Soil Microbial Activity During Secondary Vegetation Succession in Semiarid Abandoned Lands of Loess Plateau  

作　　者：JIANG Jin-Ping XIONG You-Cai JIANG Hong-Mei YE De-You SONG Ya-Jie LI Feng-Min 

机构地区：[1]Key Laboratory of Arid and Grassland Ecology of Education Ministry of China, School of Life Sciences, Lanzhou University, Lanzhou 730000 (China) [2]Key Laboratory of Arid and Grassland Ecology of Education Ministry of China, School of Resources and Environment Science, Lanzhou University, Lanzhou 730000 (China) [3]Gansu Academy of Agricultural Science, Lanzhou 730070 (China) [4]Key Laboratory of Soil Environment and Pollution Remediation, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008 (China) [5]School of Forestry and Environment Studies, Yale University, New Haven CT06511 (USA)

出　　处：《Pedosphere》2009年第6期735-747,共13页土壤圈（英文版）

基　　金：Project supported by the National Key Basic Research Program (973 Program) of China (No. 2007CB106804);the PhD candidate Training Program (No. 20060730027);the "111" Project from the State Administration of Foreign Experts Affairs (SAFEA);the Ministry of Education of China

摘　　要：To show the vegetation succession interaction with soil properties, microbial biomass, basal respiration, and enzyme activities in different soil layers （0-60 cm） were determined in six lands, i.e., 2-, 7-, 11-, 20-, and 43-year-old abandoned lands and one native grassland, in a semiarid hilly area of the Loess Plateau. The results indicated that the successional time and soil depths affected soil microbiological parameters significantly. In 20-cm soil layer, microbial biomass carbon （MBC）, microbial biomass nitrogen （MBN）, MBC/MBN, MBC to soil organic carbon ratio （MBC/SOC）, and soil basal respiration tended to increase with successional stages but decrease with soil depths. In contrast, metabolic quotient （qCO2） tended to decrease with successional stages but increase with soil depths. In addition, the activities of urease, catalase, neutral phosphatase, β-fructofuranosidase, and earboxymethyl cellulose （CMC） enzyme increased with successional stages and soil depths. They were significantly positively correlated with microbial biomass and SOC （P 〈 0.5）, whereas no obvious trend was observed for the polyphenoloxidase activity. The results indicated that natural vegetation succession could improve soil quality and promote ecosystem restoration, but it needed a long time under local climate conditions.To show the vegetation succession interaction with soil properties, microbial biomass, basal respiration, and enzyme activities in different soil layers (0-60 cm) were determined in six lands, i.e., 2-, 7-, 11-, 20-, and 43-year-old abandoned lands and one native grassland, in a semiarid hilly area of the Loess Plateau. The results indicated that the successional time and soil depths affected soil microbiological parameters significantly. In 20-cm soil layer, microbial biomass carbon (MBC), microbial biomass nitrogen (MBN), MBC/MBN, MBC to soil organic carbon ratio (MBC/SOC), and soil basal respiration tended to increase with successional stages but decrease with soil depths. In contrast, metabolic quotient (qCO 2 ) tended to decrease with successional stages but increase with soil depths. In addition, the activities of urease, catalase, neutral phosphatase, β-fructofuranosidase, and carboxymethyl cellulose (CMC) enzyme increased with successional stages and soil depths. They were significantly positively correlated with microbial biomass and SOC (P < 0.5), whereas no obvious trend was observed for the polyphenoloxidase activity. The results indicated that natural vegetation succession could improve soil quality and promote ecosystem restoration, but it needed a long time under local climate conditions.

关 键 词：microbial biomass carbon microbial biomass nitrogen SOC soil enzyme activity 

分 类 号：S158[农业科学—土壤学] S154.3[农业科学—农业基础科学]