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Inproceedings Reference Influence of shells and shell debris on backscatter strength: investigation using modeling, sonar measurements and sampling on the Belgian Continental Shelf
Acoustic interaction theory and observation highlight the strong relation between the acoustic signal responses and the physical and biological processes acting on the seafloor and in the water column. Several descriptors such as sediment texture, porosity and surface roughness are identified as the main factors affecting the acoustic reverberation and backscatter signals. Shells can influence if not dominate the scattering on the seafloor(Jackson et al., 1986; Stanic et al., 1989 and Zhang, 1996). Scattering from both inclusions and partially buried shells on the sea-floor is described by Stanton (2000), and scattering from shells as a potential mechanism explaining the scattering above 200 kHz is highlighted by Ivakin (2009). In order to improve the knowledge on this matter, several institutions with different expertise are cooperating to integrate mathematical modeling and experimental results to better quantify the influence of shells and shell debris on the acoustic signal and scattering of sonar images. Mathematical 3D models of shell objects in a sediment matrix will be used to simulate the influence of the shells on acoustic signal and scattering. The physical arrangements of shells and their spatio-temporal population trends are also considered in the modeling. The models will be supported by direct sonar measurements of seafloor areas on the Belgian Continental Shelf, combined with sampling, visual observations, classification and shape analysis of the shells and shell debris.
Located in Library / RBINS Staff Publications
Inproceedings Reference A proposal for a Devonian- Carboniferous boundary based on the Hangenberg extinction event, as suggested by the transition in the Namur-Dinant Basin (Southern Belgium).
Located in Library / RBINS Staff Publications
Inproceedings Reference The orbitally forced sequences of the Lower Tournaisian (Hastarian Substage) of Belgium: Climate reconstruction and time calibration.
Located in Library / RBINS Staff Publications
Inproceedings Reference IGCP 596– SDS Symposium, Brussels (September 20-22, 2015), Abstracts.
Located in Library / RBINS Staff Publications
Proceedings Reference IGCP 596– SDS Symposium, Brussels (September 20-22, 2015), Abstracts.
Located in Library / RBINS Staff Publications
Proceedings Reference IGCP 596-SDS Symposium, Field Guides: The Devonian and Lower Carboniferous successions in southern Belgium.
Located in Library / RBINS Staff Publications
Inproceedings Reference The Famennian succession: marine, continental and reefal facies in the Dinant Synclinorium and Vesdre area.
Located in Library / RBINS Staff Publications
Inproceedings Reference The Middle Devonian succession in the Dinant Synclinorium.
Located in Library / RBINS Staff Publications
Inproceedings Reference The Devonian– Carboniferous boundary and the Lower Carboniferous succession in the type area.
Located in Library / RBINS Staff Publications
Proceedings Reference Syntectonic emplacement of an Alkaline Massif in Burundi: consequences on fluid-rock interaction and element (REE, HFSE) mobility
Located in Library / RBINS Staff Publications