1995
DOI: 10.1016/1040-6182(95)00012-8
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New evidence on the evolution of the Po-delta coastal plain during the Holocene

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Cited by 100 publications
(63 citation statements)
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“…Lastly, in the Po River Delta the consolidation due to the anthropogenic loads resting on the land surface superposes to the natural consolidation still ongoing. In fact, this zone developed very recently, during the last few centuries, when a sharp increase in the human intervention (i.e., river diversions, construction of artificial channels and dams, land reclamation) significantly increased the river sediment transport and the delta prograded very rapidly, up to 200 m/yr, with a thick prodelta mud deposition [47]. These muds are characterized by a very high compressibility and low permeability, thus consolidation is still ongoing [11].…”
Section: Multi-band Combined Resultsmentioning
confidence: 99%
“…Lastly, in the Po River Delta the consolidation due to the anthropogenic loads resting on the land surface superposes to the natural consolidation still ongoing. In fact, this zone developed very recently, during the last few centuries, when a sharp increase in the human intervention (i.e., river diversions, construction of artificial channels and dams, land reclamation) significantly increased the river sediment transport and the delta prograded very rapidly, up to 200 m/yr, with a thick prodelta mud deposition [47]. These muds are characterized by a very high compressibility and low permeability, thus consolidation is still ongoing [11].…”
Section: Multi-band Combined Resultsmentioning
confidence: 99%
“…In this latter area, the salinity in piezometers PZSV3, PZSV4 and PZSV8 is less than what was measured previously (5 % of mean difference -see Tables 1 and 2). After pumping, the salinity varies with respect to the pre-pumping data; in the northern and central part of the forest the differences are minimal, in the northeastern part (piezometers 16,19,20), the salinity decreases after pumping.…”
Section: Measurements At Bottom Of Piezometersmentioning
confidence: 99%
“…Soils are mostly sandy and their specific characteristics depend on morphology and watertable depth. The area stratigraphy is consists of multiple series of transgressive-regressive deposits [17][18][19][20]. These sediments forming the aquifers are composed of clay layers (aquiclude) stratified with sand layers (Figure 3).…”
Section: Settingmentioning
confidence: 99%
“…From east to west, the major sedimentary units consist of: (i) a wedge of fine-grained (fine sand to silty clays) sediments representative of a shallow marine environment; (ii) littoral sands representative of the foreshore, deep-shore, and the sand dune environments adjacent and inland of the beach. The westernmost portion of the study area is characterized by the presence of clay back-shore lagoon deposits [37,38]. Some continental-type alluvial deposits (clay and silt) overlay the littoral sands and lagoon deposits in the west.…”
Section: Characterization Of the Area Of Interestmentioning
confidence: 99%