Intermediate soil acidification induces highest nitrous oxide emissions.

Global potent greenhouse gas nitrous oxide (N₂O) emissions from soil are accelerating, with increases in the proportion of reactive nitrogen emitted as N₂O, i.e., N₂O emission factor (EF). Yet, the primary controls and underlying mechanisms of EFs remain unresolved. Based on two independent but complementary global syntheses, and three field studies determining effects of acidity on N₂O EFs and soil denitrifying microorganisms, we show that soil pH predominantly controls N₂O EFs and emissions by affecting the denitrifier community composition. Analysis of 5438 paired data points of N₂O emission fluxes revealed a hump-shaped relationship between soil pH and EFs, with the highest EFs occurring in moderately acidic soils that favored N₂O-producing over N₂O-consuming microorganisms, and induced high N₂O emissions. Our results illustrate that soil pH has a unimodal relationship with soil denitrifiers and EFs, and the net N₂O emission depends on both the N₂O/(N₂O + N₂) ratio and overall denitrification rate. These findings can inform strategies to predict and mitigate soil N₂O emissions under future nitrogen input scenarios. Intermediate soil acidification alters the denitrifier community composition and induces high nitrous oxide (N₂O) emissions, which contributes to the observed acceleration of N₂O emissions from global soils [ABSTRACT FROM AUTHOR]