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Comparative study on rain splash erosion of representative soils in China

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Abstract

As the first event of soil erosion, rain splash erosion supplies materials for subsequent transportation and entrainment. The Loess Plateau, the southern hilly region and the Northeast China are subject to serious soil and water loss; however, the characteristics of rain splash erosion in those regions are still unclear. The objectives of the study are to analyze the characteristics of splash erosion on loess soil, red soil, purple soil and black soil, and to discuss the relationship between splash erosion and soil properties. Soil samples spatially distributed in the abovementioned regions were collected and underwent simulated rainfalls at a high intensity of 1.2mm/min, lasting for 5, 10, 15, and 20min, respectively. Rain splash and soil crust development were analyzed. It shows that black soil sample from Heilongjiang Province corresponds to the minimum splash erosion amount because it has high aggregate content, aggregate stability and organic matter content. Loess soil sample from Inner Mongolia corresponds to the maximum splash erosion amount because it has high content of sand particles. Loess soil sample from Shanxi Province has relatively lower splash erosion amount because it has high silt particle content and low aggregate stability easily to be disrupted under rainfalls with high intensity. Although aggregate contents of red soil and purple soil samples from Hubei and Guangdong provinces are high, the stability is weak and prone to be disrupted, so the splash erosion amount is medium. Splash rate which fluctuates over time is observed because soil crust development follows a cycling processes of formation and disruption. In addition, there are two locations of soil crust development, one appears at the surface, and the other occurs at the subsurface.

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References

  • Bradford J M, Ferris J E, Remly P A, 1987. Interrill soil erosion processes: I. Effect of surface sealing on infiltration, runoff, and soil splash detachment. Soil Sci. Soc. Am. J., 51: 1566–1571.

    Google Scholar 

  • Bradford J M, Huang C, 1992. Mechanisms of crust formation: Physical components. In: Sumner M E et al. (eds.). Soil Crusting: Chemical and Physical Processes. Florida: Lewis Publishing.

    Google Scholar 

  • Bu Chongfeng, 2006. Study on the development mechanism of soil crust and its effect on soil erosion. Beijing: Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences. (in Chinese)

    Google Scholar 

  • Fan Rongsheng, Li Zhanbin, 1993. Rainsplash and sediment transport model on the slope. Journal of Hydraulic Engineering, (6): 24–29. (in Chinese)

  • Foster G R, 1982. Modeling the erosion process. In: Haan C T (ed.). Hydrologic Modeling of Small Watersheds. St. Joseph, MI, USA, ASAE, 297–379.

    Google Scholar 

  • Gao Xuetian, Bao Zhongmo, 2001. Study on effects of rainfall and soil structure on raindrop splash. Journal of Soil and Water Conservation, 15(3): 24–26. (in Chinese)

    Google Scholar 

  • Institute of Forestry and Soil Science, Chinese Academy of Sciences, 1980. Soils in Northeast Region, China. Beijing: Science Press. (in Chinese)

    Google Scholar 

  • Jiang Zhongshan, Liu Zhi, 1989. Effect of rainfall factors and slope on splash erosion. Journal of Soil and Water Conservation, 3(2): 29–35. (in Chinese)

    Google Scholar 

  • Le Bissonnais Y, Cerdan O, Lecomte V et al., 2005. Variability of soil surface characteristics influencing runoff and interrill erosion. Catena, 62(2–3): 111–124. DOI: 10.1016/j.catena.2005.05.001

    Article  Google Scholar 

  • Li Qingkui, 1983. Red Soils of China. Beijing: Science Press. (in Chinese)

    Google Scholar 

  • Luk S H, Abrahams A D, Parson A J, 1986. A simple rainfall simulator and trickle system for hydro-geomorphological experiments. Physical Geography, 7: 344–356.

    Google Scholar 

  • Luk S H, Cai Q G, 1990. Laboratory experiments on crust development and rainsplash erosion of Loess soils, China. Catena, 17(3): 261–276.

    Article  Google Scholar 

  • Mazurak A P, Mosher P N, 1968. Detachment of soil particles in simulated rainfall. Soil Sci. Soc. Amer. Proc., 32: 716–719.

    Google Scholar 

  • Meyer L D, Wischmeier W H, 1969. Mathematical simulation of the process of soil erosion by water. Trans. ASAE, 12(6): 754–758, 762.

    Google Scholar 

  • Römkens M, Baumhardt R, Parlange J et al., 1985. Rain-induced surface seals: Their effect on ponding and infiltration. Ann. Geophys. (series B), 4(4): 417–424.

    Google Scholar 

  • Stern R, Ben-Hur M, Shainberg I, 1991. Clay mineralogy effect on rain infiltration, seal formation and soil losses. Soil Science, 152(6): 455–462.

    Article  Google Scholar 

  • Sun Honglie, Zhang Rongzu, 2004. The Principles and Practices of Zonation for Ecological Environment Construction in China. Beijing: Science Press. (in Chinese)

    Google Scholar 

  • Wakindiki I I C, Ben-Hur M, 2002. Soil mineralogy and texture effects on crust micromorphology, infiltration, and erosion. Soil Sci. Soc. Am. J., 66(3): 897–905.

    Google Scholar 

  • Wang Xiekang, Fang Duo, 1997. A physically-based model of rainsplash erosion on the slope. Journal of Sichuan University (Engineering Science Edition), 1(3): 90–102.

    Google Scholar 

  • Watson D A, Laflen J M, 1986. Soil strength, slope, and rainfall intensity effects on interrill erosion. Trans. ASAE, 29(1): 98–102.

    Google Scholar 

  • Woodburn R, 1948. The effect of structural condition on soil detachment by raindrop action. Agricultural Engineering, 29: 154–156.

    Google Scholar 

  • Yu Li, Meng Lingqin, 2000. Soil erosion by water. Scientific and Technical Information of Soil and Water Conservation, (2): 52–53, 58. (in Chinese)

  • Zhu Yuanda, Cai Qiangguo, Hu Xia et al., 2004. Effects of soil physical and chemical properties on soil crusting. Acta Pedologica Sinica, 41(1): 13–19. (in Chinese)

    Google Scholar 

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Authors and Affiliations

  1. Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, 100101, China

    Qinjuan Cheng & Qiangguo Cai

  2. Graduate University of the Chinese Academy of Sciences, Beijing, 100049, China

    Qinjuan Cheng

  3. College of Resources and Environment, China Agricultural University, Beijing, 100094, China

    Wenjun Ma

Authors
  1. Qinjuan Cheng
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  2. Qiangguo Cai
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  3. Wenjun Ma
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Corresponding author

Correspondence to Qiangguo Cai.

Additional information

Foundation item: Under the auspices of National Natural Science Foundation of China (No. 40471084), Innovation Program of Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences (No. 066U0104SZ), State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau (No. 10501-173)

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Cheng, Q., Cai, Q. & Ma, W. Comparative study on rain splash erosion of representative soils in China. Chin. Geogr. Sci. 18, 155–161 (2008). https://doi.org/10.1007/s11769-008-0155-9

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  • DOI: https://doi.org/10.1007/s11769-008-0155-9

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