. 43, 236-243, DOI: 10.1016/ j.ecolind.2014.03.001.
  • Gui, D.W., J.Q. Lei, F.J. Zeng, G.J. Mu, J.T. Zhu, H. Wang, and Q. Zhang (2010), Characterizing variations in soil particle size distribution in oasis farmlands – A case study of the Cele Oasis, Math. Comput. Model. 51, 11-12, 1306- 1311, DOI: 10.1016/j.mcm.2009.10.035. Hillel, D. (1980), Fundamentals of Soil Physics, Academic Press, New York, 413 pp.
  • Hwang, S.I., K.P. Lee, D.S. Lee, and S.E. Powers (2002), Models for estimating soil particle-size distributions, Soil Sci. Soc. Am. J. 66, 4, 1143-1150, DOI: 10.2136/sssaj2002.1143.
  • Jiao, F., Z.M. Wen, and S.S. An (2011), Changes in soil properties across a chronosequence of vegetation restoration on the Loess Plateau of China, Catena 86, 2, 110-116, DOI: 10.1016/j.catena.2011.03.001.
  • Jin, Z., Y.S. Dong, Y.C. Qi, W.G. Liu, and Z.S. An (2013), Characterizing variations in soil particle-size distribution along a grass-desert shrub transition in the Ordos Plateau of Inner Mongolia, China, Land Degrad. Develop. 24, 2, 141-146, DOI: 10.1002/ldr.1112.
  • Li, X.R., M.Z. He, Z.H. Duan, H.L. Xiao, and X.H. Jia (2007), Recovery of topsoil physicochemical properties in revegetated sites in the sand-burial ecosystems of the Tengger Desert, northern China, Geomorphology 88, 3-4, 254- 265, DOI: 10.1016/j.geomorph.2006.11.009.
  • Liu, X., G.C. Zhang, G.C. Heathman, Y.Q. Wang, and C.H. Huang (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, DOI: 10.1016/j.geoderma.2009.10.005.
  • Lobe, I., W. Amelung, and C.C. Du Preez (2001), Losses of carbon and nitrogen with prolonged arable cropping from sandy soils of the South African Highveld, Eur. J. Soil Sci. 52, 1, 93-101, DOI: 10.1046/j.1365-2389.2001. t01-1-00362.x.
  • Mandelbrot, B.B. (1967), How long is the coast of Britain? Statistical self-similarity and fractional dimension, Science 156, 3775, 636-638, DOI: 10.1126/ science.156.3775.636.
  • Mandelbrot, B.B. (1983), The Fractal Geometry of Nature, Freeman, New York, 468 pp. Millán, H. (2007), Scale cutoffs and the limits of fractal soil structure, Int. Agrophys. 21, 2, 169-172.
  • Nemes, A., J.H.M. Wösten, A. Lilly, and J.H.O. Voshaar (1999), Evaluation of different procedures to interpolate particle-size distributions to achieve compatibility within soil databases, Geoderma 90, 3-4, 187-202, DOI: 10.1016/S0016-7061(99)00014-2.
  • Reynolds, R.L., M. Reheis, J. Yount, and P. Lamothe (2006), Composition of aeolian dust in natural traps on isolated surfaces of the central Mojave Desert – Insights to mixing, sources, and nutrient inputs, J. Arid Environ. 66, 1, 42-61, DOI: 10.1016/j.jaridenv.2005.06.031.
  • SFA (2011), A Bulletin of Status Quo of Desertification and Sandification in China, State Forestry Administration of the People’s Republic of China, Bejing, http://www.greentimes.com/green/econo/hzgg/ggqs/content/2011-01/05/ content_114232.htm (in Chinese).
  • Skaggs, T.H., L.M. Arya, P.J. Shouse, and B.P. Mohanty (2001), Estimating particle-size distribution from limited soil texture data, Soil Sci. Soc. Am. J. 65, 4, 1038-1044, DOI: 10.2136/sssaj2001.6541038x.
  • Su, Y.Z., H.L. Zhao, W.Z. Zhao, and T.H. Zhang (2004), Fractal features of soil particle size distribution and the implication for indicating desertification, Geoderma 122, 1, 43-49, DOI: 10.1016/j.geoderma.2003.12.003.
  • Turcotte, D.L. (1986), Fractals and fragmentation, J. Geophys. Res. 91, B2, 1921- 1926, DOI: 10.1029/JB091iB02p01921.
  • Tyler, S.W., and S.W. Wheatcraft (1990), Fractal processes in soil water retention, Water Resour. Res. 26, 5, 1047-1054, DOI: 10.1029/WR026i005p01047.
  • Tyler, S.W., and S.W. Wheatcraft (1992), Fractal scaling of soil particle-size distribution: analysis and limitations, Soil Sci. Soc. Am. J. 56, 2, 362-369, DOI: 10.2136/sssaj1992.03615995005600020005x.
  • UNEP (1994), United Nations Convention to combat desertification in those countries experiencing serious drought and/or desertification, particularly in Africa, United Nations Environment Programme for the Convention to Combat Desertification (CCD), Interim Secretariat for the CCD, Switzerland, Geneva, 71 pp.
  • Wang, G.L., S.L. Zhou, and Q.G. Zhao (2005), Volume fractal dimension of soil particles and its applications to land use, Acta Pedol. Sin. 42, 4, 545-550.
  • Wang, X.D., M.H. Li, S.Z. Liu, and G.C. Liu (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, DOI: 10.1016/j.geoderma. 2005.08.014.
  • Wang, X.M., F.H. Chen, E. Hasi, and J.C. Li (2008), Desertification in China: An assessment, Earth-Sci. Rev. 88, 3-4, 188-206, DOI: 10.1016/j.earscirev. 2008.02.001.
  • Zha, Y., and J. Gao (1997), Characteristics of desertification and its rehabilitation in China, J. Arid Environ. 37, 3, 419-432, DOI: 10.1006/jare.1997.0290.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-2347f8ee-b36f-48f2-9c26-0282d1dd98ce
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