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Boundary layer flows, interacting with roughness elements at the sediment surface, alter the small-scale flow reglme. Consequently, pressure d~fferences are generated that are the drivlng forces for advective pore-water flow. We ~nvestigated topography-induced transport of oxygen in a permeable coastal sediment from the Mediterranean Sea (Isola del Giglio, Italy). The sediment surface was characterized by a high abundance (120 m-2) of sediment mounds (average height: 4 cm) built by the mud shrimp Callianassa truncata (Decapoda, Thalassinidea). Boundary layer flow velocities recorded in situ ranged between 2 and 16 cm S-' Detailed experiments were performed in a recirculating laboratory flow channel A natural sediment core, 20 cm deep with a surface area of 0 3 m" was exposed to a unidirectional flow of varying current velocity (3, 6, 10 cm S S ' ) . The alteration of the small-scale flow reglme a t a sediment mound was documented by vertical velocity profiles measured in 1 mm resolution with temperature-compensated thermistor probes. Oxygen distribution in the sediment was investigated with Clark-type microelectrodes. At a smooth surface, oxygen penetration depth in the permeable sediment did not exceed 4 mm, independent of flow velocity. In contrast, the topography-induced advective oxygen transport increased significantly with current speed. Oxygen reached down to almost 40 mm at the upstream foot of a 1 cm high sediment mound at a flow velocity of 10 cm S-' Thus, the oxic sediment volume increased locally by a factor of 4.8 compared to the oxic zone underneath a smooth surface. At a natural abundance of 120 mounds m-? the oxic sediment volume per mZ seabed was calculated to be 3.3-fold higher than in a seabed with a smooth surface. In a parallel experiment, advective solute transport was also demonstrated in a less permeable sediment (k = 5 r 10-12 m') from the North Sea intertidal flat. Due to the lower permeability the effect on O2 transport was less than in the Mediterranean sand, but oxygen penetration depth increased locally 2-fold a t a sediment mound under a flow velocity of 10 cm S-' The experiments showed the high spatial and temporal variability of oxygen distnbution in a coastal seabed depending on sediment surface topography, boundary layer flow velocities and sediment permeability.
Ziebis et al. (1996) studied this question.