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Chinese Journal of Applied Ecology ›› 2020, Vol. 31 ›› Issue (5): 1459-1466.doi: 10.13287/j.1001-9332.202005.024

• Special Features of Soil Ecology and Health • Previous Articles     Next Articles

Effects of long-term fertilization on soil ammonia-oxidizing microorganisms

LIU Ling-zhi, MA Shi-han, LI Xiu-ling, AN Ting-ting*, WANG Jing-kuan   

  1. National Engineering Laboratory for Efficient Utilization of Soil and Fertilizer Resources/Ministry of Agriculture Key Laboratory of Arable Land Conservation in Northeast China, College of Land and Environment, Shenyang Agricultural University, Shenyang 110866, China
  • Received:2019-10-26 Online:2020-05-15 Published:2020-05-15
  • Contact: * E-mail: atting@syau.edu.cn
  • Supported by:
    This work was supported by the Basic Scientific Research Project of Universities in Liaoning Province (LSNZD201705), the Natural Science Foundation of Liaoning Province (2019-MS-271), and the National Natural Science Foundation of China (31101504).

Abstract: Long-term fertilization can change the supply of soil carbon and nitrogen (N), with consequences on the abundance and community structure of soil microorganisms. Based on the long-term fertilization positioning experiment station of brown earth, we analyzed the dynamics of soil ammonia-oxidizing archaea (AOA) and ammonia-oxidizing bacteria (AOB) under different fertilization treatments, including no fertilization (CK), low level of inorganic N fertilizer (N2), high level of inorganic N fertilizer (N4), and organic manure combined with inorganic N fertilizer (M2N2), aiming to provide a basis for microbiological mechanism of soil N transformation and improvement of soil fertility. The results showed that the ratio of AOA to AOB abundance was 2.28-61.95 under different fertilization treatments. Compared with that in CK, the AOA abundance was reduced by 1.6%-13.6% after long-term fertilization. The abundance of AOB in N4 treatment decreased first and then increased with soil depths, but with contrary results in other treatments. The Shannon diversity index (H), evenness index (J), and Simpson index (S) of AOB were higher than those of AOA. The AOB diversity was increased at 0-20 cm soil layer in M2N2 treatment, while that of AOA was decreased. Soil AOB clustered with soil depths, and neither AOA nor AOB community clustered with fertilization treatments. In summary, long-term fertilization altered the composition of AOA and AOB. AOA was sensitive to environment, whereas AOB was more abundant and stable.

Key words: ammonia-oxidizing archaea, ammonia-oxidizing bacteria, long-term fertilization, diversity