4.7 Article

Rapid soil rewetting promotes limited N2O emissions and suppresses NH3 volatilization under urea addition

期刊

ENVIRONMENTAL RESEARCH
卷 212, 期 -, 页码 -

出版社

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.envres.2022.113402

关键词

Ammonia volatilization; Nitrous oxide emission; Dry-wet alternation; Soil moisture; Ammonia oxidizing microbes; Ureolytic microbes

资金

  1. National Natural Science Foun-dation of China [32172678]
  2. National Key Research and Develop-ment Program of China [2020YFD1000904]
  3. China Agriculture Research System of MOF [CARS-12]
  4. Fundamental Research Funds for the Central Universities [2662021ZH001]

向作者/读者索取更多资源

The alternation of dry and wet is an important factor affecting nitrous oxide emissions from soil. This study investigated the effects of drying and rewetting on the emissions of N2O and NH3 after urea application and the changes in microbial communities. The results showed that both N2O and NH3 emissions decreased during the drying process and increased slightly after rapid rewetting.
The alternation of dry and wet is an important environmental factor affecting the emission of nitrous oxide from soil. However, the consistent or opposite effects on NH3 and N2O emissions caused by adding exogenous urea in this process have not been fully considered. Here, we controlled the initial (slow drying) and final (adding water) water-filled pore space (WFPS) at 70%, 60%, or 50% through microculture experiment to simulate a process of slow drying-fertilization and rapid wetting of the soil from rice harvest to dryland crop fertilization. Through measuring soil chemical properties and the abundance and composition of related microbial communities during drying process, we studied the pathways of influence of drying and rewetting on the emission of N2O and NH3 after urea application. During the progressive drying process (WFPS decreasing from 70% to 60% and 50%), soil N2O and NH3 emissions decreased by 49.77%-72.13% and 17.89%-42.19%, respectively. After rapid rewetting (WFPS increasing from 60% to 70%, 50%-60% and 70%), N2O emissions showed a slight increase, while NH3 volatilization continued to decrease. Soil NH+4 - N and DOC contents both decreased during progressive drying, while the soil NO-3 - N content was enhanced. The drying process changed the community structure of ureC and amoA-b and reduced their abundance but had no effect on amoA-a, nirK or nirS. Correlation analysis indicated that the reductions in NH+4 - N content and the abundances of ureC and amoA-b were the main factors suppressing N2O and NH3 emissions. We believe that drying process limits the related microbial activity and substrate supply during ammonia oxidation process in terms of N2O emissions, while in terms of NH3 volatilization, it reduces the related microbial activity of urea hydrolysis process and increases the ammonium adsorption to the soil.

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