Characterisation of carbonate lake sediments as a potential filler for polymer composites

The purpose of the study was to determine whether lake sediments could be a potential raw material for the plastics industry. The examined samples were obtained in a complex process of sediment collection from Lake Swarzędzkie located in the region of Wielkopolska, Poland, followed by granulometric...

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Main Authors: Borkowski Grzegorz, Martyła Agnieszka, Dobrosielska Marta, Marciniak Piotr, Głowacka Julia, Pakuła Daria, Gabriel Ewa, Przekop Robert E.
Format: Article
Language:English
Published: De Gruyter 2023-04-01
Series:Green Processing and Synthesis
Subjects:
Online Access:https://doi.org/10.1515/gps-2022-8082
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author Borkowski Grzegorz
Martyła Agnieszka
Dobrosielska Marta
Marciniak Piotr
Głowacka Julia
Pakuła Daria
Gabriel Ewa
Przekop Robert E.
author_facet Borkowski Grzegorz
Martyła Agnieszka
Dobrosielska Marta
Marciniak Piotr
Głowacka Julia
Pakuła Daria
Gabriel Ewa
Przekop Robert E.
author_sort Borkowski Grzegorz
collection DOAJ
description The purpose of the study was to determine whether lake sediments could be a potential raw material for the plastics industry. The examined samples were obtained in a complex process of sediment collection from Lake Swarzędzkie located in the region of Wielkopolska, Poland, followed by granulometric analysis by sieving and quartz grain shape analysis, with preparation of geotechnical sheets. The works involved the examination of physico-chemical characteristics of carbonate lake sediments and the analysis of impact of the sediments’ depth extraction on their chemical composition and physico-chemical properties. The lake sediment consists mainly of calcium carbonate (CaCO3) and can be a potential filler for plastics. Tests were carried out to determine chemical composition of the sediments and their thermal stability. The thermogravimetric analysis showed the three stages of the thermal decomposition. Sediments in deeper layers of the lake are characterised by the presence of not only CaCO3 and silica, but also other chemical compounds, including aluminosilicates. In addition, as the depth increases, the average size of sediment particles changes, with the main fraction particle size being the smallest for the material from the 6–12 m depth. Additionally, carbon content systematically decreases with increasing depth.
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spelling doaj.art-a7482c66391b40a69179b633bff8a25c2023-05-06T15:42:46ZengDe GruyterGreen Processing and Synthesis2191-95502023-04-011217405010.1515/gps-2022-8082Characterisation of carbonate lake sediments as a potential filler for polymer compositesBorkowski Grzegorz0Martyła Agnieszka1Dobrosielska Marta2Marciniak Piotr3Głowacka Julia4Pakuła Daria5Gabriel Ewa6Przekop Robert E.7Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, B. Krygowskiego 10, 61-680 Poznań, PolandCentre for Advanced Technologies, Adam Mickiewicz University in Poznań, ul. Uniwersytetu Poznańskiego 10, 61-614 Poznań, PolandFaculty of Materials Science and Engineering Warsaw University of Technology, ul. Wołoska 141, 02-507 Warsaw, PolandCentre for Advanced Technologies, Adam Mickiewicz University in Poznań, ul. Uniwersytetu Poznańskiego 10, 61-614 Poznań, PolandFaculty of Chemistry, Adam Mickiewicz University in Poznań, 8 Uniwersytetu Poznańskiego, 61-614 Poznań, PolandFaculty of Chemistry, Adam Mickiewicz University in Poznań, 8 Uniwersytetu Poznańskiego, 61-614 Poznań, PolandCentre for Advanced Technologies, Adam Mickiewicz University in Poznań, ul. Uniwersytetu Poznańskiego 10, 61-614 Poznań, PolandCentre for Advanced Technologies, Adam Mickiewicz University in Poznań, ul. Uniwersytetu Poznańskiego 10, 61-614 Poznań, PolandThe purpose of the study was to determine whether lake sediments could be a potential raw material for the plastics industry. The examined samples were obtained in a complex process of sediment collection from Lake Swarzędzkie located in the region of Wielkopolska, Poland, followed by granulometric analysis by sieving and quartz grain shape analysis, with preparation of geotechnical sheets. The works involved the examination of physico-chemical characteristics of carbonate lake sediments and the analysis of impact of the sediments’ depth extraction on their chemical composition and physico-chemical properties. The lake sediment consists mainly of calcium carbonate (CaCO3) and can be a potential filler for plastics. Tests were carried out to determine chemical composition of the sediments and their thermal stability. The thermogravimetric analysis showed the three stages of the thermal decomposition. Sediments in deeper layers of the lake are characterised by the presence of not only CaCO3 and silica, but also other chemical compounds, including aluminosilicates. In addition, as the depth increases, the average size of sediment particles changes, with the main fraction particle size being the smallest for the material from the 6–12 m depth. Additionally, carbon content systematically decreases with increasing depth.https://doi.org/10.1515/gps-2022-8082sedimentsmineral fillersnatural fillerscaco3 calcite
spellingShingle Borkowski Grzegorz
Martyła Agnieszka
Dobrosielska Marta
Marciniak Piotr
Głowacka Julia
Pakuła Daria
Gabriel Ewa
Przekop Robert E.
Characterisation of carbonate lake sediments as a potential filler for polymer composites
Green Processing and Synthesis
sediments
mineral fillers
natural fillers
caco3
calcite
title Characterisation of carbonate lake sediments as a potential filler for polymer composites
title_full Characterisation of carbonate lake sediments as a potential filler for polymer composites
title_fullStr Characterisation of carbonate lake sediments as a potential filler for polymer composites
title_full_unstemmed Characterisation of carbonate lake sediments as a potential filler for polymer composites
title_short Characterisation of carbonate lake sediments as a potential filler for polymer composites
title_sort characterisation of carbonate lake sediments as a potential filler for polymer composites
topic sediments
mineral fillers
natural fillers
caco3
calcite
url https://doi.org/10.1515/gps-2022-8082
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