Molecular structure of the phosphate mineral koninckite - a vibrational spectroscopic study

JIRÁSEK, Jakub, Jiří ČEJKA, Luboš VRTIŠKA, Dalibor MATYSEK, XiuXiu RUAN a Ray L. FROST. Molecular structure of the phosphate mineral koninckite - a vibrational spectroscopic study. Journal of Geosciences. Praha: Česká geologická společnost, 2017, roč. 62, č. 4, s. 271-279. ISSN 1802-6222. Dostupné z: https://dx.doi.org/10.3190/jgeosci.243.

Základní údaje

• Originální název: Molecular structure of the phosphate mineral koninckite - a vibrational spectroscopic study
• Autoři: JIRÁSEK, Jakub (203 Česká republika, garant), Jiří ČEJKA (203 Česká republika), Luboš VRTIŠKA (203 Česká republika, domácí), Dalibor MATYSEK (203 Česká republika), XiuXiu RUAN a Ray L. FROST.
• Vydání: Journal of Geosciences, Praha, Česká geologická společnost, 2017, 1802-6222.

Další údaje

• Originální jazyk: angličtina
• Typ výsledku: Článek v odborném periodiku
• Obor: 10504 Mineralogy
• Stát vydavatele: Česká republika
• Utajení: není předmětem státního či obchodního tajemství
• WWW: URL
• Impakt faktor: Impact factor: 1.415
• Kód RIV: RIV/00216224:14310/17:00106257
• Organizační jednotka: Přírodovědecká fakulta
• Doi: http://dx.doi.org/10.3190/jgeosci.243
• UT WoS: 000423277800006
• Klíčová slova česky: koninckit; fosfát; Ramanova spektroskopie; infračervená spektroskopie
• Klíčová slova anglicky: koninckite; phosphate; Raman spectroscopy; infrared spectroscopy
• Příznaky: Mezinárodní význam, Recenzováno

Anotace

We have undertaken a study of the mineral koninckite from Litosice (Czech Republic), a hydrated ferric phosphate, using a combination of scanning electron microscopy with electron probe micro-analyzer (wavelength-dispersive spectroscopy) and vibrational spectroscopy. Chemical analysis shows that studied koninckite is a pure phase with an empirical formula Fe3+ (0.99)(PO4)(1.00) center dot 2.75 H2O, with minor enrichment in Al, Ca, Ti, Si, Zn, and K (averages 0.00X apfu). Raman bands and shoulders at 3495, 3312, 3120, and 2966 cm(-1) and infrared bands and shoulders at 3729, 3493, 3356, 3250, 3088, 2907, and 2706 cm(-1) are assigned to the nu OH stretching of structurally distinct differently hydrogen bonded water molecules, A Raman band at 1602 cm(-1) and shoulders at 1679, 1659, 1634, and 1617 cm(-1) and infrared bands at 1650 and 1598 cm(-1) are assigned to the nu(2)(delta) H2O bending vibrations of structurally distinct differently hydrogen bonded water molecules. Raman shoulders at 1576, 1554, 1541, 1532, and 1520 cm(-1) and infrared shoulders at 1541 and 1454 cm(-1) may be probably connected with zeolitically bonded water molecules located in the channels. Raman bands and shoulders at 1148, 1132, 1108, 1063, 1048, and 1015 cm(-1) and an infrared band and shoulders at 1131, 1097, 1049, and 1017 cm(-1) are assigned to the nu(3) PO43- triply degenerate antisymmetric stretching vibrations. A Raman band and a shoulder at 994 and 970 cm(-1), respectively, and an infrared band and a shoulder at 978 and 949 cm(-1), respectively, are assigned to the nu(1) PO43- symmetric stretching vibrations. Infrared shoulders at 873, 833, and 748 cm(-1) are assigned to libration modes of water molecules. Raman bands and shoulders at 670, 648, 631, 614, 600, 572, and 546 cm(-1) and infrared bands at 592 and 534 cm(-1) are assigned to the nu(4) (delta) PO(4)(3-)triply degenerate out-of-plane bending vibrations; weak band at 570 cm(-1) may coincide with the delta Fe-O bending vibration. Raman bands and shoulders at 453, 443, 419, and 400 cm(-1) are assigned to the nu(2) (delta) PO43- doubly degenerate in-plane bending vibrations. Raman bands at 385, 346, 324, 309, 275, 252, and 227 cm(-1) are assigned to the nu Fe-O stretching vibrations in FeO6 octahedra. Raman bands at 188, 158, 140, 112, 89, and 73 cm(-1) are assigned to lattice vibrations.