Hydroxylamine contributes more to abiotic N 2 O production in soils than nitrite

Abstract

Nitrite (NO2-) and hydroxylamine (NH 2 OH) are important intermediates of the nitrogen (N) cycle in soils. They play a crucial role in the loss of nitrous oxide (N2O) and nitric oxide (NO) from soil due to their high reactivity. In this study, we collected soil samples from three ecosystems (grassland, arable land, and forest with a riparian zone) and explored the contribution of NO2- and NH 2 OH to N 2 O formation in the different soils after exposure to oxic or anoxic pre-treatment. In addition, the importance of abiotic processes on the N 2 O formation from the two intermediates was studied by irradiating the soil samples with γ-irradiation. Our results demonstrate that NO2- addition induced the largest N 2 O production in the grassland soil, followed by the forest and arable soils. Only 9-39% of the produced N 2 O after NO2- addition came from abiotic processes. NH 2 OH addition increased N 2 O emissions the most from the arable soil, followed by the grassland and forest soils. The conversion of NH 2 OH to N 2 O was mostly (73-93%) abiotic. Anoxic pre-treatment decreased N 2 O production from NH 2 OH remarkably, especially for the grassland soil, while it increased N 2 O production from NO2- for most of the soils. Correlation analysis showed that NO2- effects on N 2 O production were strongly correlated to NH4+ content in soils with anoxic pre-treatment, while NH 2 OH effects on N 2 O production were strongly correlated to soil Mn and C content in soils with oxic pre-treatment. Our results indicate that NH 2 OH plays an important role for abiotic N 2 O formation in soils with low C and high Mn content, while the effect of NO2- was important mainly during biotic N 2 O production. Anoxic periods prior to N addition may increase the contribution of NO2-, but reduce the contribution of NH 2 OH, to soil N 2 O formation.