Overwinter soil nitrogen dynamics in seasonally frozen soils

An overwinter soil-monitoring study was conducted at two sites in southern Ontario. Soluble soil N accumulation at both sites occured in early winter, peaked when soil water was frozen, and then declined during the period tha t frozen soil water was present. The amount of soluble soil N accumulated w as 48 +/- 12 kg N ha(-1) at one site, and 21 +/- 6 kg N ha(-1) at the other . In both cases, the overwinter accumulation approximately doubled the amou nt of soluble N in the soil. Similar trends were observed in both mineral a nd organic N, with 60 to 74% of the accumulation occurring in the organic f orm. No clear correlations between soluble nitrogen dynamics and soil extra ctable organic carbon or soil microbial biomass carbon dynamics were observ ed. Denitrification apparently occurred in shallow soil during the thaw per iod at one-site. Since soil nitrate levels decreased before significant tha wing occurred, leaching was probably not the primary dissipation mechanism. We hypothesize that the soluble N accumulation was due to death and lysis of soil microorganims during freezing and thawing. The presence of soil ice apparently decreased the lethality of the soil enviroment, allowing N diss ipation to occur. Soil N dissipation could be due to gaseous losses, and is likely related to significant N2O fluxes commonly observed during spring t haw.