2024
Crystal-chemical effects of heat treatment on Cr- and V-bearing Ca-dominant green tourmalines (fluor-uvite, magnesio-lucchesiite)
BACIK, Peter; Petra KARDOSOVA; Jana FRIDRICHOVA; Olena RYBNIKOVA; Radek ŠKODA et. al.Základní údaje
Originální název
Crystal-chemical effects of heat treatment on Cr- and V-bearing Ca-dominant green tourmalines (fluor-uvite, magnesio-lucchesiite)
Autoři
BACIK, Peter; Petra KARDOSOVA; Jana FRIDRICHOVA; Olena RYBNIKOVA a Radek ŠKODA (203 Česká republika, domácí)
Vydání
Periodico di Mineralogia, Sapienza Universita Editrice, 2024, 0369-8963
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10504 Mineralogy
Stát vydavatele
Itálie
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 1.200
Kód RIV
RIV/00216224:14310/24:00139001
Organizační jednotka
Přírodovědecká fakulta
UT WoS
001409457100001
EID Scopus
2-s2.0-85213216670
Klíčová slova anglicky
tourmaline; fluor-uvite; magnesio-lucchesiite; heat treatment; structural breakdown
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 5. 3. 2025 16:10, Mgr. Marie Novosadová Šípková, DiS.
Anotace
V originále
We present a detailed study of thermally driven changes in Ca-dominant tourmaline using Electron Probe Microanalysis (EPMA), powder X-ray diffraction (PXRD), Raman and optical absorption spectroscopy (OAS). The KEN samples from Kenya (5 crystal fragments) can be classified as fluor-uvite, while TAN from Tanzania (5 fragments) is dominantly magnesio-lucchesiite. Tourmaline samples were thermally treated in air at 700, 800, 900, and 1000 degrees C. Both sets were green with different hues, TAN with a bluer hue than KEN. After heating, no significant visual changes were observed in TAN samples until breakdown at 1000 degrees C. In KEN, after heating at 700 degrees C, the yellowish tint disappeared. Raman spectroscopy showed no significant changes after heating. Raman luminescence spectra revealed the sharp intensive band located at 680-684 nm, accompanied by a broad band between 690 and 900 nm in all samples heated up to 900 degrees C. OAS spectra look similar, with two major bands in blue and yellow to red regions. In TAN, the bands shift with the increasing Cr/V from 608 to 604 nm. In KEN with low Cr/V, the band is located between 613-617 nm. After heating at 1000 degrees C, both samples broke down with different associations: cordierite/indialite and glass from magnesio-lucchesiite, and cordierite/indialite, mullite-like phase, spinel and glass from fluor-uvite. There was a difference in volume between the samples; both samples expanded in volume, but the KEN sample expanded more with larger pores likely resulting from a higher proportion of volatile phase in this sample.