Soil moisture deficits can reduce root respiration, but the effects ha
ve yet to be quantified at the stand level or included in models of fo
rest carbon budgets. We studied fine-root (less than or equal to 1.0 m
m diameter) respiration in four sugar maple forests for three growing
seasons in order to assess the combined effects of temperature, N conc
entration, and soil moisture on respiration rates. Fine-root respirati
on at the four sites was exponentially related to soil temperature and
linearly related to root N concentration and soil moisture availabili
ty. Most of the variability in respiration rates was explained by temp
erature. Differences in soil moisture availability explained temporal
variation within sites in respiration rate at a given temperature, whe
reas differences among sites in respiration rates resulted from site-s
pecific differences in fine-root N concentration. Periodic moisture de
ficits during 1995 and 1996 were sufficient to cause declines of up to
17% in total growing-season root respiration at affected sites. Estim
ated reductions in respiration of up to 0.8 Mg C/ha during dry years w
ere equivalent to a significant portion of annual aboveground woody bi
omass C increment, arguing for the inclusion of soil moisture availabi
lity as a predictor of root respiration when modeling C allocation in
forest ecosystems.