Abstract

AbstractThe chemical stability of weekly and biweekly throughfall collection intervals were compared at two northern hardwood stands in the Great Lakes region. Throughfall concentrations of Cl−, NO−3, SO2−4, Ca2+, Mg2+, and K+ were not significantly (p ≤ 0.05) affected by the increased collection time, where as throughfall concentrations of NH+4 and H+ collected biweekly were significantly different (p ≤ 0.05) than concentrations of these ions in weekly samples. The 1‐wk increase in collection interval at one stand decreased concentrations of NH+4 and increased concentrations of H+ 88 and 131%, respectively. The chemical instability of these ions appeared to be related to biological assimilation and/or nitrification of NH+4. Stability of these ions decreased with increasing concentrations of inorganic N in the throughfall. These changes in concentrations of NH+4 and H+ may introduce sampling bias when estimating throughfall fluxes or concentrations of these ions from biweekly collections. The decreased stability of these ions with increased concentrations of inorganic N should be an important consideration when selecting sampling intervals for stands that receive differing deposition levels of atmospheric N or have different canopy retention rates of N.

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