Application of leaf, soil, and tree ring chemistry to determine the nutritional status of sugar maple on sites of different levels of decline

Abstract

Nutrient concentrations and D.R.I.S. indices of leaves, soil chemistry and dendrochronological changes of elemental concentrations in sugar maple (Acer saccharum Marsh.) were used to determine its nutritional status on three sites of contrasting levels of decline. We hypothesized that the ratio of Al to base cations in tree rings would increase more at the most severely declining site, and that the ratios of K+ to divalent cations (Ca2+ and Mg2+) would increase slower or decrease more rapidly over time than at the less severely declining sites. Forest health, based on percentage of foliage missing, and leaf K and Mg concentrations of the three sites were ranked as follows: Morgan Arboretum > Saint-Hippolyte > Entrelacs. Soil pH, Ca, Mg, E.C.E.C. and percentage of base saturation were highest at the Morgan Arboretum, and exchangeable Al in the organic horizon was highest at Entrelacs. Concentrations of K, Ca, Mg and Al, and ratios of these elements in wood were determined for each of the following periods: 1940–1956, 1957–1973 and 1974–1989. Variations in tree ring chemistry among sites were significant for K and Al and all elemental ratios except K:Mg. Al concentration and the ratios of Al to base cations in wood were all significantly higher at Entrelacs (7.0 vs 2.6 and 2.8 mg Al kg−1 for the other two sites, respectively). Weak relationships were generally observed between leaf and soil elemental concentrations, and wood elemental concentrations. The D.R.I.S. K index and soil exchangeable K and Al showed good concordance with wood concentrations. With the exception of Mg, Al and Al:Mg, the effect of period was significant for all other elements and ratios of elements. The most severely declining stand (Entrelacs) differed from the healthiest stand by decreasing K:Ca and increasing A1:K from the 1940–1956 to the 1957–1973 period.