Integrated classification maps were produced by combining sediment grain-size and hydrological data (water renewal time, WRT) from two Mediterranean lagoons, Lesina (LL) and Varano (LV), Italy. The geophysical characteristics of the two basins, derived from detailed bathymetric charts, are quite distinct: similar to 30% of LL (mean depth similar to 1 m) but only 3% of LV (mean depth similar to 3 m) is shallower than 1 m. The sediments of both lagoons are mainly composed of mud (similar to 80%). A detailed multivariate analysis of grain-size data by Entropy Max classified the lagoon beds of LL and LV into five sedimentary facies. WRT data, computed by a hydrodynamic model, indicated different hydrological conditions in the two lagoons: LL showed a sharp west-east gradient, with a basin-wide average of similar to 190 days, whilst LV showed a fairly uniform distribution and a higher basin-wide average (similar to 260 days). The distribution of sedimentary fades and water renewal times were combined in a composite map representing the distribution of environmental patterns. The approach outlined in this study can be used to improve zonation schemes by providing a hydromorphological perspective on transitional and coastal environments.
Sediment grain size and hydrodynamics in Mediterranean coastal lagoons: Integrated classification of abiotic parameters
Sarretta Alessandro;Ferrarin Christian;Specchiulli Antonietta;Guerzoni Stefano
2014
Abstract
Integrated classification maps were produced by combining sediment grain-size and hydrological data (water renewal time, WRT) from two Mediterranean lagoons, Lesina (LL) and Varano (LV), Italy. The geophysical characteristics of the two basins, derived from detailed bathymetric charts, are quite distinct: similar to 30% of LL (mean depth similar to 1 m) but only 3% of LV (mean depth similar to 3 m) is shallower than 1 m. The sediments of both lagoons are mainly composed of mud (similar to 80%). A detailed multivariate analysis of grain-size data by Entropy Max classified the lagoon beds of LL and LV into five sedimentary facies. WRT data, computed by a hydrodynamic model, indicated different hydrological conditions in the two lagoons: LL showed a sharp west-east gradient, with a basin-wide average of similar to 190 days, whilst LV showed a fairly uniform distribution and a higher basin-wide average (similar to 260 days). The distribution of sedimentary fades and water renewal times were combined in a composite map representing the distribution of environmental patterns. The approach outlined in this study can be used to improve zonation schemes by providing a hydromorphological perspective on transitional and coastal environments.File | Dimensione | Formato | |
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