Rg. Kuperman, Litter decomposition and nutrient dynamics in oak-hickory forests along a historic gradient of nitrogen and sulfur deposition, SOIL BIOL B, 31(2), 1999, pp. 237-244
White oak (Quercus alba L.) leaf litter decomposition rates and patterns of
N, S and P immobilization and release in decomposing litter were quantifie
d in oak-hickory forests in the Ohio river valley along a long-term (severa
l decades) bulk atmospheric deposition gradient from Illinois, Indiana to O
hio. Historical data on deposition patterns between 1956-1985 showed that 3
0-y cumulative annual total (wet + dry) SO4-S concentrations were 19.9, 20.
8 and 23.9 kg ha(-1) y(-1) and total (wet + dry) N concentrations were 5.99
, 6.57 and 7.50 kg ha(-1) y(-1) in Illinois, Indiana and Ohio, respectively
. In 1988-1989, amounts of total dry N deposition in Illinois, Indiana and
Ohio were, respectively 2.71, 3.21, and 3.88 kg ha(-1) y(-1). Annual decay
rates based on 19 months of decomposition data increased (p < 0.05) with in
creased N deposition and were -0.294, -0.480, and -0.720, respectively. The
decay rates correlated highly with both the total N concentration in the f
orest floor (r(2) = 0.869, p < 0.0001) and the amount of total dry N deposi
tion (r(2) = 0.999, p = 0.007). Nitrogen mineralization from the litter was
highest in Ohio and lowest in Illinois. Immobilization of S and P occurred
only in Illinois. Litter at both the Ohio and Indiana sites showed a net m
ineralization of S and P but the rates were higher in Ohio. The results of
the study suggest that atmospheric N inputs can affect litter decomposition
and nutrient mineralization in oak-hickory forests in the lower Midwestern
United States. (C) 1998 Elsevier Science Ltd. All rights reserved.