Ecology · 1990 · 304 citations · 23 references
AgricultureEcologySoil SciencesNutrient CyclingSoil ChemistrySoil Organic MatterMicrobial BiogeochemistryNitrogen CycleNitrogen CyclingNitrogen NutritionNutrient ImmobilizationNutrient RetentionMicrobial Biomass NitrogenMicrobial Biomass NutrientsMicrobial ImmobilizationMicrobial Nitrogen ImmobilizationMicrobial Nitrogen TurnoverNitrificationPlant Nitrogen UptakePlant Uptake
Nitrogen (N) uptake by spring ephemeral communities has been proposed as a mechanism that retains N within northern hardwood forests during the season of maximum loss. To understand better the importance of these plants in retaining N, we followed the movement of 1 5 NH 4 + and 1 5 NO 3 — into plant and microbial biomass. Two days following isotope addition, microbial biomass represented the largest labile pool of N and contained 8.5 times as much N as Allium tricoccum L. biomass. Microbial immobilization of 1 5 N was 10—20 times greater than uptake by A. tricoccum. Nitrification of 1 5 NH 4 + was five times lower in cores containing A. tricoccum compared to those without the spring ephemeral. Spring N retention within northern hardwood forests cannot be fully explained by plant uptake because microbial immobilization represented a significantly larger sink for N. Results suggest that plant and microbial uptake of NH 4 + may reduce the quantity of substrate available for nitrification and thereby lessen the potential for NO 3 — loss via denitrification and leaching.
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