UC Irvine

Atmospheric nitrous oxide (N(2)O) accounts for approximately 5% of the global greenhouse effect and destroys stratospheric ozone. Soils are the most important source of N(2)O, which is produced during nitrification and denitrification. To assess the impact of environmental variables and ecosystems on N(2)O flux, we performed a meta-analysis comparing N(2)O flux in N amended and matched control plots in non-agricultural soils. We found that N(2)O release increased with N amendment in the short term. Although there were few studies in shrubland, this ecosystem showed the greatest response. The N(2)O response to N amendment was greater in year-round studies and in studies with more measurements, but lower in longer studies. The N(2)O response was greater at higher latitudes and precipitation rates. We also observed an unexpected 55% decline in the N(2)O response to N amendment over the 23 years covered by the studies. This pattern may reflect a suppression of the N(2)O response from long-term N deposition accumulation, particularly in temperate regions. Although short term increases in reactive N entering natural systems may cause positive feedbacks to the release of N(2)O, this effect may diminish over time in locations with high rates of N deposition.