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Impacts of Ammonium Sulfate Treatment on the Foliar Chemistry of Forest Trees at the Bear Brook Watershed in Maine

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The Bear Brook Watershed in Maine: A Paired Watershed Experiment

Abstract

Foliar chemistry was examined in mature sugar maple (Acer saccharum Marsh), red maple (Acer rubrum L.), American beech (Fagus grandifolia Ehrh.), and red spruce (Picea rubens Sarg.) in response to chronic, watershed-level additions of ammonium sulfate [(NH4)2SO4]. Following four years of treatment, N concentrations were significantly higher in foliage from the treated watershed for all four species, with increases ranging from 6% in American beech to 33% in sugar maple. Sugar maple foliage from the treated watershed had significantly lower Ca concentrations (18%). Concentrations of K were significantly lower in beech (13%) and red spruce (9%) from the treated watershed. Foliar Mg was not different between watersheds. Aluminum concentrations were significantly higher in the foliage from the treated watershed for beech (18%), red maple (33%), and sugar maple (65%), but no differences in Al concentration occurred in current year red spruce foliage. Red spruce foliage resampled following a fifth year of treatment contained higher concentrations of N and Al and lower concentrations of Ca and Mg in the treated watershed. Despite these differences in red spruce foliar chemistry, wood production and density did not appear to be affected by the treatment.

Differences in the foliar chemistry between the treated and untreated watershed may reflect the temporal and spatial integration of changes taking place in the soil of the treated watershed. Increased N is likely directly due to the N contained in the (NH4)2SO4 treatment. Labile Ca and other cations in the treated watershed would be expected to initially increase and then decrease in response to the treatment, with these changes beginning at the top of the forest floor. Thus, lower cation concentrations in foliage from the treated watershed may reflect the fact that cations in the uppermost portions of the soil were rapidly depleted, even though deeper soil layers were experiencing increased Ca release due to cation exchange effect of the acidification. The generally higher Al in foliage from the treated watershed is likely due to the mobilization of inorganic Al in the soil as has been reported previously for the treated watershed. Collectively these results suggest that the long-term deposition of acidifying substances containing N and S not only influence the cycling of N within these systems, but may also alter the cycling of other important nutrients and Al.

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Author notes

  1. G. White

    Present address: Environmental Assessment Technologies, Lockheed Martin Idaho Technologies, Inc., P.O. Box 1626, Idaho Falls, ID, 83415-2213, USA

Authors and Affiliations

  1. Agricultural and Resource Economics, University of Maine, Orono, ME, 04469, USA

    G. White

  2. Dept. Plant, Soil, and Environmental Sciences, University of Maine, Orono, ME, 04469, USA

    I. Fernandez

  3. Dept. of Forest Ecosystem Science, University of Maine, Orono, ME, 04469, USA

    G. Wiersma

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  1. G. White
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  2. I. Fernandez
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  3. G. Wiersma
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Editors and Affiliations

  1. Department of Geological Sciences, University of Maine, Orono, Maine, USA

    Stephen A. Norton

  2. Department of Applied Ecology and Environmental Sciences, University of Maine, Orono, Maine, USA

    Ivan J. Fernandez

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White, G., Fernandez, I., Wiersma, G. (1999). Impacts of Ammonium Sulfate Treatment on the Foliar Chemistry of Forest Trees at the Bear Brook Watershed in Maine. In: Norton, S.A., Fernandez, I.J. (eds) The Bear Brook Watershed in Maine: A Paired Watershed Experiment. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-3241-3_12

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  • DOI: https://doi.org/10.1007/978-94-017-3241-3_12

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  • Print ISBN: 978-90-481-5185-1

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