The watershed of Big Hurricane Branch, Coweeta Hydrologic Laboratory, North
Carolina, USA, was logged in 1976. We measured breakdown rates of experime
ntal leaf packs in this second-order stream prior to logging, during loggin
g, soon after logging, and 3 additional times since then. Leaf breakdown wa
s slow just after logging, apparently due to leaf burial by sediments. Ther
eafter, leaf breakdown rates have been consistently faster than before logg
ing and faster than in a reference stream. These differences may be related
to 3 factors. First, the post-logging nitrate concentration has been about
3-10 times higher than pre-logging values in Big Hurricane Branch and 5 ti
mes higher than in a reference stream. The high nutrient concentration may
be stimulating microbial decomposition processes in leaf packs. Second, dom
inance of litterfall by "medium" and "fast" processing leaves from the reco
vering forest coupled with relatively high sediment loads during storms may
hasten breakdown through physical abrasion. Third, the interaction of high
nutrients and high quality leaves may be attractive to leaf-shredding inve
rtebrates whose feeding activities may also hasten the breakdown rates.