Impact of macrozoobenthic structures on near-bed sediment fluxes

• Published in: Journal of marine systems 2009-02, Vol.75 (3), p.336-347
• Main Authors: Friedrichs, M., Leipe, T., Peine, F., Graf, G.
• Format: Article
• Language: English
• Subjects: Benthos; Boundary layer; Deposition; Erosion; Flow; Flume; Marine; Mecklenburg Bight
• ISSN: 0924-7963; 1879-1573
• DOI: 10.1016/j.jmarsys.2006.12.006

Sandy sediments in shallow coastal waters of the Baltic Sea are often characterised by large numbers of biogenic structures which are produced by macrozoobenthos species. A series of experiments was devised to quantify how the interaction of such structures with the near-bed flow regime affects the sediment flux. Most experiments were done with simplified replicates of structures generated by typical species commonly found in the Mecklenburg Bight, starting with solitary structures and regularly-spaced arrays in a range of characteristic population densities, followed by a complex benthic macrofauna community, both artificial and alive. A laboratory flume channel, equipped with an acoustic Doppler flow sensor and a topography scanning laser, was used for high-resolution measurements (2 mm horizontal step size and 0.3 mm vertical resolution) of sand erosion (220 µm median grain size, at 20 cm s − 1 ) and fine particle deposition (8 µm grain size, at 5 cm s − 1 ). Sediment transport threshold values were measured for each layout. As a rule-of-thumb, both the erosion fluxes and the deposition of suspended matter increased considerably at low population densities (below 2%, expressed as percent of the sediment surface covered, i.e. roughness density RD). Above densities of 4%, erosion almost stopped inside the test arrays, and deposition remained well below the level of unpopulated areas. An attempt to extrapolate these findings to field conditions (using field current velocity data from 2001) showed that the net flux switched from erosion to deposition for densities above 5%. These parameters can now be integrated into a numerical sediment transport model coupling waves, currents, sediment dynamics and biological processes, which is currently under construction at the Baltic Sea Research Institute (IOW), Rostock, Germany.