DENITRIFICATION AND NITROUS-OXIDE EMISSIONS FROM A BLACK CHERNOZEMIC SOIL DURING SPRING THAW IN ALBERTA

Previous field research in Alberta has suggested that denitrification occurs mostly when soil thaws in the spring, with associated soil wate r saturation. Our objective was to determine if denitrification and N2 O emission in fact take place in cold, thawing soil in the field. Deni trification and N2O flux were measured in two springs and the interven ing summer. Cylinders were placed in soil in November, 1988, and 57 kg N ha(-1) of N-15-labeled KNO3 was added. Soil N-15 mass balance techn ique showed 23 kg N ha(-1) of added-N was lost by 15 May 1989. Gas tra ppings were made (28 March to 29 April) and nearly all of the N2O emis sion (3.5 kg N2O-N ha(-1)) occurred during an 11-d period of thaw. The accumulated N2O flux from 20 June to 31 August was small (0.5 kg N2O- N ha(-1), or less); during that time there were no rainfall events int ense enough to produce water saturated soil. In 1990, N-15-labeled KNO 3 (100 kg N ha(-1)) was applied on 26 March (outset of the thaw) and m ass balance showed 32.7 kg N ha(-1) of added-N was lost by 7 May. A fl ux of 16.3 kg N2O-N ha(-1) occurred largely in a 10-d period during an d immediately after soil thaw. The N2O emitted from soil left a consid erable fraction of the lost N unaccounted for. This unaccounted N was most likely lost as gaseous N other than N2O (e.g., N-2). We conclude that large amounts of soil nitrate may be denitrified, with smaller am ounts emitted as N2O, as the soil thaws and soon thereafter.