Welcome to Chinese Journal of Applied Ecology! Today is Share:

Chinese Journal of Applied Ecology ›› 2020, Vol. 31 ›› Issue (8): 2653-2662.doi: 10.13287/j.1001-9332.202008.024

Previous Articles     Next Articles

Distribution of exogenous nitrogen fractions and their fate in moss-dominated biological soil crusts

YAO Xiao-meng1,2, XIAO Bo1,2,3*, WANG Guo-peng1,2, LI Sheng-long1,2, TIAN Le-le1,2, SUN Fu-hai1,2   

  1. 1College of Land Science and Technology, China Agricultural University, Beijing 100193, China;
    2Key Laboratory of Arable Land Conservation in North China, Ministry of Agriculture and Rural Affairs, Beijing 100193, China;
    3State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, Shaanxi, China
  • Received:2019-12-16 Revised:2020-05-19 Online:2020-08-15 Published:2021-02-15
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (41671221) and the “Light of West China” Program of the Chinese Academy of Sciences (2019).

Abstract: Nitrogen (N) labeled with 15N was evenly added into plots of moss-dominated biological soil crusts (BSCs) and bare soil on the Chinese Loess Plateau. After that, the surface BSCs and bare soil samples were continuously collected within 1-30 days. The 15N content of each N fraction in soil, microorganisms, and mosses was measured for each sample. The effects of BSCs on soil N fate and cycling was determined through analyzing the differences in the distribution of 15N fractions between the BSCs and bare soil. Our results showed that: 1) The 15N content of total N (TN), microbial biomass N (MBN), and dissolved organic N (DON) in the BSCs was 2.9, 17.5, and 9.0 times higher than that in the bare soil, respectively. The 15N content of moss plants in the BSCs was 4.73 mg kg-1. 2) The residual rate of 15N in the BSCs and bare soil was 13.0% and 3.3%, respectively, indicating that the N fixing and holding ability of BSCs was four times higher than that of bare soil. The percentage of each 15N fraction in T15N in the BSCs was in the order of MBN (54.3%)>moss plant N (22.5%)>DON (6.2%), while that in the bare soil was in the order of MBN (11.5%)>DON (2.6%). Over all, microorganisms and mosses in the BSCs had 65.3% higher capacity of N fixation as compared with the bare soil. 3) The transferred amount and storage capacity of MB15N in the BSCs were 17.2 and 20.5 times higher than that in the bare soil, respectively. Accordingly, the turnover rate of MB15N in the BSCs and bare soil was 5.8 and 7.2 times per month, respectively, with the turnover time of MB15N in the BSCs being 1.2 times longer than that in bare soil. In conclusion, BSCs fix and hold more N than bare soil and change the distribution of each N fraction, implying that BSCs play a critical role in N cycling in dryland ecosystems.

Key words: biological soil crusts, stable isotope tracer, total nitrogen, microbial biomass nitrogen, dissolved organic nitrogen, nitrogen turnover rate