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Acta Prataculturae Sinica ›› 2015, Vol. 24 ›› Issue (10): 33-39.DOI: 10.11686/cyxb2014429

• Orginal Article • Previous Articles     Next Articles

Effects of fencing and grazing on vegetation and soil physical and chemical properties in an alpine meadow in the Qinghai Lake Basin

LI Yang1, YAN Zhen-Ying2, GUO Ding1, WANG Hai-Xia2, SU Shu-Lan1, LI Xu-Dong1, FU Hua1, *   

  1. 1.College of Pastoral Agriculture Science and Technology, State Key Laboratory of Grassland Agro-ecosystems, Lanzhou University, Lanzhou 730020, China;
    2.Grassland Service Station of Qinghai, Xining 810008, China
  • Online:2015-10-20 Published:2015-10-20

Abstract: The aim of this study was to determine the effects of fencing on the productivity and structure of plant communities and on the physical and chemical properties of soil in alpine meadows. A field study was conducted in two types of degraded alpine meadows, one dominated by Kobresia pygmaea and the other dominated by Kobresia humilis, in the Qinghai Lake Basin. The results showed that the aboveground biomass of K. pygmaea and K. humilis increased by 33.8%, and 31.5%, respectively, after 2 years of exclosure. Exclosure significantly increased the proportion of aboveground biomass of sedges and members of the gramineae, and decreased the proportion of aboveground biomass of forbs. Exclosure also resulted in significant increases in plant community diversity and evenness indexes. In the K. pygmaea and K. humilis alpine meadows, grassland soil organic carbon content in the 0-10 cm soil layer increased by 10.15% and 12.74%, respectively, after 2 years of exclosure. The soil organic carbon content in the 10-30 cm soil layer did not change significantly after 2 years of exclosure. In K. humilis meadow soil, the total phosphorus content increased by 16.13% in the 0-10 cm soil layer, but was unchanged in 10-30 cm soil layer after 2 years of exclosure. In the K. pygmaea and K. humilis alpine meadows, soil bulk density increased by 6.61% and 6.25%, respectively, and pH decreased by 4.04% and 3.69%, respectively, in the 0-10 cm layer after 2 years of exclosure. In the 10-30 cm soil layers of both types of meadows, neither soil bulk density nor pH was affected after 2 years of exclosure.