Bedload transport in the Vistula River mouth derived from dune migration rates, southern Baltic Sea

Summary: In this paper, bedload sediment transport to the Baltic Sea in the main Vistula River mouth (Przekop Wisły) is estimated. For the first time in this area, investigations were performed based on the non-invasive measurement techniques with the using of hydroacoustic tools. Repeated bathymetr...

Full description

Bibliographic Details
Main Authors: Aliaksandr Lisimenka, Adam Kubicki
Format: Article
Language:English
Published: Elsevier 2019-07-01
Series:Oceanologia
Online Access:http://www.sciencedirect.com/science/article/pii/S0078323419300247
id doaj-a2cf7086f66f46e6bf40867bd22c6a28
record_format Article
spelling doaj-a2cf7086f66f46e6bf40867bd22c6a282020-11-25T00:52:24ZengElsevierOceanologia0078-32342019-07-01613384394Bedload transport in the Vistula River mouth derived from dune migration rates, southern Baltic SeaAliaksandr Lisimenka0Adam Kubicki1Maritime Institute in Gdańsk, Gdańsk, Poland; Institute of Oceanology, Polish Academy of Sciences, Sopot, Poland; Corresponding author at: Maritime Institute in Gdańsk, Dlugi Targ 41/42, 80-830, Gdańsk, Poland. Tel.: (+48 58) 301-16-41; fax: (+48 58) 301-35-13.GEO Ingenieurservice Nord-West, Wilhelmshaven, GermanySummary: In this paper, bedload sediment transport to the Baltic Sea in the main Vistula River mouth (Przekop Wisły) is estimated. For the first time in this area, investigations were performed based on the non-invasive measurement techniques with the using of hydroacoustic tools. Repeated bathymetric surveys were carried out using a multibeam echosounder for the period with hydrological conditions close to that of the long-term mean annual water discharge. Quantification of the bedload transport, as a main factor for the subaqueous Vistula delta development, involved applying the bedform tracking technique, and estimating the dune celerity by analysing the cross-correlation functions of bed elevation profiles (BEPs). The BEPs were obtained along two transects of 500 m in length situated in two different morphological parts of the river mouth – in the “shallow” and in the “deep” sites located upstream and downstream of the submerged sandbar, respectively. Contrarily to previous observations, the bedload transport was found to take place constantly. Moreover, a significant difference in a character of dune migration between the two sites of the investigated area was determined. The “shallow” dunes migrate 7 times faster (0.022 m/h) than the “deep” ones (0.003 m/h). Estimation of the daily bedload transport towards the Baltic Sea revealed values about 40.9 t/day and 8.4 t/day for “shallow” and “deep” sites, respectively. This result can probably indicate that a significant portion of sediments (ca. 80%) transported by the river during average hydrological conditions is deposited temporarily on the submerged sandbar, causing its growth. Keywords: Sand dune migration, Bedload transport, Vistula River mouthhttp://www.sciencedirect.com/science/article/pii/S0078323419300247
collection DOAJ
language English
format Article
sources DOAJ
author Aliaksandr Lisimenka
Adam Kubicki
spellingShingle Aliaksandr Lisimenka
Adam Kubicki
Bedload transport in the Vistula River mouth derived from dune migration rates, southern Baltic Sea
Oceanologia
author_facet Aliaksandr Lisimenka
Adam Kubicki
author_sort Aliaksandr Lisimenka
title Bedload transport in the Vistula River mouth derived from dune migration rates, southern Baltic Sea
title_short Bedload transport in the Vistula River mouth derived from dune migration rates, southern Baltic Sea
title_full Bedload transport in the Vistula River mouth derived from dune migration rates, southern Baltic Sea
title_fullStr Bedload transport in the Vistula River mouth derived from dune migration rates, southern Baltic Sea
title_full_unstemmed Bedload transport in the Vistula River mouth derived from dune migration rates, southern Baltic Sea
title_sort bedload transport in the vistula river mouth derived from dune migration rates, southern baltic sea
publisher Elsevier
series Oceanologia
issn 0078-3234
publishDate 2019-07-01
description Summary: In this paper, bedload sediment transport to the Baltic Sea in the main Vistula River mouth (Przekop Wisły) is estimated. For the first time in this area, investigations were performed based on the non-invasive measurement techniques with the using of hydroacoustic tools. Repeated bathymetric surveys were carried out using a multibeam echosounder for the period with hydrological conditions close to that of the long-term mean annual water discharge. Quantification of the bedload transport, as a main factor for the subaqueous Vistula delta development, involved applying the bedform tracking technique, and estimating the dune celerity by analysing the cross-correlation functions of bed elevation profiles (BEPs). The BEPs were obtained along two transects of 500 m in length situated in two different morphological parts of the river mouth – in the “shallow” and in the “deep” sites located upstream and downstream of the submerged sandbar, respectively. Contrarily to previous observations, the bedload transport was found to take place constantly. Moreover, a significant difference in a character of dune migration between the two sites of the investigated area was determined. The “shallow” dunes migrate 7 times faster (0.022 m/h) than the “deep” ones (0.003 m/h). Estimation of the daily bedload transport towards the Baltic Sea revealed values about 40.9 t/day and 8.4 t/day for “shallow” and “deep” sites, respectively. This result can probably indicate that a significant portion of sediments (ca. 80%) transported by the river during average hydrological conditions is deposited temporarily on the submerged sandbar, causing its growth. Keywords: Sand dune migration, Bedload transport, Vistula River mouth
url http://www.sciencedirect.com/science/article/pii/S0078323419300247
work_keys_str_mv AT aliaksandrlisimenka bedloadtransportinthevistularivermouthderivedfromdunemigrationratessouthernbalticsea
AT adamkubicki bedloadtransportinthevistularivermouthderivedfromdunemigrationratessouthernbalticsea
_version_ 1725242471369146368