4.8 Article

Responses of soil N2O emissions and their abiotic and biotic drivers to altered rainfall regimes and co-occurring wet N deposition in a semi-arid grassland

Journal

GLOBAL CHANGE BIOLOGY
Volume 27, Issue 19, Pages 4894-4908

Publisher

WILEY
DOI: 10.1111/gcb.15792

Keywords

climate change; greenhouse gas emissions; Leymus chinensis; nitrous oxide; precipitation amount; precipitation frequency; wet nitrogen deposition

Funding

  1. National Key Research and Development Program of China [2016YFC0500705]
  2. National Natural Science Foundation of China [31971505]
  3. Natural Science Foundation of Jilin Province [YDZJ2021ZYTS081]
  4. Fundamental Research Funds for the Central Universities [2412017FZ017, 2412020QD022]
  5. Youth Talent Support Project of Jilin Province [QT202007]
  6. China Postdoctoral Science Foundation [2021M690030]
  7. Program of Introducing Talents of Discipline to Universities [B16011]
  8. French Institute of Research for Agriculture, Alimentation and Environment

Ask authors/readers for more resources

The study found that reduced rainfall and nitrogen deposition increased soil N2O emissions in semi-arid grasslands. There was an interactive effect between rainfall amount and N deposition, indicating a complex relationship between these factors in influencing N2O emissions.
Global change factors such as changed rainfall regimes and nitrogen (N) deposition contribute to increases in the emission of the greenhouse gas nitrous oxide (N2O) from the soil. In previous research, N deposition has often been simulated by using a single or a series of N addition events over the course of a year, but wet N deposition actually co-occurs with rainfall. How soil N2O emissions respond to altered rainfall amount and frequency, wet N deposition, and their interactions is still not fully understood. We designed a three-factor, fully factorial experiment with factors of rainfall amounts (ambient, -30%) rainfall frequency (ambient, +/- 50%) and wet N deposition (with/without) co-occurring with rainfall in semi-arid grassland mesocosms, and measured N2O emissions and their possible biotic and abiotic drivers. Across all treatments, reduced rainfall amount and N deposition increased soil N2O emissions by 35% and 28%, respectively. A significant interactive effect was observed between rainfall amount and N deposition, and to a lesser extent between rainfall frequency and N deposition. Without N deposition, reduced rainfall amount and altered rainfall frequency indirectly affected soil N2O emissions by changing the abundance of nirK and soil net N mineralization, and the changes in nirK abundance were indirectly driven by soil N availability rather than directly by soil moisture. With N deposition, both the abundance of nirK and the level of soil water-filled pore space contributed to changes in N2O emissions in response to altered rainfall regimes, and the changes in the abundance of nirK were indirectly driven by plant N uptake and nitrifier (ammonia-oxidizing bacteria) abundance. Our results imply that unlike wetter grassland ecosystems, reduced precipitation may increase N2O emissions, and N deposition may only slightly increase N2O emissions in arid and semi-arid N-limited ecosystems that are dominated by grasses with high soil N uptake capacity.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.8
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available