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Acta Prataculturae Sinica ›› 2015, Vol. 24 ›› Issue (8): 24-34.DOI: 10.11686/cyxb2014395

• Orginal Article • Previous Articles     Next Articles

Effects of different years of cultivation abandonment on soil physical, chemical and microbial characteristics in the midstream and downstream of Shiyang River area

CHAI Xiao-Hong1, WANG Li-De12,3, YAO Tuo1*, HAN Fu-Gui2,3, WEI Lin-Yuan2,3, GUO Chun-Xiu2,3, ZHANG Ying-Hua2,3   

  1. 1.College of Pratacultural Science, Ministry of Education Key Laboratory of Grassland Ecosystem, Pratacultural Engineering Laboratory of Gansu Province, Sino-U.S. Center for Grazing Land Ecosystem Sustainability, Gansu Agricultural University, Lanzhou 730070, China;
    2.Gansu Desert Control Research Institute, Lanzhou 730070, China;
    3.Gansu Hexi Corridor Forest Ecosystem Research National Station, State Key Laboratory Breeding Base of Desertification and Aeolian Sand Disaster Combating, Wuwei 733000, China
  • Online:2015-08-20 Published:2015-08-20

Abstract: Soils have been investigated in midstream and downstream areas of the Shiyang River that had been previously cultivated but abandoned for different numbers of years. The research investigated physical and chemical properties (water content, organic carbon, nitrate nitrogen, ammonium nitrogen, total phosphorus, available phosphorus, total potassium, quick-available potassium, slow-available potassium) and microbes (microbial biomass C, N, P and the number of microorganisms). Results showed that soil ammonium nitrogen and total phosphorus content decreased the longer the land had been abandoned, while water content, organic carbon, nitrate nitrogen, available phosphorus, available potassium and slow-available potassium increased. There were however no significant differences in total potassium and quick-available potassium over the years. Microbial biomass C decreased in 30-40 cm soil layers in land abandoned for shorter periods (1-5 yrs), but increased for longer periods (8-31 yrs). The variability of microbial biomass N increased initially (1-4 yrs), then decreased (4-8 yrs) and finally stabilized (8-31 yrs). Except for 0-10 cm soil layers, the variability of soil microbial biomass P decreased at first (1-2 yrs), then increased (2-8 yrs) and finally decreased (8-31 yrs). Bacteria were the most frequent, followed by actinomycetes, and fungi were the least numerically significant during all stages.