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Record W4413053296 · doi:10.1016/j.ijmst.2025.07.002

Depression of pyrrhotite superstructures in copper flotation: A synchrotron X-ray powder diffraction and DFT study

2025· article· en· W4413053296 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

fundA Canadian funder is recorded on the work.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueInternational Journal of Mining Science and Technology · 2025
Typearticle
Languageen
FieldEnvironmental Science
TopicMinerals Flotation and Separation Techniques
Canadian institutionsnot available
FundersResearch Computing Centre, University of QueenslandAustralian Research CouncilGoldcorpUniversity of QueenslandNewmont CorporationAustralian Nuclear Science and Technology Organisation
KeywordsPyrrhotiteSynchrotronCopperPowder diffractionCrystallographyX-rayDiffractionMaterials scienceX-ray crystallographyChemistryMetallurgyPyriteOpticsPhysics

Abstract

fetched live from OpenAlex

Pyrrhotite naturally occurs in various superstructures including magnetic (4C) and non-magnetic (5C, 6C) types, each with distinct physicochemical properties and flotation behaviors. Challenges in accurately identifying and quantifying these superstructures hinder the optimization of pyrrhotite depression in flotation processes. To address this critical issue, synchrotron X-ray powder diffraction (S-XRPD) with Rietveld refinement was employed to quantify the distribution of superstructures in the feed and flotation concentrates of a copper–gold ore. To elucidate the mechanisms influencing depression, density functional theory (DFT) calculations were conducted to explore the electronic structures and surface reactivity of the pyrrhotite superstructures toward the adsorption of water, oxygen and hydroxyl ions (OH − ) as dominant species present in the flotation process. S-XRPD analysis revealed that flotation recovery rates of pyrrhotite followed the order of 4C<6C<5C. DFT calculations indicated that the Fe 3d and S 3p orbital band centers exhibited a similar trend relative to the Fermi level with 4C being the closest. The Fe 3d band center suggested that the 4C structure possessed a more reactive surface toward the oxygen reduction reaction, promoting the formation of hydrophilic Fe-OH sites. The S 3p band center order also implied that xanthate on the non-magnetic 5C and 6C surfaces could oxidize to dixanthogen, increasing hydrophobicity and floatability, while 4C formed less hydrophobic metal-xanthate complexes. Adsorption energy and charge transfer analyses of water, hydroxyl ions and molecular oxygen further supported the high reactivity and hydrophilic nature of 4C pyrrhotite. The strong bonding with hydroxyl ions indicated enhanced surface passivation by hydrophilic Fe–OOH complexes, aligning with the experimentally observed flotation order (4C<6C<5C). These findings provide a compelling correlation between experimental flotation results and electronic structure calculations, delivering crucial insights for optimizing flotation processes and improving pyrrhotite depression. This breakthrough opens up new opportunities to enhance the efficiency of flotation processes in the mining industry.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.269
Threshold uncertainty score0.188

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.005
GPT teacher head0.294
Teacher spread0.289 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it