Characteristics of Sediments in a Changing Environmental Conditions in Vistula Lagoon (Poland)

Abstract

The Vistula Lagoon has been evolving since its formation in the late Atlantic period. At the beginning, the changes were mainly driven by the stabilization of the Baltic Sea level, and the development of hydrographic network. Later on, anthropogenic activities have become an important factor. Hydrotechnical works conducted at the turn of the 20th century, aimed at regulating the outflow of the Vistula River waters, have significantly limited the riverine input into the lagoon. In the past, the Vistula Lagoon contained freshwater and was constantly filing with sediments that made the basin shallow. With time, the lagoon has filled with brackish water, while its area became subjected to strong interactions between the driving forces of marine and terrestrial origin. As a result, the regime of sedimentation processes in the lagoon have been changed. The interpretation of sedimentation conditions for clastic sediments was based on the analysis of grain-size parameters that had been determined on the samples of bottom sediments and suspension collected in November 2016. The obtained results were compared to the pertinent data on bottom sediments collected by the Polish Geological Institute National Research Institute in 1994. Significant contrasts in particle size distributions were found. Also, the conducted study allowed the determination of underlying causes of these changes. Due to the shallow depth of the Vistula Lagoon, the sedimentation processes in this basin are significantly influenced by resuspension phenomenon. Resuspension is responsible for the differentiation and redistribution of sediment that originates from various sources, on the bottom of the basin. The process takes place in shallower areas, but this study indicates that its effectiveness increases in the deeper areas of the lagoon, which manifests itself in the replacement of clayey silt with silt. In connection with the plans of the Polish side of the cross-cutting of the Vistula Spit, the sedimentation conditions of Vistula Lagoon will be changed.

Spatial Distribution of Heavy Metals in Bottom Sediments of the Kaliningrad Bay

“…Это можно объяснить особенностями современной седиментации, для которой характерны активные процессы ресуспензии, являющиеся мощным механизмом самоочищения донных осадков [11]. При взмучивании сорбированные подвижные формы тяжелых металлов и иные поллютанты частично опять переходят из осадков в воду, частично с илистыми частицами выносятся в море [12,13].…”

Revista de la Universidad del Zulia, Volumen 12, Número 33

“…In (Chubarenko 1994), it is shown that resuspension can cover from 40 to 100% of the lagoon water area. The sedimentary material entering the lagoon is not fixed at the bottom immediately; it is repeatedly agitated with the resedimentation of bottom sediments and the partial removal of small fractions through the strait into the sea (Blazhchishin 1999;Szymczak 2019;Chechko 2017;Cieśliński 2013;Chechko V. 2008). In genetic terms, terrigenous sedimentary formations with a large range of dimensions -boulders, gravel, pebbles, mixed-grained sands, siltstones, and silt-pelitic silts are common on the bottom surface of the Vistula Lagoon (Chechko & Blazchishin 2002; Uścinowicz & Zachowicz 1966).…”

“…In the works devoted to studying the bottom sediments of the Vistula Lagoon, the primary attention was focused, as a rule, on their upper (0-10 cm) layer. The features of the spatial distribution of the main types of sediments on the bottom surface, their granulometric fractions, and the dynamics of the surface layer of bottom sediments were revealed (Szymczak 2019;Chechko 2017). However, the vertical structure of the sedimentary strata has been studied very poorly.…”

Evolution of sedimentation in the Vistula Lagoon of the Baltic Sea due to anthropogenic impact

“…1-points for measuring the thickness of silt deposits using a geologist's drill; 2-sediment core sampling points; 3-Baltic strait; 4position of the Polish-Russian border In the works devoted to studying the bottom sediments of the Vistula Lagoon, the primary attention was focused, as a rule, on their upper (0-10 cm) layer. The features of the spatial distribution of the main types of sediments on the bottom surface, their granulometric fractions, and the dynamics of the surface layer of bottom sediments were revealed (Szymczak 2019;Chechko 2017). However, the vertical structure of the sedimentary strata has been studied very poorly.…”