THE GEOCHEMICAL DIVERSITY OF LACUSTRINE SEDIMENTS OF THE SUCHEDNIÓW WATER RESERVOIR (ŚWIĘTOKRZYSKIE VOIVODESHIP, POLAND) - PRELIMINARY RESULTS

The research area is located in central Poland, in the Świętokrzyskie Voivodeship (Kielce-Sandomierz Upland). Once heavily industrialized as the former Old Polish Industrial District area, there were many forges and iron furnances developed here. For this purpose, on many rivers of this area the ind...

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Main Authors: Tomasz Kalicki, Rafał Kozłowski, Paweł Przepióra, Mirosław Szwed
Format: Article
Language:English
Published: Geobalcanica Society 2021-07-01
Series:Acta Geobalcanica
Subjects:
Online Access:http://www.geobalcanica.org/wp-content/uploads/AGB/2021/AGB-2021-7-22.pdf
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author Tomasz Kalicki
Rafał Kozłowski
Paweł Przepióra
Mirosław Szwed
author_facet Tomasz Kalicki
Rafał Kozłowski
Paweł Przepióra
Mirosław Szwed
author_sort Tomasz Kalicki
collection DOAJ
description The research area is located in central Poland, in the Świętokrzyskie Voivodeship (Kielce-Sandomierz Upland). Once heavily industrialized as the former Old Polish Industrial District area, there were many forges and iron furnances developed here. For this purpose, on many rivers of this area the industrial ponds were built. They functioned mainly until the collapse of the metallurgical industry and the water mills as well. Built in 1974 on the Kamionka River in Suchedniów, the water reservoir was use for retention and recreational purposes. Since its construction, the reservoir has never been thoroughly dredged. In 2017, large-scale hydrotechnical works on the reservoir began, aimed at its deepening. Draining the Suchedniów water reservoir made it possible to carry out detailed sedimentological and morphological analyzes of its bottom. A large differentiation of the sedimentary environment types in the reservoir basin has been recognized. The collected samples also provided material for geochemical analyzes. The analysis was made for the content of such trace elements as Pb, Cd, Cr, Co, Cu, Mn, Ni, Zn, Sr, As, Al and Fe. The known industrial history of this area and the use of the modern reservoir, allows to attempt explain the content changes in the lacustrine sediments.
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spelling doaj.art-28bcc79cd9b149e8ace857134cd023132023-02-13T22:26:56ZengGeobalcanica SocietyActa Geobalcanica1857-98332021-07-017415916510.18509/AGB217-40159kTHE GEOCHEMICAL DIVERSITY OF LACUSTRINE SEDIMENTS OF THE SUCHEDNIÓW WATER RESERVOIR (ŚWIĘTOKRZYSKIE VOIVODESHIP, POLAND) - PRELIMINARY RESULTSTomasz Kalicki0Rafał Kozłowski1Paweł Przepióra2Mirosław Szwed3Department of Geomorphology and Geoarchaeology, Institute of Geography and Environmental Sciences, Jan Kochanowski University in Kielce, PolandDepartment of Environmental Research and Geoinformation, Institute of Geography and Environmental Sciences, Jan Kochanowski University in Kielce, Poland PolandDepartment of Geomorphology and Geoarchaeology, Institute of Geography and Environmental Sciences, Jan Kochanowski University in Kielce, PolandDepartment of Environmental Research and Geoinformation, Institute of Geography and Environmental Sciences, Jan Kochanowski University in Kielce, Poland PolandThe research area is located in central Poland, in the Świętokrzyskie Voivodeship (Kielce-Sandomierz Upland). Once heavily industrialized as the former Old Polish Industrial District area, there were many forges and iron furnances developed here. For this purpose, on many rivers of this area the industrial ponds were built. They functioned mainly until the collapse of the metallurgical industry and the water mills as well. Built in 1974 on the Kamionka River in Suchedniów, the water reservoir was use for retention and recreational purposes. Since its construction, the reservoir has never been thoroughly dredged. In 2017, large-scale hydrotechnical works on the reservoir began, aimed at its deepening. Draining the Suchedniów water reservoir made it possible to carry out detailed sedimentological and morphological analyzes of its bottom. A large differentiation of the sedimentary environment types in the reservoir basin has been recognized. The collected samples also provided material for geochemical analyzes. The analysis was made for the content of such trace elements as Pb, Cd, Cr, Co, Cu, Mn, Ni, Zn, Sr, As, Al and Fe. The known industrial history of this area and the use of the modern reservoir, allows to attempt explain the content changes in the lacustrine sediments.http://www.geobalcanica.org/wp-content/uploads/AGB/2021/AGB-2021-7-22.pdfsedimentologysuchedniów water reservoirlacustrine sedimentsgeochemical diversityold polish industrail district
spellingShingle Tomasz Kalicki
Rafał Kozłowski
Paweł Przepióra
Mirosław Szwed
THE GEOCHEMICAL DIVERSITY OF LACUSTRINE SEDIMENTS OF THE SUCHEDNIÓW WATER RESERVOIR (ŚWIĘTOKRZYSKIE VOIVODESHIP, POLAND) - PRELIMINARY RESULTS
Acta Geobalcanica
sedimentology
suchedniów water reservoir
lacustrine sediments
geochemical diversity
old polish industrail district
title THE GEOCHEMICAL DIVERSITY OF LACUSTRINE SEDIMENTS OF THE SUCHEDNIÓW WATER RESERVOIR (ŚWIĘTOKRZYSKIE VOIVODESHIP, POLAND) - PRELIMINARY RESULTS
title_full THE GEOCHEMICAL DIVERSITY OF LACUSTRINE SEDIMENTS OF THE SUCHEDNIÓW WATER RESERVOIR (ŚWIĘTOKRZYSKIE VOIVODESHIP, POLAND) - PRELIMINARY RESULTS
title_fullStr THE GEOCHEMICAL DIVERSITY OF LACUSTRINE SEDIMENTS OF THE SUCHEDNIÓW WATER RESERVOIR (ŚWIĘTOKRZYSKIE VOIVODESHIP, POLAND) - PRELIMINARY RESULTS
title_full_unstemmed THE GEOCHEMICAL DIVERSITY OF LACUSTRINE SEDIMENTS OF THE SUCHEDNIÓW WATER RESERVOIR (ŚWIĘTOKRZYSKIE VOIVODESHIP, POLAND) - PRELIMINARY RESULTS
title_short THE GEOCHEMICAL DIVERSITY OF LACUSTRINE SEDIMENTS OF THE SUCHEDNIÓW WATER RESERVOIR (ŚWIĘTOKRZYSKIE VOIVODESHIP, POLAND) - PRELIMINARY RESULTS
title_sort geochemical diversity of lacustrine sediments of the suchedniow water reservoir swietokrzyskie voivodeship poland preliminary results
topic sedimentology
suchedniów water reservoir
lacustrine sediments
geochemical diversity
old polish industrail district
url http://www.geobalcanica.org/wp-content/uploads/AGB/2021/AGB-2021-7-22.pdf
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