Monika Szczuka

Ms. Monika Szczuka

Department of General Geology and Geotourism, Faculty of Geology, Geophysics and Environmental Protection, AGH
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Research Focus & Metrics

Academic Career Length

16Years (2011-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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20 November 2020 in Minerals
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Journal Article
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RWRafał Warchulski
Rafał Warchulski
MSMonika Szczuka
Monika Szczuka
KKKrzysztof Kupczak
Krzysztof Kupczak
The study focuses on the reconstruction of the technological process in the 16th–17th century lead smelter in Sławków based on chemical and petrographic analyzes of slags. There are three main types of material at the landfill: glassy, crystalline, and weathered. Glassy slags are made of amorphous phase in which crystals of pyroxene, willemite, olivine, wüstite, and lead oxide appear. Crystalline slags are composed of wollastonite, rankinite, melilite, anorthite, quartz, and Fe oxides. Weathered slags have a composition similar to glassy slags, but they also contain secondary phases: anglesite and cerussite. Chemical analyzes confirmed that the smelter used sulphide ores, which were roasted, and the main addition to the charge was quartz sand. The smelting process took place in a brick-built furnace, under reducing conditions, with varied oxygen fugacity ranging from WM to MH buffer. The slag characteristics show a knowledge of the workers in the field of smelting methods. The addition of SiO2 allowed for the binding of elements that could contaminate the obtained lead, and at the same time, the low melting point of the material (1150 °C) and the melt viscosity (logη = 1.34 for 1150 °C) was maintained, enabling the effective separation of liquid lead.

22 August 2011 in Geological Quarterly
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Journal Article
Closed access
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MSMonika Szczuka
Monika Szczuka
AGAleksandra Gawęda
Aleksandra Gawęda
AWAnna Waśkowska
Anna Waśkowska
JGJan Golonka
Jan Golonka
KSKrzysztof Szopa
Krzysztof Szopa
FDFoteini Drakou
Foteini Drakou
Silesian Ridge in the light of petrological analyses and LA-ICP MS U-Pb analyses of the cohesive debrites from the Istebna Formation (Silesian Nappe, Outer Western Carpathians, Poland)