FN Archimer Export Format PT J TI Suspended sediment concentration field quantified from a calibrated MultiBeam EchoSounder BT AF Fromant, Guillaume Le Dantec, Nicolas Perrot, Yannick Floc'h, France Lebourges-Dhaussy, Anne Delacourt, Christophe AS 1:1,2;2:1,3;3:4;4:1;5:4;6:1; FF 1:;2:;3:;4:;5:;6:; C1 Institut Universitaire Européen de la Mer, Laboratoire Géosciences Océan – UMR 6538, Rue Dumont d’Urville, 29280 Plouzané, France Laboratoire d'Informatique Signal et Image de la Côte d'Opale, 50, rue Ferdinand Buisson, 62228, Calais, France Centre d’Etudes et d’expertise sur les Risques, l’Environnement, la Mobilité et l’Aménagement, DTecEMF, 134 Rue de Beauvais, 60280 Margny-lès-Compiègne, France Institut de la Rechercher pour le Développement, Laboratoire de l’Environnement MARin - UMR 6539, Pointe du Diable, 29280 Plouzané, France C2 UBO, FRANCE UNIV LITTORAL COTE D'OPALE, FRANCE DTECEMF, FRANCE IRD, FRANCE UM LEMAR LGO IN WOS Cotutelle UMR copubli-france copubli-univ-france IF 3.614 TC 9 UR https://archimer.ifremer.fr/doc/00690/80251/83331.pdf LA English DT Article BO Albert Lucas DE ;Acoustic backscattering;Multifrequency acoustics;Suspended sediments concentration;Acoustic inversion;MultiBeam EchoSounder AB Acoustic scattering can be used to estimate Suspended Sediment Concentration (SSC) through acoustic inversion methods. Current SSC quantification methods are mostly unable to observe both spatial and temporal variations. Here, we assess the possibility to measure both using a Multibeam Echosounder (MBES). MBES combine a large spatial covering in the water column and the capability to measure ‘on route’, allowing a better representativity of the measurements. Time-series of raw EM3002-MBES data at 300 kHz were acquired during a 5-hours field experiment at a fixed location in the Aulne macrotidal estuary (France) during ebb, ensuring sufficient SSC variations. Concurrently, 4-frequencies Acoustic Backscattering System (ABS) profiles were acquired in the water column, as well as turbidity profiles, further converted into SSC using collected water samples. An original in-situ calibration was performed on the MBES, using a tungsten sphere of known properties, which allowed corrections to be made to the volume backscattered levels over the echosounder fan. Using ABS-derived equivalent radii, the MBES backscattered signal was inverted to retrieve an SSC estimate. Good consistency between MBES time-series observations and turbidity-derived SSC is observed. This experiment demonstrates the potential use of MBES for 3-dimensional turbidity observations in coastal areas, which is of great interest for sediment flux quantification. PY 2021 PD SEP SO Applied Acoustics SN 0003-682X PU Elsevier BV VL 180 UT 000655494800043 DI 10.1016/j.apacoust.2021.108107 ID 80251 ER EF