Nitrous oxide (N 2 O) is a potent greenhouse gas with a 100-year global warming potential ~300 times higher than CO 2 , and has the third largest radiative forcing among the biogenic greenhouse gases (Myhre et al., 2013). N 2 O also depletes stratospheric ozone (Revell et al., 2012). Globally, soils are the dominant sources of both anthropogenic and natural emissions of N 2 O, with 1.7-4.8 Tg N 2 O-N year −1 emitted by agricultural soils and 3.3-9.0 Tg N 2 O-N year −1 from soils under natural vegetation (Ciais et al., 2013). Ammonia (NH 3 ) oxidation, the rate-limiting step of nitrification, is performed in soil mainly by aerobic ammonia-oxidizing bacteria