FRIDRICHOVÁ, Jana, Peter BAČÍK, Petra RUSINOVÁ, Peter ANTAL, Radek ŠKODA, Valeria BIZOVSKA and Marcel MIGLIERINI. Optical and crystal-chemical changes in aquamarines and yellow beryls from Thanh Hoa province, Vietnam induced by heat treatment. Physics and Chemistry of Minerals. NEW YORK: SPRINGER, 2015, vol. 42, No 4, p. 287-302. ISSN 0342-1791. Available from: https://dx.doi.org/10.1007/s00269-014-0719-4.
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Basic information
Original name Optical and crystal-chemical changes in aquamarines and yellow beryls from Thanh Hoa province, Vietnam induced by heat treatment
Authors FRIDRICHOVÁ, Jana (703 Slovakia), Peter BAČÍK (703 Slovakia), Petra RUSINOVÁ (703 Slovakia), Peter ANTAL (703 Slovakia), Radek ŠKODA (203 Czech Republic, guarantor, belonging to the institution), Valeria BIZOVSKA (703 Slovakia) and Marcel MIGLIERINI (703 Slovakia).
Edition Physics and Chemistry of Minerals, NEW YORK, SPRINGER, 2015, 0342-1791.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher United States of America
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 1.585
RIV identification code RIV/00216224:14310/15:00087129
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1007/s00269-014-0719-4
UT WoS 000351463100004
Keywords in English Beryl; Heat treatment; Powder X-ray diffraction; Infrared spectroscopy; Mossbauer spectroscopy; Electron microprobe; UV/Vis/NIR spectroscopy; Raman spectroscopy
Tags AKR, rivok
Changed by Changed by: Ing. Andrea Mikešková, učo 137293. Changed: 7/4/2016 15:27.
Abstract
Optical and crystal-chemical changes in two beryl varieties after the heat treatment were determined using a wide spectrum of analytical methods. Studied aquamarines are generally more enriched in Fe (up to 0.25 apfu) and alkali (up to 0.08 apfu) than yellow beryls (up to 0.07 apfu Fe, up to 0.04 apfu alkali). The determined c/a ratio of 0.997-0.998 classified all our studied beryls as "normal" beryls. While no crystal structure changes were observed in samples heated to 700 A degrees C, those heated to 900 and 1,100 A degrees C exhibited cracks and fissures. Reduced Fe occurred in samples heated between 300 and 700 A degrees C, and subsequent oxidation from 900 to 1,100 A degrees C induced changes in their colour and clarity. The Fe-bearing beryl colour is controlled by the position of the absorption edge and the presence of a broad band attributed to Fe2+ in the NIR region. Blue colour results from the absorption edge located deeper in the UV region and the presence of broad band in the NIR region. Shift of absorption edge to the visible region at the presence of the broad band gives a yellow colour. Although our studied beryls are enriched in H2O I molecule due to their low alkali content, the H2O II molecule is also present. The following two dehydration processes were observed: (1) release of one double-coordinating H2O II molecule at 300-500 A degrees C and (2) total dehydration at 900-1,100 A degrees C. The observed cracks and fissures likely resulted from channel water release in large beryl crystals.
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