Chapter 7 Sediment Transport Processes in Coastal Lagoons
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Cited by (33)
Hydromorphodynamics modeling of dredging and dumping activities in Mirim lagoon, RS, Brazil
2023, Ocean EngineeringLarge chocked lagoon as a barrier for river–sea flux of dissolved pollutants: Case study of the Azov Sea and the Black Sea
2023, Marine Pollution BulletinEvolution of ancient harbours in deltaic contexts: A geoarchaeological typology
2019, Earth-Science ReviewsCitation Excerpt :Today, lagoons constitute around 6400 km2 of the Mediterranean coastline (Cataudella et al., 2015), but their surface areas were even more significant in Antiquity. In fact, due to base-level sedimentary inputs, most have been totally or partially infilled (Boyd et al., 1992; Oertel et al., 1992; Nichols and Boon, 1994; Duck and Figueiredo da Silva, 2012). This phenomenon is particularly evident on the Kuban Delta where various authors have reconstructed the transformation of the former Taman archipelago into a peninsula, shaped by the progressive infilling of the former Bosphorus channels linking the Black and the Azov Seas (Brückner et al., 2010; Kelterbaum et al., 2011; Fouache et al., 2012; Giaime et al., 2014 and Giaime et al., 2016; Fig. 13).
Storm impacts on hydrodynamics and suspended-sediment fluxes in a microtidal back-barrier estuary
2018, Marine GeologyCitation Excerpt :Coastal lagoons tend to trap inorganic sediment and organic matter (Kjerfve, 1994) but are not necessarily passive features destined to infill with sediment (Nichols and Boon, 1994). Sediment delivered to back-barrier estuaries is generally a combination of riverine input, shoreline erosion, overwash or aeolian transport from barrier islands, and delivery from the coastal ocean (Nichols and Allen, 1981); reworking of sediment on the lagoon seabed can also be considerable (Nichols and Boon, 1994). Understanding how sediment fluxes can both modify and be controlled by local and regional morphology can lead to greater insight to how these systems evolve and how they may change in the face of changing sediment supply, connectivity with the ocean, and rising sea level.
Evolution of Çolpan barrier and lagoon complex (Lake Van-Turkey): Sedimentological and hydrological approach
2018, Quaternary InternationalCitation Excerpt :But fresh water input to Çolpan lagoon may be explained either ground-water recharge and/or the rainfall due to the lack of fluvial feeder system. Sediment infill, water level fluctuations, tectonism, and human impact are the most common elements affected to the evolution of the coastal barriers and lagoons (Boyd et al., 1992; Nichols and Boon, 1994). Especially the water level fluctuations have leading role to changing of shore profile and coastal processes on the closed basin water bodies as Caspian Sea, Lake Baikal, Lake Urmia or Lake Van (Degens et al., 1978; Ignatov et al., 1993; Urabe et al., 2004; Tourian et al., 2015).