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Chinese Journal of Applied Ecology ›› 2005, Vol. 16 ›› Issue (10): 1872-1878.

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Soil C,N and P contents and their relationships with soil physical properties in wetlands of Dongting Lake floodplain

PENG Peiqin1,2, ZHANG Wenju2,3, TONG Chengli2, QIU Shaojun1,2, ZHANG Wenchao1,2   

  1. 1. College of Resource and Environment, Hunan Agricultural University, Changsha 410128, China;
    2. Key Laboratory of Subtropical Agro-ecology, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China;
    3. College of Resource and Environment, Huazhong Agricultural University, Wuhan 430070, China
  • Received:2004-12-07 Revised:2005-04-04 Online:2005-10-15 Published:2005-10-15

Abstract: Eight representative soil profiles were installed on three types of wetland (two profiles on Carex spp.-dominated floodplain,four on Phragmites-dominated floodplain,and two on paddy soil) in Dongting Lake floodplain of China in 2004,and their C,N and P contents,microbial biomass C,N and P,<0.001 mm clay particles,and bulk density were measured.The results indicated the spatial distribution of soil C and N and soil microbial biomass C,N,and P were very similar in the profiles (0~100 cm) of three types of wetland,being decreased gradually with depth,except for soil TP which was constant in the profiles.The percentages of soil microbial biomass C,N and P to soil organic C,total nitrogen and total phosphorus decreased gradually with depth.In top layer (0~10 cm),the contents of soil organic C and microbial biomass C and the percentage of soil microbial biomass C to organic C were 19.63~50.20 g·kg-1,424.63~1 597.36 mg·kg-1,and 3.17%~4.82%,respectively,the contents of soil total N and microbial biomass N and the percentage of soil microbial biomass N to total N were 1.85~4.45 g·kg-1,57.90~259.47 mg·kg-1,and 3.13%~6.42%,respectively,and the content of soil microbial biomass P and the percentage of soil microbial biomass P to soil total P was 24.16~200.99 mg·kg-1 and 1.09%~11.20%,respectively.The bulk density of soil top layer (0~10 cm) was 0.65~1.04 g·cm-3,and the content of <0.001 mm clay particles was 26.24%~39.48%.The contents of soil organic C and N and microbial biomass N and P in 0~10 cm layer were the highest in Carex spp.-dominated floodplain,followed by paddy soil,and Phragmites-dominated floodplain.Also in 0~10 cm layer,the soil microbial biomass C in Carex spp.-dominated floodplain and paddy soil was higher than that in Phragmites-dominated floodplain,while the soil bulk density in Phragmites-dominated floodplain was higher than that in paddy soil,and much higher than that in Carex spp.-dominated floodplain.The amount of soil <0.001 mm clay particles in Carex spp.-dominated floodplain and Phragmites-dominated floodplain was higher than that in paddy soil.In these three types of wetland,soil organic C and N and microbial biomass C,N and P had a significant logarithm correlation (P<0.01) with <0.001 mm clay particles,and a significant index correlation (P<0.01) with bulk density.

Key words: Wetland, Soil microbial biomass C, N, and P, Bulk density, Soil clay granule, Profiles

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