Nature of Scapolite Color: Ab Initio Calculations, Spectroscopy, and Structural Study

Author:

Shendrik Roman12ORCID,Chukanov Nikita V.23,Bogdanov Alexander1ORCID,Myasnikova Alexandra1ORCID,Pankrushina Elizaveta4ORCID,Zolotarev Anatoly A.5,Babkina Anastasiia6ORCID,Popova Ekaterina5,Vigasina Marina F.2ORCID,Aksenov Sergey M.7ORCID,Ilyin Grigoriy7ORCID,Pekov Igor V.2

Affiliation:

1. Vinogradov Institute of Geochemistry, Siberian Branch of Russian Academy of Science, 664033 Irkutsk, Russia

2. Faculty of Geology, Moscow State University, 119991 Moscow, Russia

3. Federal Research Center of Problems of Chemical Physics and Medicinal Chemistry, Russian Academy of Sciences, 142432 Chernogolovka, Russia

4. Zavaritsky Institute of Geology and Geochemistry, Ural Branch of the Russian Academy of Sciences, 620110 Ekaterinburg, Russia

5. Institute of Earth Sciences, Saint-Petersburg State University, St. Petersburg 199034, Russia

6. Research Center of Optical Materials Science, ITMO University, Saint-Petersburg 197101, Russia

7. Laboratory of Arctic Mineralogy and Material Sciences, Kola Science Centre, Russian Academy of Sciences, Apatity 184200, Russia

Abstract

The article describes the results of a comprehensive study of the extra-framework components of scapolites using quantum–chemical calculations, electronic and vibrational spectroscopy, and single-crystal X-ray diffraction and crystal structure refinement. The ab initio calculations were performed using an embedded-cluster approach of extra-framework components in various cation surroundings. As a result, through comparing the experimental and ab initio calculation results, the energies of the electronic and vibrational transitions of various extra-framework components (CO3)2−, (CO3)·−, S3·−, S2·−—as well as the role of these components in the process of the lowering of the symmetry—were determined for scapolites belonging to the marialite–meionite solid–solution series. The nature of the various colors of the scapolites has also been established. Colors from purple to blue are a result of the presence of radiation-induced pairs of defects: carbonate radical anions (CO3)·− and F-centers. However, polysulfide S3·− radical anions are found in some violet scapolites.

Funder

Russian Science Foundation

Materials and Technologies for the Development of Radiation Detectors, Luminophores, and Optical Glasses

state task

state task of the Russian Federation

Elizaveta Pankrushina

Publisher

MDPI AG

Reference59 articles.

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3. Composition and I4/m-P42/n phase transition in scapolite solid solutions;Seto;Am. Mineral.,2004

4. The crystal chemistry of the scapolite-group minerals. I. Crystal structure and long-range order;Sokolova;Can. Mineral.,2008

5. The crystal chemistry of the scapolite: Investigation of the marialite–meionite solid solution series by means of the Rietveld method;Sokolova;Probl. Crystallogr.,1999

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