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Dep. of Civil and Environmental Engineering, 151 Link Hall, Syracuse Univ., Syracuse, NY 13244
* Corresponding author (cejohns{at}syr.edu).
We conducted a resurvey of the O horizon in 2001 in watersheds previously sampled in 1984 under the Direct/Delayed Response Program (DDRP) to evaluate the effects of reductions in acidic deposition in the northeastern United States. In this 17-yr interval, median base saturation in the Oa horizon decreased from 56.2% in 1984 to 33.0% in 2001. Effective cation exchange capacity (CECe), normalized to soil C concentration, showed no significant change between 1984 and 2001. The change in base saturation was the result of almost equivalent changes in C-normalized exchangeable Ca (CaN) and exchangeable Al (AlN). The median CaN declined by more than 50%, from 23.5 to 10.6 cmolc kg–1 C, while median AlN more than doubled, from 8.8 to 21.3 cmolc kg–1 C. We observed the greatest change in soil acid–base properties in the montane regions of Central New England (CNE) and Maine, where base saturation decreased by more than 50% and median soil pH in 0.01 M CaCl2 (pHs) decreased from 3.19 to 2.97. Changes in median concentrations of other exchangeable cations were either statistically insignificant (MgN, KN) or very small (NaN). We observed no significant change in the median values of either total soil C content (%C) or total soil N content (%N) over the 17-yr interval. The acidification of the Oa horizon between 1984 and 2001 occurred despite substantial reductions in atmospheric acidic deposition. Our results may help to explain the surprisingly slow rate of recovery of surface waters.
Abbreviations: AlN, exchangeable aluminum normalized to soil carbon concentration ANC, acid neutralizing capacity BBWM, Bear Brook Watershed in Maine CaN, exchangeable calcium normalized to soil carbon concentration CAAA, Clean Air Act Amendments CEC, cation exchange capacity CECe, effective cation exchange capacity CECeN, effective cation exchange capacity normalized to soil carbon concentration CNE, Central New England DDRP, Direct Delayed Response Project KN, exchangeable potassium normalized to soil carbon concentration MgN, exchangeable magnesium normalized to soil carbon concentration NaN, exchangeable sodium normalized to soil carbon concentration pHs, soil pH in 0.01 M calcium chloride (CaCl2) pHw, soil pH in deoinzed water %C, total soil carbon content %N, total soil nitrogen content %BS, soil percent base saturation
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