Effects of freeze-thaw on soil nitrogen and phosphorus availability at the Keerqin Sandy Lands, China

被引:10
|
作者
Zhao Q. [1 ,2 ]
Zeng D.-H. [1 ,2 ]
Fan Z.-P. [1 ,2 ]
机构
[1] Daqinggou Ecological Station, Institute of Applied Ecology, Chinese Academy of Sciences
[2] Institute of Applied Ecology, Chinese Academy of Sciences
基金
中国国家自然科学基金; 国家科技攻关计划;
关键词
Freeze-thaw; Nitrification; Phosphorus availability; Temperate semi-arid region;
D O I
10.1007/s11676-008-0007-6
中图分类号
学科分类号
摘要
A laboratory simulated freeze-thaw was conducted to determine the effects of freeze-thaw on soil nutrient availability in temperate semi-arid regions. Soil samples were collected from sandy soils (0-20 cm) of three typical ecosystems (grassland, Mongolian pine plantation and poplar plantation) in southeastern Keerqin Sandy Lands of China and subjected to freeze-thaw treatment (-12°C for 10 days, then 20°C for 10 days) or incubated at constant temperature (20°C for 20 days). Concentrations of the soil NO3 --N, NH4 +-N, NaHCO3 extractable inorganic P (LPi) and microbial biomass P (MBP) were determined on three occasions: at the start of the incubation, immediate post-thawing and at the 10th day post-thawing. The results showed that soil net nitrification and N mineralization rates at three sites were negatively affected by freeze-thaw treatment, and decreased by 50%-85% as compared to the control, of which the greatest decline occurred in the soil collected from poplar plantation. In contrast, the concentration of soil NH4 +-N, NaHCO 3 extractable inorganic P (LPi) and microbial biomass P were insignificantly influenced by freeze-thaw except that LPi and NH4 +-N showed a slight increase immediate post-thawing. The effects of freeze-thaw on soil N transformation were related to soil biological processes and the relatively constant available P was ascribed to severe soil aridity. © 2008 Northeast Forestry University.
引用
收藏
页码:44 / 48
页数:4
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