Abstract

The distribution and effects on soil chemistry of shrub alders (Alnus spp.) occurring in the understory of the boreal forest of Alaska were examined. Understory alder ramet distribution was mapped on three sites; ramet density ranged from 150 to 5280 ramets/ha. Allometric biomass models were developed for alder ramets; maps of the spatial distribution of ramets and of estimated aboveground alder biomass are presented. Biomass of alders in the understory ranged from 20 to 690 g•m−2. The total nitrogen of soils collected beneath alder and from areas without alder differed among the three sites and between two sampling episodes. In undisturbed forest, alder soils tended to have more nitrogen than nonalder soils. On the two sites where background soil fertility was low, a greenhouse bioassay matched these results: alder soils had greater nutrient-supplying capacity than nonalder soils. In soil collected after the sites were harvested, however, results varied. Areas that had supported dense alder before harvesting had more soil nitrogen than areas with no alder at only one site, and at another site, alder soils had significantly less total nitrogen. This study suggests that the effect of understory alders on the boreal forest soil mosaic is a function of site characteristics such as canopy openness and soil background fertility.

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