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Sound Velocity in a Thin Shallowly Submerged Terrestrial-Marine Quaternary Succession (Northern Adriatic Sea)

Geological Survey of Slovenia, Dimičeva ulica 14, 1000 Ljubljana, Slovenia
Department of Geology, University of Ljubljana, Faculty of Natural Sciences and Engineering, Aškerčeva 12, 1000 Ljubljana, Slovenia
Sirio d.o.o., Kvedrova cesta 16, 6000 Koper, Slovenia
Author to whom correspondence should be addressed.
Water 2020, 12(2), 560;
Received: 30 December 2019 / Revised: 14 February 2020 / Accepted: 15 February 2020 / Published: 18 February 2020
(This article belongs to the Special Issue Landscapes and Landforms of Terrestrial and Marine Areas)
Estimating sound velocity in seabed sediment of shallow near-shore areas submerged after the Last Glacial Maximum is often difficult due to the heterogeneous sedimentary composition resulting from sea-level changes affecting the sedimentary environments. The complex sedimentary architecture and heterogeneity greatly impact lateral and horizontal velocity variations. Existing sound velocity studies are mainly focused on the surficial parts of the seabed sediments, whereas the deeper and often more heterogeneous sections are usually neglected. We present an example of a submerged alluvial plain in the northern Adriatic where we were able to investigate the entire Quaternary sedimentary succession from the seafloor down to the sediment base on the bedrock. We used an extensive dataset of vintage borehole litho-sedimentological descriptions covering the entire thickness of the Quaternary sedimentary succession. We correlated the dataset with sub-bottom sonar profiles in order to determine the average sound velocities through various sediment types. The sound velocities of clay-dominated successions average around 1530 m/s, while the values of silt-dominated successions extend between 1550 and 1590 m/s. The maximum sound velocity of approximately 1730 m/s was determined at a location containing sandy sediment, while the minimum sound velocity of approximately 1250 m/s was calculated for gas-charged sediments. We show that, in shallow areas with thin Quaternary successions, the main factor influencing average sound velocity is the predominant sediment type (i.e. grain size), whereas the overburden influence is negligible. Where present in the sedimentary column, gas substantially reduces sound velocity. Our work provides a reference for sound velocities in submerged, thin (less than 20 m thick), terrestrial-marine Quaternary successions located in shallow (a few tens of meters deep) near-shore settings, which represent a large part of the present-day coastal environments. View Full-Text
Keywords: sound velocity; Quaternary sediment; submerged alluvial plain sound velocity; Quaternary sediment; submerged alluvial plain
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MDPI and ACS Style

Novak, A.; Šmuc, A.; Poglajen, S.; Celarc, B.; Vrabec, M. Sound Velocity in a Thin Shallowly Submerged Terrestrial-Marine Quaternary Succession (Northern Adriatic Sea). Water 2020, 12, 560.

AMA Style

Novak A, Šmuc A, Poglajen S, Celarc B, Vrabec M. Sound Velocity in a Thin Shallowly Submerged Terrestrial-Marine Quaternary Succession (Northern Adriatic Sea). Water. 2020; 12(2):560.

Chicago/Turabian Style

Novak, Ana, Andrej Šmuc, Sašo Poglajen, Bogomir Celarc, and Marko Vrabec. 2020. "Sound Velocity in a Thin Shallowly Submerged Terrestrial-Marine Quaternary Succession (Northern Adriatic Sea)" Water 12, no. 2: 560.

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