Journal of Marine Science and Engineering (Dec 2022)

A Potential Beach Monitoring Based on Integrated Methods

  • Isabella Lapietra,
  • Stefania Lisco,
  • Luigi Capozzoli,
  • Francesco De Giosa,
  • Giuseppe Mastronuzzi,
  • Daniela Mele,
  • Salvatore Milli,
  • Gerardo Romano,
  • François Sabatier,
  • Giovanni Scardino,
  • Massimo Moretti

DOI
https://doi.org/10.3390/jmse10121949
Journal volume & issue
Vol. 10, no. 12
p. 1949

Abstract

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This study focuses on the analysis of sandy beaches by integrating sedimentological, geomorphological, and geophysical investigations. The beach represents an extremely variable environment where different natural processes act simultaneously with human activities, leading to the gathering of different methodologies of the Earth Sciences to study its evolution in space and time. The aim of this research is to propose a potential procedure for monitoring the morpho-sedimentary processes of sandy beaches by analyzing the textural and compositional characteristics of the sands and quantifying the volumes involved in the coastal dynamics. The study area includes two Apulian sandy beaches (Torre Guaceto and Le Dune beach) that are representative of the coastal dynamics of a large sector of the central/northern Mediterranean Sea involving the southern Adriatic Sea and the northern Ionian Sea. Sedimentological and ecological investigations allowed to describe the textural and compositional characteristics of the beach sands by interpreting their sand provenance and the physical/biological interactions within the beach. The topographic surveys carried out with a Terrestrial Laser Scanner and an Optical Total Station, aimed to quantify the variations of sediment volume over time, whereas the Delft3d software was applied to analyze the effects of the dominant wave motion on the sedimentary dynamics. Lastly, the geophysical techniques which included Sub Bottom Profiler procedures, Ground Penetrating Radar investigation, and resistivity models enabled us to calculate the sand sediment thickness above the bedrock.

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