Oxygen concentrations within forest floor litter were studied at various wa
ter contents and oxygen consumption rates. A micromanipulator moved micro-e
lectrodes (dia 7.5 mu m) downward at a velocity of 2 mu m s(-1). In oxygen
profiles, particles and pores could be identified. The sizes of these parti
cles agreed with particle sizes derived from a thin section of the same for
est floor material. In oxygen profiles, no gradients in concentration occur
red in litter macropores at water contents of 2-3.9 g g(-1) dry weight, whi
ch represented the average range in field water contents. By contrast, stee
p oxygen gradients occurred inside organic particles. Larger organic partic
les in general had lower intraparticle oxygen concentrations, compared to s
maller organic particles and in some particles oxygen was absent (> 250 mu
m dia). These anoxic sites occurred at all water contents (2-3.9 g g(-1) dr
y weight) and oxygen consumption rates (0.4-3.2 mu mol g(-1) h(-1)). The an
oxic organic matter fraction of the forest floor did not significantly incr
ease with water content nor with a stimulated oxygen consumption rate due t
o addition of glucose. The recognition that permanent anoxic sites exist in
litter helps us understand how anaerobic processes, such as denitrificatio
n, may contribute to forest floor N2O production. (C) 1999 Published by Els
evier Science Ltd. All rights reserved.