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Membrane‐covered platinum electrodes with a tip diameter of 2–8 µ m were used for an amperometric assay of dissolved oxygen in marine sediments. The oxygen profile extended to 3–5‐mm depth in nonilluminated sediment; even at high light intensities and at low temperatures it did not extend below 10‐mm depth in a homogeneous sandy sediment. Oxygen profiles recorded during light‐dark cycles were used to estimate the rates of oxygen production and consumption and also to calculate the apparent diffusion coefficient for oxygen in the sediment. Apparently macrofaunal activity, rather than molecular diffusion and water turbulence, was important for the occasional transport of oxygen into deeper layers and thus for the provision of oxidized conditions (positive redox potential) down to 5–10 cm below the sediment surface.
Revsbech et al. (Thu,) studied this question.