Environmental Earth Sciences

, Volume 68, Issue 3, pp 633–639

Soil conservation and sustainable eco-environment in the Loess Plateau of China

Original Article

Abstract

The Loess Plateau is well known to the world because of its thick loess and severe soil erosion. Loess is a highly erosion-prone soil that is considerably susceptible to water erosion. The Loess Plateau also has a long cultivation history, hence population growth, vegetation degeneration serious soil and water loss were obviously problems on Loess Plateau. This article analyzes several strategies of soil and water conservation on the Loess Plateau, such as terracing, planting trees, natural vegetation rehabilitation and construction of warp land dams. Different periods had different strategies of soil and water conservation and each strategy had its characteristics and effects. Finally, the research directions and future perspectives of the Loess Plateau were discussed, including the strategies of sustainable eco-environment of Loess Plateau in China.

Keywords

Soil erosion Soil conservation Sustainable eco-environment Loess Plateau 

References

  1. Cai QG (2001) Soil erosion and management on the Loess Plateau. J Geograph Sci 11(1):53–72CrossRefGoogle Scholar
  2. Chen YZ, Jing K, Cai QG (1988) Modem erosion and management. Science Press, Beijing, pp 39–43 (in Chinese)Google Scholar
  3. Cheng Y, Jing K (1989) Coarse sediment sources of the Yellow River and their recent changes. Meteorology Press, Beijing, pp 69–73 (in Chinese)Google Scholar
  4. Liu DS (1985) Loess and environment. Science Press, Beijing (in Chinese)Google Scholar
  5. Liu GB (1999) Soil conservation and sustainable agriculture on the loess plateau: challenges and prospects. Ambio 28(8):663–668Google Scholar
  6. Ren HY, Wen ZM, Yang QK (2003) The re-vegetation and changes in species diversity in the hilly and gully region on Loess Plateau—as seen by the case study in Wuqi County. Agric Res Arid Areas 21(2):154–158 (in Chinese)Google Scholar
  7. Tang KL (2004) Soil and water conservation in China. Science Press, Bejing (in Chinese)Google Scholar
  8. Xu JX (2006) Temporal variation in sediment transferring function of the Lower Yellow River and the formative causes. Geograph Res 25(2):276–284 (in Chinese)Google Scholar
  9. Zhang XB, An ZS (1994) Relationship between forests and loess thicknesses in the Loess Plateau Region. Bull Soil Water Conserv 14(6):1–4 (in Chinese)Google Scholar
  10. Zhang XB, Zhang YQ (1995) Use of Caesium-137 to investigate sediment sources in the Hekouzhen-Longmen Basin of the Middle Yellow River, China. Sediment Water Qual River Catchments 8:353–362Google Scholar
  11. Zhang XB, Walling DE, Quine TA et al (1997) Use of reservoir deposits and Caesium-137 measurements to investigate the erosion response of a small drainage basin in the rolling Loess Plateau region of China. Land Degrad Dev 8:1–6CrossRefGoogle Scholar
  12. Zhang XB, Walling DE, He XB et al (2009) Use of landslide-dammed lake deposits and pollen tracing techniques to investigate the erosion response of a small drainage basin in the Loess Plateau, China, to land use change during the late 16th century. Catena 79:205–213CrossRefGoogle Scholar

Copyright information

© Springer-Verlag 2012

Authors and Affiliations

  • Zhou Ping
    • 1
  • Wen Anbang
    • 1
  • Zhang Xinbao
    • 1
  • He Xiubin
    • 1
  1. 1.Institute of Mountain Hazards and Environment, Chinese Academy of Sciences and Ministry of Water ResourcesThe Key Laboratory of Mountain Surface Processes and Ecological RegulationChengduChina

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