To cite this version:Sabrina Lucas, Frédéric Moulin, Katell Guizien. Oscillating grid mesocosm for studying oxygen dynamics under controlled unsteady turbulence. Limnology and Oceanography : methods, 2016, 14 (1), pp. 1-13. 10.1002/lom3.10064. hal-01281737 Oscillating grid mesocosm for studying oxygen dynamics under controlled unsteady turbulence
AbstractIn shallow environments, common unsteady flows, such as tides, waves or wind-driven currents modulate the diffusive boundary layer thickness that controls the exchange of electron acceptors for mineralization and oxidation processes in surficial sediment. This study demonstrated the ability of an oscillating grid mesocosm to (1) produce homogenous turbulence at the sediment-water interface of multiple sediment cores (between-core variability < within core variability; 16% on average); (2) simulate diffusive boundary layer thickness dynamics on different timescales by easy control of turbulence intensity and (3) study transient oxygen dynamics of organic matter mineralization under varying turbulent conditions. The relationship between turbulence intensity and oxygen diffusive boundary layer thickness, and oxygen penetration depth in the sediment was investigated with different organic matter enrichments and sediment permeability. Oxygen diffusive boundary layer thickness decreased linearly as U RMS increased. Oxygen penetration depth increased with turbulence intensity, and converging to an upper limit with a larger value for low (3.28 mm 6 5.8%) than for high (1.77 mm 6 11.8%) organic matter content in muddy sediment. In sandy sediment, advective flows and resuspension led to a continuous increase of oxygen penetration depth with turbulence intensity, up to 13.2 mm 6 19% for turbulent velocities of 9.6 cm s
21. This mesocosm device will enable the experimental study of microbial dynamics under transient oxygen dynamics, to improve early diagenesis modeling under unsteady flows.In shallow waters (rivers, coastal zones, or lagoons), organic matter (OM) accumulates in bed sediment after passing through the water column from the photic zone or watersheds. Particulate organic material falling at the sediment-water interface (SWI) modifies the chemical composition of the sediment and evolves during the so-called "early diagenesis." This process controls the biogeochemical cycle of carbon and others elements, such as nitrogen and sulfur (Froelich et al. 1979) through various biological (bioturbation and bacterial activity) and chemical (oxidation, precipitation) processes (Aller 1994). Moreover, this particulate OM mineralization contributes to the supply of carbon, nutrients and energy necessary for the metabolism of benthic organisms. Thus, the rate of degradation of OM in sediment is a key end-member for the carbon balance of the planet, because sedimentation rates greater than mineralization rates lead to a net sink of carbon through the storage of OM in impermeable sediments (Aller et al. 1996).OM mineralization occurs mainly in surficial sediment, where it ...