2012
DOI: 10.1061/(asce)ww.1943-5460.0000156
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Anthropogenic Effects on Coastal Sediment Fluxes in a Nontidal Gulf System

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Cited by 8 publications
(5 citation statements)
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“…8a). Coastal abrasion did not stop here even during massive pulp dumping from the amber factory, which is due to the predominance of along-shore sediment transport to the south, towards Baltiysk (Ostrowski et al 2012, Chubarenko andBabakov 2016). The sand partially transferred to the north is caught by a canyon at the center of Donskaya Bay and carried to the base of the underwater abrasion cliff (Orlenok et al 2004) (see Fig.…”
Section: West Coastmentioning
confidence: 92%
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“…8a). Coastal abrasion did not stop here even during massive pulp dumping from the amber factory, which is due to the predominance of along-shore sediment transport to the south, towards Baltiysk (Ostrowski et al 2012, Chubarenko andBabakov 2016). The sand partially transferred to the north is caught by a canyon at the center of Donskaya Bay and carried to the base of the underwater abrasion cliff (Orlenok et al 2004) (see Fig.…”
Section: West Coastmentioning
confidence: 92%
“…2b). The abrasion rates are maximal for the coast at the south pier, amounting to 0.7-1 m/year (Ostrowski et al 2012) or as much as 1.9 m (Atlas 2016) or 2-3 m/year (Bobykina and Karmanov 2009, Burnashov 2011a) according to various estimates. Judging by the fact that whole bricks from the destroyed fortress were carried to the south and beached, the strong influence of the south pier on the coastal hydro-morphodynamics can be traced over at least 3-4 km to the south.…”
Section: Vistula Spitmentioning
confidence: 99%
“…The views of the supporters of the third variant, who depended the discharge of flows on the Vistula Spit [4], based mostly on the calculations of the resulting fluxes of the wind [6] and wave [12,33,41,45,55] energy derived from wind statistics over periods 1949-1976 and 1958-2001 and, partially, on the analysis of regularities of the alongshore distribution of mineralsindicators [12]. Thus, there is no clear answer to the question regarding the final direction of sediment transport within the Sambian-Vistula arc.…”
Section: Hydrophysical Processesmentioning
confidence: 99%
“…The Vistula Spit (both the abovementioned segment and the spit proper, from its root to the Baltiysk Strait) is built entirely of sandy sediments. Grain sizes are variable along the spit, with the median diameter d 50 = 0.18-0.31 mm south-west of the Baltiysk Strait, d 50 = 0.16-0.23 mm in the region of the Polish-Russian border (Babakov et al 2010) and 0.19-0.24 mm in the remaining (Polish) part of the Vistula Spit (Ostrowski et al 2012). According to our observations, large amounts of sandy sediments in the nearshore zone of the Vistula Spit favour the occurrence of up to three bars.…”
Section: Vistula Spit (Region 1)mentioning
confidence: 99%