Soil degassing during watering: An overlooked soil N2O emission process

Environ Pollut. 2018 Nov;242(Pt A):257-263. doi: 10.1016/j.envpol.2018.06.103. Epub 2018 Jun 30.

Abstract

Pulse diffusive nitrous oxide (N2O) emission following water application is well documented, whereas N2O emission caused by soil water-air displacement during the watering process (termed as soil degassing) has been largely overlooked. Watering-induced N2O emissions from ten different soils in China were quantified, and found to range from 74.4 ± 6.7 to 678.1 ± 36.6 μg N2O m-2 h-1 in surface watered (SW) soils, and from 45.6 ± 4.4 to 358.1 ± 23.6 μg N2O m-2 h-1 in subsurface watered (SUW) soils. These N2O fluxes were much larger than the diffusive N2O flux from the same soil either under dry (7.9%-9.6% water filled pore space, WFPS) or wet (85.1%-93.6% WFPS) conditions. The watering process (the water infiltration process upon irrigation/rainfall or the process of shallow groundwater uplifting) resulted in massive N2O emissions.

Keywords: Nitrous oxide; Rainfall; Shallow groundwater lifting; Soil degassing; Watering.

MeSH terms

  • Agricultural Irrigation
  • Air Pollutants / analysis*
  • China
  • Models, Chemical*
  • Nitrous Oxide / analysis*
  • Rain
  • Soil / chemistry*
  • Water

Substances

  • Air Pollutants
  • Soil
  • Water
  • Nitrous Oxide