VÖRÖŠ, Dominik, Daniela ŘIMNÁČOVÁ, Lujza MEDVECKÁ, Eva GERŠLOVÁ a Mercedes DÍAZ-SOMOANO. The impact of saline mine water on fate of mineral elements and organic matter: The case study of the Upper Silesian Coal Basin. Chemosphere. Elsevier, 2021, roč. 284, December, s. 131397-131406. ISSN 0045-6535. Dostupné z: https://dx.doi.org/10.1016/j.chemosphere.2021.131397.
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Základní údaje
Originální název The impact of saline mine water on fate of mineral elements and organic matter: The case study of the Upper Silesian Coal Basin
Autoři VÖRÖŠ, Dominik (garant), Daniela ŘIMNÁČOVÁ, Lujza MEDVECKÁ (703 Slovensko, domácí), Eva GERŠLOVÁ (203 Česká republika) a Mercedes DÍAZ-SOMOANO.
Vydání Chemosphere, Elsevier, 2021, 0045-6535.
Další údaje
Originální jazyk angličtina
Typ výsledku Článek v odborném periodiku
Obor 10505 Geology
Stát vydavatele Velká Británie a Severní Irsko
Utajení není předmětem státního či obchodního tajemství
WWW URL
Impakt faktor Impact factor: 8.943
Kód RIV RIV/00216224:14310/21:00119987
Organizační jednotka Přírodovědecká fakulta
Doi http://dx.doi.org/10.1016/j.chemosphere.2021.131397
UT WoS 000703855900007
Klíčová slova anglicky Sediments; Mine water; Organic matter; Adsorption capacity; Major and trace elements
Příznaky Mezinárodní význam, Recenzováno
Změnil Změnila: doc. Mgr. Eva Geršlová, Ph.D., učo 16745. Změněno: 9. 10. 2023 16:06.
Anotace
The work presented here provides a complex environmental impact of sediments in vicinity to the area of the former Lazy coal mine site in the Upper Silesian Coal Basin (Czech Republic). The main aim of this work has been to determine the degree of contamination, to describe the organic matter, and to carry out sorption isotherms to see the size and distribution of pores in the monitored sediments that are the crucial parameters to assumption of removal mechanisms of elements carried in mine water. The results show that the greatest enrichment of Mn, Sr, Ba, and was in sediments of the first tens of meters from the mine water discharge sediments. Ba and Sr were precipitated as mineral barite and thus formed a dominant insoluble component in the river sediments, which were further carried by water flow towards the water reservoirs. Predominant amounts of fossil material and smaller quantities of carbonized and recent organic matter were altered by weathering and erosion processes. The coal materials have a relatively beneficial sorption capacity, which increases with the carbon content. The overburden waste should be considered for use in removing heavy metals in-situ.
VytisknoutZobrazeno: 28. 4. 2024 12:25