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Chinese Journal of Applied Ecology ›› 2010, Vol. 21 ›› Issue (2): 312-316.

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Seasonal variations of soil organic carbon and microbial biomass carbon in degraded desert steppes of Inner Mongolia.

WU Yong-sheng1,2,3;MA Wan-li3,4;LI Hao3;LÜ|Gui-fen3;LU Ping3   

  1. 1College of Resources Science &Technology, Beijing Normal University, Beijing 100875, China|2State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing 100875, China|3College of Life Science and Technology, Inner Mongolia Normal University, Huhhot 010022, China|4Planning and Design Academy of Forestry Products Industry, State Forestry Administration, Beijing 100714, China
  • Online:2010-02-20 Published:2010-02-20

Abstract: Sampling sites were installed in Damao Banner, Siziwang Banner, and Sunite Right Banner of Inner Mongolia, which represented lightly, moderately, and heavily degraded desert steppes, respectively, and surface (0-20 cm) soil samples were collected to analyze the quantitative characteristics and seasonal dynamics of soil organic carbon (SOC) and microbial biomass carbon (MBC) in these steppes. The SOC and MBC contents decreased with the increasing degradation degree of desert steppe. The total amount of soil culturable microbes in lightly and moderately degraded desert steppes was higher than that in heavily degraded desert steppe, except in summer 2006, and the MBC content and the quantity of soil culturable microbes were higher in summer and autumn than in spring and winter. Correlation analysis showed that there was a significant positive correlation between SOC and MBC (P<0.01), suggesting that both SOC and MBC could be used as the sensitive indicators to evaluate the degradation degree of desert steppe.

Key words: desert steppe, soil organic carbon, microbial biomass carbon, flooding, Distylium chinense, net photosynthetic rate, light response model, photosynthetic parameter.