Effect of banning grazing on alpine meadow soil organic carbon, physio-chemical properties and enzyme activities in Binggou Watershed, Qilian Mountains
View Fulltext  View/Add Comment  Download reader
  
DOI:10.7606/j.issn.1000-7601.2017.04.27
Key Words: Qilian Mountain  alpine meadow soil  organic carbon  enzyme activity
Author NameAffiliation
QIU Li-hua School of Agriculture and Biotechnology of Hexi University,Zhangye, Gansu 734000, China
Zhangye in Gansu Province Suna County Agricultural Technology Promotion Center, Zhangye, Gansu 734400, China 
QIN Jia-hai School of Agriculture and Biotechnology of Hexi University,Zhangye, Gansu 734000, China 
ZHANG Yong School of Agriculture and Biotechnology of Hexi University,Zhangye, Gansu 734000, China 
Hits: 1617
Download times: 1436
Abstract:
      The experiment was conducted to determine the influence of banning grazing on alpine meadow soil organic carbon, physio-chemical properties and enzyme activities at Ice Valley, Qilian Mountain. The results showed that the vegetation coverage, soil biomass and organic matter content of alpine meadow soil were decreased significantly after grazing for three years. Organic matter content, organic carbon density, total porosity, aggregate, field capacity, NPK content and enzyme activity at 0~20 cm layer was decreased, and soil bulk density, CaCO3 and soluble salt content was increased. Compared with grazing, the soil bulk density, CaCO3 and soluble salt content at 0~20 cm layer in area of grazing prohibition were increased by 14.15%, 6.35%, and 1.27%, and organic matter content, organic carbon density, total porosity, aggregate, and field capacity by 29.76%, 22.82%, 9.45%, 6.49%, and 7.69%, respectively; while the urease, sucrase, phosphatase and calatase activities and total NPK was reduced by 33.77%, 26.11%, 42.00%, 29.31%, 25.97%, 15.56% and 12.17%, respectively. In conclusion, the influencing depth of grazing on organic carbon, soil bulk density, total porosity, field capacity decreased, soluble salt content, NPK and enzyme activity was 0~20 cm soil depth, whereas that on aggregate was 0~40 cm soil depth.