The use of predominance area diagrams (PAD) to determine the oxygen and sulfur fugacities prevailing during historical metallurgical processes: the case of fifteenth to seventeenth century copper slags from Polichno (Old Polish industrial district)

被引:0
作者
Kupczak, Krzysztof [1 ]
Warchulski, Rafal [1 ]
Gaweda, Aleksandra [1 ]
Slezak, Marta [2 ]
Migas, Piotr [2 ]
机构
[1] Univ Silesia Katowice, Inst Earth Sci, Fac Nat Sci, Bedzinska 60, PL-41200 Sosnowiec, Poland
[2] AGH Univ Krakow, Fac Met Engn & Ind Comp Sci, Dept Met Forming & Met Engn, Mickiewicza 30, PL-30059 Krakow, Poland
关键词
Slags; Predominance area diagrams; Process reconstruction; Smelting; Temperature; MEDIEVAL SLAGS; MINERALOGY; MOUNTAINS; LEAD;
D O I
10.1186/s40494-024-01171-y
中图分类号
C [社会科学总论];
学科分类号
03 ; 0303 ;
摘要
The study presents the first use of predominance area diagrams (PADs) to determine oxidation-reduction conditions during reconstructing historical copper smelting processes. The smelting temperature and oxygen and sulfur fugacities during smelting were determined based on experiments and the geochemical (ICP-MS/ES, XRF) and mineralogical (SEM, EPMA) analyses of the fifteenth to seventeenth century slags from Polichno (Holy Cross Mountains, Poland). Results obtained during high-temperature experiments allowed to determine the slags' solidus and liquidus temperatures. The liquidus temperature was in the range of 1100-1200 degrees C, and the solidus temperature was in the range of 800-1100 degrees C. Data on temperature conditions were used in thermodynamic calculations to construct predominance area diagrams and then to determine the ranges of oxygen and sulfur fugacities in which the formation of slags was possible. Slags from Polichno were formed with the oxygen fugacity in the range of logPO2\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\text{logP}_{{\text{O}}_2}$$\end{document} = - 4.30 (POL1, POL4 at 1200 degrees C) to - 14.08 atm. (POL3 at 1090 degrees C). In turn, the sulfur fugacity during slag formation ranged from logPS2\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\text{logP}_{{\text{S}}_2}$$\end{document} = - 2.50 (POL5 at 1200 degrees C) to - 6.92 (POL4 at 1060 degrees C) atm. The relatively high sulfur availability confirms using sulfide ores without prior roasting. The wide range of sulfur and oxygen fugacity indicates the process's heterogeneity.
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页数:17
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