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Chinese Journal of Applied Ecology ›› 2010, Vol. 21 ›› Issue (3): 631-639.

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Spatial characteristics of soil organic carbon and nitrogen storages in Songnen Plain maize belt.

ZHANG Chun-hua1,2|WANG Zong-ming1|REN Chun-ying1|SONG Kai-shan1; ZHANG Bai1|LIU Dian-wei1   

  1. 1Northeast Institute of Geography and Agricultural Ecology, Chinese Academy of Sciences, Changchun 130012, China|2Graduate University of Chinese Academy of Sciences, Beijing 100049, China
  • Online:2010-03-20 Published:2010-03-20

Abstract: By using the data of 382 typical soil profiles from the second soil survey at national and county levels, and in combining with 1:500000 digital soil maps, a spatial database of soil profiles was established. Based on this, the one meter depth soil organic carbon and nitrogen storage in Songnen Plain maize belt of China was estimated, with the spatial characteristics of the soil organic carbon and nitrogen densities as well as the relationships between the soil organic carbon and nitrogen densities and the soil types and land use types analyzed. The soil organic carbon and nitrogen storage in the maize belt was (163.12±26.48)Tg and (9.53±1.75)Tg, respectively, mainly concentrated in meadow soil, chernozem, and black soil. The soil organic carbon and nitrogen densities were 5.51-25.25 and 0.37-0.80 kg·m-2, respectively, and the C/N ratio was about 7.90-12.67. The eastern and northern parts of the belt had much higher carbon and nitrogen densities than the other parts of the belt, and upland soils had the highest organic carbon density [(19.07±2.44) kg·m-2], forest soils had the highest nitrogen density [(0.82±0.25) kg·m-2], while lowland soils had the lower organic carbon and nitrogen densities.

Key words: soil organic carbon density, soil nitrogen density, soil organic carbon storage, soil nitrogen storage, C/N, Songnen Plain maize belt, dye tracer experiment, stained path number, crack area density, soil surface characteristics.