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Phase Equilibria and Trace Element Deportments in Fe–O–Al2O3–SiO2 Slags and Molten Copper Matte at 1473 K (1200 °C), Fixed p(O2) and p(SO2), and Silica/Magnetite Saturation

Crossref DOI link: https://doi.org/10.1007/s11663-024-03431-5

Published Online: 2025-02-04

Published Print: 2025-06

Update policy: https://doi.org/10.1007/springer_crossmark_policy

Authors

Tian, Miao https://orcid.org/0000-0002-9066-5529
Klemettinen, Lassi https://orcid.org/0000-0001-9633-7131
Chen, Min https://orcid.org/0000-0003-0544-4359
Taskinen, Pekka https://orcid.org/0000-0002-4054-952X
Tiljander, Mia

O’Brien, Hugh https://orcid.org/0000-0002-7900-579X
Lindberg, Daniel https://orcid.org/0000-0002-8442-1237
Funding

Funding for this research was provided by:

Aalto University
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Text and Data Mining valid from 2025-02-04

Version of Record valid from 2025-02-04
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Article History

Received: 10 July 2024

Accepted: 17 December 2024

First Online: 4 February 2025

Change Date: 9 April 2025

Change Type: Correction

Change Details: A Correction to this paper has been published:

Change Details: https://doi.org/10.1007/s11663-025-03506-x

Updates are available Correction dated 2025-04-09

Click to view Correction: https://doi.org/10.1007/s11663-025-03506-x