Abstract

Fluxes of nitrous oxide (N2O) and nitric oxide (NO) were measured on a drained and forested peatland in 1992-1995. Net mineralization and nitrification were studied in situ in 1993-1994. Nitrogen additions in 1992 as KNO3, NH4Cl, or urea (100 kg N ·ha-1) were used to study the fate and transformations of N in peat. The mean N2O emissions during the growth season in 1993 were 1.9, 2.6, 3.3, and 3.5 mg N ·m-2 ·day-1 in the control soil, KNO3, NH4Cl, and urea-treated soils, respectively. Mean NO fluxes during the growth season in 1993 averaged 0.3, 0.4, 0.7, and 0.6 mg N ·m-2 ·day-1 in the control soil, KNO3, NH4Cl, and urea treatment, respectively. Annual net N mineralization was 87 kg N ·ha-1 in the control soil and 107, 129, and 91 kg ·ha-1 in the KNO3, NH4Cl, and urea-treated soils, respectively. Added N increased the fluxes of N oxides at least for a year after the treatments. The study showed that forests on drained N-rich peat soils may be significant sources of N2O and NO and that their production of nitrogenous trace gases is enhanced by additional N.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call