Journal of Arid Land

, Volume 9, Issue 2, pp 188–199 | Cite as

Effects of vegetation types on soil water dynamics during vegetation restoration in the Mu Us Sandy Land, northwestern China

  • Xiaona Yu
  • Yongmei Huang
  • Engui Li
  • Xiaoyan Li
  • Weihua Guo


The arid and semi-arid northwestern China has been undergoing ecological degradation and the efforts to reverse the ecological degradation have been undertaken for many years. Some shifting dunes have been fixed and the vegetation has been partially recovered in certain areas and the Mu Us Sandy Land in the Ordos Plateau is an example of the success. The present study attempts to reveal the relationships between the vegetation restoration and ecohydrology in the Mu Us Sandy Land. We continuously measured soil water content at 10-min intervals under three vegetation types (i.e., shifting dune, shrub-dominated community, and herb-dominated community) in the Mu Us Sandy Land from April 2012 to October 2013. The results show the infiltration coefficient increased with increased rainfall amount and eventually reached a stable value. Infiltration coefficients were 0.91, 0.64, and 0.74 in the shifting dune, in the shrub-dominated community, and in the herb-dominated community, respectively. Cumulative infiltration and soil texture are two vital factors affecting the depths of rainfall penetration. Only rainfall events larger than 35.0 mm could recharge soil water at the 60–80 cm layer in the herb-dominated community. Our results imply that the expected forward succession of restored vegetation may be destined to deterioration after reaching the climax simply because of following two facts: (1) soil water is mainly retained at shallower layer and (2) plant fine roots mainly distribute in deeper layer in the herb-dominated community.


ecohydrology soil water content vegetation restoration Artemisia ordosica community 


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This work was supported by the National Natural Science Foundation of China (41130640, 41321001, 31470402), the Program for Changjiang Scholars and Innovative Research Team in University (IRT1108), and the Fundamental Research Funds for the Central Universities (2012CXQT07).


  1. Angelaki A, Sakellariou-Makrantonaki M, Tzimopoulos C. 2013. Theoretical and experimental research of cumulative infiltration. Transport in Porous Media, 100(2): 247–257.CrossRefGoogle Scholar
  2. Carlyle-Moses D E. 2004. Throughfall, stemflow, and canopy interception loss fluxes in a semi-arid Sierra Madre Oriental matorral community. Journal of Arid Environments, 58(2): 181–202.CrossRefGoogle Scholar
  3. Castellano M J, Valone T J. 2007. Livestock, soil compaction and water infiltration rate: evaluating a potential desertification recovery mechanism. Journal of Arid Environments, 71(1): 97–108.CrossRefGoogle Scholar
  4. Cheng X L, An S Q, Li B, et al. 2006. Summer rain pulse size and rainwater uptake by three dominant desert plants in a desertified grassland ecosystem in northwestern China. Plant Ecology, 184(1): 1–12.CrossRefGoogle Scholar
  5. Cobos D R, Chambers C. 2010. Calibrating ECH2O Soil Moisture Sensors, Application Note. Pullman, USA: Decagon Devices Inc., 1–7.Google Scholar
  6. Guo K. 2000. Cyclic succession of Artemisia ordosica Krasch. community in the Mu Us Sandy grassland. Acta Phytoecologica Sinica, 24(2): 243–247. (in Chinese)Google Scholar
  7. Hajiaghaei A, Rashidi M, Sadeghi M A, et al. 2014. Prediction of soil infiltration rate based on silt and clay content of soil. American-Euransian Journal of Agricultural & Environmental Science, 14(8): 702–706.Google Scholar
  8. He Z B, Zhao W Z, Liu H, et al. 2012. The response of soil moisture to rainfall event size in subalpine grassland and meadows in a semi-arid mountain range: a case study in northwestern China’s Qilian Mountains. Journal of Hydrology, 420–421: 183–190.CrossRefGoogle Scholar
  9. Heisler-White J L, Knapp A K, Kelly E F. 2008. Increasing precipitation event size increases aboveground net primary productivity in a semi-arid grassland. Oecologia, 158(1): 129–140.CrossRefGoogle Scholar
  10. Lambers R, Rietkerk M, van den Bosch F, et al. 2001. Vegetation pattern formation in semi-arid grazing systems. Ecology, 82(1): 50–61.CrossRefGoogle Scholar
  11. Hudson B D. 1994. Soil organic matter and available water capacity. Journal of Soil and Water Conservation, 49(2): 189–194.Google Scholar
  12. Jeddi K, Chaieb M. 2010. Changes in soil properties and vegetation following livestock grazing exclusion in degraded arid environments of South Tunisia. Flora—Morphology, Distribution, Functional Ecology of Plants, 205(3): 184–189.CrossRefGoogle Scholar
  13. Konwar J. 2016. Soil texture and total organic matter content and its influences on soil water holding capacity of Municipality soils of Moran in Sivasagar district of Assam, India. International Journal of Scientific Research, 5(1): 536–537.Google Scholar
  14. Lebron I, Madsen M D, Chandler D G, et al. 2007. Ecohydrological controls on soil moisture and hydraulic conductivity within a pinyon-juniper woodland. Water Resources Research, 43(8): W08422, doi: 10.1029/2006WR005398.CrossRefGoogle Scholar
  15. Li X J, Li X R, Song W M, et al. 2008. Effects of crust and shrub patches on runoff, sedimentation, and related nutrient (C, N) redistribution in the desertified steppe zone of the Tengger Desert, Northern China. Geomorphology, 96(1–2): 221–232.CrossRefGoogle Scholar
  16. Li X R, Ma F Y, Xiao H L, et al. 2004. Long-term effects of revegetation on soil water content of sand dunes in arid region of Northern China. Journal of Arid Environments, 57(1): 1–16.CrossRefGoogle Scholar
  17. Li X R. 2005. Influence of variation of soil spatial heterogeneity on vegetation restoration. Science in China Series D: Earth Sciences, 48(1): 2020–2031.CrossRefGoogle Scholar
  18. Li X R, Kong D S, Tan H J, et al. 2007. Changes in soil and vegetation following stabilisation of dunes in the southeastern fringe of the Tengger Desert, China. Plant and Soil, 300(1–2): 221–231.CrossRefGoogle Scholar
  19. Li X R, Zhang Z S, Huang L, et al. 2013. Review of the ecohydrological processes and feedback mechanisms controlling sand-binding vegetation systems in sandy desert regions of China. Chinese Science Bulletin, 58(13): 1483–1496.CrossRefGoogle Scholar
  20. Li X Y, Zhang S Y, Peng H Y, et al. 2013. Soil water and temperature dynamics in shrub-encroached grasslands and climatic implications: results from Inner Mongolia Steppe ecosystem of north China. Agricultural and Forest Meteorology, 171–172: 20–30.CrossRefGoogle Scholar
  21. Liu G S. 1996. Soil Physical and Chemical Analysis & Description of Soil Profiles. Beijing: Standards Press of China, 38–39. (in Chinese)Google Scholar
  22. Liu N, Zhou L H, Chen Y, et al. 2014. Identification and evaluation of desertification reversal in China: indicators and methods review. Sciences in Cold and Arid Regions, 6(3): 190–200.Google Scholar
  23. Liu S G. 1997. A new model for the prediction of rainfall interception in forest canopies. Ecological Modelling, 99(2–3): 151–159.CrossRefGoogle Scholar
  24. Millennium Ecosystem Assessment. 2005. Ecosystems and Human Well-Being: Desertification Synthesis. Washington D.C.: World Resource Institute: 18–20.Google Scholar
  25. Rietkerk M, van de Koppel J. 1997. Alternate stable states and threshold effects in semi-arid grazing systems. Oikos, 79(1): 69–76.CrossRefGoogle Scholar
  26. Sala O E, Lauenroth W K. 1982. Small rainfall events: an ecological role in semiarid regions. Oecologia, 53(3): 301–304.CrossRefGoogle Scholar
  27. Su Y Z, Li Y L, Cui J Y, et al. 2005. Influences of continuous grazing and livestock exclusion on soil properties in a degraded sandy grassland, Inner Mongolia, northern China. Catena, 59(3): 267–278.CrossRefGoogle Scholar
  28. van de Koppel J, Rietkerk M, Weissing F J. 1997. Catastrophic vegetation shifts and soil degradation in terrestrial grazing systems. Trends in Ecology & Evolution, 12(9): 352–356.CrossRefGoogle Scholar
  29. van de Koppel J, RietkerK M, Van Langevelde F, et al. 2002. Spatial heterogeneity and irreversible vegetation change in semiarid grazing systems. The American Naturalist, 159(2): 209–218.CrossRefGoogle Scholar
  30. van de Koppel J, Rietkerk M. 2004. Spatial interactions and resilience in arid ecosystems. The American Naturalist, 163(1): 113–121.CrossRefGoogle Scholar
  31. Walkley A, Black I A. 1934. An examination of the Degtjareff method for determining soil organic matter, and a proposed modification of the chromic acid titration method. Soil Science, 37(1): 29–38.CrossRefGoogle Scholar
  32. Wang Q S, Dong X J, Chen X D, et al. 1997. Study on some features of Artemisia ordosica community at the different successional stages. Acta Phytoecologica Sinica, 21(6): 531–538. (in Chinese)Google Scholar
  33. Wang S, Fu B J, Gao G Y, et al. 2013. Responses of soil moisture in different land cover types to rainfall events in a re-vegetation catchment area of the Loess Plateau, China. Catena, 101: 122–128.CrossRefGoogle Scholar
  34. Wang T, Wu W, Xue X, et al. 2004. Spatial-temporal changes of sandy desertified land during last 5 decades in northern China. Acta Geographica Sinica, 59(2): 203–212. (in Chinese)Google Scholar
  35. Wang X P, Li X R, Kang E S, et al. 2003. The infiltration and redistribution of precipitation in revegetated sand dunes in the Tengger Desert, Shapotou, China. Acta Ecologica Sinica, 23(6): 1234–1241. (in Chinese)Google Scholar
  36. Wang X P, Kang E S, Zhang J G, et al. 2004. Comparison of interception loss in shrubby and sub-shrubby communities in the Tengger desert of northwest China. Journal of Glaciology and Geocryology, 26(1): 89–94. (in Chinese)Google Scholar
  37. Wang X P, Li X R, Xiao H L, et al. 2007. Effects of surface characteristics on infiltration patterns in an arid shrub desert. Hydrological Processes, 21(1): 72–79.CrossRefGoogle Scholar
  38. Wang X P, Zhang Y F, Hu R, et al. 2012. Canopy storage capacity of xerophytic shrubs in Northwestern China. Journal of Hydrology, 454–455: 152–159.CrossRefGoogle Scholar
  39. Wilcox B P, Breshears D D, Turin H J. 2003. Hydraulic conductivity in a Piñon–juniper woodland. Soil Science Society of America Journal, 67(4): 1243–1249.CrossRefGoogle Scholar
  40. Yang X, Zhang K, Jia B, et al. 2005. Desertification assessment in China: an overview. Journal of Arid Environments, 63(2): 517–531.CrossRefGoogle Scholar
  41. Zhang H J, Wu B, Yang W B, et al. 2012. Soil moisture characteristics of Artemisia ordosica community at different succession stages in Mu Us Sandy Land. Journal of Desert Research, 32(6): 1597–1603. (in Chinese)Google Scholar
  42. Zhang X S. 1994. Principles and optimal models for development of Maowusu Sandy grassland. Acta Phytoecologica Sinica, 18(1): 1–16. (in Chinese)Google Scholar
  43. Zhang Z H, Li X Y, Jiang Z Y, et al. 2013. Changes in some soil properties induced by re-conversion of cropland into grassland in the semiarid steppe zone of Inner Mongolia, China. Plant and Soil, 373(1): 89–106.CrossRefGoogle Scholar

Copyright information

© Xinjiang Institute of Ecology and Geography, the Chinese Academy of Sciences and Springer - Verlag GmbH 2017

Authors and Affiliations

  • Xiaona Yu
    • 1
  • Yongmei Huang
    • 2
  • Engui Li
    • 2
  • Xiaoyan Li
    • 2
  • Weihua Guo
    • 1
  1. 1.Institute of Ecology and Biodiversity, College of Life ScienceShandong UniversityJinanChina
  2. 2.College of Resources Science and TechnologyBeijing Normal UniversityBeijingChina

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