Evidence map›Paper›PMID 41461840›Full record

ArticleScientific reports2025

Forensic gemmological investigation based on optical and crystal-chemical changes in topaz from Ouro Preto and Caraí, Brazil, induced by heat treatment.

Jana Fridrichová, Peter Bačík, Olena Rybnikova, Ján Štubňa, Daniel Furka, Samuel Furka, Jan Cempírek, Radek Škoda, Tomáš Vaculovič

Abstract read
In one paragraph

Article in Scientific reports, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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0citing papers in PubMed
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1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

0 citing papers in PubMed.

No citing paper in PubMed yet.

4 · The record

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5 · Who and what money

Authors and funding

9 authors.

Jana FridrichováDepartment of Mineralogy, Petrology and Economic Geology, Faculty of Natural Sciences, Comenius University in Bratislava, Ilkovičova 6, Bratislava, 842 15, Slovakia. jana.fridrichova@uniba.sk.
Peter BačíkDepartment of Mineralogy, Petrology and Economic Geology, Faculty of Natural Sciences, Comenius University in Bratislava, Ilkovičova 6, Bratislava, 842 15, Slovakia.
Olena RybnikovaDepartment of Mineralogy, Petrology and Economic Geology, Faculty of Natural Sciences, Comenius University in Bratislava, Ilkovičova 6, Bratislava, 842 15, Slovakia.
Ján ŠtubňaGemmological Laboratory, Department of Geography Geoinformatics and Regional Development, Faculty of Natural Sciences and Informatics, Constantine the Philosopher University in Nitra, Nábrežie mládeže 91, Nitra, 94901, Slovakia.
Daniel FurkaDepartment of Physical and Theoretical Chemistry, Faculty of Natural Sciences, Comenius University, Ilkovičova 6, Bratislava, 842 15, Slovakia.
Samuel FurkaDepartment of Physical and Theoretical Chemistry, Faculty of Natural Sciences, Comenius University, Ilkovičova 6, Bratislava, 842 15, Slovakia.
Jan CempírekDepartment of Geological Sciences, Faculty of Science, Masaryk University, Kotlářská 2, Brno, 611 37, Czech Republic.
Radek ŠkodaDepartment of Geological Sciences, Faculty of Science, Masaryk University, Kotlářská 2, Brno, 611 37, Czech Republic.
Tomáš VaculovičDepartment of Chemistry, Faculty of Science, Masaryk University, Kamenice 5, Brno, 625 00, Czech Republic.

Funding

Agentúra na Podporu Výskumu a Vývoja APVV-18-0065Vedecká Grantová Agentúra MŠVVaŠ SR a SAV VEGA-1/0189/23
6 · The paper itself

Abstract

Topaz is frequently subjected to heat treatment and irradiation to enhance colour, particularly to produce the market's most preferred salmon pink and sky blue varieties. However, an insufficient description of these processes can lead to fraudulent practices. This experimental and forensic mineralogical and gemmological study investigates eighteen heat-treated topaz samples from Ouro Preto (OP) and Caraí (CA), Brazil, using electron microanalysis, LA-ICP-MS, Raman, and optical absorption spectroscopy before and after heat treatment at various temperatures. The most significant optical changes were observed at 300 °C when the CA sample lost its colour from sky blue to colourless, while OP samples retained their imperial orange colour up to 500 °C before transitioning to pink at 700 °C. Chemically, the CA samples are rich in F (> 1.8 apfu) with low trace element concentration (Fe ≤ 125 ppm, Ge ≤ 153 ppm), falling to the pegmatite and greisen field of topaz origin. The OP samples contain less F (1.4-1.5 apfu) but higher trace element contents (Cr up to 204 ppm, Ti up to 115 ppm, Fe, Mn, Ge < 64 ppm), consistent with a hydrothermal origin. Raman spectra show no significant inter-sample variation, but their luminescence spectra feature strong differences: Mn acts as the luminophore in CA samples, while Cr

Indexed as

Chemical compositionGemmologyHeat treatmentOptical absorption spectroscopyRaman spectroscopyTopaz

Identifiers

PMID41461840
PMCPMC12848008

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